Refine
Year of publication
Document Type
- Article (60)
- Doctoral Thesis (54)
Language
- English (114) (remove)
Has Fulltext
- yes (114)
Is part of the Bibliography
- no (114)
Keywords
- - (25)
- Vietnam (7)
- Geochemie (5)
- Fernerkundung (4)
- Ostsee (4)
- Tourismus (4)
- behavior change (4)
- bentonite (4)
- Adaptation (3)
- Biosphärenreservat (3)
Institute
- Institut für Geographie und Geologie (114) (remove)
Publisher
- MDPI (20)
- Copernicus (12)
- Springer Nature (12)
- Frontiers Media S.A. (5)
- Wiley (5)
- SAGE Publications (2)
- De Gruyter (1)
- Elsevier (1)
- Nature Publishing Group (1)
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.
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.
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.
Wadi Wurayah area is located in the north of Fujairah Emirates between the towns of Khor Bidiyah Fakkan and Oman on the Gulf Coast Line in Fujairah Emirates, United Arab Emirates. It lies within a priority World Wide Fund for Nature ( WWF) Global 200 Ecoregions ( ecoregion 127, Arabian Highland Woodlands and Shrublands ), a rich diversity of sheltering rare and endangered mountainous and freshwater habitats and species , and providing opportunities for the revival and sustenance of local livelihoods. However, as most of the United Arab Emirates and the region , the area is undergoing dramatic changes linked to economic diversification and promotion of tourism. The United Arab Emirates in 1999 approved the programmed of work from the UN convention of Biological Diversity ( CBD). This momentum must be used wants it or disappear. In a first move , the United Arab Emirates established the federal Environment Agency ( FEA) that produced the Environmental Law of 1999 with the role to encourage each to Emirates assess its land and coastal / marine resources, formulate plans for establishing protected areas , upgrade those that may already exist , and help implement the environment law. In early 2006, UAE created its first Ministry of Environment and Water ( MEW ), which was before the Ministry of Agriculture and Fisheries. Environmental issues and a greater role of the civil society are now higher on the agenda of the United Arab Emirates government , partner of the Emirates Wildlife Society ( EWS ), the World Wide Fund for Nature ( WWF) - UAE Project Office is the only international conservation NGOs operating in the UAE that plays a pioneering role in partnering with local- governmental institutions to establish win- win solutions. The United Arab Emirates is making tremendous efforts in diversification is the development of tourism. Too often tourism mass , With all of its negative environmental consequences is privileged. However, the more traditional Emirates are seeking alternatives that would preserve their environment and respect the traditional lifestyles of the local communities. This study aims to help a sustainable biosphere reserve integrating oneself local traditional and lifestyle with the conservation of biodiversity and habitat inimitable by providing a model of economical incentives unique to the region . In order to further the implementation of the Wadi Wurayah Biosphere Reserve, this study will: • Implement a set of carefully - targeted actions in Wadi Wurayah and its hinterland and therefore Fujairah Emirates. • Work to demonstrate the feasibility and viability of combining environmental protection in a sensitive area with the preservation of traditional activities. • Support the capacity building of key national and local authorities and selected partners in the Emirates of Fujairah and the UAE So that they have the awareness and skills to fully realize the aims of the study . To set out and develop options for sustainable natural resource management in the proposed Wurayah Biosphere Reserve , one of the UAE as examples of marginal dry lands , building on environmental information system was the best choice using Geographic information systems (GIS ) as a tool. This has been classified to there steps of work: Field Survey and Analysis Lab Office work. As a first step, this study used to survey this area in the light of the work done by the EWSWWF and the Fujairah Municipality, to evaluate the potential and the feasibility of the creation of a Biosphere Reserve. The traditional field survey has been carried out in three batches between January 2007 and January , 2009 for sample collection using specially tailored database forms that suit the properties and nature of the variables measured, and the database . Design The information obtained from field survey included the Landscape and their local classification and distribution , local habitats , water catchments areas , local rangeland systems and indigenous agro -ecological zones. This information in addition to the laboratory analysis has then be transformed into GIS format, and overlaid with the base maps of the study area in order to produce a georeferenced maps. Various types of maps required according the selected works related to area of study have been used as an input data for the GIS system An integrated management methodology / approach has been proposed associated with the plan of work throughout the forthcoming years. The plan of work is designed to be as consistent as possible with that of the concept of the UNESCO 's Man and Biosphere Program.
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.
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.
