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Northern peatlands are ecosystems with unique hydrological properties, storing about 400-500 Gt of carbon. As the production rate of organic material is higher than its decomposition, which is slowed down in the wet and cold environment, peatlands store a great amount of carbon. Carbon assimilated from the atmosphere during photosynthesis by plants is partly lost due to autotrophic and heterotrophic respiration as carbon dioxide (CO2), as methane (CH4) or/and as dissolved organic carbon. The proportion of each carbon component is strongly controlled by environmental conditions as temperature, radiation, precipitation and subsequent water table changes and active role of vegetation. With predicted changes in the global climate, changes in the influence of environmental parameters on peatland ecology are expected. Thus thorough research is essential for a better understanding of mechanisms which influence carbon cycling in peatlands. In this thesis, various components of the carbon cycle were studied at two boreal peatland sites (Ust Pojeg in Komi Republic in Russian Federation and Salmisuo in Eastern Finland) using the micrometeorological eddy covariance method. The focus was placed on the temporal changes of the controlling parameters, ranging from a few days during short snow thawing through the rest of the year. At the Salmisuo site, two measurement seasons allowed to address possible inter-annual variation. We observed that diurnal variations in methane emissions which are typically controlled by vegetation during the growing season, might appear during snow melt as a result of the influence of physical factors rather than biological factors. The diurnal pattern in methane emissions was caused by the interaction of the freeze-thaw cycle and near urface turbulence. During the night time, when surface temperatures fell below zero and caused formation of the ice layer, methane emissions were only around 0.8 mg m-2 h-1, however after the increase in temperature and melting of the ice layer they reached peak values of around 3 mg m-2 h-1. The near surface turbulence had a significant influence on methane emissions, however only after the thawing of the ice layer. The effect of changing environmental parameters over the year was further elaborated on a carbon dioxide time series from the Ust Pojeg site. The generally accepted effects of temperature on ecosystem respiration during the night are not stable throughout the year and can change rapidly during the growing season. Using moving window regression analysis I could show that the strength of the exponential relationship between ecosystem respiration and temperature is changing during the year. This was in correspondence with recent publications elaborating on sub-seasonal changes of the controlling parameters. In general, measurements from the Ust Pojeg site represent estimates of annual CO2 and CH4 fluxes with an annual carbon balance of -94.5 g C m-2 and a new contribution to the quantification of trace gases emissions from a Russian boreal peatland. The inter-annual comparison of net ecosystem exchange (NEE) measurements with previously published data on CH4 and DOC flux from the Salmisuo site showed that the NEE of CO2 is the most important component of the carbon balance at this site. However, primary production was not responsible for the inter-annual changes in NEE. Rather, the effects of water table position during the year had a strong influence on ecosystem respiration, which was probably due to the influence on soil respiration, and higher NEE was observed during the year with smaller primary production, but higher water table levels. The effects of higher precipitation and higher water table during the wet year were shown to increase CH4 flux and the export of DOC, but their effects could not compensate for changes in ecosystem respiration. In the presented thesis intra- and inter- annual changes in carbon flux components and their controls, in our case attributed mostly to hydrological conditions in combination with other environmental parameters as temperature and the role of peatland vegetation, are discussed.
