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Perception of climate change-related forest dieback in mountain forests among the local population
(2023)
Mountain forests provide multiple benefits but are threatened by climate change-induced forest dieback. Although many studies summarize perceptions of forest ecosystem services, relatively few deal with mountain forests. The local population’s perception of forest dieback in mountain forests in relation to climate change has rarely been investigated so far. Their perspective is relevant as local people are often deeply attached to “their” forests, they actively use forest ecosystems and—as voters and taxpayers—they need to support the state’s adaptation and funding measures. Therefore, this study investigates the climate change and forest dieback perception of local inhabitants in two mountain areas of Southern Germany (the German Alps and the Bavarian Forest) with a quantitative survey based on representative online samples (n = 709). Relying conceptually on van der Linden’s (J Environ Psychol 41:112–124, 2015. https://doi.org/10.1016/j.jenvp.2014.11.012) climate change risk perception model, the results show that experiential processing, cognitive and socio-cultural factors are related to locals’ forest dieback and climate change perception, while socio-demographics show no or few connections. Nearly two-thirds (64.7%) of the respondents perceive moderate to strong forest dieback, while more than half (55.0%) of the respondents already observe consequences of climate change. The perceptions of climate change and forest dieback are positively correlated with medium to high strength. This shows that forest dieback could be interpreted as an indicator of climate change, which is difficult to observe due to its long-term nature. We identify three groups of respondents regarding preferred forest adaptation strategies to climate change. In general, respondents support nature-based forest adaptation strategies over intense measures.
Toarciconiopteryx dipterosimilis gen. et sp. nov. is described from the Lower Toarcian of Grimmen (Western Pomerania, Germany) based on a hind wing. This enigmatic wing superficially resembles a dipteran forewing, but analysis in detail establishes that it belongs to the Neuroptera. We assign it to the Coniopterygidae with great confidence by its great concordance with the hind wings of that family, but a small possibility remains that it might belong to the Dipteromantispidae, although the very derived haltere-like hind wings of all its known members are entirely unlike it. We, therefore, consider it to be the oldest record of Coniopterygidae. We create the new subfamily Toarciconiopteryginae subfam. nov. for it, which is distinguished from other Coniopterygidae by its hind wings possessing two branches of RP and a proximal forking of M. These conditions are also known in some Sialidae (Megaloptera), supporting the hypothesis that Coniopterygidae is the sister group of all other Neuroptera, as Megaloptera is considered by most authors to be sister to Neuroptera. New interpretations of some aspects of the Coniopterygidae venation are proposed.
Peatlands contribute to a wide range of ecosystem services. They play an important role as carbon sinks in their natural state, but when they are drained, they cause carbon emissions. Rewetting drained peatlands is required to reduce carbon emissions and create new carbon sinks. However, drained peatlands are commonly used as grassland or croplands; therefore, alternative agriculture schemes are required following rewetting. Paludiculture, i.e., agriculture on wet and rewetted peatlands, is an option in these areas after rewetting to produce biomass sustainably. Monitoring of peatland management is challenging, yet needed to ensure a successful rewetting and plantation of, e.g., Phragmites australis and Typha spp., two plants which are commonly used in paludiculture. Remote sensing is an excellent tool for monitoring the vegetation composition of vast rewetted peatland regions. However, because many peatland species have similar spectral characteristics, such monitoring is ideally based on high-spatial, high-temporal hyperspectral images. Data that complies with all these requirements does not exist on a regular basis. Therefore, we assessed the potential for mapping peatland vegetation communities in the Peene and Trebel river basins of the federal state of Mecklenburg-Western Pomerania, Germany, using multi-date hyperspectral (PRISMA) data. We used regression-based unmixing to map fractions of different peatland vegetation classes. Results were analyzed with regard to the contribution of multi-date observations and, in comparison, to multispectral datasets (Landsat-8/Sentinel-2). Our results showed that different classes are best mapped at different observation dates. The multi-date hyperspectral datasets produced less Mean Absolute Error (MAE = 16.4%) than the single-date hyperspectral images (ΔMAE + 1%), with high accuracies for all classes of interest. Compared to the results obtained with multispectral data from similar acquisition dates and annual spectral-temporal metrics (STM), the results from hyperspectral data were always clearly superior (ΔMAE + 4%). Besides the superior performance during comparisons, our results also indicate that information that can be derived from the hyperspectral data with the regression-based unmixing goes clearly beyond that of discrete classification. With more hyperspectral sensors coming up and an expected higher availability of multi-data hyperspectral imagery, these data can be expected to play a bigger role in the future monitoring of peatlands.
Das vorliegende Essay gibt einen Überblick zum Standortauswahlprozess für die Endlagerung des hochradioaktiven Abfalls in der Bundesrepublik Deutschland. Dieses Verfahren stellt einen Paradigmenwechsel gegenüber dem früheren Versuch der Ausweisung eines Standortes dar, indem zunächst einzig geologische Kriterien hinsichtlich der Sicherheit der Einlagerung und nicht politisch-wirtschaftliche Einzelinteressen von Regionen entscheidend sein sollen. Der aktuelle Stand der Forschung bildet weitergehende Wissensbedarfe gut ab. Derzeit besonders diskutierte Aspekte im Rahmen der Einengung der großen Teilgebiete auf Standortregionen zur übertägigen Erkundung werden angesprochen.
Monitoring and assessing groundwater quality according to European directives and national regulations is usually based on interpolation techniques, e.g. Kriging. However, contour maps of hydrochemical parameters often suggest a spurious local accuracy and can therefore lead to inappropriate action measures. Here, the early concept of extension variance combined with the Voronoi tessellation regionalization is proposed. The mosaic-like representation of pollutant concentrations in Voronoi polygons avoids misinterpretations caused by interpolation. The additional calculation of the extension variance, which is based on fundamental geostatistical assumptions, allows for estimating the probability that a given threshold is exceeded. This concept is further extended to hydraulically delimitable groundwater bodies, thus ensuring that hydraulic boundaries are considered. A method is here described for the assessment of groundwater quality with respect to nitrate concentration in the principal aquifer of the state Mecklenburg-Western Pomerania in Germany.
Der inhabergeführte Einzelhandel steht vor besonderen Herausforderungen bei der Einführung und Etablierung digitaler Kundenkommunikationsmaßnahmen (KKM). Im vorliegenden Beitrag wird untersucht, welche Maßnahmen im Zuge der Coronapandemie eingeführt worden sind und welche dieser Maßnahmen besonders zukunftsfähig sein können. Darüber hinaus wird die Bedeutung von regionalen Netzwerken beim Wissenstransfer über digitale Maßnahmen betrachtet. Für die Untersuchung wurde in den drei Bundesländern Nordrhein-Westfalen, Sachsen und Sachsen-Anhalt im März 2022 eine Online-Befragung von Inhabern durchgeführt und durch fünf Experteninterviews im April und Mai 2022 ergänzt. Für die Vergleichbarkeit der gewonnenen Ergebnisse wird eine großflächige Handelsstudie der IHK Köln und dem ibi Research Institut Regensburg aus dem Jahr 2020 herangezogen. Dabei stellte sich heraus, dass insbesondere die digitale Sichtbarkeit für den Erhalt der inhabergeführten Einzelhandelsgeschäfte in Zukunft von zentraler Bedeutung sein wird. Ferner präsentieren sich die sozialen Medien mit ihrer perspektivisch ausgestatteten Verkaufsfunktion als geeignetes Instrument. Außerdem konnten durch eine differenzierte Betrachtung von Branchen und Zielgruppen sowie unterschiedlichen Ansätzen für den Einstieg in die digitale Kundenkommunikation zukunftsfähige und individuelle Maßnahmen identifiziert werden.
Nebenströme der Agrar- und Ernährungswirtschaft – vom Abfallprodukt zur wertvollen Ressource!?
(2023)
Die Nutzung von organischen Abfällen und Nebenströmen ist ein wichtiger Baustein für die Transformation zu einem nachhaltige(re)n Agrar- und Ernährungssystem. Die damit einhergehenden Kreislaufsysteme werden in der Literatur unter dem Begriff der Circular Bioeconomy diskutiert. Der Beitrag greift diese Diskussionen auf und liefert empirische Befunde aus der Raps- und Zuckerrübenproduktion, wo große Mengen an Nebenströmen speziell auf der Verarbeitungsstufe anfallen (z. B. Presskuchen, Extraktionsschrot, Rübenschnitzel, Melasse). Für diese organischen Stoffe haben sich unterschiedliche Verwertungspfade etabliert, sodass sie mittlerweile ein wichtiges Element der betrieblichen Wertschöpfung darstellen. Die Verwertung geschieht in beiden Bereichen durch intersektorale Vernetzungen, die sich je nach Wertschöpfungspotenzial und Lager‑/Transportfähigkeit der Biomasse über verschiedene Raumebenen erstrecken (lokal/regional, national, international). Ebenso spielen unternehmerische Merkmale wie auch der institutionelle Kontext eine Rolle bei der Nebenstromverwertung.
The reduction of individual carbon consumption could make an important contribution to the worldwide effort to limit global warming. Based on Bandura’s theory of moral disengagement, we hypothesized that the propensity to morally disengage concerning high-carbon behaviors (e.g., eating meat or traveling by plane) is one important factor that prevents individuals from reducing their carbon footprint. To measure the propensity to morally disengage in high-carbon-related behavior contexts, a questionnaire (MD-HCB) was developed and psychometrically validated in an online study with a German sample (N = 220). Confirmatory factor analyses revealed that the final nine-item scale had a one-dimensional structure, as intended. The internal consistency of the scale was excellent (Cronbach’s α = 0.94) and the scale interpretation had predictive validity for both past low-carbon consumption behavior and the intention to engage in such behavior in the future. Correlational analyses with relevant existing instruments confirmed the construct validity of the interpretations that can be drawn from the MD-HCB, as its resulting score is related to, yet separable from, the general tendency to morally disengage and is meaningfully connected to related constructs. A pre-study with a student sample (N = 89) not only helped to identify limitations in the study design but also showed a weak predictive ability of moral competence concerning high-carbon consumption behavior and intention to change. Based on our findings, future media campaigns designed to increase people’s intention to reduce high-carbon behavior could focus on the modification of common cognitive disengagement strategies.
The multi-level perspective has been criticized for being functionalistic and paying little attention to actor-based perspectives. Nevertheless, for the identification and assessment of potential change agents in a sustainability transition, a clear conceptual and methodological approach is necessary. This paper, thus, develops a multi-dimensional typology of niche, regime, and hybrid actors, which is conceptually grounded in transition studies and empirically illustrated by a cluster analysis based on a survey of pig and poultry farmers in Germany, France, and the Netherlands. Animal husbandry is chosen as a case study because a significant share of the environmental impact within the agri-food system is attributed to this sector and there is evidence for resistance to change by mainstream actors. Conceptually, the paper provides a framework of constitutive elements for different kinds of actors and contributes to an extension of the niche–regime dichotomy by adding the group of hybrid actors. The empirical results show that cluster analysis is a suitable approach to identify conceptually meaningful differences among interviewed farmers. Among pig and poultry farmers, the regime actors are by far the largest group. The smaller group of hybrid actors, however, has large potential to act as boundary spanners. A particularly interesting finding is that several larger farms are among the group of niche actors which hints at the possibility that larger farms are not necessarily resistant to change.
The occurrence and distribution of organochlorine pesticides (OCPs) in aquatic systems is a matter of global concern and poses significant toxicological threats to both organisms and human health. Despite the extensive use of OCPs for pest and disease control in southern Africa, relatively few studies have examined the occurrence and toxicological risks of OCP residues in the region. This study investigates the composition, distribution, and potential sources of OCP contamination in sediments from Richards Bay, a rapidly developing industrial port on the northeast coast of South Africa. Surface sediments collected from Richards Bay Harbour and surrounding areas indicate that OCP contamination in the region is widespread. Total concentrations (∑OCP) in surface samples ranged from 135 to 1020 ng g−1, with hexachlorocyclohexanes (∑HCH; 35–230 ng g−1) and dichlorodiphenyltrichloroethanes (∑DDT; 12–350 ng g−1) the dominant contaminant groups detected. Metabolite isomeric compositions indicate that the presence of aldrin and endosulfan likely result from historical agricultural usage, while recent input of γ-HCH, heptachlor, and endrin may be linked to the illegal use of old pesticide stockpiles. Total DDT concentrations were dominated by p,p′-DDT (80 ± 64 ng g−1), which was attributed to its ongoing use in malaria vector control in the region. A 210Pb-dated sediment core revealed that OCP input to the local environment increased dramatically from relatively low concentrations in the mid-1940s (∑OCP, 355 ng g−1) to peak levels (∑OCP, 781 ng g−1) in the 1980s/1990s. An overall decrease in ∑OCP concentration from the mid-2000s is likely related to restrictions on use following the Stockholm Convention in 2004. Despite current restrictions on use, OCP concentrations exceeded sediment quality guidelines in the vast majority of cases, raising concerns for protected estuarine and mangrove habitats in the area, as well as for local fishing and farming communities.
Thermally treated kaolinite is used to develop a range of alumino‐silicate‐based precursor materials but its behavior during plasma spraying has not been well‐researched. In this study, two types of kaolinite samples were investigated in the form of low defect (KGa‐1b) and high defect (KGa‐2) varieties. The extreme temperatures of the plasma stream (up to 20 000 K) induced flash melting to produce a highly porous alumino‐silicate glass without any crystallization of new Al−Si oxide minerals. The glass is comprised largely of intact or deformed spheres (average diameters 1.14–1.44 μm), which indicates rapid quenching and solidification before impact. The subspherical structures contain up to 40 % closed pore space caused by the rapid escape of water during melting. The low‐density, porous alumino‐silicate glass coatings with predicted specific surface areas (>0.95 m2/g) and hardnesses >1.8 GPa represent a potentially reactive but physically stable substrate ideal for further chemical functionalization.
Late Pleistocene glacitectonism at the southern Scandinavian Ice Sheet margin caused folding and thrusting of Upper Cretaceous chalk layers and Pleistocene glacial deposits in parts of the southwestern Baltic Sea area in Europe. Beside Møns Klint (SE Denmark), the Jasmund Glacitectonic Complex (JGC) on Rügen Island (NE Germany) is a similar striking example of glacitectonic deformation creating large composite ridges. In spite of a long research history and new results from modern datasets, the structural development of the JGC is still poorly understood, especially the detailed evolution of the southern JGC and its relationship to the northern JGC remain enigmatic. In this contribution, we demonstrate how the understanding of the JGC benefits from the application of established structural geological methods comprehending the formation of fold-and-thrust belts. The methods include cross-section balancing of the eastern coast (southern JGC) and quantification of the amount of folding and faulting. The proposed geometric model shows the current fold-and-thrust stack of glacially deformed sedimentary strata ca. 5720 m in length evolved by shortening from the original length (11,230 m) by 5510 m (49.1%). We present a spatial and temporal development of fault-related folding with a transition from detachment folds through fault-propagation folds to fault-bend folds. Together with morphological information from a digital elevation model, the thrust faults mapped in the cliff section are mainly inclined towards the S to SW and imply that a local glacier push occurred from the south. These results highlight the complexity and individual architecture of the JGC when compared to other Pleistocene and modern glacitectonic complexes. Resolving its structural development provides new insight into the deformation history and shortening of this spectacular glacitectonic complex lying in the southwestern Baltic Sea region.
There is a current need for developing improved synthetic porous materials for better constraining the dynamic and coupled processes relevant to the geotechnical use of underground reservoirs. In this study, a low temperature preparation method for making synthetic rocks is presented that uses a geopolymer binder cured at 80 °C based on alkali-activated metakaolin. For the synthesised sandstone, the key rock properties permeability, porosity, compressive strength, and mineralogical composition, are determined and compared against two natural reservoir rocks. In addition, the homogeneity of the material is analysed structurally by micro-computed tomography and high-resolution scanning electron microscopy, and chemically by energy dispersive X-ray spectroscopy. It is shown that simple, homogenous sandstone analogues can be prepared that show permeability-porosity values in the range of porous reservoir rocks. The advance in using geopolymer binders to prepare synthetic sandstones containing thermally sensitive minerals provides materials that can be easily adapted to specific experimental needs. The use of such material in flow-through experiments is expected to help bridge the gap between experimental observations and numerical simulations, leading to a more systematic understanding of the physio-chemical behaviour of porous reservoir rocks.
Calcitic valves of non-marine ostracodes are important geochemical archives. Investigations of the relationship between the ranges of oxygen and carbon isotope values of modern ostracode populations and their host water provide important information on local or regional conditions and influences. Here we present the first δ18Oostracode and δ13C of the freshwater ostracode species Cytheridella ilosvayi along with the isotopic composition of the waters in which the ostracodes calcified, δDwater, δ18Owater, δ13CDIC values—covering a large geographical range (Florida to Brazil). With this data we extended a newly developed approach based on the estimation of δ18O values of monthly equilibrium calcites as references for the interpretation of δ18Oostracode values. The expected apparent oxygen isotope fractionation between CaCO3 and H2O is correlated with temperature with smaller values occurring at higher temperatures as valid at isotope equilibrium (δ18Ocalcite_eq). Uncertainties about the expected equilibrium calcites derive from incomplete knowledge of high-frequency variations of the water bodies caused by interplay of mixing, evaporation, and temperature. Coincidence between δ18Oostracode and δ18Ocalcite_eq is restricted to few months indicating a seasonal calcification of Cytheridella. There is a characteristic pattern in its difference between mean δ18Oostracode and δ18Ocalcite_eq which implies that Cytheridella provides a synchronous life cycle in its geographical range with two calcification periods in spring (May, June) and autumn (October). This ubiquitous life cycle of Cytheridella in the entire study area is considered to be phylogenetically inherited. It might have originally been adapted to environmental conditions but has been conserved during the migration and radiation of the group over the Neotropical realm.
There is broad scientific consensus that current food systems are neither sustainable nor resilient: many agricultural practices are very resource-intensive and responsible for a large share of global emissions and loss of biodiversity. Consequently, current systems put large pressure on planetary boundaries. According to economic theory, food prices form when there is a balance between supply and demand. Yet, due to the neglect of negative external effects, effective prices are often far from representing the ‘true costs’. Current studies show that especially animal-based foodstuff entails vast external costs that currently stay unaccounted for in market prices. Against this background, we explore how informational campaigning on agricultural externalities can contribute to consumer awareness and tolerance of this matter. Further, we investigate the socially just design of monetary incentives and their implementation potentials and challenges. This study builds on the informational campaign of a German supermarket displaying products with two price tags: one of the current market price and the other displaying the ‘true’ price, which includes several environmental externalities calculated with True Cost Accounting (TCA). Based on interpretations of a consumer survey and a number of expert interviews, in this article we approach the potentials and obstacles of TCA as a communication tool and the challenges of its factual implementation in agri-food networks. Our results show that consumers are generally interested in the topic of true food pricing and would to a certain extent be willing to pay ‘true prices’ of the inquired foods. However, insufficient transparency and unjust distribution of wealth are feared to bring about communication and social justice concerns in the implementation of TCA. When introducing TCA into current discourse, it is therefore important to develop measures that are socially cautious and backed by relevant legal framework conditions. This poses the chance to create a fair playing (‘polluter pays’) with a clear assignment of responsibilities to policy makers, and practitioners in addition to customers.
Circular economies are an important pillar of sustainable production and consumption. This particularly applies to the agri-food industry, which is characterised by large amounts of organic waste and by-product streams posing a serious challenge for many food producers. Therefore, respective firms increasingly adopt circular economy business models (CEBMs) to manage these resource flows effectively. However, there is only little knowledge on the functioning of CEBMs in bio-based industries, especially from a socio-economic perspective. We address this gap by exploring enablers and motivations behind such business models as well as the institutional contexts they are embedded in. In methodological terms, we adopt a case study approach using the example of potato production in Lower Saxony (northwest Germany). The core of the paper is a qualitative in-depth analysis of four potato processors, adopting varying business models to valorise their by-product streams (e.g. peels, scraps, pulp) either ‘in-house’ or in partnerships with external partners. The findings show that the implementation of CEBMs results from a complex interplay of internal and external enablers, with economic considerations as the main impetus for the management of biological reverse cycles. Thereby, we found a shifting economic logic in the assessment of potato by-products from disposable waste to valuable resources for other sectors (e.g. livestock farming, bioenergy, biofuels). While being encouraged by targeted policies, the companies studied feel increasingly affected by emerging sustainability discourses, prompting them to (re)design and (re)frame their CEBMs in view of environmental and societal issues.
Thyreophora is a clade of globally distributed herbivorous ornithischian dinosaurs. The earliest forms are known from the Early Jurassic, and their latest surviving representatives witnessed the end-Cretaceous mass extinction. Throughout their evolutionary history, these ‘shield bearers’ became lumbering quadrupeds, evolved a wide array of bony armor, plates and spikes, as well as sweeping tail weapons in the form of tail clubs and thagomizers. An isolated new thyreophoran osteoderm from a Lower Jurassic Konservatlagerstätte near Grimmen is described and, with the aid of micro-CT data, compared to an osteoderm of the early diverging thyreophoran Emausaurus ernsti from a different stratigraphic horizon at the same locality.