Mind the gap: Information gaps and bridging options in assessing in-situ conservation achievements
(2008)
The biodiversity crisis has gained political attention on a global level. The “2010 Target” of the Convention on Biological Diversity (CBD) aims to significantly reduce the loss of biodiversity by 2010. In order to achieve this, a network of representative and effectively managed protected areas is to be established. The effectiveness of protected areas thus represents one indicator for progress towards the CBD’s 2010 Target. However, indicators require information. The present study, in a first step, reviews the availability of open access long-term ecological data for assessing protected area effectiveness. This review shows two parallel – though contradictory – phenomena: data overkill and data scarcity. While the number of online databases providing open access data on biodiversity has grown tremendously, no long-term ecological data for a larger set of protected areas can be openly accessed. Reasons for this data scarcity are discussed. Based on this lack of information, in a second step, a method to bridge information gaps through social science research is aspired. An innovative Conservation Success Framework is developed, which defines and relates conservation needs, conservation capacity and conservation actions, its three main components. The basic assumption is that conservation can only be successful where the conservation capacity exists that is required to implement the conservation actions determined by the conservation needs. The framework was used to develop open and closed questionnaires for application in two Mexican biosphere reserves, the Sierra Gorda and the Sierra de Manantlán. As "conservation success" is often immeasurable in protected areas in practice due to unspecific conservation objectives the term is for the case studies substituted by “conservation achievements”, i.e. clearly noticeable effects from conservation actions. Overall, almost 60 interviews were conducted with different stakeholder groups. The gained information is validated through social science research techniques, such as triangulation of perspectives and active and passive observation. Based on this, conservation needs are identified and conservation capacities summarised and discussed for both case study sites. Implemented conservation actions addressing identified conservation needs and conservation capacity constraints are then analysed. In addition, noticeable effects from conservation actions on the state of biodiversity at case study sites, i.e. the conservation achievements, are described. Where locally available, non-open access data (as opposing open access data) are used to verify the findings from the social science research. Identified conservation achievements at both case study sites are evident both from quantitative information (for example forest cover increase according to non-open access data) and qualitative information (for example perceived change in the occurrence of illegal activities according to interviews). In addition, rather “intangible” indicators that can only be revealed through qualitative surveys are identified for both sites. This study thus highlights the crucial importance of integrating different types of data, ecological and socio-economic, as well as quantitative and qualitative ones. The present study concludes with a series of recommendations 1) to local practitioners at the two case study sites, and 2) to the international conservation community. Local practitioners may benefit from the present study because its results provide for each site a) an overview of existing conservation needs and implemented conservation actions; b) an easy way to identify action gaps; c) a baseline to identify progress indicators; and d) an overview of diverse perspectives on the current effectiveness of the biosphere reserves. These benefits are considered of particular importance as they can be influential in the revision of the site’s management plans, which both are now approximately ten years old and will soon be revised. The international conservation community will not be able to make a clear statement in the year 2010 about the effectiveness of protected areas on a global level due to a lack of information and transparency. However, the year 2010 should not be considered an end point for measuring progress in in-situ conservation; instead protected area quality standards must be created, effectiveness evaluations institutionalised and efforts to foster regular reporting must continue. Consequently, a scheme of consolidated actions from local to national and international level is proposed that could help to sustainably bridge existing information gaps and close them on the long run. In the end, progress reporting on the effectiveness of protected areas, and other indicators, can only improve if different governance levels “mind the information gaps” in cooperation, until continued information gathering and sharing hopefully closes these gaps one day.
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.
Although the Pleistocene deposits exposed in the steep coastal cliffs of Mecklenburg-Vorpommern have been studied for more than a century, the depositional conditions of many lithostratigraphic units remain unclear. There is, in particular, a question whether the individual tills (locally more than 9 successive till units) are mainly subglacial deposits or resedimented (mass flows) in origin (at least in part). The Pleistocene deposits preserve information concerning the former glacial depositional processes. Detailed micromorphological analysis of these deposits can provide key information regarding these processes and thereby aid in the reconstruction of former glacial environments. The island of Rügen is located on the southwestern Baltic Sea coast and was situated in the marginal zone of the Scandinavian Ice Sheet during the last glacial period (Weichselian). Therefore, the region is considered as an ideal area for reconstructing the complex fluctuations in the position of the margin of this ice sheet as it expanded across the Baltic Sea and into northern Germany. Successive glacial advances and retreats of the ice sheet can be reconstructed by specific glacial sedimentation processes and flow-direction criteria derived from a variety of glacial deposits. The investigation area is located near Sassnitz on Rügen, where an imbricated and folded Weichselian succession disconformably overlies Maastrichtian chalk bedrock. The individual till units were sampled for micromorphological analyses to identify the former depositional conditions. Detailed description of the sedimentology and variation in facies, the description of macroscale deformation structures provides the context for the detailed micromorphology study. The three dimensional analysis of the microfabrics is based on the microstructural mapping methodology which enables the identification and interpretation of polyphase deformation within subglacial sediments.
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.
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.