Mit zunehmend beobachtbaren Klimawandelauswirkungen steigt die Bedeutung, die Klimawandelanpassung als Ergänzung zu Vermeidung hat. Das gilt für Industrieländer wie für Entwicklungsländer, für ökologische wie soziale Systems und insbesondere für sozial-ökologische Systeme. Um wirksame Anpassungseffekte erzielen zu können, müssen Anpassungsmaßnahmen jedoch durchführbar sein. Welche Faktoren die Durchführbarkeit behindern oder steigern, wird am Beispiel dreier deutscher Biosphärenreservate (Mittelelbe, Schaalsee und Südost-Rügen) mittels Experteninterviews und eine qualitativen Meta-Analyse wissenschaftlicher Publikationen über Hindernisse und Erfolgsfaktoren für Anpassung untersucht. Die Ergebnisse zeigen verschiedene Schlüsselkategorien an Faktoren, beispielsweise Klimawandelwahrnehmung, verfügbare Wissens- sowie finanzielle und personelle Ressourcen, den politischen und den sozio-ökonomischen Kontext. Die insgesamt identifizierten Faktoren umfassen sowohl interne, als auch externe Faktoren: - intern: Klimawandelwahrnehmung und Klimawandelwissen/-information - extern: verfügbare Ressourcen und politische und ökonomische Rahmenbedingungen Daher müssen Ansätze, die die Durchführbarkeit von Klimawandelanpassungen steigern wollen, interne und externe Faktoren integrieren. Vor diesem Hintergrund wird ein theoriebegründetes Konzept zur Steigerung der Durchführbarkeit entwickelt. Es setzt sich aus fünf Bausteinen zusammen: 1) anpassungsunterstützende Klimawandelwahrnehmung stärken 2) bestehende Klimawandelwissen verbessern 3) No-regret und robust Anpassungsoptionen identifizieren 4) die politische Unterstützung für Anpassung steigern 5) ausreichende finanzielle und personelle Ressourcen sowie Infrastruktur bereitstellen Diese Bausteine in die Tat umzusetzen erfordert gemeinsame, disziplin- und sektorenübergreifende Anstrengungen von Wissenschaft, Politik und Gesellschaft. Aufgrund ihres Selbstvertändnisses sind Biosphärenreservate geeignete Instrumente und Lernlaboratorien, um solche Anstregungen zu unterstützen und Modellregionen zur Steigerung der Durchführbarkeit von Klimawandelanpassungen zu sein. Effectively applying these building blocks requires cross-sectoral, concerted efforts between science, policy and society. Due to their concept, biosphere reserves appear well suited to foster such efforts and to become model regions to enhance the feasibility of climate change adaptation.
Global change, amongst others characterized by increasing temperatures, altered precipitation patterns, an increase of extreme climatic events and continued atmospheric depositions of pollutants, is expected to severely impact forest ecosystems worldwide. The complex interplay between different factors acting upon tree growth, combined with regional patterns in climatic change calls for a region specific evaluation of the possible consequences on forest ecosystems. For northeastern Germany regional climate models identify a rise in temperatures and a change in precipitation patterns. Drier summers and wetter winters together with an increase in extreme weather events are seen as the most pronounced changes that will occur during the 21st century. In this thesis I analysed past growth rates and climate-growth relationships in different stands of beech (Fagus sylvatica L.) and oak (Quercus robur L.) along a gradient of decreasing precipitation in a space for time approach. Special attention was paid to the influence of summer drought, soil waterlogging and the importance of site conditions in modulating the reactions to these climatic stressors. Departing from these retrospective analyses, future growth trends are modelled for beech, oak and Scots pine (Pinus sylvestris L.), based on projections of a regional climate model until the year 2100. Furthermore, I studied the influence of sudden and extreme shifts in hydrological conditions on the growth of oaks in a drained peatland that was subject to catastrophic rewetting. All analyses of this thesis are based on ring-width and wood anatomical features applying a variety of dendrochronological methods. The gradient approach revealed similar climate-growth relationships for beech and oak on drought exposed, sandy sites, where water availability during early summer was the main growth-limiting factor for both species. Decreasing precipitation rates towards the East are associated with higher drought susceptibility, especially for beech. As a result, competitive superiority of beech over oak decreases. In a drier future the competitive balance between the two species may shift (rank reversal). During the past decades beech has shown larger interannual growth variability and a higher number of growth depressions. These changes might indicate that increasing temperatures and climatic variability are already affecting its growth patterns and climate sensitivity. This is in line with the prospective modelling approach. According to our models, growth trends will turn negative for beech and oak towards the end of the 21st century, with beech showing the highest growth reduction (23% compared to the reference period 1971-2000). For pine, modelled growth rates show only minor changes. Whereas beech and oak shared a high common signal on the dry sites, the two species differed in high frequency ring patterns on the wet sites. On poorly drained, loamy soils beech, with its superficial root system, suffered from summer droughts. In contrast, on these sites ring-width of pedunculate oak was not correlated to summer moisture conditions resulting in differing interannual ring patterns between dry and wet sites. Wet periods with high soil water saturation did not have a negative influence on the growth of either species. Such a lack of response is not surprising for oak, which is generally known as rather tolerant to soil waterlogging, but it indicates an unexpectedly high tolerance of beech to stagnating wetness. Using the natural laboratory of an oak forest that suffered a catastrophic flooding I could show that slower grown trees that had likely been suppressed displayed a higher adaptive capacity compared with bigger, dominant trees. Many of the previously dominant individuals died within 18 years after the event. Trees that survived the groundwater rise displayed a typical ring pattern: growth was suppressed for a few years, but afterwards recovered and even surpassed previous growth rates, most likely as a result of competition release. The sudden hydrological change left a clear imprint in ring patterns and wood anatomical features in both the dying and the surviving trees. This differentiated imprint may be helpful for a better interpretation of growth patterns found in subfossil bog oaks, an important climate proxy of the Holocene. The insights gained from this thesis support existing concerns about drought induced growth decline for oak, but especially for beech. Changes in precipitation patterns might lead to wetter conditions during winter, but these will likely have only little effect on growth. Both s show rather high resilience to stagnating wetness. More likely, it are extreme events like prolonged droughts or heavy rainfalls that might breach thresholds in the ability of the two species to cope with too much or too little water. Such extreme events thus pose a strong risk to the future growth performance of both oak and beech.