Diagenetic illite growth in porous sandstones leads to significant modifications of the initial pore system which result in tight reservoirs. Understanding and quantifying these changes provides insight into the porosity-permeability history of the reservoir and improves predictions on petrophysical behavior. To characterize the various stages of diagenetic alteration, a focused ion beam – scanning electron microscopy (FIB-SEM) study was undertaken on aeolian sandstones from the Bebertal outcrop of the Parchim Formation (Early Permian Upper Rotliegend group). Based on 3D microscopic reconstructions, three different textural types of illite crystals occur, common to many tight Rotliegend sandstones, namely (1) feldspar grain alterations and associated illite meshworks, (2) tangential grain coats, and (3) pore-filling laths and fibers. Reaction textures, pore structure quantifications, and numerical simulations of fluid transport have revealed that different generations of nano-porosity are connected to the diagenetic alteration of feldspars and the authigenic growth of pore-filling illites. The latter leads to the formation of microstructures that range from authigenic compact tangential grain coatings to highly porous, pore-filling structures. K-feldspar replacement and initial grain coatings of illite are composed primarily of disordered 1Md illite whereas the epitaxially grown illite lath- and fiber-shaped crystals occurring as pore-filling structures are of the trans-vacant 1Mtv polytype. Although all analyzed 3D structures offer connected pathways, the largest reduction in sandstone permeability occurred during the initial formation of the tangential illite coatings that sealed altered feldspars and the subsequent growth of pore-filling laths and fibrous illites. Analyses of both illite pore-size and crystallite-size distributions indicate that crystal growth occurred by a continuous nucleation and growth mechanism probably controlled by the multiple influx of potassium-rich fluids during late Triassic and Jurassic times. The detailed insight into the textural varieties of illite crystal growth and its calculated permeabilities provides important constraints for understanding the complexities of fluid-flow in tight reservoir sandstones.
Ocean literacies: the promise of regional approaches integrating ocean histories and psychologies
(2023)
The current concept of ocean literacy reflects a prerequisite for achieving ocean sustainability. Existing ocean literacy reflects a fundamentally western view of oceans that works in tension with ocean literacy goals. Although ocean literacy practitioners and researchers are, laudably, starting to incorporate Indigenous knowledges and perspectives from BIPOC communities, attention to historical change continues to be left out of ocean literacy, to the detriment of ocean literacy goals. This article points out that, given the reality that human-ocean relationships have changed over time, and differed among cultural groups in the past as well as in the present, ocean literacy needs to incorporate ocean history at a foundational level. Because there are historical differences in human relationships with oceans, it stands to reason that regional ocean literacies must be more effective than a universal and timeless ocean literacy framework. Following the logical efficacy of a regional approach to ocean literacy, this article further argues that regional ocean literacies should involve the systematic inclusion of emotional elements. Regional ocean literacies should be constructed through knowledge co-production, involving diverse types of expertise, knowledge and actors to produce context-specific knowledge and pathways towards a sustainable future. To fully exploit the potential of ocean literacy, there is a need for the UN Ocean Decade to work towards regional and place-based approaches that incorporate history as well as culture in an iterative and collaborative process involving diverse types of expertise, knowledge and actors.
Giant clam (Tridacna) distribution in the Gulf of Oman in relation to past and future climate
(2022)
The Oman upwelling zone (OUZ) creates an unfavorable environment and a major biogeographic barrier for many coral reef species, such as giant clams, thus promoting and maintaining faunal differences among reefs on the east and west side of the Arabian Peninsula. We record the former existence of Tridacna in the Gulf of Oman and review its stratigraphic distribution in the Persian Gulf to provide new insights on the connectivity of coral reef habitats around southern Arabia under changing climate and ocean conditions. Fossil shells were carbon-14 dated and employed as sclerochronological proxy archives. This reveals that the Omani population represents a last glacial colonization event during the Marine Isotope Stage 3 interstadial under colder-than-present temperatures and variable upwelling intensity linked to Dansgaard-Oeschger climate oscillations. It was favored by temperatures just above the lower threshold for the habitat-forming reef coral communities and instability of the upwelling barrier. We conclude that the distribution of Tridacna in the northern Arabian Sea is generally limited by either strong upwelling or cool sea surface temperature under gradually changing climate conditions at the interglacial-glacial scale. Opportunities for dispersal and temporary colonization existed only when there was a simultaneous attenuation of both limiting factors due to high-frequency climate variability. The OUZ will unlikely become a future climate change refuge for giant clams because they will be exposed either to thermal stress by rapid anthropogenic Indian Ocean warming or to unfavorable upwelling conditions.
Global change is one of the major challenges our society faces in recent times and is becoming increasingly noticeable in all aspects of our lives. In the last ten years, reports about droughts in Europe increased, contrary to expected natural climate variations and are attributed as indicators of climate change. Droughts resulted in a severe decrease in water levels of lakes, rivers and reservoirs, posing socio-economic and environmental challenges. Climate scenarios by the Intergovernmental Panel on Climate Change (IPCC) project increasing temperatures, more frequent, longer and/or more intense heat waves and warm spells, and an increase in aridity with short-term droughts in the upcoming decades for Western and Central Europe. Some areas – such as Northeast Germany – are already affected by negative water balances and the lowering of lake and groundwater levels. Additionally to possible challenges in water availability, excess nutrients and heavy metals from industrial emissions, agricultural fertilisers and land use changes lead to declining water quality. In the past century, extensive eutrophication and environmental pollution have become major water quality issues in many freshwater bodies.
Nonetheless, water and its availability in a sufficient quantity and quality are prerequisites for life and must be prioritised in future development. The European Union aims for a good status in all surface and groundwater bodies by 2027 regarding their ecological, chemical and quantitative status. However, a profound understanding of eutrophication, pollution sources, and water bodies' reference conditions – referring to pre-anthropogenic conditions – should be available for each system to apply integrated restoration strategies. Moreover, an in-depth understanding of long-term climate variability and its dynamics is indispensable to approach these climate change challenges and reliably predict water availability.
During the past decades, numerous paleoenvironmental studies have been carried out on Northern German sediment archives, using mainly lacustrine sediments to reconstruct hydroclimatic variability, often inferring lake-level variations as key indicators. However, most studies were carried out in areas affected by more maritime or continental climate. Studies from the transition zone are rare. Only few existing studies offer high-resolution records and/or robust chronologies, which limits the understanding of past environmental changes significantly. Besides, the Northern German lowlands have been anthropogenically affected since at least the Neolithic (~5.6 ka cal BP) and, in particular, forest composition and density have recently been shown to have at least partially an impact on lake-level variations. However, a reliable distinction between climatic impacts and anthropogenic interferences is widely missing, which is a problem because many studies were conducted on rather small lacustrine systems in which expected anthropogenic signals are higher, and single events may overprint the climatic signals. These biases lead to an incoherent picture of the past hydroclimatic variability in Northern Germany during the Holocene. To overcome this situation, it is inevitable to identify a suitable sedimentary archive from the transition zone – preferably a large lacustrine system in which natural (supra-)regional paleoenvironmental signals are expected to be not overprinted by single events. Moreover, it is necessary to establish robust chronologies and apply high-resolution methods to infer past environmental changes in a high temporal resolution. Taken together, this could contribute to an enhanced understanding of past environmental and climatic changes in Northern Germany.
This thesis consolidates the evidence for Schweriner See to act as a suitable sedimentary archive in Northern Germany for (supra-)regional climate reconstructions. Schweriner See is a large lowland lake in Northern Germany located within the transition zone from maritime to continental climate. In the first step, (paleo)lacustrine landforms, i.e. beach ridges, subaerial nearshore bar, and a silting-up sequence, are investigated along the north-eastern shoreline using a combined approach of sedimentology (e.g. grain size variations) and the relatively novel method of luminescence profiling offering relative age determinations to understand depositional processes and their chronological framework. Absolute age information is mainly inferred by OSL dating. Secondly, an important prerequisite to interpreting information obtained from lacustrine sediment archives is a thorough understanding of processes controlling sedimentation. Schweriner See is characterized by a complex morphometry, which influences in-lake processes, i.e. i) in-lake productivity, ii) carbonate precipitation and iii) wind- and wave-induced processes, resulting in a distinct spatial heterogeneity. This thesis shows that it is crucial first to understand sedimentary depositional processes and controlling mechanisms to i) select suitable coring location(s) and ii) reconstruct paleoenvironmental and hydroclimatic variations reliably.
Based on bathymetric considerations and inferred in-lake processes, two main coring locations were identified to infer i) the anthropogenic impacts and ii) hydroclimatic variations. Short sediment records from the shallow water areas (< 15 m water depth) cover the most recent environmental history of Schweriner See. A well-dated sedimentary record (210Pb/137Cs and 14C dating) links distinct sedimentary and geochemical changes with historical events. Schweriner See was extensively affected by lake-wide eutrophication and contamination, closely related to sewage and population dynamics within the catchment. The water quality only improved after the German Reunification in 1990 CE when sewage was precluded from Schweriner See. Contamination trends at Schweriner See showed similar trends to different archives along the southern Baltic Sea, implying a common regional driving mechanism, e.g. environmental legalisation.
A well-dated sediment record from the profundal zone (52 m water depth) allowed the reconstruction of large-scale atmospheric conditions during the past 3 ka cal BP by inferring winter temperature variability, the moisture source region and/or evaporative lake water enrichment, which resemble variations in the North Atlantic Oscillation (NAO). The NAO greatly influences the Central European climate, affecting, for example, surface air temperature, precipitation or storm tracks. During 3-2.8 ka and 2.1-0.8 ka cal BP, predominantly positive NAO conditions are reconstructed, which are characterized by warmer winter temperatures, moisture conditions bringing isotopically enriched precipitation from the southern/central North Atlantic to Northern Central Europe and/or warmer temperatures that may result in a higher evaporative isotopic lake water enrichment as a result of northwards displaced westerlies. Conversely, during 2.8-2.1 ka and 0.8-0.1 ka cal BP, results correspond to predominantly negative NAO phases influenced by southwards displaced westerlies. Frequent atmospheric blocking allows for the intrusion of northerly or easterly winds, resulting in colder winter temperatures, isotopically depleted precipitation from the Northern Atlantic and Arctic region and/or a lower evaporative lake water enrichment. In addition to these long-term changes in atmospheric conditions, short-term hydroclimatic variations have been reconstructed, mainly reflecting lake-level variations in conjunction with precipitation variability, with the proxy signal being additionally amplified by wind speed and wave motion. Comparisons with other archives support these results.
So far, the paleoenvironmental reconstruction is limited to the Late Holocene, but initial dating results imply possible interferences until the Late Pleistocene. Therefore, future studies should focus on extending the profundal record from Schweriner See further back in time, providing a high-resolution record covering both the Holocene and possibly the Late Pleistocene.
Die Herausforderungen des globalen Klimawandels stehen seit mehreren Jahrzehnten auf der gesellschaftlichen und politischen Tagesordnung. Die Folgen der Erderwärmung haben das Potential, die heute bestehenden ökologischen, sozialen und wirtschaftlichen Systeme in unbekanntem Ausmaß zu stören. Ungeachtet dieser Tatsache bleibt die mediale Aufmerksamkeit auf das Thema größtenteils überschaubar. Das Ziel der Arbeit ist es, ein Bild der Tagesschau Medienagenda im Jahr 2022 zu zeichnen. Im Fokus steht hierbei die Berichterstattung über die Klimakrise im Verhältnis zu anderen sozio-ökonomischen Krisen, wie der COVID19-Krise, der Wirtschaftskrise, der Energiekrise und dem Angriffskrieg gegen die Ukraine. Zur inhaltlichen Auswertung der Tagesschau-Hauptsendung wurde eine qualitative Inhaltsanalyse durchgeführt. Über theoretische Annäherungen, wie den Agenda-Setting-Ansatz und den Framing-Ansatz, konnten Rückschlüsse über die Medienwirkung und das Verhältnis der Krisen zueinander getroffen werden. In der computerbasierten Auswertung mit MAXQDA wurde herausgestellt, dass die Klimakrise mit anderen gesellschaftsrelevanten Themen um Sendeplätze konkurriert. Vor allem der Kriegsausbruch in der Ukraine dominierte die Berichterstattung im Jahr 2022. Darüber hinaus wurde die Klimakrise in der Tagesschau vor allem als Thema politischer Konflikte geframed. Im Jahr 2022 war außerdem der Frame der Klimakrise als Teil multipler Krisen präsent. Dieser suggerierte eine Gleichwertigkeit aller aufkommenden Konflikte, welche der Klimakrise und ihren tiefgreifenden Folgen nicht gerecht wird. Um diese Rolle angemessen zu berücksichtigen, muss der Journalismus innovative Wege finden, um eine ressortübergreifende Berichterstattung des Themas zu erreichen. Nur so können die komplexen wissenschaftlichen Erkenntnisse über die Erderwärmung als Basis für die dringliche Abmilderung der Klimakrise vermittelt werden. Verschiedene Ansätze einer solchen Berichterstattung werden diskutiert.
Based on extensive investigations along the coast and in the coastal waters of NE Germany, a lithostratigraphic classification of the Holocene coastal deposits is presented. Their characteristics, i.e. the lithofacies, reflect the spatial change in hydrodynamics, sediment supply, salinity, bioproduction, etc. in the accumulation space. The displacement of the facies associated with the sea-level rise of the Baltic Sea led to the formation of regularly occurring vertical depositional sequences. From these regular profiles, four lithostratigraphic formations and two subformations of the coastal deposits can be delineated as approximately homogeneous sedimentary bodies, which are described in detail, defined in terms of their spatial extent and classified with regard to the time of accumulation.
The exchange of water and dissolved elements between the continents and the oceans occurs via different routes in the hydrological cycle, such as rivers, atmospheric exchange, and submarine groundwater discharge (SGD). In addition, the elemental fluxes in the coastal waters may strongly depend on benthic water-solid-microbe interactions close to the sediment-water interface. It is becoming increasingly recognized that SGD can impact diagenesis and act as a source of water and dissolved substances for coastal ecosystems. The qualitative and quantitative assessment of SGD is still challenging as it requires the identification of suitable geochemical tracers for the complex hydrological and biogeochemical processes in the subterranean estuary. In this study, geochemical analyses were combined with geophysical, hydrological, and biological investigations to gain insights into the mechanisms driving SGD in coastal waters. In addition, onshore ground and surface waters were evaluated to identify the processes controlling the potential end member. The surveys were performed along the Baltic Sea coast: Warnow River and Wismar Bay in Germany, the Gulf of Gdańsk and Puck Bay in Poland, and Hanko Bay in Finland. The results suggest that the analyzed surface water system was strongly impacted by seasonal variations, while SGD displayed a much more stable composition throughout the year. New areas of SGD were also identified along the Baltic Sea. It was also observed that anthropogenic coastal infrastructures could promote SGD affecting the water balance and the benthic fluxes. At other sites, the SGD was associated with natural structures such as pockmarks. The stable isotopic composition of the fresh component of SGD was close to the meteoric water at most sites; however, old groundwaters from distinct aquifers were identified. Combining all sites, SGD showed high variability, ranging from near 0 to up to 300 L m-2 d-1, and the saline SGD was more dominant than the fresh component. The fluxes obtained at one site were even higher than the surface runoff. SGD was higher on sandy sediments, but the elemental fluxes were relatively low. Despite low SGD at muddy sites, interfacial elemental fluxes, enhanced by intense diagenesis in the top sediments, resulted in higher chemical fluxes to the water column. The sediment porewater gradients at the SGD impacted sites suggest that the advective upward flow of groundwater increased the elemental fluxes across the sediment-water interface. Therefore, the dissolved substances of SGD are partly impacted by the processes in the soil zone and aquifer during groundwater development, and partly impacted by the early diagenetic process in the surface sediments. Overall, this study shows the importance of SGD for the biogeochemical cycles of coastal waters. Moreover, 6 it can be concluded that a combination of interdisciplinary approaches can provide a better understanding and assessment of SGD in a specific environment. Although all the studies presented here are local, the methodology and results presented in this thesis can be replicated and thus provide assistance in other coastal areas.
Autoclaved aerated concrete (AAC) is a building material that combines heat insulation
properties with sufficient mechanical strength for masonry construction. Compared to
ordinary concrete, the matrix is highly porous (>50%) and hardened by a hydrothermal curing
process at 150°C - 200°C. During this process, quartz sand and portlandite react to form first
calcium silicate hydrates (C-(A)-S-H) with Ca/Si ratios <1.3 and then tobermorite. Especially
tobermorite, which has a much larger crystallite size than C-(A)-S-H, provides improved
mechanical strength. This reaction sequence is influenced by many parameters and
additives of which calcium sulfate is probably the most important. Despite several attempts to
investigate these hydrothermal reactions, the actual reaction mechanism involved when
adding sulfate ions is not fully understood. It has been suggested that the addition of ca.
1.5 wt% significantly improves the mechanical properties due to the enhanced formation and
arrangement of tobermorite in the porous matrix. Since the sulfate content in AAC waste is
exceeding regulatory threshold for low-quality reuse in some countries, the aim of this study
was to investigate in detail the reaction mechanisms involving sulfate addition. Such
knowledge may open up the possibility to improve AAC production and to avoid the need for
sulfate addition. To achieve this goal, this research work focused on investigating the
hydrothermal curing process to determine the sequence of hydrothermal reactions and the
spatial distribution of the phases formed. For this purpose, a new setup for in situ X-ray
diffraction was specifically designed to study hydrothermal reactions and to conduct time
intensive experiments on a normal laboratory diffractometer. In order to quantitatively
evaluate the in situ measurements by Rietveld analysis using TOPAS, it was also necessary
to develop atomistic structure models for C-(A)-S-H phases. This was made possible by
adopting a supercell approach that was previously used to describe turbostratically stacked
clay minerals. The structure models, derived from tobermorite, are placed in an otherwise
empty supercell to simulate the C-(A)-S-H nanostructure. Adopting these methodological
advances, it was possible to obtain absolute phase quantities from in situ data and to track
the reaction kinetics of the hydrothermal curing process. These results were then combined
with ex situ X-ray diffraction and scanning electron microscopy. Confirming previous studies,
the major effect of sulfate ions was the formation and decomposition of hydroxylellestadite. It
was further revealed that C-(A)-S-H formation was delayed during hydroxylellestadite
formation, which is supposed to support the silicate ion diffusion and hence the tobermorite
formation at a stage critical for improved hardening of AAC. This can be linked to the
formation of lower amounts of capillary pores in the range of 1-5 µm, as observed by
scanning electron microscopy, and therefore a lower concentration of inherent defects that
resulted in the improved mechanical properties. This research work highlights how important the spatial distribution of crystallites is for the properties of a building material and how this
distribution can be influenced by small alterations in reaction chemistry.
Der Begriff Nachhaltigkeit hat längst Eingang in den deutschen Sprachgebrauch gehalten. Doch
wie verhält es sich mit dem Verständnis zum Paradigma Nachhaltigkeit, welches sich im
soziologischen, ökonomischen und ökologischen Wirkungsgefüge bewegt? Aufgrund ihrer
sozialen Relevanz, ihrer distributiven Verflechtungen und ihrer Bedeutung für den
Wohlfahrtsstaat kommt Unternehmen eine große Bedeutung zu. Hilfreich für die Erforschung
des komplexen und dynamischen Nachhaltigkeitsprozesses sind individualisierte Sichtweisen in
räumlichen Abgrenzungen. Biosphärenreservate, die weltweit von der UNSECO als
Modellregionen für nachhaltige Entwicklung als solche anerkannt wurden, bieten sich hierfür
an. Die übergeordnete Forschungsfrage dieser Arbeit lautet daher: Wie wird in den UNESCOBiosph
ärenreservaten die nachhaltige Entwicklung, speziell verantwortungsvolles Wirtschaften,
exemplarisch verwirklicht?
Eine Einordnung in den Nachhaltigkeitsdiskurs zeigt aktuelle Perspektiven auf und stellt die
Nachhaltigkeitsforschung im Kontext der Biosphärenreservate sowie die Bedingungen für
verantwortungsvolles Wirtschaften vor. Als forschungsrelevante Zielgruppen wurden die
Verwaltungen der UNSECO-Biosphärenreservate (BR), Multiplikatoren der Wirtschaft (z.B.
kommunale Wirtschaftsförderungen, IHK, Handwerkskammern, Bauern- und
Wirtschaftsverbände) sowie Unternehmen in bzw. an BR identifiziert. Mithilfe von
leitfadengestützten Experteninterviews und hybriden Fragebögen erfolgte die Datenerhebung,
die mit der Grounded Theory bzw. grafisch ausgewertet wurden.
Die Datenerhebung hat gezeigt, dass BR-Verwaltungen bislang überwiegend für
Umweltschutzbelange mandatiert und für die Einflussnahme hinsichtlich verantwortungsvollen
Wirtschaftens auf Kooperationspartner angewiesen sind. Wirtschaftsbezogene Aktivitäten sind
innerhalb ihrer Netzwerke der Partnerbetriebe etabliert, sie fokussieren überwiegend die
Direktvermarktung regionaler Produkte und die Inwertsetzung der naturverträglichen
Tourismusangebote. Innerbetriebliche Prozesse werden von einigen BR-Verwaltungen mit
Beratungsangeboten zu Umweltmanagementsystemen (z.B. EMAS) begleitet. Etliche BR weisen
wenn überhaupt nur einen geringen Besatz an Industrie- oder Dienstleistungsunternehmen, ihre
Verwaltungen haben daher auch kaum Berührungspunkte zu den Betrieben des sekundären und
tertiären Sektors außerhalb der Tourismusbranche. Die auf repräsentative Kulturräume
ausgerichteten Zonierungskonzepte der BR können diesbezüglich überdacht werden. Deutlich
wird, dass Handlungskompetenzen in wirtschaftsorientierten Themenkomplexen (Beratung zu
Fördermöglichkeiten, Innovationen, Technologieanwendung, Unternehmensgründung, mobiles
Arbeiten, Aus- und Weiterbildung, Vereinbarkeit von Beruf und Familie, Fachkräftesicherung,
Zertifizierungen, Produktentwicklung, Prozessoptimierung, Digitalisierung) nach Institutionen
durch die Wirtschaftsvertreter überwiegend den IHK, den Handwerkskammern und
Wirtschaftsförderungen und weniger den BR-Verwaltungen zugeschrieben werden.