This thesis aims at improving the current representation of adaptation in economic frameworks of climate change by a) accounting for the time-dependent evolution of the adaptive capacities of countries and b) quantifying unwelcome feedbacks of the adaptation process. In this context, it is proposed that economic assessments of climate change incorporate adaptation as a cyclic and phase-dependent process while devising their cost methodologies. A phase-dependent process acknowledges the existence of adaptation barriers while a cyclic process accounts for potential unwanted feedbacks of adaptation. By analyzing economic assessments against this framework, it is shown that dependencies between phases of adaptation and phases altogether are often disregarded. Furthermore, potential negative consequences associated with adaptation are rarely considered and adaptation is generally assumed to be unconstrained. The assumption of unconstrained adaptation is only acceptable in the context of high adaptive capacity. This concept was further investigated through a review of vulnerability assessments regarding their operation of the adaptive capacity component. It was found that adaptive capacity is mostly equated to proxies that reflect the knowledge, financial and livelihood capacities of the system under analysis. With this theoretical considerations in mind, a dynamic representation of adaptive capacity was elaborated at a country-level. The Human Development Index (HDI) was used as a proxy of the adaptive capacity of countries and its evolution in time extrapolated. The time required for countries to achieve developed world standards of human development was then estimated. The results indicate that between 2005 and 2020, half of the world population will live in countries with low adaptive capacity. This percentage is then progressively reduced to 15% in the year 2050, with marked regional differences. The time required for a country to achieve an appropriate level of development sets a clear constraint on when, and to what extent, the country can engage on climate change adaptation. This does not imply that adaptation will not take place before development occurs. Rather, it calls for adaptation options to be tailored in order to t the current and future adaptive capacities of countries. Obtaining higher levels of adaptive capacity is likely to be associated with negative consequences for the climatic system. The statistical relation between HDI and per-capita emissions of countries was established and future projections made. Between 2010 and 2050 approx. 300 Gt of CO2 are estimated to be associated with the increase of adaptive capacities of current developing countries. This value represents about 30% of the allowed CO2-budgets to restrict global temperatures to an increase of 2 degrees by 2100 compared to pre-industrial times - conditional to a 25% risk of failing to meet the target. For the case of sea-level rise, the modelling framework DIVA (Dynamic Interactive Vulnerability Assessment) was used in order to illustrate the drawbacks of a simplistic representation of adaptation. The results show that adaptation via the construction of protective infrastructure might be economically feasible for particular countries. For others, modeled results fail to provide a clear choice between adaptation or inaction. The assumption of unconstrained adaptation resulted in the valuation of costly protection options whose financial and knowledge requirements can be at odds with the capacities of some coastal countries - namely developing countries. Further, infrastructural protection as adaptive measure to prevent coastal damages can have the counter-productive effect of raising the amount and value of assets at risk. This is a direct result of DIVA disregarding the potential unwelcome feedbacks of adaptation itself. In conclusion, the full potential of economic assessments of climate adaptation is likely to remain unlocked as long as adaptation continues to be misrepresented. The methodologies discussed in this work provide a way forward to alleviate this deficiency in forthcoming assessments. For the case of sea-level rise, the modeling framework DIVA (Dynamic Interactive Vulnerability Assessment) was used in order to illustrate the drawbacks of a simplistic representation of adaptation. The results show that adaptation via the construction of protective infrastructure might be economically feasible for particular countries. For others, modeled results fail to provide a clear choice between adaptation or inaction. The assumption of unconstrained adaptation resulted in the valuation of costly protection options whose financial and knowledge requirements can be at odds with the capacities of some coastal countries - namely developing countries. Further, infrastructural protection as adaptive measure to prevent coastal damages can have the counter-productive effect of raising the amount and value of assets at risk. This is a direct result of DIVA disregarding the potential unwelcome feedbacks of adaptation itself. In conclusion, the full potential of economic assessments of climate adaptation is likely to remain unlocked as long as adaptation continues to be misrepresented. The methodologies discussed in this work provide a way forward to alleviate this deficiency in forthcoming assessments.
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)
Geopolymers (GPs) are inorganic binders created by adding alkaline solution (e.g. KOH) to silicates such as furnace slag, fly ash or clay to dissolve Si and Al that polymerises and precipitates to form an inorganic binder material while hardening. GP properties are similar to ordinary Portland cement regarding their high compressive strength or low shrinkage but they are particularly notable for a high resistance to acid and fire. However, the most significant advantage of GP cements is their low CO2 footprint. The most common clay used as GP raw material is kaolin. The aim of this study is to investigate the suitability of illitic clays as a cheaper alternative to kaolin and determine the necessary preparation steps required to produce effective GP binder materials. Three clays dominated by dioctahedral 2:1 layer silicates, in particular interstratifications of mica and smectite were investigated: (1) Illitic clay from Friedland, Northern Germany, containing an irregularly stacked illite-smectite interstratification (R0 I-S), (2) rectorite from Arkansas, USA, as a regular interstratification of mica and smectite, and (3) clay stated as “sárospatakite” from Füzérradvány clay deposit, Northern Hungary, containing a long range ordered I-S (R3). The three types of I-S interstratification-rich clays were extensively characterised and the Friedland clay, as the most probable raw material for GP production, was studied in more detail including several size fraction analyses. These results are used to investigate and determine the parameters necessary to produce suitable precursors for GP binders. Different approaches of clay activation to yield a highly reactive material by milling and heating were examined. Milling was found to be suitable as a preparation step after heating breaking up sintering aggregates to create pathways for the alkaline solution, but not as a substitute for heating. Important parameters for the precursor design such as temperature, time, and heating rate are determined and discussed. Geopolymerisation is considered to be a multi-parameter system and is influenced strongly by the degree of dehydroxylation, Si:Al ratio, or amount of 5-fold coordinated Al. However, in contrast to kaolin-based systems, none of these parameters explain why the illitic Friedland clay heated to 875 °C was found to be most suitable for GP binders. Based on leaching experiments and specific surface area (AS) measurements of the heated Friedland clay, a conceptual model is presented to explain the observed relationship between the heating temperature and the subsequent compressive strength of the GP cement. An optimum between the counteracting reactions of decreasing AS (fewer particles must be covered with GP phase) and decreasing Si+Al dissolved (less GP phase created) is necessary, which exists at 875 °C for the Friedland clay. In this state enough GP phase is created to bind all remaining sintering aggregates to form a cement with high compressive strength. This relationship can be expressed as (Si+Al) / AS (sum of dissolved Si and Al divided by the surface area of grains that must be covered with GP phase), and can be used as a predictive tool for determining the optimal heating temperature. The results presented in this thesis indicate that illitic clays are suitable raw materials as GP binders if the necessary preparation steps of dehydroxylation, sintering and grinding are made. Proxies used to evaluate the optimal conditions for making GP binders are determined including the (Si+Al) / AS ratio as a key relationship that controls the cementation process and determines its ultimate hardness.