Climate change threatens marine ecosystems by simultaneous alterations and fluctuations in several abiotic factors like temperature, salinity and pH. Therefore, a strong ability to cope with varying environmental factors is indispensable for marine organisms. Especially, larvae of meroplanktonic species will be affected by predicted alterations in environmental conditions as planktonic larval stages are considered the most sensitive stages during life history (Anger 2001).
The European shore crab Carcinus maenas, as an ecological key species, was chosen as a model species to investigate multiple stressor effects on early life history stages of marine meroplanktonic invertebrates. The life cycle of C. maenas is biphasic consisting of five pelagic larval stages (four zoeal and one megalopal stage), followed by benthic juvenile and adult phases. The metamorphic molt from the last zoeal stage to the semi-benthic Megalopa includes dramatic changes in ecology, habitat, behavior, feeding, morphology, and physiology. During life history, zoeal stages of C. maenas are of particular interest in the course of climate change as these stages are more vulnerable than the following developmental stages to alterations in abiotic factors.
The aim of the present thesis was to develop an integrative view on effects of long-term exposure, from hatching to metamorphosis, to increased temperature and hypo-osmotic conditions on early life history stages of C. maenas. We wanted to gain insights into larval responses to climate driven environmental variables, more specifically, on how tolerance to low salinity is affected by increased temperatures.
Consequently, the present study investigated the effect of long-term exposure to twelve different sub-lethal temperature and salinity combinations in an ecological relevant range on larval development of C. maenas. In a multidisciplinary approach, larval responses in performance (survival and developmental duration) and morphology were measured. Furthermore, analysis on larval ontogeny and organogenesis created the foundation for analysis of larval response to multiple stressors in anatomy.
Results of the present thesis demonstrated that despite their different life-styles and external morphology, brachyuran larvae are smaller versions of their adults when regarding their inner organization: the adult bauplan unfolds from organ anlagen compressed into miniature organisms. In addition, they provide an overall picture of seemingly gradual organogenesis across larval development and the metamorphic molt, an insight that contrasts with the abrupt external morphological changes during metamorphosis. Gradual anatomical changes in e.g. osmoregulatory structures like gills and antennal glands allowed for ontogenetic shifts of tolerance to temperature and salinity during zoeal development and successive increase in osmo- and thermoregulatory capability. On the other hand, osmoregulatory structures as seen for adults were underdeveloped during zoeal development and therefore do not qualify for osmoregulatory function for these stages. This potentially explains the higher sensitivity of zoeae to hypo-osmotic conditions.
Early life history stages of C. maenas were affected on all response levels by the tested multiple stressors. The interaction of temperature and salinity was of antagonistic type, resulting in general reduced stress for larval stages. Nevertheless, low salinity had a strong negative impact on survival, while increased temperature caused ann acceleration of development. Furthermore, the size of zoeae of C. maenas was driven by the interaction of temperature and salinity, with extreme conditions, causing diminished growth, thus resulting in smaller larval size. On the other hand, larval shape was only slightly affected by changes of abiotic factors. Volume of the digestive gland and the heart of larvae from long-term exposure to sub-lethal temperatures and salinities showed high variability.
Larval responses were affected by the stressors intensities: moderately high temperatures lessened the negative effects of low salinities, while extreme high temperatures exceeded the ameliorating effect of temperature on stressful salinity conditions. On the other hand, the tolerance to temperature and salinity increased during larval development indicating an ontogenetic shift in response to multiple stressors with development. In addition, performance, morphology, and multiple stressor interaction showed intrapopulation variability among larvae hatched from different females, and between experimental periods.