Mehrheitlich beurteilen die befragten Unternehmen die Handlungsfähigkeit von BRVerwaltungen
hinsichtlich des Naturschutzes, der Vermarktung regionaler Produkte und
Dienstleistungen sowie von Agrarumweltmaßnahmen positiv. Dagegen ist den Unternehmen
die Handlungsfähigkeit der BR-Verwaltungen auf den Gebieten der Verkürzung von
Planungsverfahren, der Prozessinnovation, des Energiemanagements und der
Fachkräftesicherung weitestgehend unbekannt. Eine große Mehrheit der Unternehmer meint
zudem, dass sich die Ziele und Aktivitäten der BR-Verwaltungen vorrangig auf
Naturschutzmaßnahmen beziehen. Weiterhin meinen sie, richtet die sich die Unterstützung von
Unternehmen überwiegend auf die Vermarktung regionaler Produkte und traditionelles
Handwerk. Die 17 Nachhaltigkeitsziele der Vereinten Nationen haben bislang keinen
breitenwirksamen Bekanntheitsgrad in der befragten Unternehmerschaft gefunden.
In einem integrierten Verständnis fließen ökologische und soziale Aspekte der Nachhaltigkeit in
die konzeptionellen Grundlagen der BR ein, die ökonomische Dimension dagegen reduziert sich
oft auf die Bereiche Landwirtschaft und Tourismus. Weiterführende Aktivitäten hinsichtlich
nachhaltigen Wirtschaftens überlassen BR-Verwaltungen derzeit überwiegend der Expertise
wirtschaftsfördernder Institutionen, die sich aus ihrer Sicht originär mit innerbetrieblichen
Prozessen befassen.
Der Austausch von Grundlagendaten oder Ergebnissen bisheriger Datenerhebungen zwischen
den BR-Verwaltungsstellen – einem potenziellen Wesensmerkmal von Modellregionen – wird
durch das Fehlen entsprechender Infrastruktur deutlich erschwert, bzw. ist nicht möglich.
Technische und personelle Ressourcen für die digitale Datenaufbereitung und -pflege in den BRVerwaltungen
sind überwiegend nicht vorhanden.
Mit der Anerkennung eines BR durch die UNESCO muss auch seine Anerkennung als
Modellregion für nachhaltige Entwicklung durch alle beteiligten Interessengruppen
einschließlich seiner Bewohner einhergehen.
The deep geological underground represents an important georesource for the short-
term storage of renewable energy and the long-term reduction of greenhouse gas emissions. To ensure the economic viability and safety of any subsurface storage project, detailed characterisation of the quality and integrity of the reservoir and its cap rock is required. This characterisation includes the accurate determination of the petrophysical properties, such as porosity and permeability, as well as the potential mineral reactions, such as the dissolution of reactive phases, which may occur during the lifespan of such a project. Clay minerals are common components of many reservoir systems and, depending on their type and structure, can have a significant impact on storage and transport properties. These processes are, however, currently not well understood. In order to address these issues, the main focus of this thesis is on mineralogical analyses using X-ray diffraction (XRD) and microstructural studies using focused ion beam scanning electron microscopy (FIB-SEM) together with micro X-ray computed tomography (µXCT) to gain a better understanding of the influence of clay minerals on reservoir and cap rock properties.
A central part of this thesis focuses on the analysis of clay minerals and pore structures of the Bebertal Sandstone of the Parchim Formation (Early Permian, Upper Rotliegend), which is considered a natural analogue for the tight reservoir sandstones of the North German Basin. Two illite polytypes with a variety of characteristic structures have been identified in the Bebertal sandstone. Disordered 1Md illite forms the majority of the observed structures, which include omnipresent grain coatings, altered permeable feldspar grains and pore-filling meshwork structures. Trans-vacant 1M illite represents the second and youngest generation of authigenic illite and occurs as fibrous to lath-shaped particles that grew into open pore spaces and led to a significant reduction in porosity and permeability during late diagenesis. Based on these results, a model for the formation of illite polytypes in the aeolian layers of the Bebertal sandstone was developed that describes the temporal and spatial evolution of porosity and permeability during diagenesis. Information from this model was then used to improve the prediction of permeability of the Bebertal sandstone based on µXCT pore space models and direct numerical simulations. To achieve this, a micro-scale pore space model was created that allowed the simulation of permeability reduction by clay minerals by including nanoporous illite domains based on a novel morphological algorithm. By performing Navier-Stokes-Brinkman simulations, more accurate predictions of permeabilities with respect to experimentally determined values were obtained compared to conventional Navier-Stokes simulations.
The detailed characterisation of the Bebertal sandstone has shown that natural reservoir rocks are usually complex heterogeneous systems with small-scale variations in texture,
composition, porosity and permeability. Flow-through experiments on the Bebertal sandstone revealed that the coupled geochemical and hydrodynamic processes that occur during the dissolution of calcite could not be predicted by reactive transport models. Therefore, as part of this thesis, a novel approach for developing synthetic sandstones at low temperatures based on geopolymer binder was developed. It is shown that simpler and more homogeneous porous materials can be produced with porosity and permeability values in the range of natural sandstones. These can be used to better understand the dynamic and coupled processes relevant to the storage of renewable energy in reservoir rocks through improved experimental constraints.
The final part of this thesis reports on a detailed clay mineral and pore space study of
three shale formations and one mudstone that were identified as potential seals for the Mt. Simon sandstone reservoir in the Illinois Basin. During the Illinois Basin - Decatur Project, this reservoir was used for the sequestration of one megaton of supercritical carbon dioxide. In order to better assess the quality of the sealing units and to better understand the role of the intergranular clay mineral matrix as potential pathway for fluid migration, a multi-scale evaluation was conducted that included thin section analysis, quantitative evaluation of minerals by scanning electron microscopy (QEMSCAN), mercury intrusion capillary pressure (MICP) measurements, quantitative XRD and high-resolution FIB-SEM. The results allow for the classification of the studied formations into primary and secondary seals and emphasise the importance of three-dimensional clay-mineral-related pore structure characterisations in cap rock studies. XRD proved the most reliable method for the identification and quantification of clay minerals in the studied cap rocks and mudstones. In contrast, FIB-SEM and QEMSCAN provided the spacial constraints for reconstructing fluid flow pathways within the clay mineral matrix.
Overall, this thesis highlights the importance of the precise identification of clay minerals in geological reservoirs and their cap rocks. It also illustrates the need for three-dimensional characterisation and modelling of the associated small pore structures for an improved understanding of the rocks diagenetic history as well as the prediction of the transport and storage properties of these crustal reservoir systems.
Der Einfluss von Zentrum-Peripherie-Sturkturen auf Kommunalfinanzen wird aus geographischer Sicht empirisch untersucht. Die Rechnungsergebnisse der Kommunen im Zeitraum von 2013 bis 2016 der fünf ostdeutschen Bundesländer dienen als Berechnungsgrundlage. Die Dissertation gliedert sich in vier Teile, die Fragen zu Zusammenhängen und Wechselwirkungen zwischen Zentren und Peripherien beantworten. Dabei sind vor allem planerisch festgelegte Zentrale Orte und externe Nutzer im Fokus der Untersuchungen. Im letzten Teil wird die Frage diskutiert, wie sich planerische Belange in das fiskalische Instrument „kommunaler Finanzausgleich“ integrieren lassen.
Underground hard coal mining operations irreversibly disrupt the pre-existing mechanical equilibrium of the geological media. The employment of high-recovery methods modifies the stress field of the sedimentary sequence, generating movement and faulting of the rock layers above and below mined seams. These new fracture zones do affect the original conditions of the hydrogeological system by modifying flow pathways and increasing the permeability of the rock sequence. Moreover, the surface area of rock exposed to air and water is increased, conditioning the water-rock interaction. Despite this rather clear conceptualization, flow and reactive transport processes in fractured overburdens are rarely modeled simultaneously. Discrete setups that consider fractures and porous matrix require extensive characterization of both media, which is impractical for regional case studies. As a result, most post-mining models explicitly ignore fracture structures by employing the equivalent porous approach or even both media with lumped parameter models. However, omitting either medium represents a delicate simplification, considering that mining-related fractures control the rate and direction of water flow within moderately permeable but relatively highly porous rock sequences.
In this dissertation, the specific contribution of fractured and matrix continua to the transient discharge and water quality of a post-mining coal zone is quantified and evaluated. For this purpose, dual and multiple interacting continua models are employed to simulate fluid flow and reactive mass transport in fractured and variable water-saturated rock sequences. The effectiveness of the models is evaluated by simulating the origin, generation and transport of acid mine drainage (i.e., water with elevated concentrations of hydrogen, iron, sulfate and chloride) within the shallow overburden of the Ibbenbüren Westfield. Compared to other coal districts in Germany, this area is strongly delimited by the local geology and topography, resulting in a well-defined hydrogeological system to test the models. Petrographic and chemical analyses performed on core samples from the area show the strong influence of mining-derived fractures on the water-rock interaction within the Carboniferous sequence. The presence of oxidized pyrite along with amorphous iron hydroxide phases in weathering fronts on both sides of the fractures demonstrates the exchange of solutes and gases between the fractured and the porous matrix media.
Based on the previous evidence, the TOUGHREACT software is employed to characterize flow and reactive transport processes in the Westfield. However, each of the two processes is simulated at separate stages to have more control in the adjustment of sensitive parameters for which little information is available. For the flow component, a dual continuum model, with Richard’s equations is used to characterize the unsaturated water flow in both fractured and matrix media. Under this approach, the model adequately reproduces the bimodal flow behavior of the discharges measured in the mine drainage for the years 2008 and 2017. Simulation results show how the fractured continuum generates intense discharge events during the winter months while the rock matrix controls smooth discharge limbs in summer, when water is slowly released back to the fractures. With the flow component calibrated, the second part of the study incorporates the geochemical processes into the model based on actual data from the rock samples. Their simulation requires extending the two-continuum setup to a multiple continua model with five nested block strings: one for the fractures and four for the rock matrix. This further subdivision prevents under-representations of kinetic reactions with short equilibrium length scales and numerical instabilities due to lack of chemical and flow gradients. As a result, the new multiple continua model provides good agreement with respect to long- and short-term concentrations and discharge trends measured in the mine drainage. The flow of oxygen and meteoric water through the fractured continuum leads to a high and steady release of hydrogen, iron and sulfate ions derived from pyrite oxidation in the matrix continua closest to the fractures. Moreover, high chloride concentrations result from the mixing and gradual release of relatively immobile solutes in the matrix as they interact with percolating water in the fracture. Both findings are equally congruent with the reactive pyrite oxidation and iron hydroxide precipitation fronts identified in the fractured core samples.
In the end, the multiple continua models, the simulation procedure and the results of the benchmark and sensitivity analysis scenarios developed for the Westfield pave the way for the application of the approach in other mining zones. The first candidate emerges in the Ibbenbüren Eastfield, where a coupled elemental-isotopic approach included in this thesis has confirmed that water-conducting fracture zones are primary elements for solute generation and transport in the first 300 meters of the overburden. In the latter case, calibration and verification of the models can be complemented with measurements of δ34S in sulfates and δ18O, δ2H, and Tritium in water.
The skull is an extremely informative part of the vertebrate body. Skulls are
involved to hunt, feed and drink, to nurse, fight, dig, and to many other activities.
Also, main sensory organs are situated on the head in order to enable a given
animal to see, smell, taste, feel, listen, equilibrate and think; hence, the head is the
main connection to the external world. It follows that a skull, with and without soft
tissue, can tell a lot about its owner. Each skull consists of many individual bones
constituting regions (e.g., snout and braincase) that represent different aspects of an
anatomical mosaic, which in turn allows deeper (palaeo)biological insights.
In the past three centuries, palaeontologists dug out countless fossils from all
over the world and from many preserved periods and groups, including dinosaurs.
Hence, public and private collections house numerous fossil skull specimens. To
further enlighten our understanding of palaeoecological, physiological and
phylogenetic affinities of dinosaurian representatives belonging to different groups,
and in order to reveal new aspects on their (neuro)anatomy, behaviour, ontogeny
and evolution, a thoroughly examination with modern techniques is the aim of this
thesis.
In order to get a phylogenetically broad understanding, fossil remains from at
least four extinct species, including Irritator challengeri (a theropod: mostly bipedal
carnivores) from the Early Cretaceous of northeastern Brazil, Europasaurus holgeri
(a sauropod: long-necked, quadrupedal herbivores) from the Late Jurassic of Lower
Saxony, Emausaurus ernsti together with an unnamed taxon from the Early Jurassic
of Mecklenburg-Western Pomerania, and Struthiosaurus austriacus, Late
Cretaceous of eastern Austria (the latter three are thyreophorans: armoured, mostly
quadrupedal herbivores), were in closer focus. To document and digitally reconstruct
cranial bones and cavities therein, the material was examined with micro computed
tomography (microCT). On this basis, the full morphology of the preserved anatomy
was revealed, described and contextualized, for example, in conjunction with
comparative anatomy and biomechanical considerations. During this process, further
methods were used to investigate and depict individual fossils: macro- and microphotography,
photogrammetry and phylogenetic analyses, each encompassing
multiple sub-tasks and being supported by 3D prints.
As part of the result, it was possible to formulate reasoned assumptions about
the lifestyle of the taxa in focus. For instance, the neuroanatomy and the osteological
characteristics of the spinosaurid Irritator challengeri implicate that this taxon was an
agile hunter with a habitually inclined snout that was specialized in catching relatively
small prey with a robust dentition and a comparably weak - but fast - bite, with a
remarkable jaw mechanism which enabled the animal to kinetically widen the
pharynx during lower jaw depression. The (neuro)anatomy of I. challengeri, S.
austriacus, E. ernsti and E. holgeri presented here, enrich our knowledge about a
plethora of (lifestyle-related) aspects of these animals, their closer relatives and the
prehistoric world they lived in.
Seas and oceans are essential for the global ecosystem. Entire societies, economies and countless livelihoods rely on their good environmental status. Yet, pressures on marine environments are increasing. An extensive assessment and monitoring of marine habitats is a vital precondition for understanding these systems and their sustainable conservation. Remote sensing methods can temporally accelerate the mapping, improve the spatial resolution and support the interpretation of large areas. Hydroacoustic becomes the method of choice for areas deeper than the coastal zone as optical signals are limited by strong attenuation in the water column. Apart from depth measurements for the creation of bathymetric charts, the recording of backscatter strength is useful for the characterization of the seafloor surface. The direct influence of the inhabiting benthic community on the backscattered signal is rarely considered, although it can be utilized for the detection of benthic life. Information about habitat-specific backscatter responses or a hydroacoustic remote sensing catalog for benthic habitats is missing so far.
The multibeam echosounder (MBES) has the advantage of recording both, bathymetry and backscatter strength simultaneously with related incidence angle. Further, recent technological developments allow to change between frequencies. Angular range curves supported the quantification of backscatter strength of different frequencies. Acoustic data sets were complemented by ground truthing in form of sedimentological and biological samples as well as video profiles. Study areas were located offshore the island of Sylt in the North Sea as well as in vicinity to Oder Bank and close to the coast offshore Hohe Düne/Rostock, both in the Baltic Sea. Investigated habitats included sand areas inhabited by tubeworms, loose mussel clusters on top of sand areas, seagrass meadows, coarse sand and gravel areas, and a reef covered by mussels.
Multifrequency backscatter maps, combining frequencies between 200 kHz and 700 kHz, illustrate small-scale features at the seafloor not visible in monofrequent maps. Key habitats showed a specific backscatter response, which can partly be related to macrobenthic flora and fauna. Data sets recorded with a (partly calibrated) MBES in three different month (May, August, October) revealed that backscatter strength can further detect spatial as well as temporal habitat dynamics. Alterations in the sediment composition at the seafloor surface of the ecologically valuable coarse sand and gravel areas were caused by seasonal changes in local hydrodynamics.
A newly developed 3D seismic lander has the ability to support hydroacoustic remote sensing as an additional, non-destructive ground truthing method utilizing a high frequency of 130 kHz to image the shallow subsurface. Buried objects, e.g., stones, shells, fruit gummy worms, as well as sediment disturbances could be detected and visualized in a laboratory experiment. The 3D seismic lander is likely to improve the investigation of volume scatter contribution to backscatter strength and is potentially applicable for the imaging of bioturbation.
This work first sets out to find if economic, ecological, or social incentives drive consumers towards or against dietary decisions (Contribution A). It then develops a framework of TCA for food to describe economically conveyed incentives that are tied to ecological and social indicators within the food market (Contribution B). The framework is subsequently enhanced and broadened to include a deeper understanding and broader field of indicators for more holistic TCA calculations (Contributions C and D). Lastly, based on these calculations, TCA of food is implemented in a factual use case as the framework and calculations are deployed for commodities of a German supermarket chain; then consumer, as well as expert feedback is used for the discussion on socially responsible campaigning and policy change (Contribution E).
The dissertation looks at bioeconomy innovation at different levels through the lens of economic geography. By progressing from the meta to the micro-scale, it tries to find answers to how the interrelated concepts of bioeconomy and innovation are embedded in these respective contexts while consecutively concretising bioeconomy and de-fuzzing it. To do that, it adopts a mixed-methods approach that starts general and ends specific, going from the meta-scale of literature over the macro-scale of three distinct areas in which bioeconomy is discussed to the meso-level of central actors of a European funding network before, lastly, considering case studies at the micro-scale. Throughout, the thesis aims to spatialise the bioeconomy by shedding light on the term and its drivers across multiple geographic layers. It thereby not only offers new insights into dimensions of innovation in the bioeconomy but also contributes to the discipline of economic geography by applying some of its essential theoretical ideas to an emerging political framework.
Growth corridors have been an instrument of
economic development for decades but have gained new
attention in regional economic development policies in recent years, e.g., in Sub-Saharan Africa or Southeast Asia.
They are seen by policy makers and private businesses as
catalysts of regional economic integration, pushing traditional businesses into increasingly complex international
value chains. However, the outcomes of such development
initiatives are still barely understood. Critics argue that development policies are based on simplified models that are
unable to sufficiently address the complexity of regional
development. Policies on value-chain development, for
example, can lead to conflicts, external dependencies,
land rush, and a polarization of wealth. Growth corridors
often go hand-in-hand with socio-economic transformations and land-use conflicts. This paper first discusses the
theoretically possible desired and undesired regional socio-economic effects of modern corridors. Second, we illustrate the potential and challenges to realize integrative
(or inclusive) development by contrasting three growth
corridors: the SAGCOT growth corridor in Tanzania, the
Walvis Bay-Ndola-Lubumbashi Development Corridor
(WBNLDC) in Namibia, Zambia and Zimbabwe, and the
growth corridors in the Greater Mekong Subregion (GMS)
Are old regions less attractive? Interregional labour migration in a context of population ageing
(2021)
Abstract
Regional demographic change is often conceptualized as a circular process, where out‐migration continuously worsens conditions of population ageing and shrinkage. Thus, if migration acts as a consequence as well as cause of ageing, migration patterns should be influenced by the age structure of origin and destination regions. This paper analyses individual‐level migration decisions of full‐time employees across 326 German regions between 1997 and 2013 using binary choice models. The results show that individuals are more likely to migrate out of and less likely to migrate towards ageing regions. Moreover, the identified patterns are consistent with age‐selective migration reinforcing ageing processes and polarization of demographic structure.
Abstract
We investigated four subaerial (paleo)lacustrine landforms at the north‐eastern shoreline of Schweriner See, north‐eastern Germany. These included two beach ridges, one subaerial nearshore bar and a silting up sequence located close to a fossil cliff, which marks the former maximum extent of Schweriner See. We used luminescence profiling with a SUERC portable OSL device (POSL) on all four sediment sequences in combination with sedimentological investigations such as grain size, loss‐on‐ignition and magnetic susceptibility to provide information on the various formations in a lacustrine depositional environment. The POSL reader was used on pre‐treated polymineral samples to gain an insight into luminescence distribution within the individual sediment sequences, but also among the four sequences. POSL proved valuable to understand depositional processes, which were not visible in lithology or sedimentological parameters. With somewhat larger uncertainty this method provides relative chronologies of the sediment sequences. Additionally, we carried out radiocarbon dating and full optical stimulated luminescence (OSL) dating to establish a chronological framework. OSL ages proved to be more reliable to date beach ridges in this setting than radiocarbon samples, which were severely influenced by sediment reworking. This combined approach of sedimentological analyses, luminescence profiling and absolute age determinations revealed details in depositional processes at Schweriner See which otherwise would have remained undetected. Furthermore, it helped to set these subaerial (paleo)lacustrine landforms in a chronological framework.
Body-size variability results from a variety of extrinsic and intrinsic factors (environmental and biological influences) underpinned by phylogeny. In ostracodes it is assumed that body size is predominantly controlled by ecological conditions, but investigations have mostly focused on local or regional study areas. In this study, we investigate the geographical size variability (length, height, and width) of Holocene and Recent valves of the salinity-tolerant ostracode species Cyprideis torosa within a large geographical area (31°–51° latitude, and 12°–96° longitude). It is shown that distant local size clusters of Cyprideis torosa are framed within two large-scale geographical patterns. One pattern describes the separation of two different size classes (i.e., morphotypes) at around ∼42° N. The co-occurrence of both size morphotypes in the same habitats excludes an environmental control on the distribution of the morphotypes but rather could point to the existence of two differentiated lineages. Generally, correlations between valve size and environmental parameters (salinity, geographical positions) strongly depend on the taxonomic resolution. While latitude explains the overall size variability of C. torosa sensu lato (i.e., undifferentiated for morphotypes), salinity-size correlations are restricted to the morphotype scale. Another large-scale pattern represents a continuous increase in valve size of C. torosa with latitude according to the macroecological pattern referred as Bergmann trend. Existing explanations for Bergmann trends insufficiently clarify the size cline of C. torosa which might be because these models are restricted to intraspecific levels. The observed size-latitude relationship of C. torosa may, therefore, result from interspecific divergence (i.e., size ordered spatially may result from interspecific divergence sorting) while environmental influence is of minor importance. Our results imply that geographical body-size patterns of ostracodes are not straightforward and are probably not caused by universal mechanisms. Consideration of phylogenetic relationships of ostracodes is therefore necessary before attempting to identify the role of environmental controls on body size variability.