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.
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.
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 dissertation aims at developing means to integrate conservation and development in biosphere reserves in Madagascar. Despite a multitude of concepts such as UNESCO biosphere reserves, Integrated Conservation and Development Projects and community-based natural resource management, gaps between conservation and development remain to exist. In a qualitative case study in Mananara-Nord and Sahamalaza Iles-Radama Biosphere Reserves in Madagascar data was collected on biosphere reserve management, local use of natural resources and socio-cultural aspects that influence natural resource use. Furthermore, natural values local people associate with the forest were investigated. Analysis revealed that management capacities constitute a limiting factor in biosphere reserve management. Collaboration between management, local people and international organisations fosters the achievement of both conservation and development. However, collaboration is only possible if (i) clear rules are formulated and (ii) partners have a vision in common. Based on the theory of social capital, newly introduced and locally existent rules/institutions having an influence on the use of natural resource were categorized in bonding, linking and bridging social capital. Furthermore, the perception of natural values was classified in instrumental and non-instrumental values and assigned to ecosystem services identifying the importance of nature for human well-being. With the capabilities approach Amartya Sen defined human well-being as the achievement of those capabilities a person considers valuable. This includes aspects that assure livelihoods on the one hand and aspects that are conducive to well-being on the other, thus both being relevant for development. In the dissertation capabilities are based on both instrumental and non-instrumental natural values and consequently offer an opportunity to demonstrate and characterise the relationship between nature and human well-being. Social and natural values provide orientation for a biosphere reserve management. The category bonding social capital (social values) describes local socio-cultural aspects in communities and their importance for collaborative processes. Natural values provide the management with guiding principles to foster nature conservation and to integrate locally existent capabilities. Supporting and furthering these capabilities enables the development of new capabilities of all concerned persons. The dissertation demonstrates various possibilities to build bridges between (i) nature conservation and development, (ii) natural and social sciences, (iii) formal regulations and local socio-cultural aspects and (iv) diverse actors. Implementation of a social monitoring is recommended together with local stewards and Malagasy students to collect information about the perception of natural and social values and use them as guiding principles for biosphere reserves. Collaboration with national and international scientific institutions can foster this process.
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.
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.
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.
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.
The objectives of the present work are to relate the spatial distribution of benthic macrofauna in the Baltic Sea to patterns in environmental variables describing near-bottom hydrographical conditions and sediment characteristics, analyzing the data for two various spatial extents. The first case study is devoted to an exploratory statistical description of the prevailing ecological structure within the limited area attached to the region of the Mecklenburg Bight. Key environmental descriptors of spatial distribution of macrofaunal communities were disclosed within the area of investigation: water depth, regarded as a proxy for other environmental factors, and total organic content. Distinct benthic assemblages that are discriminated by particular species (Hydrobia ulvae–Scoloplos armiger, Lagis koreni–Mysella bidentata and Capitella capitata–Halicryptus spinulosus) were defined. Each assemblage is related to different spatial subarea and is characterized by a certain variability of environmental factors. This study represented the basis for the predictive modelling of species distribution in the selected investigation area, which constituted the next part of the investigation. Species-specific models predicting the probability of occurrence relative to environmental and sedimentological characteristics were developed for 29 representative macrofaunal species using a logistic regression modelling approach. Subsequently, the technique for a predictive modelling of species distributions in response to abiotic parameters based on single-factor logistic regression models, utilizing Akaike’s information criterion (AIC) and Akaike weights for multimodel inference, was used. Thus, probabilities of occurrence for selected exemplary species (Arctica islandica, Hediste diversicolor, Pygospio elegans, Tubificoides benedii and Scoloplos armiger) were modelled and mapped. Finally, the investigation proceeded on a large spatial scale. The discriminating ability of such factors as salinity, bathymetry, and sediment characteristics (considered only generally due to the lack of more detailed data) to explain the occurrence of typical macrozoobenthic species on the Baltic Sea-wide extend was tested. Full coverage macrofauna distribution maps, though being increasingly demanded, are generally lacking, with information being merely restricted to point observations. In contrast to spatial interpolation, periled by presence of short distance changes in community structure and dependence of the result on density of the samples, predictive habitat suitability modelling allows to objectively produce distribution maps at a level of detail limited only by the availability and resolution of the environmental data. Various literature sources and available databases were analyzed in respect to the information on macrozoobenthos distribution in the Baltic Sea, resulting in the compilation of an extensive list of taxa and an inventory dataset on species distribution for the whole Baltic Sea. The study demonstrates the need to analyze species’ relationships in gradient systems such as the Baltic Sea and provides a basis for a tool to predict natural and anthropogenic forced changes in species distribution.
In 1992, the international regime 'Agenda 21' was agreed upon. Accordingly, countries worldwide have been undergoing reforms in their water management into Integrated Water Resources Management (IWRM). The implementation is promoted by international actors. The main institutional aspects of IWRM are the river basin approach, clear property rights allocation, and application of economical instruments. In former centrally planned economies, the process of IWRM implementation has been coincided with transformation for the market economy. The implementation of institutional aspects of IWRM in countries under transition is connected with high transaction costs. Against this background, the comparative empirical study was initialised in order to analyse institutional change of water management towards IWRM in Vietnam and in Poland. Two models of river basin organisations were examined. Consequently, pros and cons of decentralised polycentric and hierarchical unicentric river basin organisations have been evaluated. Formal institutions were studied with the use of an in-depth review of legislation in Vietnam and in Poland. The EU Water Frame Directive (EU WFD) and other international policies were also examined. For the empirical study in Vietnam and in Poland, actors were interviewed as experts. The results of the study on both countries were discussed separately, and conclusions were drawn in a comparative manner. Water management reforms towards IWRM in Vietnam and in Poland have been generating multi-level governance processes including international, national and sub-national levels. The implementation of IWRM in Vietnam is supported by international donor agencies. In Poland, the implementation of the EU WFD is coordinated by the European Commission in a hierarchical manner. In comparison to international joint-development projects in Vietnam, the European Commission enforces international IWRM policy more effectively. Since the resumption of ODA in early 1990s, water resources management has been institutionalised in Vietnam by international support. In 1998, a Water Law was established in Vietnam. The intended separation of water resources management from water service provisions caused fragmentation between the Ministry of Natural Resources and Environment, and the Ministry of Agriculture and Rural Development, respectively. This ‘silo-effect’ has been intensified by the competition for international ODA. The power struggles affect even agencies within ministries. Polycentric river basin committees have been established as entities subordinated to the Ministry of Agriculture and Rural Development, as well as the Ministry of Natural Resources and Environment. However, because of weak property rights allocation and the absence of administrative powers, the river basin organisations work ineffectively. The river basin has not yet been established as a sub-national area of political action. Decisions sustained to be made at central level and are affected by the information problem due to largely centralised organisations of Vietnamese water management. The sub-national level is characterised by very low planning and management capacities. In Poland, unicentric river basin organisations were established in 1991. They are aligned with hydrological borders. Water resources planning and management are carried out according to river basins and water regions in order to implement the EU WFD. The river basin has been established as a new area of decision-making. Conflicts between local-governments have been resolved after the reforms. Nevertheless, spatial management planning, environmental protection planning, water service delivery, etc., are further carried out by local self-governments. To integrate water resources planning and management with these services, horizontal coordination is of critical importance. However, this is hampered by problems of ‘spatial fit’. Moreover, a high degree of horizontal cross-border communication increases information problems in hierarchical organisations. Thus, features of polycentric governance models become increasingly important in order to fully implement the EU WFD in Poland.
Monitoring of Calcite Precipitation in Hardwater Lakes with Multi-Spectral Remote Sensing Archives
(2017)
The primary objective of this study is to practically apply geostatistical tools that can help to improve an evaluation of groundwater quality for a particular area. The Nam Dinh area, an area of 70 x 70 km2, located in the Southern part of the Red River Delta, was selected as a source for different data sets to be used as case studies. A set of geostatistical tools has thus been applied to the different real data sets which were collected from the coastal Quaternary aquifers in the different campaigns. This gives us a yardstick by which the success of a specific approach can be measured. Throughout the thesis a series of the case studies are, in turn, represented in order to get insight into and an understanding of what various geostatistical tools can do and, more importantly, what their shortcomings are. There are nine different methods of data analyses use in this thesis, which include: (1) Major Ion Comparison, (2) Graphic Plots, (3) Exploratory Statistical Data Analysis, (4) Variogram Analysis, (5) Spatial Estimation Using Kriging, (6) Cluster Analysis, (7) Principle Component Analysis, (8) Multivariate Regionalization Analysis, and (9) Contamination Risk Mapping Using Indicator Kriging. First, major ion comparison and graphic analysis are performed in order to get a general hydrogeochemical view of the collected datasets, before stepping into a further geostatistical approach. By these analyses, various groundwater types are observed and a general hydrochemical trend is visualized using Stiff- and Piper diagrams as well as site maps. The major ion ratios in relation to TDS concentration are compared to investigate the origin of water. Second, a statistical exploratory data analysis is applied to describe the important features of the data by which the character of a specific hydrogeochemical variable might be recognized. Deviations from the Gaussian probability model are detected and appropriate transformations for a formal analysis in geostatistics are selected. Since the Theory of Regionalized Variables (Mathéron 1971; short term: Geostatistics) assumes Gaussian distribution the hydrochemical variables used here are checked for normality. These analyses show that although the data are facing some problems such as outliers and they are very positively skewed at the linear scale, this can effectively be minimized by transforming the data to log-scale. Third, both variogram analyses and Kriging techniques are used to spatially estimate a rectangular 36x36 estimation grid within an