To reduce global greenhouse gas emissions in order to limit global warming to 1.5°C, individuals and households play a key role. Behavior change interventions to promote pro-environmental behavior in individuals are needed to reduce emissions globally. This systematic literature review aims to assess the a) evidence-based effectiveness of such interventions and b) the content of very successful interventions without limiting the results to specific emitting sectors or countries. Based on the “PICOS” mnemonic and PRISMA statement, a search strategy was developed, and eligibility criteria were defined. Three databases (Embase, PsycInfo, and Web of Science) were searched to retrieve and review potential literature. As a result, 54 publications from 2010 to 2021 were included in the analysis. The results show that most interventions only have small positive effects or none at all. A total of 15 very successful interventions focused on the sectors of mobility, energy, and waste and incorporated improved (infra-) structures, education, feedback, enablement or made the sustainable option the default. Six evidence-based recommendations for content, timing, and setting are deducted and given for interventions on enhancing pro-environmental behavior (PEB). In summary, although the various interventions and intervention types to promote PEB differ in their effectiveness, very successful interventions have common elements. Future research should focus on high-/low-impact and high-/low-cost behavior to develop interventions that aim at high-impact but low-cost behavior changes, or avoid low-impact but high-cost behavior.
Semi-arid Mongolia is a highly sensitive region to climate changes, but the region’s Holocene paleoclimatic evolution and its underlying forcing mechanisms have been the subject of much recent debate. Here we present a continuous 7.4 ka sediment record from the high-altitude Shireet Naiman Nuur (Nuur = lake) in the central Mongolian Khangai Mountains. We extensively dated the sediments and analyzed elemental composition and bulk isotopes for lake sediment characterization. Our results show that 14C-dating of bulk organic carbon and terrestrial macrofossils provide a robust and precise chronology for the past 7.4 ± 0.3 cal ka BP at Shireet Naiman Nuur and 14C-ages are mostly in stratigraphic order. The 14C-based chronology is confirmed by paleomagnetic secular variations, which resemble the predictions of spherical harmonic geomagnetic field models. The very good chronological control makes paleomagnetic secular variation stratigraphy a powerful tool for evaluating and refining regional 14C-chronologies when compared to the record presented here. The lake sediment proxies TOC, N, log (Ca/Ti) and log (Si/Ti) reveal increased lake primary productivity and high growing season temperatures from 7.4 ± 0.3 to 4.3 ± 0.2 cal ka BP, which is likely the result of stronger summer insolation and pronounced warming. Reduced summer insolation thereafter results in decreased productivity and low growing season temperatures at Shireet Naiman Nuur from 4.3 ± 0.3 cal ka BP until present day. The globally acknowledged 4.2 ka event also appears as a pronounced cooling event at Shireet Naiman Nuur, and additional abrupt cooling events occurred during minima in total solar irradiance at ∼3.4, 2.8 and 2.4 ka BP. Low lake primary productivity and growing season temperatures are likely the result of longer ice cover periods at the high-altitude (2,429 m a.s.l.) Shireet Naiman Nuur. This leads to shorter mixing periods of the lake water which is supported by more positive δ13CTOC because of increased incorporation of dissolved HCO3
− by aquatic producers during periods of longer ice cover.
Madagascar houses one of the Earth’s biologically richest, but also one of most endangered, terrestrial ecoregions. Although it is obvious that humans substantially altered the natural ecosystems during the past decades, the timing of arrival of early inhabitants on Madagascar as well as their environmental impact is still intensively debated. This research aims to study the beginning of early human impact on Malagasy natural ecosystems, specifically on Nosy Be island (NW Madagascar) by targeting the sedimentary archive of Lake Amparihibe, an ancient volcanic crater. Based on pollen, fungal spore, other non-pollen palynomorph, charcoal particle and diatom analyses combined with high-resolution sediment-physical and (in)organic geochemical data, paleoenvironmental dynamics during the past three millennia were reconstructed. Results indicate a major environmental change at ca. 1300 cal BP characterized by an abrupt development of grass (C4) dominated and fire disturbed landscape showing the alteration of natural rain forest. Further, increased soil erodibility is suggested by distinct increase in sediment accumulation rates, a strong pulse of nutrient input, higher water turbidity and contemporaneous increase in spores of mycorrhizal fungi. These parameters are interpreted to show a strong early anthropogenic transformation of the landscape from rain forest to open grassland. After ca. 1000 cal BP, fires remain frequent and vegetation is dominated by forest/grassland mosaic. While natural vegetation should be dominated by rain forest on Nosy Be, these last results indicate that human continuously impacted the landscapes surrounding the lake. At a local scale, our data support the “subsistence shift hypothesis” which proposed that population expansion with development of herding/farming altered the natural ecosystems. However, a precise regional synthesis is challenging, since high-resolution multi-proxy records from continuous sedimentary archives as well as records located further north and in the hinterland are still scarce in Madagascar. The lack of such regional synthesis also prevents precise comparison between different regions in Madagascar to detect potential (dis)similarities in climate dynamics, ecosystem responses and anthropogenic influences at the island’s scale during the (late) Holocene.
In this article, we address the climate crisis as a moral issue and discuss the relevant moral and emotional processes and the role of the media underlying the motivations of individuals to behave in a less carbon-emitting manner. We provide theoretical insights from social psychology and emotion research and empirical data based on an online survey from Germany (N = 979). In the theoretical part, we outline the role of emotions in influencing carbon-related behavior, with a particular focus on self-condemning (e.g., guilt or shame), self-praising (e.g., pride), or other-suffering emotions (e.g., empathy). We further summarize the reasons for the low influence of the media on carbon-related behavior compared to the COVID-19 pandemic. The empirical results confirm that participants reported other- suffering and self-condemning emotions in response to news content and rated their likelihood of personal behavior change as high when confronted with news about the climate crisis on a daily basis, as has been widely the case during the COVID-19 pandemic. We argue that the media is responsible for regularly reporting on the victims of the climate crisis in order to generalize self-condemning and other-suffering emotions into affective attitudes. Opinion leaders can function as role models for low-carbon behavior.
Open and analysis-ready data, as well as methodological and technical advancements have resulted in an unprecedented capability for observing the Earth’s land surfaces. Over 10 years ago, Landsat time series analyses were inevitably limited to a few expensive images from carefully selected acquisition dates. Yet, such a static selection may have introduced uncertainties when spatial or inter-annual variability in seasonal vegetation growth were large. As seminal pre-open-data-era papers are still heavily cited, variations of their workflows are still widely used, too. Thus, here we quantitatively assessed the level of agreement between an approach using carefully selected images and a state-of-the-art analysis that uses all available images. We reproduced a representative case study from the year 2003 that for the first time used annual Landsat time series to assess long-term vegetation dynamics in a semi-arid Mediterranean ecosystem in Crete, Greece. We replicated this assessment using all available data paired with a time series method based on land surface phenology metrics. Results differed fundamentally because the volatile timing of statically selected images relative to the phenological cycle introduced systematic uncertainty. We further applied lessons learned to arrive at a more nuanced and information-enriched vegetation dynamics description by decomposing vegetation cover into woody and herbaceous components, followed by a syndrome-based classification of change and trend parameters. This allowed for a more reliable interpretation of vegetation changes and even permitted us to disentangle certain land-use change processes with opposite trajectories in the vegetation components that were not observable when solely analyzing total vegetation cover. The long-term budget of net cover change revealed that vegetation cover of both components has increased at large and that this process was mainly driven by gradual processes. We conclude that study designs based on static image selection strategies should be critically evaluated in the light of current data availability, analytical capabilities, and with regards to the ecosystem under investigation. We recommend using all available data and taking advantage of phenology-based approaches that remove the selection bias and hence reduce uncertainties in results.
The switch from working in-office to working from home in the context of the COVID-19 pandemic had a significant impact on people’s mobility behavior. In view of the need for action arising from the ongoing challenge of climate change, these changes should be seen as an opportunity to reduce emissions in the traffic sector. The aim of this study was to analyze changes in work-related mobility that occurred during the COVID-19 pandemic using the case of a multinational medium-sized retail chain situated in semi-rural Germany. The case study allowed us to examine those changes in connection with individual attitudes and perspectives of the company and its employees. Thus, we quantitatively recorded the mobility behavior of the company’s employees, followed by an expert interview to ascertain the company’s perspective. We found a reduction in the frequency of commuting and business trips made by employees, which seemed to continue beyond the COVID-19 crisis. However, according to our findings these changes were not based on individual motivation to act in a climate-aware manner but are subject to the framework conditions created by employers for the adoption of climate-friendly behavior. The results of this work could be used by companies and policymakers to create such favorable framework conditions.
This thesis aims to investigate effects of anthropogenic environmental impact on the Richards Bay area. Located on the east coast of South Africa, Richards Bay Harbour evolved into the country’s premier bulk cargo port. The Associated change in land-use and industrial as well as agricultural pollution pose environmental, ecological and human health risks. Here, sedimentological and geochemical investigations focus on the port as final sink for environmental and industrial pollutants, such as metal concentrations, organochlorine pesticides and microplastics.
The study is based on investigations of surface sediment samples from the water-sediment interface to identify spatial distribution patterns, as well as sediment cores to follow temporal changes. Endmember modelling of grainsize distributions, proved to be a viable parameter to distinguish different accumulation spaces and enabled the classification into six harbour sub-basins. Subsequent investigations on the content of microplastics, Polyethylene terephthalate (PET) and Low-density polyethylene (LDPE), showed that these different types of microplastics predominate in two different areas: PET appears to be directly tied to higher populated (tourism) beaches, while LDPE is deposited in low-current sub-basins. Increased metal concentrations link to activities at the bulk cargo berths, where especially Cr and Cu concentrations exceeded the local sediment guideline thresholds. In the areas of high metal concentrations, bioindicators (ostracods, foraminiferas, diatoms) also indicate increased shares of malformed specimens. Multiple recovered sediment cores recorded changes in recent export practices, indicating ceased Cu handling and increased Cr handling over the past decade. Noticing multiple possible influencing factors on elemental distributions, created by the surrounding geological and industrial impact, the usefulness of different normalisers (Al, Fe, Rb, Ti and silt fraction) for Cr, Cu, Co and Pb concentrations was compared and site specific baseline metal concentrations were defined. This identified Al and Rb to be effective normalisers in Richards Bay and Fe or Ti to be affected by local conditions. Data of organochlorine pesticide pollution was gathered in the area of Richards Bay, Goedertrouw Dam and Umlalazi River. The two dominant groups of contaminants detected are dichlorodiphenyltrichloroethanes (ΣDDT, 12 – 350 ng g-1), linked to the use of malaria vector control, and hexachlorocyclohexanes (ΣHCH 35 – 230 ng g-1), an agricultural insecticide. Both indicate recent entry and exceed sediment quality guideline limits, raising concern for local communities and estuarine environments. Seismic data was used to investigate the preindustrial evolution of the incised valley system and bayhead delta at Richards Bay Harbour. A stratigraphically supported development model was created. The thesis shows that harbour sediment is an important sink for inorganic and organic contaminants. Each investigation on environmental pollutants, such as metals, pesticides, microplastics or bioindicator analyses, indicates their deposition in distinct harbour sub-basins. Therefore, their effect can be spatially differentiated and related to plausible sources of pollution. Richards Bay thus represents a variously affected system along the South African coast, in which it is necessary to take environmental protection measures in terms of sustainable and environmentally friendly management.
Here, we provide a detailed taxonomic reassessment of a historically collected chondrichthyan dental assemblage from the lower Kimmeridgian of Czarnogłowy in north-western Poland and discuss its significance for better understanding hybodontiform diversity patterns prior to their post-Jurassic decline in fully marine environments. In spite of its low taxonomic diversity, consisting of four large-toothed taxa (viz., Strophodus udulfensis, Asteracanthus ornatissimus, Planohybodus sp. and cf. Meristodonoides sp.), this assemblage is remarkable in that there are only very few Mesozoic hybodontiform assemblages with more large-toothed genera or even species. Comparisons with other European Late Jurassic hybodontiform-bearing localities demonstrate fairly homogenous distribution patterns characterized by large-bodied epipelagic forms of high dispersal ability. This is in stark contrast to post-Jurassic hybodontiform associations, which are dominated by smaller species that were predominantly bound to marginal marine and continental waters, suggesting a major reorganization of chondrichthyan communities during the Early Cretaceous.
Bentonite is currently proposed as a potential backfill material for sealing high-level radioactive waste in underground repositories due to its low hydraulic conductivity, self-sealing ability and high adsorption capability. However, saline pore waters, high temperatures and the influence of microbes may cause mineralogical changes and affect the long-term performance of the bentonite barrier system. In this study, long-term static batch experiments were carried out at 25 °C and 90 °C for one and two years using two different industrial bentonites (SD80 from Greece, B36 from Slovakia) and two types of aqueous solutions, which simulated (a) Opalinus clay pore water with a salinity of 19 g·L−1, and (b) diluted cap rock solution with a salinity of 155 g·L−1. The bentonites were prepared with and without organic substrates to study the microbial community and their potential influence on bentonite mineralogy. Smectite alteration was dominated by metal ion substitutions, changes in layer charge and delamination during water–clay interaction. The degree of smectite alteration and changes in the microbial diversity depended largely on the respective bentonite and the experimental conditions. Thus, the low charged SD80 with 17% tetrahedral charge showed nearly no structural change in either of the aqueous solutions, whereas B36 as a medium charged smectite with 56% tetrahedral charge became more beidellitic with increasing temperature when reacted in the diluted cap rock solution. Based on these experiments, the alteration of the smectite is mainly attributed to the nature of the bentonite, pore water chemistry and temperature. A significant microbial influence on the here analyzed parameters was not observed within the two years of experimentation. However, as the detected genera are known to potentially influence geochemical processes, microbial-driven alteration occurring over longer time periods cannot be ruled out if organic nutrients are available at appropriate concentrations.
: Compacted bentonite is currently being considered as a suitable backfill material for sealing
underground repositories for radioactive waste as part of a multi-barrier concept. Although showing
favorable properties for this purpose (swelling capability, low permeability, and high adsorption
capacity), the best choice of material remains unclear. The goal of this study was to examine and
compare the hydration behavior of a Milos (Greek) Ca-bentonite sample (SD80) in two types of
simulated ground water: (i) Opalinus clay pore water, and (ii) a diluted saline cap rock brine using
a confined volume, flow-through reaction cell adapted for in situ monitoring by X-ray diffraction.
Based on wet-cell X-ray diffractometry (XRD) and calculations with the software CALCMIX of the
smectite d(001) reflection, it was possible to quantify the abundance of water layers (WL) in the
interlayer spaces and the amount of non-interlayer water uptake during hydration using the two
types of solutions. This was done by varying WL distributions to fit the CALCMIX-simulated XRD
model to the observed data. Hydrating SD80 bentonite with Opalinus clay pore water resulted
in the formation of a dominant mixture of 3- and 4-WLs. The preservation of ca. 10% 1-WLs and
the apparent disappearance of 2-WLs in this hydrated sample are attributed to small quantities of
interlayer K (ca. 8% of exchangeable cations). The SD80 bentonite of equivalent packing density
that was hydrated in diluted cap rock brine also contained ca. 15% 1-WLs, associated with a slightly
higher concentration of interlayer K. However, this sample showed notable suppression of WL
thickness with 2- and 3-WLs dominating in the steady-state condition. This effect is to be expected for
the higher salt content of the brine but the observed generation of CO2 gas in this experiment, derived
from enhanced dissolution of calcite, may have contributed to the suppression of WL thickness. Based
on a comparison with all published wet-cell bentonite hydration experiments, the ratio of packing
density to the total layer charge of smectite is suggested as a useful proxy for predicting the relative
amounts of interlayer and non-interlayer water incorporated during hydration. Such information is
important for assessing the subsequent rates of chemical transport through the bentonite barrier.
Influencing Factors for Sustainable Dietary Transformation—A Case Study of German Food Consumption
(2022)
In a case study of Germany, we examine current food consumption along the three pillars of sustainability to evaluate external factors that influence consumers’ dietary decisions. We investigate to what extent diets meet nutritional requirements (social factor), the diets’ environmental impact (ecological factor), and the food prices’ influence on purchasing behavior (economic factor). For this, we compare two dietary recommendations (plant-based, omnivorous) with the status quo, and we examine different consumption styles (conventional, organic produce). Additionally, we evaluate 1446 prices of food items from three store types (organic store, supermarket, and discounter). With this, we are able to evaluate and compare 30 different food baskets along their health, environmental, and economic impact. Results show that purchasing decisions are only slightly influenced by health-related factors. Furthermore, few consumers align their diet with low environmental impact. In contrast, a large share of consumers opt for cheap foods, regardless of health and environmental consequences. We find that price is, arguably, the main factor in food choices from a sustainability standpoint. Action should be taken by policy makers to financially incentivize consumers in favor of healthy and environmentally friendly diets. Otherwise, the status quo further drives especially underprivileged consumers towards unhealthy and environmentally damaging consumption.
Im neoliberalen Wettbewerb um Einwohner, Touristen und Unternehmen gehören diskursive Repräsentationen zu den wichtigsten Zuschreibungen von Städten und Regionen. Dies trifft besonders auf schrumpfende Regionen zu, welche dem Druck des interregionalen und internationalen Wettbewerbs besonders ausgesetzt sind. Diese Repräsentationen werden dabei durch sprachliche Äußerungen und Handlungen erschaffen. Diese Dissertation untersucht anhand der drei Städte Rostock, Stralsund und Greifswald, welche unterschiedlichen diskursiven Repräsentationen sich jeweils aus den Sprecherpositionen der überregionalen Printmedien, des Stadtmarketings und der touristischen Angebotsseite durch Airbnb-Angebote ergeben. Durch den methodischen Ansatz der lexikometrischen Diskursanalyse werden verschiedene schriftliche Produkte analysiert. Während die Berichterstattung in den Medien Rostock und Greifswald eine starke und dynamische Stadtentwicklung zuschreibt und sie sich damit von den Stigmata der schrumpfenden Städte und Regionen lösen, nimmt Stralsund eine untergeordnete Rolle ein und scheint tatsächlich eher durch einen Schrumpfungsdiskurs geprägt zu sein. Die Selbstdarstellung der Städte durch das Stadtmarketing hebt erwartungsgemäß die positiven Aspekte der jeweiligen Stadt hervor. Dabei wird jedoch durch jede Stadt ein anderer Schwerpunkt gewählt. Auch die touristischen Darstellungen der Städte durch die Airbnb-Angebote erzeugen trotz räumlicher Nähe und damit ähnlichen Ausgangssituationen jeweils sehr unterschiedliche Aspekte des städtischen Tourismus hervor. Während in Rostock das Flair und Ambiente der studentisch geprägten Quartiere hervorgehoben wird, wird in Greifswald der klassische Strandurlaub am Bodden beworben. Stralsund profitiert in der touristischen Darstellung stark von seinem Status als UNESCO-Weltkulturerbe.
Die Dissertation beschäftigt sich mit der für die Humangeographie aktuellen Assemblage-Theorie. Thematisch fokussiert sich die Arbeit auf die Nutzung der Fischbestände und die Zusammenkunft dieser Nutzung mit Politik. Dadurch weist das bearbeitete Thema einen klaren Bezug zu aktuellen gesellschaftlichen Entwicklungen und zur derzeitigen wissenschaftlichen Diskussion auf. Die Stärke der Arbeit liegt in den Überlegungen zur Assemblage-Theorie und deren Operationalisierung für die geographische Forschung. Ausgangspunkt dieser Überlegungen bildet das Buch ‚Tausend Plateaus Kapitalismus und Schizophrenie, Band 2‘ von DELEUZE, G. und GUATTARI, F. in der deutschen Übersetzung von 1992. Darauf aufbauend wird näher auf die Denk- und Herangehensweise eingegangen und der thematische Fokus (Fischereipolitik) mit dem theoretischen Ansatz (Assemblage) verkettet.
Pilot sites are currently used to test the performance of bentonite barriers for sealing high-level radioactive waste repositories, but the degree of mineral stability under enhanced thermal conditions remains a topic of debate. This study focuses on the SKB ABM5 experiment, which ran for 5 years (2012 to 2017) and locally reached a maximum temperature of 250 °C. Five bentonites were investigated using XRD with Rietveld refinement, SEM-EDX and by measuring pH, CEC and EC. Samples extracted from bentonite blocks at 0.1, 1, 4 and 7 cm away from the heating pipe showed various stages of alteration related to the horizontal thermal gradient. Bentonites close to the contact with lower CEC values showed smectite alterations in the form of tetrahedral substitution of Si4+ by Al3+ and some octahedral metal substitutions, probably related to ferric/ferrous iron derived from corrosion of the heater during oxidative boiling, with pyrite dissolution and acidity occurring in some bentonite layers. This alteration was furthermore associated with higher amounts of hematite and minor calcite dissolution. However, as none of the bentonites showed any smectite loss and only displayed stronger alterations at the heater–bentonite contact, the sealants are considered to have remained largely intact.
ABSTRACT
The small terrestrial gastropod Vertigo pseudosubstriata Ložek, 1954 is one of the rarest glacial indicator species in the Pleistocene of Central and Eastern Europe. In all, this species has been found at only about 15 sites in Europe. V. pseudosubstriata was initially described as a fossil in Central Europe and was discovered only later alive in Central Asia. With regard to its modern distribution, 25 habitats with V. pseudosubstriata have been examined in Tien Shan and in the central and southern Altai. These findings seem to capture the contemporary distribution of the species and provide information on the boundaries of its ecological requirements. These data are of great significance for the interpretation of the fossil assemblages. Since the few fossil specimens in Europe date from very different glacial periods in the Elsterian, Saalian Complex and Weichselian, it can be concluded that V. pseudosubstriata apparently immigrated in at least three distinct waves. Most of the Pleistocene specimens in eastern Central Europe and Eastern Europe are reported from archaeological sites of the Upper Middle Weichselian (Gravettian), roughly between 33 and 29 ka cal
bp. In this paper, we review all reported modern and fossil occurrences and discuss the species' ecological range.
According to a basic model, the formation of the coastal barriers in the southwestern Baltic can be divided into four evolutionary stages which are characterized by different rates of sea-level rise and varying relations between sediment supply and accommodation space. This model is tested using the example of a strandplain of the island Usedom, along with a local sea-level curve that reflects even smaller fluctuations of the water table and a detailed chronostratigraphy based on OSL measurements that allows the correlation of the morphodynamics with specific climatic phases. The resulting evolution scheme generally confirms the basic model but the timing of the stages depends on the inherited relief and has to be adjusted locally. A comparison with barriers from the W and SW Baltic region shows that the development during the past 5000 years was controlled by climate fluctuations which caused minor variations of the rather stable sea level and consequential changes in sediment supply, accommodation space and foredune deposition. Progradation decline can mainly be related to cool and windy climate phases which centered around 4.2, 2.8, 1.1, and 0.3 ka b2k, while increasing progradation correlated with warmer climate around 3.5, 2.0, and 0.9 ka b2k. The climate warming and the increasing sea-level rise in the recent past, however, led to shrinking progradation rates and may indicate a critical point beyond which the main progradation trend of the past turns into erosion.
This work scrutinises the policy shift in Germany with the change in leitmotif from biotechnology to bioeconomy and examines the associated implications at various levels. The emergence and implementation of innovation policy funding programmes show that the policy transition did not follow a linear sequence. Neither excessive prioritisation nor neglect of a selected sector can be confirmed in this analysis. However, the policy shift from biotechnology to bioeconomy has not only consequences in terms of its content, but also affects the spatial distribution of R&D funding. Against the background of existing polarisation tendencies and the growing acknowledgement of inclusive innovation policy approaches, this study examines the importance the bioeconomy can assume in the reduction of regional disparities. In ‘organisationally thick’ regions, depending on the involvement of private actors, specialisation and regional branching can be observed. It is found that, for rural regions, the bioeconomy can be an appropriate tool for regional development, since other industries are often not present.
Climate change has strongly affected mountain forests through an increasing intensity and frequency of disturbances and forest dieback in recent decades. However, given the strong relevance of forest dieback and potential impacts on forest stakeholders and local inhabitants, it is surprising that this research field is seldom investigated to date. Therefore, this study deals with the perception of climate change-related consequences as well as possible silvicultural adaptation strategies for the Bavarian Forest. Since it can be assumed that various forest ecosystem services will be increasingly in demand in the future, participation by all stakeholders is essential. Therefore, a sequential, mixed-method approach (qualitative and quantitative survey) allows developing concrete guidelines and strategies for adaptive management, in which the diverse social demands on forests can be adequately taken into account.
Zusammenfassung
Die Forschungsfragen sind:
(a) Wer sind die relevanten Akteure auf dem Gebiet der Umweltbildung im Waterberg Distrikt?
(b) Wie sind die Akteure vernetzt und welche Kooperationen existieren?
(c) Welche Bevoelkerungsgruppen partizipieren an den bestehenden Umweltbildungsangeboten?
Die Hypothese ist, dass insbesondere einkommensschwache Schichten der schwarzen Bevölkerung nicht an den Angeboten teilnehmen.
Das Untersuchungsgebiet Waterberg Distrikt in der Limpopo Provinz wird wie viele andere laendlich gepraegte Distrikte in Suedafrika von ungleichen Machtverhaeltnissen, hoher Arbeitslosigkeit und Spaetfolgen der Apartheid bestimmt. Es gibt nur wenige Studien, die die aktuelle Situation der Umweltbildung im Waterberg Distrikt ausreichend
analysieren (Baber, de Klerk und Walker 2003).
Die Arbeit basiert auf der Nutzung mehrerer sozialempirischer Methoden, wie schriftliche und muendliche Befragungen (Interviews) waehrend der Forschungsaufenthalte
zwischen 2009 und 2018/19 sowie Feldbeobachtungen zwischen 1995 und 2018/19 im Untersuchungsgebiet Waterberg Distrikt. Alle in der Forschungsarbeit befragten Akteure (Schulen, Wildtierfarmen, Naturreservate) vermitteln Umweltbildung. Ein einheitliches Konzept der Akteure in der Umweltbildung für den Waterberg Distrikt gab es bisher nicht, hier setzt die Untersuchung an.
Die Diskrepanz zwischen wohlhabenden weißen Landbesitzern und Investoren auf der einen Seite, und den kleineren, armen Gemeinden mit vorwiegend schwarzen Bevoelkerungsgruppen auf der anderen Seite ist für die Region praegend. Weitere Hindernisse für eine Teilnahme an den Umweltbildungsangeboten sind Chancenungleichheit in der
Bildung. Das Potenzial der Umweltbildung für eine nachhaltige Entwicklung des Waterberg Distrikts ist vorhanden und die Arbeit zeigt auf, wie die Arbeit der Akteure gestärkt und Synergien besser genutzt werden können.
Der im Waterberg Distrikt gut etablierte Oekotourismus kann durch bessere Vernetzung mit der Umweltbildung profitieren und somit zum wirtschaftlichen Aufschwung in der Region beitragen. Der Ökotourismus kann sich zukuenftig mit verschiedenen Varianten, wie Natur-, Agro-, Geo-, Biopark- und Wissenschaftstourismus weiter profilieren.
Das Waterberg Biosphaerenreservat spielt nicht nur eine herausragende Rolle in den Raumentwicklungsplaenen der Limpopo Provinz und vor allem im Waterberg Distrikt,
sondern auch im Oekotourismus und in der Umweltbildung. Umwelterbe, Artenvielfalt und oekologisch sensible Gebiete muessen aktiv geschuetzt und verwaltet werden und es
gilt sicherzustellen, dass sie nicht durch andere Aktivitaeten (z.B. Minenprospektionen) beeintraechtigt werden.
Das Waterberg Biosphaerenreservat sollte in seinen originaeren Aufgaben gestaerkt werden, damit die gesamte Bevoelkerung des Distrikts besser integriert wird und vom Biosphaerenreservat profitieren kann. Es liegt vor allem in der Verantwortung der Waterberg Distriktverwaltung, das Biosphaerenreservat zu unterstuetzen und weiterzuentwickeln (vgl. Blaauw 2018). Somit kann es zukuenftig die langfristige Lebensfaehigkeit der einzigartigen Landschaft foerdern, lokale Identitaet und Stolz schaffen und die Abwanderung aus laendlichen Gebieten in die Metropolen verringern. Mithilfe der Nutzung von Synergieeffekten und weitreichenderen Kooperationen werden langfristig auch die Lebensgrundlagen, Einkommen sowie Beschaeftigung der benachteiligten schwarzen Bevölkerungsgruppen in der Region verbessert. Eine Partizipation aller Interessensgruppen und kollektive Entscheidungsfindung, basierend auf wissenschaftlichen Erkenntnissen, wird die Gemeinschaft staerken, um die Bevölkerung auf die globalen Herausforderungen der Zukunft vorzubereiten (vgl. UNESCO 2015)
Abstract
Interbedded contourites, turbidites and pelagites are commonplace in many deep‐water slope environments. However, the distinction between these different facies remains a source of controversy. This detailed study of calcareous contourites and associated deep‐marine facies from an Eocene–Miocene sedimentary succession on Cyprus clearly documents the diagnostic value of microfacies in this debate. In particular, the variability of archetypical bi‐gradational contourite sequences and their internal subdivision (bedding, layering and lamination) are explored. Contourites can be distinguished from turbidites, pelagites and hemipelagites by means of carbonate microfacies in combination with bed‐scale characteristics. Particle composition provides valuable information on sediment provenance. Depositional texture, determined by the ratio between carbonate mud and bioclasts, is crucial for identifying bi‐gradational sequences in both muddy and sandy contourites, and normally‐graded sequences in turbidite beds. Equally important are the type and preservation of traction structures, as well as the temporality and impact of bioturbation. Shell fragmentation under conditions of increased hydrodynamic agitation (textural inversion) is recognized as a carbonate‐specific feature of bioclastic sandy contourites.
Abstract
Peatlands are lands with a peat layer at the surface, containing a large proportion of organic carbon. Such lands cover ≈1 000 000 km2 in Europe, which is almost 10% of the total surface area. In many countries, peatlands have been artificially drained over centuries, leading to not only enormous emissions of CO2 but also soil subsidence, mobilization of nutrients, higher flood risks, and loss of biodiversity. These problems can largely be solved by stopping drainage and rewetting the land. Wet peatlands do not release CO2, can potentially sequester carbon, help to improve water quality, provide habitat for rare and threatened biodiversity, and can still be used for production of biomass (“paludiculture”). Wisely adjusted land use on peatlands can substantially contribute to low‐emission goals and further benefits for farmers, the economy, society, and the environment.
Multiproxy investigations of lacustrine sediments from Laguna Azul (52 °S) document multi-millennial Holocene influences of Southern Hemispheric Westerlies (SHW) on the hydroclimatic variability of south-eastern Patagonia. During the last 4000 years, this hydroclimatic variability is overprinted by centennial warm/dry periods. A cool/wet period from 11,600 to 10,100 cal. BP is succeeded by an early Holocene dry period (10,100–8300 cal. BP) with a shallow lake, strong anoxia, methanogenesis and high salinity. Between 8300 and 4000 cal. BP the influence of SHW weakened, resulting in a freshwater lake considered to be related to less arid conditions. Since 4000 cal. BP, regional temperature decreased accompanied by re-intensification of SHW reaching full strength since 3000 cal. BP. Centred around 2200, 1000 cal. BP and in the 20th century, Laguna Azul experienced century-long warm/dry spells. Between these dry periods, two pronounced moist periods are suggested to be contemporaneous to the ‘Dark Age Cold Period’ and the ‘Little Ice Age’. Different from millennial SHW variations, centennial fluctuations appear to be synchronous for South America and the Northern Hemisphere. Changes in solar activity, large volcanic eruptions and/or modulations of ocean circulation are potential triggers for this synchronicity.
Der globale Rückgang der Artenvielfalt, verursacht durch das intensive Eingreifen des Menschen in die Ökosysteme, zählt zu den großen Herausforderungen der kommenden Jahrzehnte, nicht zuletzt im Interesse des Menschen, dessen Existenz dadurch zunehmend bedroht wird. Auch Wälder sind von dieser Entwicklung betroffen. In Deutschland über Jahrhunderte zu Forsten umgebildet, die vorwiegend der Holzproduktion dienten, führte dies zu monotonen Strukturen, in denen natürliche Elemente wie Totholz nicht den notwendigen Platz haben, um die zahlreichen davon abhängigen Arten zu versorgen. Derzeit findet jedoch – ausgelöst durch wissenschaftliche Befunde – ein gesellschaftliches Umdenken statt, das natürliche Waldelemente vermehrt in Wirtschaftswälder integrieren möchte.
Vor dem Hintergrund der sich durch diese Entwicklungen abzeichnenden Veränderung der Wälder wurde nun erstmals für das deutsche Bundesland Bayern flächenrepräsentativ untersucht, wie die Bevölkerung dieser Veränderung gegenübersteht, und wie die kulturellen Ökosystemleistungen von Wäldern, also die Beiträge des Ökosytems Wald für das menschliche Wohlergehen, wahrgenommen und beurteilt werden. Im Vordergrund standen dabei das natürliche Erbe und die Erholung. Dazu wurde eine repräsentative Online-Befragung mit 2473 Probanden durchgeführt, in die zwei leicht modifizierte Choice Experimente eingebunden wurden. Mit ihrer Hilfe sollten nicht nur die Präferenzen für bestimmte Waldzustände und Maßnahmen zur Sicherung der Artenvielfalt aufgedeckt, sondern auch festgestellt werden, welche Trade-offs zwischen ihren gesellschaftlichen, ökologischen und ökonomischen Folgen bestehen. Auch die Einstellung der Befragten gegenüber der Natur allgemein, und Totholz speziell, war Gegenstand der Studie. Zudem wurde über Reisekostenmodelle versucht, die Erholungsleistung der bayerischen Wälder zu bemessen, um sie in Relation zu den anderen Leistungen zu setzen.
Es zeigte sich, dass die Einstellung der bayerischen Bevölkerung gegenüber der Natur und vor allem gegenüber Totholz überwiegend positiv ist, auch wenn unterschiedliche Formen der Umwelteinstellung identifiziert werden konnten. In den Präferenzanalysen ergaben sich positive Zahlungsbereitschaften für solche Waldnaturschutzprogramme, die zu einer Verbesserung der Habitatverfügbarkeit für gefährdete Arten in allen Wäldern, nicht nur in einzelnen Schutzgebieten führen würden. Dabei sind ebenfalls Unterschiede zwischen verschiedenen Waldmanagementstrategien, sowie zwischen bestimmten sozio-demographischen Subgruppen festzustellen. Darüber hinaus konnte ein hoher Wert der Erholungsleistung der bayerischen Wälder ermittelt werden, der sich nicht wesentlich verändern würde, wenn mehr natürliche Strukturen zugelassen werden. Somit wäre diese kulturelle Ökosystemleistung auch weiterhin gewährleistet, vorausgesetzt, dass keine Extremzustände angestrebt werden. Aus Sicht der Forstpraxis und des Naturschutzes ist von besonderem Interesse, dass die Trade-offs, welche zwischen der Gesellschaft und diesen beiden Akteursgruppen bestehen, allen drei Seiten zugute kommen können.
The achievement and monitoring of a good environmental status on continental shelf seas requires
the use of acoustic remote sensing techniques due to their range. The interpretation of acoustic signals
for the identification of benthic communities, however, is still in its infancy. In this thesis, the results
of two field campaigns conducted in a sandy environment off the shore of Sylt Island (North Sea)
utilizing ship- and lander-based acoustic and optical remote sensing techniques are discussed. The
objective of the thesis is a better knowledge of the impact of the polychaete Lanice conchilega on
physical seafloor properties, especially roughness at a cm to mm scale, which is relevant for
understanding acoustic scatter. The results show a clear impact of L. conchilega on roughness even in
sparse populations of less than 2% coverage. However, these sparsely populated areas could not be
reliably identified with acoustic data; a denser population of L. conchilega provided a clearer signal for
the acoustic remote sensing methods. The results are promising regarding the broader use of acoustic
remote sensing techniques for environmental monitoring in selected habitats, although the
determination of minimum population thresholds that can be identified will require further studies.
A hydroxy-sodalite/cancrinite zeolite composite was synthesized from low-grade calcite-bearing kaolin by hydrothermal alkali-activation method at 160 C for 6 h. The effect of calcite addition on the formation of the hydroxy-sodalite/cancrinite composite was investigated
using artificial mixtures. The chemical composition and crystal morphology of the synthesized zeolite composite were characterized by X-ray powder diffraction, infrared spectroscopy, scanning electron microscopy, and N2 adsorption/desorption analyses. The average specific surface area is around 17–20 m2g-1, whereas the average pore size lies in the mesoporous range (19–21 nm). The synthesized zeolite composite was used as an adsorbent for the removal of heavy metals in aqueous solutions. Batch experiments were employed to study the influence of adsorbent dosage on heavy metal removal eciency. Results demonstrate the effective removal of significant quantities of Cu, Pb, Ni, and Zn from aqueous media. A comparative study of synthesized hydroxy-sodalite and
hydroxy-sodalite/cancrinite composites revealed the latter was 16–24% more effcient at removing heavy metals from water. The order of metal uptake effciency for these zeolites was determined to be Pb > Cu > Zn > Ni. These results indicate that zeolite composites synthesized from natural calcite-bearing kaolin materials could represent effective and low-cost adsorbents for heavy metal removal using water treatment devices in regions of water hortage.
The Müritzeum is a nature discovery centre and a museum in the heart of the Mecklenburg Lake District. It is the first natural history museum in Mecklenburg-Vorpommern, with natural history collections that are over 150 years old, and are still growing today. The collections contain about 290 000 specimens from the fields of botany, zoology and geology. An extensive library and an archive are also
part of the museum. Collecting, preserving and researching natural history are our main spheres of activity. The exhibition in the Müritzeum offers the visitor a comprehensive insight into the development of the nature and landscape of northeastern Germany and of Mecklenburg-Vorpommern and the Lake Müritz region in particular. The largest aquarium for indigenous freshwater species in Germany enables visitors to imagine themselves in the underwater world of the Mecklenburg Lake District.
Archaeological discoveries in the Tollense Valley represent remains of a Bronze Age battle of ca.1300–1250 BCE, documenting a violent group conflict hitherto unimagined for this period of time in Europe, changing the perception of the Bronze Age. Geoscientific, geoarchaeological and palaeobotanical investigations have reconstructed a tree- and shrubless mire characterised by sedges, reed and semiaquatic conditions with a shallow but wide river Tollense for the Bronze Age. The exact river
course cannot be reconstructed, but the distribution of fluvial deposits traces only a narrow corridor, in which the Tollense meandered close to the current riverbed. The initial formation of the valley mire dates to the transition from the Weichselian Late Glacial to the early Holocene.
The site at the southern shore of Krakower See shows the Quaternary geology of the surrounding
area. The local Quaternary sequence comprises a thickness of 50–100m of Quaternary deposits while
the surface morphology is dominated by the ice marginal position of the Pomeranian moraine, which
passes through the area. The bathymetry of the lake basin of Krakower See indicates a predominant
genesis by glaciofluvial erosion in combination with glacial exaration. Past research in this area has focussed
on the reconstruction of Pleniglacial to Holocene environmental changes, including lake-level
fluctuations, aeolian dynamics, and pedological processes and their modification by anthropogenic
land use.
Eine nachhaltige Entwicklung bedeutet eine dauerhaft mögliche Entwicklung innerhalb des ökologischen Erdsystems. Durch das weltweite Bevölkerungswachstum, den ansteigenden Wohlstand und nicht-nachhaltige Lebensweisen drohen die ökologischen Belastungsgrenzen unsere Erde jedoch überschritten zu werden bzw. wurden teilweise bereits überschritten. Dies hat zur Folge, dass nachfolgende wie auch parallel existierende Generationen nicht die gleichen Möglichkeiten zur Erfüllung ihrer Bedürfnisse haben, wie die heute in den Industriestaaten lebenden. Die landwirtschaftliche Erzeugung trägt dabei einen bedeutenden Teil zu dieser Bedrohung und Überschreitung der planetaren Grenzen bei, denn insbesondere der hohe und weiter ansteigende Konsum von tierischen Produkten weltweit hat zahlreiche ökologisch, jedoch auch sozial und gesundheitlich nachteilige Folgen. Einer der grundlegenden problematischen Aspekte tierischer Produkte ist der hohe Energieverlust im Laufe des Veredlungsprozesses von pflanzlichen Futtermitteln zu Fleisch- und Milchprodukten. Die Folge sind große intensiv genutzte Landwirtschaftsflächen, die notwendig sind, um jene Futtermittel zu produzieren. Dies führt zu Biodiversitätsverlusten, Treibhausgasemissionen, Landraub und gesundheitlichen Problemen aufgrund des Pestizidgebrauchs. Weitere Konsequenzen eines hohen Konsums tierischer Produkte umfassen einen hohen Wasserbedarf, Flächenkonkurrenzen zwischen dem direkten Lebensmittel- und dem Futtermittelanbau, aber auch den ethisch bedenklichen Umgang mit Tieren sowie Gefahren für die menschliche Gesundheit, z. B. koronare Herzerkrankungen und Antibiotikaresistenzen.
Begründet liegt dieser hohe und weiter wachsende Konsum tierischer Produkte in persönlichen, sozialen, ökonomischen und politischen sowie strukturellen Faktoren, wobei in vorliegender Arbeit auf den durch die westeuropäische Kultur geprägten Menschen fokussiert wird. Persönliche und soziale Hindernisse für einen reduzierten Konsum tierischer Lebensmittel liegen insbesondere in einem fehlenden Wissen, dem psychologischen Phänomen der kognitiven Dissonanz, mangelnder Achtsamkeit sowie dem Druck sozialer Normen. Wirtschaftspolitische und strukturelle Hindernisse umfassen eine wachstumsorientierte Ökonomie, fehlende Preisanreize für einen nachhaltigen Konsum sowie eine Infrastruktur, die den Konsum tierischer Produkte begünstigt.