area of 70 x 70 km based on the sampled locations (85, 45 and 74 and 38 visited locations for the Pleistocene RS, the Pleistocene DS, the Holocene RS, the Holocene DS, respectively). These estimated values are then used to map the spatiotemporal variability of groundwater quality. In practice, estimation of unknown values and mapping of concentrations of a specific variable can, of course, easily be created by many available software programs. However, error variances are always present in any estimation due to a level of uncertainty, so the reliability of how these estimates could be yielded has also been evaluated in this case study. A critical assessment of all possible variations, tightly related to the seasonal change, directional influence, spatial distribution and prediction error is conducted and concluded. Fourth, Cluster Analysis (CA), Principle Component Analysis (PCA) and Multivariate Regionalization Analysis (RA) are applied to three main datasets of all Quaternary aquifers in the Nam Dinh area to discover the relationships among measured hydrochemical parameters by which we can detect and regionalize major factors which have an impact upon groundwater quality. These approaches are also to overcome the plethora of data that is usually a common problem for any one who has already tackled groundwater data. In this case study both clustering and R mode principal component analyses are thus performed based on the following parameters: The log-transformed concentrations of all measured major ions and of NO3-, NO2-, NH4+, PO42-, i.e. 11 variables from three different datasets of the main aquifers. By cluster analysis three classes of water types, ranging from freshwater to brackish-saltwater types, are typically grouped. Finally, Indicator Kriging (IK) is performed to evaluate the risks of arsenic contamination. The focus of this approach is to assess contamination risk expressed as probability of exceeding threshold- values. The region may thus be subdivided into “safe” and “unsafe” zones on the basis of probability maps which mark contaminated all places where the risk of arsenic contamination exceeds a given threshold for drinking water purpose. By this case study, it is shown that Indicator Kriging is a useful method which has some advantages for many contamination studies. Firstly, it is well known as the non-parametric technique which can be appreciably used when a dataset does not reach normal shape or nearly normal shape as in this situation. Secondly, the outlier problem that often exists in any analysis can be overcome when applying this method. Thirdly, it can be applied in practice to delimit a study area into “safe zone” or “unsafe zone” from which decision-making on the water supply can be decided for the remediation of a contaminated water source or selecting an appreciative source for exploitation. The combined use of spatial (Geostatistics) and multivariate statistical measures have proven to be of major assistance in questions of assessing groundwater quality especially in less sampled regions. A major advantage lies in the possibility of simultaneously creating spatial estimates as well as estimation confidence limits.
Tourism is booming on global level since many decades and developing countries often capture tourism as a lever to push up their economy. Many regions in Vietnam invest lots of money in this development hoping to change the traditional economic structure. Located in the North Central Vietnam, about 170 km from Ha Noi capital to the south at the coastline, Sam Son is known as an ideal location for holiday makers. Currently the number of tourist has been counted to millions. Realizing its potential, the local authorities decided to enlarge and improve tourism to become the biggest tourism center in the North Central part of Vietnam. As many mass tourism destinations, Sam Son is facing several hidden drawbacks, which are generated by a (too) fast growth. Thats why unexpected problems may occur very soon. One path to mitigate weaknesses and to strengthen the positive impacts of tourism is to develop tourism in a more sustainable manner. As the very first step Sam Son needs to delineate a proper strategy and to establish a powerful "Destination Management System". Although several studies have been conducted already, the destination lacks reliable empirical data. This research intends to fill the gap by supplying concrete information with specific focus on “making tourism more sustainable”. In the study methodological triangulation has been applied to collect data and information. Besides literature review and secondary data analysis, two surveys - statistically well secured - have been conducted: A household survey with more than one thousand questionnaires to record the situation and opinion of local people and a visitor survey with 1139 face-to-face interviews to collect structural data about current guests in Sam Son as well as to explore their behaviour. Moreover expert and stakeholder interviews were included to supplement the information basis. As the research acquired the information directly from local people and from tourists by face-to-face interviews several weaknesses could be unveiled which official statistical data cannot show. There are three facets out of balance in terms of economic benefit: Compared with the political awareness and the financial support the tourism sector does not ensure the livelihood of an adequate number of people; the economic benefits from tourism are very unequally distributed and also the spatial dimension indicates a strong imbalance - only people living directly in the core area of tourism participate in tourism sector, the positive impact of tourism does not reach till the outskirts. In addition social and environmental problems are recognized by a majority of local people as consequences of tourism in the region. Regarding the touristic demand side a very low level of satisfaction has been detected: A small variety and low quality of touristic offers are the main reasons of dissatisfaction. The most exiting finding is that tourists treasure environment in the destination, whereas this aspect is underestimated in the locals view. In addition, tourists are really willing to pay for an improvement of environmental and touristic quality! Even if the amount of voluntary payments is very low, the total sum can enable the local government to develop the destination in a very proper way. Although this is a case study the results deliver valuable information and furthermore a concrete delineated roadmap for all destinations, which are in the same situation as Sam Son today. It is an example how to analyze and evaluate the present condition and how to continue in a proper way towards a more sustainable tourism development.