Nichtregierungsorganisationen (NRO) als Teil des sog. Dritten Sektors, neben der Wirtschaft und der Politik, und als Vertreterinnen der Gesellschaft sind essentielle Akteurinnen in nationalen und internationalen Gestaltungsprozessen. Sie werden zumeist von der Gesellschaft oder zumindest Teilen der Gesellschaft unterstützt und können durch Öffentlichkeitsarbeit und andere Maßnahmen auf politische und ökonomische Protagonisten Druck ausüben. Somit sind NRO als potentielle Schnittstelle zwischen Gesellschaft, Politik und Wirtschaft vielversprechende Einrichtungen um den Konsum tierischer Produkte zu senken. Aufgrund der o. g. multidimensionalen Auswirkungen des hohen Konsums tierischer Produkte, haben insbesondere NRO, die die Ziele Umweltschutz, Ernährungssicherung, Tierschutz und Gesundheitsförderung verfolgen, potentiell Interesse an einer Reduktion des Fleisch-, Milch- und Eikonsums.
Studien über NRO in Schweden, Kanada und den USA weisen jedoch darauf hin, dass Umweltorganisationen sich in ihrer Arbeit für eine Begrenzung des Klimawandels nur in begrenztem Umfang für eine pflanzenbetonte Ernährungsweise einsetzen. Aufgrund der o. g. mehrdimensionalen Folgen eines hohen Konsums tierischer Lebensmittel weitet vorliegende Arbeit den Erhebungsumfang aus und umfasst die Untersuchung von deutschen Umwelt-, Welternährungs-, Gesundheits- und Tierschutzorganisationen in Hinblick auf deren Einsatz für eine Reduktion des Fleisch-, Milch- und Eikonsums.
Die Erhebung umfasst die Untersuchung von 34 der wichtigsten deutschen NRO mittels Material- und Internetseitenanalyse, vertiefende leitfadengestützte Expert*inneninterviews mit 24 NRO sowie eine Fokusgruppendiskussion zur Ergebniskontrolle, wobei das zentrale Element dabei die Expert*inneninterviews darstellen. Insgesamt entspricht der Forschungsprozess der Grounded Theory Methodologie (GTM), einem ergebnisoffenen, induktiven Vorgehen. Die Forschungsfragen umfassen neben der Analyse des aktuellen Umfangs des Einsatzes für eine pflanzenbetonte Ernährungsweise insbesondere die Einflussfaktoren auf diesen Umfang sowie die umgesetzten Handlungsstrategien für eine Reduktion des Konsums tierischer Lebensmittel.
Entsprechend der GTM steht am Ende des Forschungsprozesses vorliegender Arbeit ein Modell, das die Erkenntnisse in einer verdichteten Kernkategorie zusammenfasst. Als zentrales Ergebnis der Erhebung kann das ‚Modell der abwägenden Bestandssicherung‘ gesehen werden. Es weist, in Übereinstimmung mit der Literatur, darauf hin, dass NRO als Teil der Gesellschaft von der Außenwelt abhängig sind, d. h. von ihren Mitgliedern und staatlichen wie privaten Geldgeber*innen, aber auch von parallel agierenden NRO, Medien und gesellschaftlichen Entwicklungen. Dies kann unter der Überschrift der ‚Einstellung relevanter Interessensgruppen‘ zur Thematik der tierischen Lebensmittel gefasst werden. Auf der anderen Seite steht die ‚Einstellung der Mitarbeitenden‘ einer NRO, da die Themenaufnahme der Problematik eines hohen Fleisch-, Milch- und Eikonsums auch davon abhängt, welche Bedeutung die Mitarbeitenden dieser Thematik zusprechen und inwiefern sie bereit sind sie in das Maßnahmenportfolio aufzunehmen. Wenn sowohl die Interessensgruppen als auch die Mitarbeitenden einer NRO der Themenaufnahme befürwortend gegenüber gestellt sind, so ist ein umfassender Einsatz für eine Reduktion des Konsums tierischer Lebensmittel von dieser NRO zu erwarten. Dies trifft in vorliegender Erhebung vorwiegend auf Tierschutzorganisationen und einige Umweltorganisationen zu. Der gegenteilige Fall einer fehlenden Thematisierung tierischer Produkte tritt ein, wenn weder relevante Interessensgruppen, noch die Mitarbeitenden einer NRO die Themenaufnahme befürworten oder als dringlich erachten. Dies kann insbesondere bei Welternährungs- und Gesundheitsorganisationen beobachtet werden. Wenn die Mitarbeitenden einer NRO die Thematisierung der Problematik tierischer Lebensmittel befürworten, die relevanten Interessensgruppen jedoch ablehnend gegenüber derartigen Maßnahmen stehen, ist eine zurückhaltende Thematisierung zu erwarten, die sich auf Informationstexte bspw. auf den Internetseitenauftritten der NRO beschränkt. Dies ist v. a. bei Umwelt- und Welternährungsorganisationen erkennbar. Der vierte Fall, dass die Interessensgruppen einer NRO für eine Reduktion des Konsums tierischer Produkte eintreten würden, nicht jedoch die Mitarbeitenden der NRO, konnte in vorliegender Erhebung nur in Ansätzen bei Umweltorganisationen beobachtet werden.
Der Hauptgrund, warum NRO, insbesondere Welternährungs- und Gesundheitsorganisationen, die Problematik des hohen Konsums tierischer Produkte nicht oder nur in geringem Umfang aufnehmen, liegt in der o. g. Abhängigkeit der NRO von öffentlichen Geldgeber*innen, wie auch von privaten Spender*innen und Mitgliedern (‚Einstellung relevanter Interessensgruppen‘). Weitere Faktoren umfassen bspw. die Arbeitsteilung wie auch den Wettbewerb zwischen NRO, insofern dass auf andere NRO verwiesen wird und Nischen für eigene Themen gesucht werden.
Neben den Gründen für den Umfang der Thematisierung des hohen Konsums tierischer Lebensmittel wurden auch Strategien erfragt, die die NRO anwenden um denselben zu senken. Hierbei wurde insbesondere die Öffentlichkeitsarbeit in verschiedenen Ausrichtungen genannt und als sehr wirksam eingeschätzt. Vor allem emotional ausgerichtete, positiv formulierte, zielgruppenspezifische und anschaulich dargestellte Kampagnen können als effektiv eingeschätzt werden. Auch politische oder juristische Maßnahmen, wie Lobbyismus oder Verbandsklagen werden von den NRO durchgeführt, wobei die befragten NRO auf der bundespolitischen Ebene derzeit kaum Potential sehen Änderungen herbeizuführen; auf Regionen- oder Länderebene jedoch realistischere Einflussmöglichkeiten sehen.
Als nächste Schritte für NRO im Sinne einer (verstärkten) Thematisierung der Problematik tierischer Lebensmittel können folgende Maßnahmen geraten werden:
• Eine Erhebung der Meinung von Mitgliedern und Spender*innen zu der o. g. Themenaufnahme in das Maßnahmenportfolio der jeweiligen NRO. Dies ist insbesondere bei NRO sinnvoll, die unsicher über die Reaktion ihrer Mitglieder und Spender*innen auf einen Einsatz für eine Reduktion des Konsums tierischer Produkte sind.
• Eine Prüfung von alternativen Finanzierungsmöglichkeiten, die eine Abhängigkeit von staatlichen Geldern verringern. Hierdurch würde der Bedeutung von NRO als Teil des Dritten Sektors neben Politik und Wirtschaft gerecht und die Einflussmöglichkeiten auf dieselben erhöht.
• Eine vermehrte Kooperation zwischen NRO innerhalb einer Disziplin und zwischen Disziplinen, sodass bspw. im Rahmen eines Netzwerkes aufeinander verwiesen werden kann. Dies ermöglicht die Einhaltung der jeweiligen Organisationsphilosophien und Kernkompetenzen trotz Zusammenarbeit mit NRO, die andere Herangehensweisen an die Förderung einer pflanzenbetonten Ernährungsweise verfolgen. Zudem ermöglicht diese Netzwerkbildung eine erhöhte Wettbewerbsfähigkeit mit dem ökonomischen und politischen Sektor.
• Die Anerkennung der Handlungsfähigkeit von NRO als Pionierinnen des Wandels. Als Dritter Sektor neben der Politik und Wirtschaft kommt NRO eine große Bedeutung in der Beeinflussung gesellschaftlicher Prozesse, insbesondere auf zwischenstaatlicher Ebene zu. Auch komplexe Themen und, angesichts der Überschreitung der planetaren Grenzen, dringliche weltumfassende Themen können von kleinen, regionalen NRO aufgegriffen werden.
• Die Fortführung von bewährten Maßnahmen zur Reduktion des Konsums tierischer Produkte, wie verschiedene Formen der Öffentlichkeitsarbeit, kann als sinnvoll erachtet werden. Hinzu können neue Inhalte genommen werden, wie bspw. die Förderung eines achtsamen Konsumstils durch naturnahe Lernorte. Für eine Umsetzung wissenschaftlicher Erkenntnisse zu Verhaltensänderungen hinsichtlich nachhaltiger Konsumstile ist eine verstärkte Zusammenarbeit mit Forschungseinrichtungen sinnvoll.
Diese Erkenntnisse hinsichtlich der Gründe für eine Thematisierung der Problematik tierischer Produkte durch NRO lassen sich evtl. auch auf andere Themen übertragen, die von NRO aufgegriffen werden können, wie bspw. die Kritik an Flugreisen. Zudem ist es denkbar, dass die auf Deutschland beschränkte Analyse auch auf weitere, insbesondere westlich geprägte Länder übertragen werden kann.
Monitoring of Calcite Precipitation in Hardwater Lakes with Multi-Spectral Remote Sensing Archives
(2017)
Arne Bünger leistet mit den Ergebnissen seiner Untersuchungen der Innovations- und Adaptionsfähigkeit, der Nachhaltigkeitsorientierung sowie der Identifizierung von verschiedenen Akteurstypen in der Schweine- und Geflügelproduktion einerseits und der Algen- und Insektenproduktion andererseits einen Beitrag zum besseren Verständnis von sozio-technischen Transformationen und stärkt den bislang unterrepräsentierten Raum- und Akteursbezug in der Transformationsforschung. Dies und eine Analyse von Innovationspotenzialen und Nachhaltigkeitsorientierung im tri-nationalen Vergleich tragen zur Schließung von aktuellen Forschungslücken bei.
The importance of investments by emerging country multinationals to industrialised economies has risen continuously as illustrated by the growing number of Chinese merger and acquisitions (M&A) of German Mittelstand firms. This dissertation aims to analyse the effects of institutional distances on the M&A process. To this end, William Scott’s concept of institutions is newly operationalized to investigate institutional distances on the intra-firm, regional and international level. Through interviews with involved firms, intermediaries and key persons with dual backgrounds, the effects on different dimensions of the subsidiaries’ embeddedness as well as various mechanisms of institutional work during and after the M&A are evaluated.
The southern Baltic Sea embodies an incomparable geological archive of the tectonic evolution of the 450 Ma old Trans‐European Suture Zone (TESZ). This WNW to NW trending suture formed during the collision of Baltica and Avalonia and has accommodated the repeatedly changing stress regimes since then, as evidenced by numerous fault zones and systems. The German offshore part in the vicinity of Rügen Island is strongly block‐faulted, with each block showing a specific geological pattern, enabling the reconstruction of the structural evolution of the area.
The work of this thesis is part of the USO working group of the University of Greifswald and the Geological Survey of Mecklenburg‐Western Pomerania, which aims to build a unified three‐dimensional tectonic model of the southern Baltic Sea area. This thesis presents the results of new structural investigations of the Arkona, Wolin and Gryfice blocks north and east of Rügen. Especially, conflicting structural analyses in the previous work are united into a consistent model.
The integrated interpretation of 144 reprocessed seismic vintage lines (original Petrobaltic data) and 23 high resolution academic seismic sections (from the Universities of Hamburg and Bremen), with additional consideration of on‐ and offshore wells, revealed 19 seismostratigraphic horizons that subdivide the succession between the Proterozoic basement and the Upper Cretaceous. Up to 100 faults of superior fault zones and systems control the tectonic situation. Besides NW trending deep faults formed during the Palaeozoic, for instance the Wiek and Nord Jasmund faults, and NNW trending Mesozoic faults and flexures that belong to the Western Pomeranian Fault System, other major faults such as the Adler‐Kamień Fault Zone document the polyphase evolution of this area.
The restoration of selected seismic sections support the evaluation of separately generated faults and their reactivation, leading to a subdivision of the tectonic evolution of the area into six stages:
(1) The Caledonian Orogeny (Ordovician/Silurian) was accompanied by a NE‐SW compression, resulting in the formation of the TESZ and an accretionary wedge within the upper crust. (2) The following S to SW trending extension of the Variscan Foreland (Devonian/Carboniferous) triggered the
evolution of the Middle Devonian Old Red Rügen Basin south of the Wiek Fault. Further WNW to NW trending faults (e.g. Nord Jasmund Fault) subdivided the basin. (3) The advancing Variscan Orogeny (Late Carboniferous) caused an increasing NE‐SW orientated compression and subsequently reactivated faults and tilted blocks (e.g. Lohme Sub‐block). (4) The North German Basin and Mid Polish Trough formed by thermic subsidence in the S to SE of the research area during the Permo‐Carboniferous. Simultaneously, the evolution of the Gryfice Graben as part of the Teisseyre‐Tornquist Zone commenced. (5) Due to the Arctic‐North Atlantic Rifting an E‐W trending extension increased. Consequently, grabens such as the Gryfice Graben continued their subsidence. As the stress system rotated counter‐clockwise, the shear strength increased along the NE trending faults. The Western Pomeranian Fault System developed due to intense transtension during the Keuper and Jurassic, and is characterised by pull‐apart structures. (6) In the Upper Cretaceous, a NE‐SW compression, forced by the Africa‐Iberia‐Europe convergence, triggered the reactivation of faults and flexures as reverse ones, the inversion of grabens (e.g. Gryfice Graben), and the formation of anticlines, for instance at the Wolin Block.
This thesis combines the calculation of gridded time structure maps and a detailed fault pattern analysis, and represents the base for a velocity‐ and subsequently depth‐based 3D modelling.
Die dynamische Bevölkerungsentwicklung Ostdeutschlands seit 1990 zeigt am Beispiel der Entstehung einer Residualbevölkerung die unterschiedlichen Variationen der Selektivität von Wanderungen: Einer Bevölkerung, die aufgrund langfristig wirkender selektiven Wanderungsverluste im ländlich-peripheren Raum ein spezifisches demographisches Verhalten aufweist.
Der Wanderungsverlust Ostdeutschlands mit über 2,5 Millionen Menschen hat tiefgreifende Auswirkungen auf die alters-, geschlechts- und bildungsspezifische Bevölkerungsstruktur der neuen Bundesländer hinterlassen. Auch wenn die jungen Generationen zumeist das politisch geeinte Deutschland leben, existieren mit Blick auf die vorliegenden demographischen Prozesse und Strukturen bis heute nahezu zwei deutsche Staaten.
Die Entwicklungen sowie die Auswirkungen insbesondere der räumlichen Bevölkerungsbewegung wurden entsprechend dem Stand der Forschung vor dem Hintergrund der Situation Ostdeutschlands vorgestellt und die darauf aufbauenden Forschungsthesen benannt. Das bisher nur theoretische Konstrukt der Residualbevölkerung, die Interdependenz aus natürlicher und räumlicher Bevölkerungsbewegung, wurde anhand von unterschiedlichen demographischen Parametern (u. a. hohe Fertilität, hohe Mortalität, starke Wanderungsverluste, großes Frauendefizit, Überalterung) eingeordnet und damit als messbar definiert.
Am Beispiel Mecklenburg-Vorpommerns konnte anschließend gezeigt werden, wie sich die Bevölkerungsstruktur des ehemals jüngsten Bundeslandes aufgrund der selektiven Migration innerhalb eines Vierteljahrhunderts in das älteste umkehrte. Um diesen Verlauf nachzuvollziehen, wurden auf Gemeindeebene die unterschiedlichen Bewegungsentwicklungen ab 1990 dargestellt: Der Rückgang der Sterblichkeit, der Wiederanstieg der Fertilität sowie der sich manifestierende Wanderungsverlust junger Frauen. Daran anschließend zeigten Strukturberechnungen, wie sowohl das Billeter-Maß als auch Geschlechterproportionen, die umfassenden Auswirkungen der Bewegungen auf den Bevölkerungsstand und dessen Struktur Mecklenburg-Vorpommerns: Einen stetigen Rückgang der Bevölkerungszahlen, ein über-proportionales Frauendefizit in jüngeren Altersjahren und eine fortlaufend beschleunigte Alterung der Bevölkerung.
Vor dem Hintergrund dieser Rahmenbedingungen wurde für die Zeiträume 1990-2001 und 2002-2013 jeweils eine Clusteranalyse durchgeführt, die als Ergebnis eine Typisierung von Gemeinden hinsichtlich einer messbaren Residualbevölkerung ermöglichten. Entsprechend der Vordefinition eines solchen migrationellen Konstruktes konnte für etwa jede fünfte Gemeinde in Mecklenburg-Vorpommern solcherart demographische Bedingungen identifiziert werden. Diese Gemeinden liegen tendenziell im Binnenland und fern der Zentren – eine zentrale Verortung konnte nicht festgestellt werden. Von Gemeinde zu Gemeinde unterschieden sich die demographischen Parameter teils stark, so dass von einflussreichen lokalen (nicht betrachteten) Rahmenbedingungen ausgegangen werden muss.
Dagegen konnten auch Gemeinden ohne residuale Züge identifiziert werden. Etwa jede dritte Gemeinde Mecklenburg-Vorpommerns wies keine Parameter einer Residualbevölkerung auf. Diese Regionen waren vor allem in der Nähe der Zentren und der Küste zu finden. Die verbliebenen Gemeinden zeigten nur kurzfristig oder nur im geringfügigem Maße Indizien für eine solche Bevölkerung – das betraf etwa die Hälfte aller Gemeinden im Land.
Nach der gesamtgemeindlichen Analyse wurde die Bevölkerungs- und Sozialstruktur der dabei betroffenen Gemeinden Strasburg (Um.) im Landkreis Vorpommern-Greifswald und Dargun im Landkreis Mecklenburgische Seenplatte detailliert analysiert. Die Bevölkerungsentwicklung beider Betrachtungsgemeinden entsprach der vieler ostdeutscher Kleinstädte im ländlichen Raum nach der politischen Wende: Während die Gemeinden in der DDR Bevölkerungswachstum erfuhren oder zumindest gleichbleibende Bevölkerungszahlen als regionales Zentrum aufwiesen, verursachte die Abwanderung vor allem junger Menschen und ein manifestierter Sterbeüberschuss nach 1990 stetig rückläufige Zahlen.
In diesen beiden Gemeinden wurden dann nicht gesamtgemeindliche Bevölkerungszahlen analysiert, sondern vielmehr die Zusammensetzung einer Gemeindebevölkerung vor dem Hintergrund ihres Migrationsstatus differenziert. Für den Zeitraum 1979-2014 wurden deshalb anhand dieses Status die Bevölkerungen beider Gemeinden in Sesshafte und Zugezogene unterteilt. Aufgrund der sowohl vorhandenen Sterbe- als auch Geburtsstatistik war es möglich, die natürliche und räumliche Bevölkerungsbewegung der insgesamt fast 22.000 Men-schen direkt herauszuarbeiten. Die sesshafte Bevölkerung repräsentiert dabei die Menschen, die am ehesten dem Typus „Residualbevölkerung“ entsprechen.
Nach Berechnung der Mortalitäten für unterschiedliche Zeiträume ergab sich tendenziell eine höhere Sterblichkeit bzw. geringere Lebenserwartung der Sesshaften gegenüber den Zuzüglern bei Frauen wie Männern. Wurden darüber hinaus die Zugezogenen nach Lebensdauer in den Betrachtungsgemeinden differenziert, ergab bei beiden Geschlechtern eine längere Zugehörigkeit zu den Gemeinden auch eine höhere Sterblichkeit. Damit wurde einerseits die generell höhere Mortalität des ländlich-peripheren Raums gegenüber dem urbanen Raum bestätigt. Andererseits entspricht die höhere Sterblichkeit der sesshaften gegenüber der der nichtsesshaften Bevölkerung den Vorüberlegungen zur Residualbevölkerung.
Darüber hinaus wurde zusätzlich der Parameter „Bedürftigkeit“ berücksichtigt. Hier konnte erwartungsgemäß für beide Betrachtungsgemeinden die höchste Sterblichkeit der von Sozial-leistungen betroffenen Menschen festgestellt werden. Je länger dabei die Bezugsdauer, umso höher war die aufgezeigte Mortalität – dies sogar zumeist vor der sesshaften Bevölkerung. Bezieher von Sozialhilfe waren im Vergleich zu Beziehern von Wohngeld am stärksten betroffen; Unterschiede bei Männern besonders stark vertreten. Die Nichtbezieher wiesen bei beiden Geschlechtern die geringste Sterblichkeit auf.
Neben der Mortalität wurde als zweite Variable der natürlichen Bevölkerungsbewegung die Fertilität der beiden Bevölkerungsgruppen untersucht. Hier ergaben sich jedoch keine signifikanten Unterschiede zwischen beiden Bevölkerungsgruppen
Im Bereich der Periodenfertilität wiesen Zuzügler gegenüber den Sesshaften eine erhöhte Fertilität auf. Berechnungen der Kohortenfertilität ergaben wiederrum eine leicht höhere Fertilität der Sesshaften. Auch eine detaillierte Analyse der Zuzüglerinnen offenbarte kein einheitliches Bild. Mit Blick auf die Bedürftigkeit war festzustellen, dass die Bezieherinnen eine deutlich höhere Fertilität gegenüber Nichtbezieherinnen – unabhängig von der Bezugsdauer – aufwiesen. Im Ergebnis wurde damit zwar die generell höhere Fertilität des ländlich-peripheren Raums gegenüber dem urbanen Raum bestätigt. Die entsprechenden Vorüberlegungen zur Fertilität der sesshaften gegenüber der nichtsesshaften Bevölkerung konnten aber nicht eindeutig verifiziert werden.
Die gesamtheitliche Betrachtung der Gemeindeberechnungen zeigte demzufolge ein zweitgeteiltes Bild: Die Ergebnisse der Mortalität bestätigen die Annahmen zur Residualbevölkerung, die Ergebnisse der Fertilität nur in Teilen. Auch wenn die festgestellten Fertilitäts- und Morta-litätsunterschiede ortsbehaftet sind – sei es durch Umwelteinflüsse vor Ort oder die Art der Menschen zu leben: Je länger die Menschen in Regionen mit einem bestimmten Fertilitäts- und Mortalitätsniveau leben, umso stärker passen sie sich diesem an – in beide Richtungen.
Vor dem Hintergrund sowohl der Typisierung aller Gemeinden als auch der beiden Betrach-tungsgemeinden ist zu konstatieren, dass beide Variablen der natürlichen Bevölkerungsbewegung nichtgleichberechtigt nebeneinander zur Erklärung einer Residualbevölkerung fungieren müssen. Unter der Beibehaltung der theoretischen Annahmen ist dementsprechend zukünftig von einer Residualbevölkerung mit Schwerpunkt einer hohen Mortalität einerseits und mit Schwerpunkt einer hohen Fertilität andererseits auszugehen. Das bisher in der Literatur benannte Frauendefizit stellt darüber hinaus nur einen Parameter unter mehreren dar und sollte bei nachfolgenden Betrachtungen nicht als alleiniger Indikator dienen.
Unter Berücksichtigung der Ergebnisse sowohl aus beiden Gemeinden als auch aus den Clus-teranalysen wurde ein Modell einerseits zur Entstehung der Residualbevölkerung, andererseits zum Wirken der selektiven Migration generell erstellt. In Abhängigkeit von Alter und Geschlecht und unter Voraussetzung einer langfristig konstanten Wanderungsbewegung konnte so der theoretische Einfluss der räumlichen Bevölkerungsbewegung auf die Bevölkerungsstruktur – und damit indirekt auch auf die natürliche Bevölkerungsbewegung – vereinfacht projiziert werden.
Der ostdeutsche ländlich-periphere Raum ist abschließend als Sonderform des ländlich-peripheren Raums einzuordnen. Die hier gezeigte Residualbevölkerung kann als ein Indikator für – den gesellschaftlichen, kulturellen und wirtschaftlichen Verwerfungen geschuldeten – langfristige Wanderungsverluste eingeordnet werden. Die überproportional ausgeprägte Bedürftigkeit im ländlich-peripheren Raum kann deshalb auch als ein Merkmal der Sesshaftigkeit eingeordnet werden.
Insofern ist die Residualbevölkerung, vor dem Hintergrund der darüber hinaus als perspektivisch ungünstig erachteten Zukunftsaussicht, als Bevölkerungsgruppe eines Raumes abnehmender Entwicklungsstufe zu verstehen. Es ist daher ratsam, einerseits eine Verbesserung der Lebenssituation betroffener Menschen in ländlich-peripheren Räumen zu erwirken und andererseits diesen Herausforderungen raumplanerisch stärkeres Gewicht zu verleihen. Die zukünftige dahingehende Gestaltung ländlich-peripherer Räume in Ostdeutschland bedarf aus Sicht des Autors deshalb mehr an Autarkie sowie flexibler Kreativität.
Glacitectonic deformation in the Quaternary caused the tectonic framework of large-scale folds and displaced thrust sheets of Maastrichtian (Upper Cretaceous) chalk and Pleistocene glacial deposits in the southwestern Baltic Sea area.
A wide spectrum of methods has been compiled to unravel the structural evolution of the Jasmund Glacitectonic Complex. The analyses of digital elevation models (DEM) suggest a division into two structural sub-complexes – a northern part with morphological ridges striking NW–SE and a southern part with SW–NE trending ridges. Geological cross sections from the eastern coast (southern sub-complex) were constructed and restored using the software Move™ and the complementary module 2D Kinematic Modelling™.
The final geometric model of the southern sub-complex shows a small-scale fold-and-thrust belt. It includes three different orders of architectural surfaces (see PEDERSEN, 2014): erosional surfaces and the décollement (1st order), thrust faults (2nd order), and beds outlining hanging-wall anticlines as well as footwall synclines (3rd order). Thrust faults of the southern structural sub-complex are mainly inclined towards south, which indicates a local glacier push from the S/SE.
The glacitectonic structures have a surface expression in form of sub-parallel ridges and elongated valleys in between. Geomorphological mapping and detailed landform analyses together with the structural investigations provide an insight into the chronology of sub-complexes formation. The northern part of the glacitectonic complex is suggested to have been formed before the southern one, considering the partly truncated northerly ridges and their superimposition by the southern sub-complex.
Although there is a high number of scientific publications on the glacitectonic evolution of Jasmund, these presented models often lack a consistent theory for the development integrating all parts of the 100 km2 large complex. Therefore, the combination of all results leads to a more self-consistent genetic model for the entire Jasmund Glacitectonic Complex.
Die Entstehung und Herausgabe von touristischen Karten der DDR. Eine historisch-kritische Analyse
(2018)
Mit der vorliegenden Dissertation wird erstmals ein zeitlich umfassender Überblick über die touristische Verlagskartographie in der DDR gegeben. Als „Leitverlag“ steht der Landkartenverlag bzw. Tourist Verlag im Mittelpunkt der Arbeit, dessen Geschichte zugleich den Untersuchungszeitraum 1945–1994 vorgibt. Darüber hinaus werden weitere Verlage, kartographische Betriebe und Institutionen betrachtet, die im Osten Deutschlands mit der Herstellung und Herausgabe von touristischen Karten befasst waren.
Das halbe Jahrhundert ostdeutscher Verlagsgeschichte lässt sich in fünf inhaltlich abgrenzbare Entwicklungsphasen einteilen. Phase 1 (1945–1952) war gekennzeichnet durch eine von der Besatzungsmacht UdSSR überwachte und im Aufbau befindliche Verlagslandschaft. In jenen Jahren gelang es nur dem von Kurt Schaffmann gegründeten Landkartenverlag, eine volle Sortimentsbreite touristischer Karten (Stadtpläne, Wanderkarten, Verkehrskarten) aufzubauen, jedoch vorerst noch regional eingeschränkt. In Phase 2 (1953–1965) wurde durch die Verstaatlichung von Verlagen und der sich anschließenden Konzentration der Herausgabe die Grundlage für ein staatlich kontrolliertes Verlagswesen geschaffen. Dabei war zugleich die Sortimentsvielzahl zugunsten einer klar formulierten Programmstruktur aufgegeben worden. Für Phase 3 (1966–1976) war die Herstellung und Herausgabe eines komplett neuen Verlagsprogramms prägend. Vorausgegangen waren Beratungen in Moskau und Ost-Berlin, die zu verschärften Sicherheitsmaßnahmen im Kartenwesen führten. Fortan wurden alle für die Öffentlichkeit bestimmten Karten nur noch mit verzerrten Maßstäben produziert. Phase 4 (1977–1989) beinhaltet die Tätigkeit des VEB Tourist Verlag Berlin/Leipzig, der neben Karten nun auch für touristische Literatur verantwortlich zeichnete. Bis auf Koeditionen mit Verlagen benachbarter sozialistischer Staaten stagnierte die Kartenherausgabe, denn zunehmend wurden Kapazitäten durch den Devisen bringenden Kartographieexport in die BRD gebunden. In der Phase 5 (1990–1994) gelang es dem Tourist Verlag nicht, eine gefestigte Stellung in der gesamtdeutschen Marktwirtschaft zu erringen. Durch den Verkauf seitens der Treuhandanstalt an J. Fink – Kümmerly + Frey ließ sich das Schicksal nur um wenige Jahre hinauszögern; am Ende stand die Liquidation des traditionsreichen Unternehmens. Damit wird zugleich der Schlusspunkt der Betrachtungen fixiert.
Im Laufe ihrer Geschichte war die ostdeutsche Verlagskartographie verschiedensten Restriktionen unterworfen. Zensur in Form sogenannter Genehmigungsverfahren, Bevormundung durch staatliche Anleitung und Kontrolle sowie die Sicherheitsdoktrin der sowje-tischen Führungsriege gaben den Rahmen vor, in dem Karten für die Öffentlichkeit entstehen konnten. Seit Mitte der 1960er Jahre führte die ausschließliche Verwendung von verzerrten Kartengrundlagen zu Erzeugnissen, in denen das Ermitteln von exakten Streckenlängen unmöglich wurde. Zusammen mit diversen Tarnmaßnahmen für Grenzgebiete, Militärobjekte und Industrieanlagen sowie weiteren Manipulationen des Karteninhalts, entstand ein von Fachleuten und Nutzern oft kritisiertes Verlagsprogramm.
Während in den ersten Jahren nach Ende des Zweiten Weltkriegs noch zahlreiche Stadtpläne in den Handel gelangten, wurde ab Mitte der 1960er Jahre nur noch eine eingeschränkte Anzahl von Orten mit adäquatem Kartenmaterial bedacht. Zudem sind die Erzeugnisse fortan mit sogenannten „gleitenden Maßstäben“ erstellt worden. Die Pläne genügten für die grobe Orientierung, touristischer Inhalt war sorgsam eingearbeitet.
Als Ausgangsmaterial für Wander- und Touristenkarten in verschiedenen Maßstäben diente ab 1966 die von der staatlichen Kartographie eigens zur Verfügung gestellte,
verzerrte Übersichtskarte im Maßstab 1 : 200 000. Fuß- und Radwanderer bekamen die daraus resultierenden Auswirkungen am meisten zu spüren. Da auch das Kartenbild recht grob war, genoss diese Kartengruppe einen allgemein schlechten Ruf.
Bei den Verkehrskarten haben sich die Verzerrungen umso weniger bemerkbar gemacht, je länger die zu fahrenden Strecken waren. Wegen ihres Detailreichtums wurden die Karten sogar im Ausland geschätzt – Mairs Geographischer Verlag aus Stuttgart hatte die „Reise- und Verkehrskarte“ in seine international bekannte Reihe der „Generalkarten“ integriert.
Somit ist insbesondere den touristischen Karten, die zwischen 1965 und 1989 produziert worden sind, eine unzureichende Note zu attestieren. Die differenzierte Betrachtung des Gesamtzeitraumes zeigt aber auch, dass Pauschalurteile über die touristische Kartographie in der DDR nicht angemessen sind.
Im Forschungsfeld Klimaschutz und Nachhaltigkeitszertifizierung werden in dieser Arbeit die Treibhausgasemissionen durch Verwendung von Rapsbiodiesel gemäß EU Nachhaltigkeitsvorgaben der EU RED thematisiert. Regionales Bezugssystem sind gemäß EU-Vorgabe die NUTS2-Gebiete. Für 35 NUTS2-Regionen Deutschlands wurden Treibhausgasemissionen, die dem praxisnahen Rapsanbau zugerechnet werden können, berechnet.
Ein entwickeltes sogenanntes Rechenmodul mit dem Rapsanbauverfahren von der Bodenbearbeitung über die Düngung erfasst, beinhaltet einen vom Ifeu-Institut erschaffenen THG-Rechner, der die THG-Emissionen gemäß IPCC-und RED-Vorgabe berechnet. Um zwei Forschungslücken zu schließen, wurden mithilfe des Rechenmoduls insbesondere die Differenzierung der Stickstoffdüngung und die Regionalspezifik von Rapsanbauverfahren beschrieben. Zentraler Parameter ist die Düngung, mit Unterscheidung üblicher Stickstoffmineraldünger, und zusätzlich im Rechenmodul implizierte Wirtschaftsdünger. Die eigentliche Modellierung typischer regionaler Rapsanbauverfahren für 35 NUTS2-Gebiete mit 10 erforderlichen Anbauparametern erfolgte mit der Unterstützung und dem Fachwissen regionaler Experten der Landeseinrichtungen für Landwirtschaft. Folgende Ergebnisse werden dargestellt:
o Quantifizierung der THG-Anbauemissionen definierter Rapsanbauverfahren.
o Quantifizierung der entsprechenden Stickstoffsalden unter Berücksichtigung der Anrechenbarkeit des Stickstoffs aus Wirtschaftsdünger nach Vorgaben der Dün-geverordnung.
o Wirtschaftlichkeit definierter regionaler Rapsanbauverfahren.
o Modellierung von Minderungsverfahren nach Expertenrat.
o Rechenbeispiel Mecklenburg-Vorpommern – Optimierungsvariante nach Dün-geverordnung
o Einschätzung der Erreichbarkeit des Untersuchungszielwerts im Modell.
o Die von der EU gewünschte räumliche Bezugsgröße NUTS2-Region erfordert Durchschnittswerte für unterschiedlich große Gebiete.
o Mit dem entwickelten Rechenmodul sind Anbauverfahren und die erforderlichen Rechengrößen präziser bestimmbar und einzelbetrieblich planbar.
Die THG-Verminderung ist mit folgenden drei Stellschrauben möglich:
(1) N-Düngung (N2O-Feldemissionen) - Mineraldünger (die Vorkettenemissionen implizieren) sind möglichst zu vermindern und am Bedarf gemäß Düngeverordnung zu orientieren (auch um hohe N-Salden zu vermeiden),
(2) Wirtschaftsdünger (generell ohne Vorkettenemissionen) sind effizient einzusetzen, d.h. der N-Gehalt muss berücksichtigt werden,
(3) Dieselkraftstoffeinsatz im Anbauverfahren sollte möglichst verringert werden.
In M.-V. werden wesentliche politische Entscheidungen regelmäßig von Hinweisen auf Bevölkerungsprognosen begleitet. Dabei sind es Bevölkerungsvorausberechnungen, deren Ergebnisse maßgeblich von den getroffenen Annahmen, den zugrundeliegenden Bevölkerungsdaten und der Methodik abhängen. In Kombination mit deren weiteren Prinzipien handelt es sich eher um Modelle, deren Aussagekraft bezüglich eines langen Prognosezeitraumes stark limitiert ist. Da alternative Instrumente demgegenüber deutlich zurückstehen, können Infrastrukturentscheidungen nicht in ausreichendem Maße abgesichert werden.
Vor dem Hintergrund, dass M.-V. bspw. durch eine geringe Bevölkerungsdichte oder eine Vielzahl kleiner Gemeinden gekennzeichnet ist, sollte es die oberste Prämisse sein, langfristig weithin akzeptierte Strukturen zu schaffen, die den Gemeinden eine Perspektive gibt. In diesem Sinne ist der bisherige Ansatz der Stärkung der Zentren und der infrastrukturellen Marginalisierung der übrigen Gemeinden nicht erstrebenswert. Diesem Ansatz wird eine Flexibilisierung von Infrastruktur entgegengestellt, mit der alles erfasst wird, was im politisch gesetzten Auftrag bestehende Funktionsdefizite ausgleicht oder abdeckt. Gleichzeitig wird dem Begriff der Daseinsvorsorge eine Absage erteilt, da von Grunddaseinsfunktionen bei einem staatlichen Rückzug aus der Fläche nicht mehr gesprochen werden kann. Andernfalls würden bspw. die über 65-Jährigen nicht in die Zentren „flüchten‟. Zudem muss festgehalten werden, dass mit der Flexibilisierung des Begriffes Infrastruktur auch eine Neuinterpretation der Begriffe Mobilität und Verkehr einhergeht. Mobilität zeichnet bisher durch eine technische Überbetonung aus und zielt auch auf Ortsveränderungen ab. Damit überschneidet sich Mobilität definitorisch mit Verkehr. Zugleich ist die Rolle der Infrastruktur von nachrangiger Bedeutung. Die Integration des flexiblen Infrastrukturbegriffes führt zu einer Mobilität, die einfach die Fähigkeit zur Interaktion beschreibt und Verkehr wird zu konkreten Handlungen von Subjekten oder sozialen Gruppen. Beide sind dann nur noch von den individuellen Präferenzen und der Infrastruktur abhängig, wobei die Unplanbarkeit der individuellen Präferenzen festgehalten werden muss. Die infrastrukturelle Abhängigkeit zeigt sich auch bei Vulnerabilität und Resilienz. Während Vulnerabilität für Prozesse und deren Wirkungen auf Systeme sowie Organisationen in Abhängigkeit von Infrastruktur steht, bezeichnet Resilienz den Umgang mit vulnerablen Prozessen in Abhängigkeit von der Infrastruktur und der Zielsetzung. Aufgrund der nur unzureichend vorhandenen Informationen über die Gemeinden in M.-V. stand die Verbesserung der empirischen Basis gegenüber de-taillierten Maßnahmen im Fokus.
Ganz allgemein vollzog sich auf der Gemeindeebene zwischen 1990 und 2012 eine sehr vielschichtige Entwicklung. Das betrifft neben der Einwohnerzahl auch die altersgruppenspezifische Betrachtung, die der Beschäftigung sowie die Gemeindefinanzen. In Bezug zu den Einwohnerzahlen führte der Zensus zu eine deutlichen Bereinigung der Statistik. Jedoch wurde eine Rückrechnung für frühere Jahre per Gerichtsentscheid für unzulässig erklärt. Daher behalten die Werte vor 2011 ihre Gültigkeit. Während in den Jahren vor 2000 eine deutliche Suburbanisierung erkennbar war und sich in den Stadt-Umland-Bereichen entsprechende arbeitsräumliche Verflechtungen etablierten, hat sich die Suburbanisierung in der Folgezeit stark abgeschwächt und teilweise ins Gegenteil verkehrt. Getragen wird diese Entwicklung insbesondere durch die 20 - 25 sowie die über 65-Jährigen. Während bei den 20 - 25 Jährigen die ökonomischen Motive überwiegen, welche eine selektive Reurbanisierung stützt, hat die Wanderung der über 65-Jährigen eher infrastrukturelle Gründe. Die infrastrukturelle Marginalisierung der kleinen Gemeinden trifft auf eine Altersgruppe, die in zunehmenden Maße zu keiner Kompensation mehr fähig ist und so in Richtung der zentralen Orte abwandert. Alternativ zieht es diese Altersgruppe auch in touristisch bedeutsame Gemeinden. Damit tritt eine planerisch opportune Wanderungsbewegung ein, welche die Prämisse der Stärkung der Zen-tren unterstützt. Diese Segregation vollzieht sich vor einer dispersen Siedlungsstruktur, welche durch die politische Rahmensetzung und gezielte Vermarktungsstrategien in der Vergangenheit verfestigt wurde, die den individuellen Präferenzen viel Freiraum ermöglichte. Die Infrastrukturkonzentration destabilisiert die Strukturen und fördert wiederum die Arbeitsplatzkonzentration in den Zentren. Allein die Ober- und Mittelzentren vereinten 2012 60 % der SV Beschäftigungsverhältnisse. Die Arbeitsplätze sind damit weit stärker konzentriert als die Bevölkerung und hohe Auspendlerquoten die Folge. Dabei obliegt der Ausgleich infrastruktureller Defizite den Gemeinden, die wiederum eine hohe fremdbestimmte Ausgabenlast zu bewältigen haben. Demgegenüber steht ein KFA, der sich nicht an den realen Aufwendungen orientiert, so dass infolgedessen die Investitionen reduziert wurden. Des Weiteren sind finanzielle Spielräume kaum vorhanden. Im Ergebnis markiert bspw. die selektive Bevölkerungsentwicklung oder die Handlungsunfähigkeit der Gemeinden, die aus der Entwicklung der Gemeindefinanzen resultiert, jeweils einen vulnerablen Prozess, die bisher nicht adäquat bewältigt werden. Die Stärkung der Zentren kann nur im Hinblick auf die politische Zielsetzung als eine positive Resilienzstrategie für eine Handvoll Gemeinden bezeichnet werden.
Um eine zukünftige Alternativendiskussion anzuregen, wurden die Gemeinden im Anschluss einer multivariaten Analyse unterzogen. Zur Absicherung der Ergebnisse wurde eine Prüfung auf Normalverteilung sowie eine Untersuchung auf stochastische Unabhängigkeit vorgeschaltet. Die Prüfung auf Normalverteilung hat ergeben, dass diese für keine der 165 Variablen vorlag. Die maßgebliche Ursache hierfür liegt in der Betrachtungsebene der administrativen Einheiten und dem hohen Anteil der Gemeinden bis 2.000 Einwohner. Allerdings sind die Gemeinde gerade Untersuchungsgegenstand dieser Arbeit, so dass sich eine Änderung der Betrachtungsebene ausschloss. Folglich führte die Gliederung der administrativen Einheiten in M.-V. in Abhängigkeit von den Einwohnerzahlen zu Autokorrelationen zwischen den einzelnen Variablen. Diese Zusammenhänge bestanden auch bei Variablen mit einem zeitlichen Trend, so dass als Folge der Prüfung auf stochastische Unabhängigkeit die Clusteranalyse in zwei Analysen mit jeweils einem Variablenblock geteilt wurde. Die Anzahl der betrachteten Variablen reduzierte sich hierbei auf insgesamt 88. Das Resultat der ersten Clusteranalyse waren 5 Klassen, wobei Rostock eine eigene Klasse bildete. Die anderen Städte wie Greifswald, Stralsund, Neubrandenburg, Wismar sowie Schwerin formten ihrerseits einen Cluster und die übrigen Gemeinden verteilten sich auf die anderen drei Klassen. Insbesondere zahlreiche Tourismusgemeinden und zentrale Orte traten in einem eigenen Cluster deutlich hervor. Die Dominanz der großen Gebietskörperschaften zeigte sich auch in der zweiten Clusteranalyse, wobei sich die Struktur mit 6 Klassen als sehr stabil erwies. Die Ergebnisse wurden nach-folgend in einer Typisierung zusammengefasst, wobei sich 14 Regionaltypen erga-ben, deren Interpretation 7 Haupttypen offenbarte. Neben Rostock als Regiopole treten u. a. Regionalzentren, Kleinstgemeinden oder Gemeinden mit eingeschränkter Leistungsfähigkeit auf. Durchaus bemerkenswert ist der Umstand, dass einige Gemeinden von Usedom und Rügen eher Stadt-Umland-Gemeinden entsprechen und solche mit einer eingeschränkten Leistungsfähigkeit eher im Osten des Landes anzutreffen sind. Daneben sind Tourismusgemeinden ähnlich strukturiert wie Mittelzentren und zahlreiche Grundzentren grenzen sich lediglich über ihren Status von anderen Landgemeinden ab. Darüber hinaus grenzt sich diese Gliederung deutlich von der des Landes mit den ländlichen Gestaltungsräumen ab. Zur Identifizierung dieser wurden Kriterien herangezogen, die stochastisch nicht unabhängig sind, welche zur Basis für ein politisch motiviertes Ranking wurden. Die damit aufgeworfene These von der fragwürdigen Zukunftsfähigkeit, ist in erster Linie politisch determiniert.