The non-natural substances in commonly used UV protection creams such as TiO2, are known to have a photocatalytic side effect, which is very harmful to human skin. This study presents some properties of clays and clays minerals concerning UV protection potential, which can be very helpful for the development of new UV protection cream generation. Clays and clay minerals are demonstrated that they have potential to absorb UV-radiation. The structures of clay particles in cream were shown to be dependent on the layer charge of clay minerals. The total amount of Fe2C>3 in chemical composition of clay plays a key role in determining the UV-absorption ability of the clay matter. Moreover, the UV-absorption ability also depends on the expandable or non- expandable property of the clay. The studies were also performed on the mixtures of wool-wax-alcohol cream and nanosuspension obtained by the extraction of fungi mass Ganoderma pfeifferi by using plantacare together with clay. The combination of clays and nanosuspension increased its UV-absorption ability. The skin model test was performed in vivo in mouse ears with skin flora Escherichia coli and infectious bacteria Staphylococcus aureus in order to determine the effects of cream samples on skin under UV irradiation and skin infection. From the results of characterization of clays and clay minerals properties in UV protection cream, this study also brings some ideas about products designing.
Using geopolymers can reduce significant amounts of CO2-emissions during the production compared to Portland cement. Although illite/smectite clays are very abundant on earths crust and rich in SiO2 and Al2O3, studies of their geopolymerization potential are rare. Thus, the illite/smectite clay of Friedland (NE Germany) was calcined (850 °C) and ground to form a reactive metaclay and then mixed with synthetic gibbsite (to test the effect of Al-concentration) and 6 molar NaOH or KOH, in order to study their geopolymerization at 25, 50 and 75 °C within 28 days. The raw clay, the precursors, and the geopolymers were characterized by XRF, XRD, SEM-EDX, Flame-AAS, nitrogen adsorption and compressive strength test. 25 °C was too low to initiate the geopolymerization of illite/smectite. Increasing the curing temperature increased the reactivity of meta-illite/smecite. Si and Al dissolution was confined to the first 24 h, followed by the hardening of the geopolymers within 28 days. At 50°C, KOH-activation formed amorphous and mesoporous aluminosilicates, which significantly cemented the particles and agglomerates of the metaclay. Consequently, geopolymers with high compression strength (~38 N/mm2) were formed. Adding 10 wt% Gibbsite (precursor Si/Al = 2.1) to the metaclay strengthened the formation of amorphous aluminosilicates and increased the compression strength of the geopolymer by 20 % from 38 - 45 N/mm2. At 75 °C, the reactivity of the metaclay in NaOH was higher than in KOH. NaOHactivation at that temperature formed geopolymers with high compression strength (~30 N/mm2) due to the cementation by microporous phillipsite (K-, Na-zeolite) crystals. Thus, alkali-activation of the calcined and ground meta-illite/smectite from Friedland form high strength geopolymers under hydrothermal conditions.
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.
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.
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.
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.
Tidal flats represent the transition zone between the terrestrial and marine realm. They are subject to pronounced dynamics due to distinct tidal and seasonal variations of physical, chemical, and biological parameters significantly influencing redox-sensitive element cycles. Thus, redox-sensitive trace metals may be suitable indicators for variations in bioproductivity and microbial activity. Therefore, seasonal and tidal dynamics of manganese, iron, molybdenum, uranium, and vanadium were studied in the water column and sediments of tidal systems of the German Wadden Sea (southern North Sea) in the years 2007 to 2009 involving also previously analysed data from year 2002. To demonstrate the response of the trace metal cycles on phytoplankton blooms and enhanced biological activity time series data of nutrients and phytoplankton dynamics were also involved in this study. Pronounced cycling is seen for pelagic manganese revealing distinctly higher values during low tide. Complex seasonal cycling showing maxima of dissolved manganese in spring and late summer and a depletion period in early summer is caused by benthic-pelagic coupling and reflection of exhaustion and replenishing periods in the surface sediments. Vanadium dynamics are coupled to the manganese cycling due to vanadium scavenging and release during manganese oxide formation and reduction, respectively. Molybdenum and uranium behave almost conservatively following changes in salinity and thus, being slightly enhanced during high tide. Deviations from conservative behaviour are found to occur during breakdowns of summer phytoplankton blooms. In the following, significant enrichments of manganese, molybdenum, iron, and uranium are observed in the shallow pore waters. These coherences are assumed to be caused by a tight coupling of geochemical, biological, and sedimentological processes. Intense release of organic matter during the breakdowns of algae blooms leads together with enhanced bacterial activity in summer to the formation of organic- and trace metal-rich aggregates which are deposited and incorporated into the tidal surface sediments. Microbial decomposition of the aggregates and corresponding shifts in redox-conditions effect a release of dissolved trace metals into the pore water. Subsequently, the trace metals are fixed in the sediment as sulphides, adsorbed to organic compounds or released to the overlying bottom water. Furthermore, two tidal systems, one from the East Frisian and one from the North Frisian Wadden Sea are compared. Although, both areas show different hydrodynamical, sedimentological, and ecological conditions similar manganese dynamics are observed implying that this is a common behaviour in the entire Wadden Sea. However, distinct quantitative differences appear showing a 6-fold higher level of dissolved manganese in the water column of the East Frisian area. This is explained by a higher manganese release from tidal flat sediments and a larger sediment area/water volume ratio compared to the North Frisian area. Detailed time-series data of the nutrients phosphate, silica, and nitrite+nitrate are used to verify model simulations and to calculate nutrient export budgets considering tidal and seasonal variations. The model results imply an export of nutrients from the tidal flats into the open waters of the German Bight which is in the same order of magnitude as the combined discharge of the rivers Elbe, Weser, and Ems. To investigate the importance of the Wadden Sea as a potential manganese source for the North Sea, transects were carried out into several tidal flat areas of the North Frisian Wadden Sea. The results suggest that the North Frisian Wadden Sea is a less important source for dissolved manganese compared to the East Frisian area. In contrary, the export of particulate manganese seems to be more important showing distinctly higher concentrations in the North Frisian study areas in summer. The influence of sediment permeability and bioturbation on trace metal budgets of the pore waters are investigated in natural and experimentally manipulated tidal flat sediments. Advective pore water transport in highly permeable sandy sediments and bioturbation promote exchange processes at the sediment/water interface probably leading to reduced nutrient and trace metal enrichments in the shallow pore waters. Furthermore, the penetration of oxygen into deeper sediment layers induces a release of sulphidic bound molybdenum to the pore water. During laboratory experiments with natural anoxic sediments an effective oxidative molybdenum release is determined during resuspension of the sediments in oxic seawater. Thus, pronounced sediment resuspension during storm events is suggested to cause significant release of molybdate from displaced anoxic sediment components thereby enhancing the molybdate level of the open water column. In addition to the examination of recent biogeochemical processes, the paleo-environmental influence on geochemical and microbiological processes in Holocene and Pleistocene sediments of the East Frisian study area were analysed in an interdisciplinary study. It is found that the microbial abundance and activity are higher in the Holocene than in the Pleistocene sediments. However, this is mainly caused by present environmental conditions. The impact of the paleo-environment on the microbiology is less pronounced. The lithological succession affects hydrological processes which enable the transfer of electron donors and acceptors for present early diagenetic processes into deep sediment layers. The paleo-environmental imprint is still detectable but the modern biogeochemical processes dominate in the sediment-pore water system.
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.
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.
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.
Urban Green Areas – their functions under a changing lifestyle of local people, the example of Hanoi
(2013)
Hanoi is a rapidly developing city - in terms of area, population and economy. It also has to face social and environmental problems that often accompany the fast development of a city. Increasing environmental pollution leads to a decrease in living conditions, such as clean water, housing, social services, etc., for most of the city’s inhabitants. Other well-known social problems in cities worldwide also occur in Hanoi nowadays, for example inequality, food supply, and unemployment. In addition, the society is altering; lifestyle- change is a permanent process. Today, it seems that the changing process in Asian countries is rather leap-frogging than continuously. Although many research projects concerning to urban green areas in Hanoi have been completed recently, less is known about utilization of parks&gardens in a practical and systematic way. This study aims at contributing to fulfills the gaps with up-to-date facts and figures of parks’ utilization in the inner city of Hanoi. Based on “grounded theory”, triangular methodology was applied to collect empirical data in four main parks in the inner city of Hanoi namely: Thong Nhat, Bach Thao, Hoan Kiem, and Lenin. Scientific observations, visitor countings were done in 2010-2011; including 2143 face-to-face interviews to park users covering the course of the year and a small online-poll of 113 responses. Thirteen interviews with experts have been done in several phases and taken into account for discussing and testing hypotheses. Empirical results have shown that utilization of the parks is in abundance in terms of the use - numbers as well as activities. A comparison between the courses of the day for parks in Berlin and Hanoi shown that the time of using parks in Hanoi is earlier in the day. In details, there is 25% and 1.4% of total daily visitors went to parks in Hanoi and Berlin,, respectively. However, the biggest peak in park-visiting time for both cities is in the afternoon. The findings also clarified that students and retirees are the major users even though there is some different in structures of park user among the four parks. The length of stay depends on how large and interesting a park is. In this aspect, Hanoi parks are very poor in facilities showing by a long list of missing facilities in the parks. However, as there is no alternative, parks in Hanoi still attract a high number of visitors. In general, results from this study have shown a close relationship among socio-economic and political situations in Vietnam with UGAs and its utilization. Influencing factors on parks’ utilization were also indentified, which are social changes, lifestyle changes, economic situation, conflicts in land usage, and maintaining cost for UGAs. Three given hypotheses were confirmed: i) the demand of public UGAs in inner Hanoi will grow mid-term and increase strongly long-term; ii) Hanoi’s residents will claim strongly for more parks in the future; ii) The number of conflicts inside the area of UGAs, among the visitors will occur very soon and require a specific master plan for the development and the management of UGAs. Finally, based on the weaknesses of UGAs in Hanoi recently, two groups of recommendations were also suggested to improve UGAs. Firstly, in terms of quality – quantity: • Retain each square meter of green space as UGA – do not unblock any green space for construction; • The existing UGA have to be well maintained. Secondly, in terms of management – planning: • Elaborate a UGA-masterplan for (inner) Hanoi; • Keep UGA management in the responsibility of public bodies; • Implement participation of affected population defector in the process of planning and management (as it has already been written in planning guidelines); • Be aware of potential conflicts among park user groups; • Establish an UGA monitoring system – involving regular (or even permanent) countings based on up-to-date technology; Realize horizontal partnering structures.
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.
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.