Insgesamt zeigt sich mit der Handlungsmaxime „Stärkung der Zentren‟ ein vulnerabler Prozess, der sich in der Gemeindeentwicklung deutlich niederschlägt. Zur Vermeidung einer weiteren Vertiefung ist zunächst eine theoretische Neuausrichtung, wie sie in Grundzügen vorgestellt wurde, notwendig. Dabei ist die Forderung, dass Infrastruktur flexibilisiert werden muss, nicht neu. Sie wurde bspw. schon in Zusammenhang neuer interkommunaler Kooperationsformen postuliert. Die bisherige normative Fixierung der langfristigen Infrastrukturentwicklung über ROG und LPlG manifestiert die Reduzierung des ländlichen Raumes auf seinen existentiellen Kern und ignoriert gewachsenen Strukturen und individuelle Präferenzen der lokalen Bevölkerung. Im nächsten Schritt sollten die Bevölkerungsprognosen um andere Instrumente ergänzt werden, um frühzeitig bestimmte Entwicklungen aufzudecken und zu gestalten. Hierbei sollten die Akteure vor Ort, insbesondere die Gemeinden, auch in der Lage sein, die Gestaltungskompetenz wahrzunehmen. Das setzt voraus, dass zur Erfüllung der Pflichtaufgaben keine Liquiditätskredite erforderlich sind. Sollte eine aufgabengerechte Finanzausstattung nicht möglich sein, muss die derzeitige Aufgabenverteilung zwischen den Kommunen, dem Land sowie dem Bund neu geregelt werden. Eine fremdbestimmte Aufgabenträgerschaft und starre Richtwerte hinsichtlich der infrastrukturellen Ausgestaltung sind Mittel der Vergangenheit, die eine Flexibilisierung und mehr gemeindliche Selbstverantwortung nicht zulassen. Danach kann man beginnen über eine Gemeindegebietsreform Organisationsschwächen zu beseitigen und eine Resilienzstrategie zu verfolgen, die sich nicht allein in einer weiteren Infrastrukturkonzentration erschöpft.
Coastal and marginal seas – like the Baltic Sea – serve as natural reaction sites for the turnover and accumulation of land-derived inputs. The main location for the modification and deposition of the introduced material is, in most cases, not the water mass, but the sediment. Its key function as central reactor in the interaction between land and sea has so far been insufficiently studied and assessed. This study was part of the interdisciplinary SECOS project that aimed to identify and evaluate the service functions of sediments in German coastal seas in the context of human use with a focus on the Baltic Sea. One of its goals was to assess sediment functions related to the intermediate storage or final sink of imported material like nutrients and contaminants, and quantify their inventory as well as their mass accumulation rates on multi-decadal to multi-centennial time scales. For that, a detailed examination of the natural and anthropogenic processes that interfere with sediment accumulation in the south-western Baltic Sea basins is essential.
Certain basal Teleostei from the Early Jurassic of Mecklenburg-Western Pomerania (Germany) and the Late Jurassic of the Franconian Alb (Bavaria, Germany), the Swabian Alb (Baden-Württemberg, Germany) and the western Jura-Mountains (Ain, France) are described. The present doctoral dissertation includes four studies, dealing with representatives of “Pholidophoriformes”, Leptolepidae and Orthogonikleithridae. These studies include anatomical descriptions of new taxa and reviews of poorly known fishes. Furthermore, the stratigraphic and palaeobiogeographical distributions of the examined taxa are discussed.
Quang Xuong is considered as one of the most developed districts in Thanh Hoa Province in terms of agricultural. The major purpose of this research is to find good places to suggest for annual crops production in the case study. Therefore, the assessment of land potential productivity, land suitability, and land cover/land use change in different periods is essential for making strategies of sustainable agricultural development as this will help land-users and land managers to discover the potential and limitations of the current existing land conditions to make appropriate policies and plans for future land use. Its results will provide basic information to make reasonable decisions for investments and rational reclamations of cultivated land before and after each crop season in order to meet the objectives of sustainable development in terms of economic efficiency, social acceptability, and environmental protection. The research site is located at latitudes 19 degree 34 minute N - 19 degree 47 minuteN and at longitudes 105 degree 46 minute E - 105 degree 53 minute E. The total area is about 227km2; in which 128km2 is in use for agricultural activities. Based on soil classification methods by FAO-UNESCO (1988), the agricultural land is classified into six main soil groups, including Arenosols, Salic Fluvisols, Fluvisols, Gleysols, Acrisols, and Leptosols, 12 soil units and 18 sub-units. The largest area belongs to the Fluvisols group with 9358.29ha and the smallest area is identified as the Leptosol group with 219.33ha. Most of the soil in this district has low to moderate nutrition, but in general, they are still suitable for agricultural production. There are 42 land units defined in the land mapping, which can be different from each other by one or more land characteristics. The land mapping unit is created from the overlay of all thematic maps of soil chemicals, soil physical characteristics, and relative topography together by application of GIS techniques. It presents land characteristics and properties in this case study and will be used in comparasion with a particular crop requirement for growth in land suitability evaluation process. A certain land unit may be suitable for one or more types of different land use. It is also classified as highly suitable for a specific land utilization type, but less suitable or unsuitable for other crops. For example, in this study, land unit 26 is determined as highly suitable (S1) for growing paddy rice and maize, but it falls into moderately suitability (S2) for groundnut crop by using parametric (square root) method used in this thesis. Depending on the kind of crops need to be evaluated and its requirement for development compared with each land unit characteristics, land-users will determine the best suitable place for crop production. Identification of land use change in different periods of time has become a central key to monitoring of land resources. It is relatively important for effective land management to protect the land resources, especially the land used for agricultural production from overuse and environmental changes. The sprawl of inhabitant areas, development of rural infrastructures, and industrialization are responsible for serious losses of agricultural land. In this study, remote sensing techniques were applied to studying the trends of land cover change in the abovementioned district in a period of about 24 years from 1989 to 2013. ArcGIS software was adopted to develop the land cover and the change of land use maps from 1989 to 2013. Two satellite images with moderate resolution were collected from USGS Earth Explorer website, Landsat5 TM for 1989 and Landsat8 OLI & TIRS for 2013. After image geo-processing, the images were classified into six land cover categories by applying supervised classification method (Maximum Likelihood). The six main obtained land cover types were built-up areas, agricultural land, forest land, water surface area, salty land, and unused land. The overall accuracies of land cover maps for 1989 and 2013 were 94.08% and 92.91%, respectively. The results of change detection analysis indicate that the cultivated, water surface and unused lands decreased by 22%, 17%, and 91%, respectively. In other side, the built-up and salty land increased by 78%, 58%, respectively and forest land increased from 52.69ha in 1989 to 395.76ha in 2013. The assessment of land potential productivity for agricultural production and land suitability for selected annual crops was based on FAO guidelines for land evaluation (FAO, 1976, 1985, and 1993) which were adopted and slightly modified for compatibility with Vietnamese conditions. All related data were stored, analyzed, mapped and presented in ArcGIS software. Weighted Linear Combination Method developed by Hopkins (1977) and GIS techniques were used to analyze and determine the land potential for agricultural use in the study area. The results show that 5.26%, 83.10%, 10.06%, and 1.57% of the investigated areas were assessed as high potential, moderate potential, low potential and very low potential for growing crops. Regarding land suitability evaluation, the simple limitation, parametric (square root), and AHP methods were used to evaluate the suitability levels for selected crops, including paddy rice, sweet potato, groundnut, maize, potato, sesame, soybean, and green pepper. The obtained results indicate that each applied method provides different results of land suitability level for a specific crop in certain land units compared to the other two methods, and OM, soil pH, soil texture, and relative topography were found out as the main limitation factors which affected land suitability level. The study also suggests that three different methods as abovementioned can be expanded and applied in other places with the appropriate factors used for land suitability evaluation according to particular area conditions.
A large portion of the earth's surface is covered with various vegetation classes (i.e. grassland, wetland and agricultural area, forest) of many diverse species and canopy configurations. The ability to assess and to monitor canopy parameters, such as biomass, leaf area index, and vegetation water content, is of vital importance to the study of different agronomic processes. Remote sensing techniques provide a unique capability towards probing different vegetation types and canopy by operating at different bands, observation angle etc. Over the past decades, significant progress has been made in remote sensing techniques of land processes specially vegetation characteristics through development of advanced ground-based, airborne and space-borne microwave sensors, methods and approaches such as theoretical, semi-empirical and empirical models, needed for analyzing the data. These activities have sharply increased in recent years since the launch of different active and passive satellites and sensors. Remote Sensing (RS) science and techniques combined with ground truth data can provide new tools for advanced agricultural crop applications. It has been demonstrated that RS has the ability to estimate biophysical parameters of agricultural crops over time at local, regional, and global scales. In this study, RS images in visible/near infrared (VIS/NIR) domain as well as microwave domain combined with ground truth data were used to assess biophysical parameters of agricultural crop during their whole growing season at Durable Environmental Multidisciplinary Monitoring Information Network (DEMMIN) test site in North East Germany. Ground truth studies were carried out for 31 weeks during 17th April – 13th November 2013 over three crop lands including winter wheat, barley and canola. Landsat 8 OLI, Landsat 7 ETM+ were used for the VIS/NIR studies and TerraSAR-X synthetic aperture radar (SAR) images were used to study biophysical parameters of agricultural crops in microwave part of electromagnetic spectrum. The analysis was conducted by calculating different vegetation indices (VIs) to estimate the biomass (fresh and dry), LAI, and vegetation water content (VWC) of three crops using Landsat 8 OLI and Landsat 7 ETM+ combined with ground truth data. A new concept of Soil Line retrieval from Landsat 8 image was also developed to estimate plant biophysical parameters using soil line related vegetation indices in optical domain of electromagnetic spectrum. Different approaches including univariate, multivariate stepwise regression and semi-empirical water cloud model was also used to estimate the biophysical parameters of agricultural crop using TerraSAR-X data in microwave domain of electromagnetic spectrum. Perhaps the most important conclusion of this study is that the RS approach can provide useful information about estimating agricultural crop parameters over time and local scale, which can therefore provide valuable information to aid the agronomy community.
Tourism is a multifaceted economy and based on existing nature, as well as on culture in a geographical space to become a successful destination for tourism. The topic of this survey is how tourism in the transitioning country of Vietnam influences culture and nature or vice versa. A special focus will be on the transitioning aspect. This study gives insights about how in the transitioning country of Vietnam, tourism can act as an additional driver of change in terms of nature and culture or if tourism is only adapting to these changes. Therefore in the beginning the subject of ‘social-ecological transformation’ is described and furthermore the situation in Vietnam will be introduced. The key aspects here will be within the range of geography and sociology. It becomes evident, that scientific views on this topic are rather diverse, but nevertheless many theoretical aspects can be observed also in the investigation area Vietnam. Within the country several aspects of economic transition already became reality, while others, like social, ecological or political reforms, are still at the beginning. The empirical part of this study deals with existing thoughts, according to the topic of transition, in relation to tourism development and respectively to environmental understanding, by analyzing and comparing positions of 21 international and Vietnamese experts, 569 international tourists and 710 Vietnamese students. By doing so, similarities within opinions about tourism development and the environmental situation in the country became observable. While tourism is rated as a mostly positive development, the current environmental situation has mostly been criticized by all survey participants. Apart from that, connections between both aspects (tourism economy and nature) are often of no importance or the relationship is identified to be just a rudimentary one. In case of these opinions, involvement within one social group and personal experience is of larger importance than cultural conditioning (European or Asian), e.g. own travels, own jobs and own education. This fact becomes visible by very similar ratings of environmental problems on the one hand and the beauty of natural landscapes on the other hand, done by both survey groups; namely international tourists and Vietnamese students.
This thesis aims to develop a palaeogeographic and chronostratigraphic model of the southwestern Baltic Sea area, to improve our understanding of the depositional history of the Late Pleistocene on both a local and a transregional scale. New sedimentological, palaeontological and numerical age data will be presented from three reference sites located at the coast of NE Germany. So far, the chronostratigraphic assignment of Saalian and Weichselian sediments of NE Germany has been based mainly on lithostratigraphic methods and on sparse numerical age data, resulting in a fragmentary age database. Modern sedimentological approaches, such as facies analyses, have been applied only at a few isolated profiles. Thus, a reliable reconstruction of the depositional environments and their stratigraphic positions is still missing for the study area, which makes the correlation between Pleistocene successions from NE Germany and other circum-Baltic regions problematic. To address these lithostratigraphic and geochronologic issues, three crucial profiles were re-investigated using a multiproxy approach, including sedimentological, geochronological, and palaeontological techniques. The Glowe and Kluckow sites are located on the peninsula of Jasmund (Rügen Island), whereas the Klein Klütz Höved (KKH) section is situated between Wismar and Travemünde at the coast of the Mecklenburg Bay. The age-constraining of critical horizons was conducted by luminescence dating of feldspar and quartz grain minerals. Together, these successions represent the Late Saalian to Late Weichselian period and give rise to the following picture. The Glowe and Kluckow sections reveal that ice-free conditions dominated the study site between 47 and 42 ka. Deposition occurred in a steppe-like environment with moderate summers and cool winters. Meandering and braided river systems inhabited by various freshwater species, such as Anodonta cygnea, Pisidium amnicum and Perca fluviatilis, shaped the landscape. A subsequent cooling phase resulted in the establishment of a periglacial landscape and the formation of ice-wedges. This phase is shown in this thesis to be connected to the Klintholm advance documented at 34±4 ka in Denmark. Furthermore, the data indicate the formation of a lacustrine basin during the transition of MIS 3 to MIS 2 under sub-arctic climate conditions. A potential link to the Kattegat ice advance (29 – 26 ka) will be proposed. At 23±2 ka, the study area was characterised by proglacial and ice-contact lakes related to the Last Glacial Maximum ice advance of the Scandinavian Ice Sheet (SIS). This is the first documented SIS advance of Weichselian age, which reached Jasmund at 22±2 ka. The KKH sedimentary succession comprises deposits of Late Saalian to Late Weichselian age: after a period of deglaciation between ~139-134 ka (Termination II; MIS 6), which is preserved in a glaciofluvial sequence deposited in a braided river system, a lacustrine environment was established in an arctic to subarctic climate. During this time, the landscape was vegetated by typical Late Saalian flora communities. The Eemian interglacial is represented by lacustrine to brackish deposits covering the reference pollen zones 1 to 3. During this initial part of the Eemian, thermophile forest elements spread (Quercus, Ulmus), indicating a deciduous forest. The presence of brackish ostracods represents the influence of a marine transgression between 300 and 750 years after the beginning of the Eemian period. A hiatus of more than 90,000 years separates the Eemian from the overlying Late Weichselian sediments. During the Late Weichselian period, the deposition at KKH was dominated by glaciolacustrine and subglacial facies, where the first Weichselian ice advance occurred at 20±2 ka. The sedimentological and geochronological findings in this thesis provide valuable information for the reconstruction of the palaeoenvironmental history from the Late Saalian to Late Weichselian period. The Late Saalian palaeoenvironmental setting is reconstructed, including Termination II and the initial phase of the Eemian interglacial. Furthermore, the Eemian marine transgression is shown to have occurred 300 to 750 years after the beginning of this interglacial. The first proven Weichselian advance of the SIS approached NE Germany between ~23 and ~20 ka. In contrast, there is no evidence to support a pre-LGM advance of Weichselian age to the study area, as proposed by several authors, neither at Glowe and Kluckow, nor at the KKH site. Based on the presented results, and contra what was previously assumed, the MIS 3 Ristinge and Klintholm advance of the SIS, documented in Denmark, did not reach NE Germany.
The present doctoral dissertation comprises new studies on the fossil vertebrate assemblage recovered from the late Early Jurassic marine “Green Series” clay deposits of Grimmen and Dobbertin in north-eastern Germany that contribute to fill the gap of knowledge regarding its faunal composition and its relevance for understanding Early Jurassic vertebrate life. The investigations led to the recognition of wide range of vertebrate taxa, including basal gravisaurian sauropods, secondarily marine reptiles, a diverse fauna of leptolepid fishes, and a new genus and species of pycnodontiform fishes. In addition, a taxonomic revision of the Early Jurassic saurichthyid fish Saurorhynchus was performed, leading to the identification of two new, previously unnamed species. The results provide new insights into the taxonomic, systematic, and ecological diversity of Early Jurassic vertebrates, and hence add significant new data to our knowledge on Lower Jurassic vertebrate palaeobiodiversity patterns.
The focus of this study is on the geochronological and paleo-climatic characterization of late Pleistocene glaciations in Turgen and the Khangai Mountains located in central and western Mongolia. These two mountain ranges form a 700 km long NW-SE transect through Mongolia and allow assumptions of the temporal and causal dynamics of the regional late Quaternary glaciations and their correlation to other mountain glacier records from Central and High Asia. In order to evaluate extent and timing of the Pleistocene glaciations in Mongolia, geomorphological mapping and cosmogenic radionuclide (CRN) surface exposure dating (10Be) were carried out in four valley systems located in the Khangai and Turgen Mountains. Additionally, a coupled 2-D surface energy balance and ice flow model was used to determine steady-state conditions for glaciers under various climatic scenarios. With this model it is possible to test combinations of temperature and precipitation settings, which would produce glacier configurations that fit the field-mapped ice extent. In total, 47 glacial boulders and roche moutonnées were sampled, prepared and AMS measured to determine the absolute timing of moraine formation and ice retreat based on 10Be surface exposure dating. Of these, 27 samples were obtained from the Khangai Mountains (three separate moraine sequences) and 20 samples were taken from the Turgen Mountains (two moraine sequences). The dating results (presented as minimum ages) give evidence for a late Pleistocene maximum ice expansion during late MIS 5 (81−78 ka) and major ice advances during MIS 2 (26−20 ka) in both mountain ranges. Only in the Khangai Mountains (central Mongolia) very significant glacier advances also occurred during mid-MIS 3 (49−35 ka), which exceeded the ice limits set during the MIS 2 glaciation. A final ice position, constructed shortly before the onset of full ice retreat was formed between 19-16 ka, and is likely to represent a recessional ice stillstand, or alternatively a final ice readvance during the early part of the last-glacial-interglacial-transition (LGIT) in both mountain ranges. Energy/mass balance and ice flow modeling results suggest that climatic conditions during the MIS 5 and MIS 3 maximum advances in the Khangai Mountains were depressed between a ∆T of -6.0 to -5.2 °C with a precipitation factor of 1.25-1.75 (P = 125-175 %, compared to modern conditions), and a ∆T of -5.3 to -4.4 °C (P = 75-125 %), respectively. For the MIS 2 ice advances modeling results from the Turgen and Khangai Mountains suggest a temperature depression ∆T of -5.7 to -4.6 °C (at 22 ka; P = 25-50 %) in the East-Turgen, and a ∆T of -7.5 to -6.6 °C (at 20 ka; P = 25-50 %) in the Chulut area (Khangai Mountains). These results document a 1.8 - 2 °C difference of the modeled temperatures required to expand the studied paleo-glaciers in the Turgen and Khangai mountains to their field-mapped MIS 2 ice limits, highlighting a spatially differentiated pattern of paleo-temperature lowering across the studied 700 km NW-SE transect. Taken together, the presented record indicates that the largest ice advance in both investigated mountain ranges occurred during the MIS 5 / MIS 4 transition, despite earlier suggestions by previous studies that the local glacial maximum would be associated with the coldest periods of the last glacial cycle (i.e. MIS 4 or MIS 2). Glacier systems in the Khangai Mountains also increased substantially during MIS 3 (local LGM) in response to cool but comparable wet conditions, probably with a greater-than-today input from winter precipitation and an additional input of recycled moisture from expanded paleo-lakes in the Valley of the Great Lakes. The lack of a severe cooling during the MIS 3 ice advances, and probably also during the late MIS 5 ice expansion, suggests that variations in atmospheric circulation patterns, with its significance for controlling the regional precipitation/moisture supply, was a key driver for these late Pleistocene ice advances in Mongolia. This notwithstanding, there is also clear evidence for the development of an extensive glaciation during MIS 2, coinciding with a period of severe cooling and hyperarid conditions. This highlights that glacier systems in Mongolia responded sensitively, both, to variations in moisture supply and its seasonal distribution, and to the marked insolation minima during the last glacial cycle.