In conclusion, this study highlighted direct effects of abiotic factors on all investigated response levels in early life history stages of the meroplanktonic larvae of the invertebrate C. maenas. High mortality rates combined with higher sensitivity confirm that planktonic early life history stages are the bottleneck during life history of this species. Nevertheless, early life history stages of C. maenas had the ability to cope with wide ranges of changing environmental factors. The antagonism between temperature and salinity on larval development offers potential for early life history stages to persist in a changing world. Furthermore, anatomical structures allow for slight eurytolerance and potentially for compensation of abiotic stress. Overall, slight increases in temperature, driven by climate change may enable larvae of C. maenas to tolerate exposure to moderately low salinities and, combinedwith intrapopulation variability, potentially allows for population persistence. Summarized, this study emphasizes the importance of testing a wide range of ecologically relevant traits in developing pelagic larvae in order to properly characterize their response to environmental change.
Changes in abundance and phenology of planktonic larvae like the zoeae of C. maenas have major potential to change a species‘ population structure significantly, and furthermore indirectly affect whole community and ecosystem structures. Therefore, this thesis may serve as a bridge to future studies in evolutionary and ecological developmental biology.
Bats are special: although they have a small body size, bats are extremely long-lived and have a low annual reproductive output, which puts them at the ‘slow’ end of the slow-fast continuum of mammalian life-histories. Species typically respond to climate change by genetic adaptation, range shifts or phenotypic plasticity. However, limited dispersal behavior in many bat species and long generation times make it very likely, that adaptive responses in bats are rather driven by phenotypic plasticity than by genetic adaptation or range shifts. Changing weather patterns, a higher frequency of extreme weather events and overall rising temperatures, caused by climate change, will impact phenology, energy supply and energy expenditure. In species where adult survival largely shapes population dynamics, it is thus of crucial importance to understand how climate change affects individual fitness and fitness relevant traits by altering behavior and development.
In my study, I investigated how weather impacts behavior, fitness and fitness relevant traits in free ranging Natterer’s bats from two geographical regions (south vs. north) in Germany. In the Nature Park Nossentiner/Schwinzer Heide (northern region, NSH), long-term data for investigations on population dynamics are partially collected by hibernation counts. Although counting hibernating bats is a regularly applied method, it is still unclear to which degree human visits in the hibernaculum trigger energy consuming arousals and thus increase energy expenditure. Thus, I first investigated if hibernation counts potentially threaten winter survival by assessing the number of energy consuming arousals of hibernating Natterer’s bats (Myotis nattereri) and two other bat species (Pipistrellus spp., Plecotus auritus) using thermal imaging. Additionally, I used light barriers in the hibernacula to investigate the relative impact of winter temperatures and human visits on flight activity of hibernating bats. Secondly, I investigated effects on survival and reproduction during summer by analyzing capture-mark-recapture data from summer roosts. Data from summer roosts have been collected since 2011 in Würzburg (WB, south) and 1990 in the Nature Park (NSH, north). Based on these data, I analyzed the effect of intrinsic (e.g. age) and extrinsic(e.g. different weather parameters) factors on individual survival probability and reproductive success. I further focused on the question if individual body size is a fitness relevant trait in Natterer’s bats and how body size of young bats is affected by summer temperatures.
During hibernation, ambient temperatures were the most important driver for bat activity and were positively correlated with the number of flight passes in the light barrier, suggesting that bats can exploit foraging opportunities more frequently during warm weather bouts. Monitoring caused only a small number of arousals and only a slight increase in activity, which was less severe on warmer days, when activity was generally higher. Thus, I propose that benefits of hibernation counts outweigh the costs of human presence in the hibernaculum and unlikely threaten winter survival in hibernating bats.
In spring, increased precipitation during a short time window strongly reduced the probability of successful reproduction in first-year females (females that returned from first hibernation, FY). In terms of timing, this sensitive period comprises the implantation or early pregnancy, a time before substantial investment into embryo development. Moreover, I identified a positive correlation between a large body size and reproductive success in FY females. Given the evidence that suitable weather conditions during early life support juvenile growth and thus a large body size, my findings suggest that reproduction may be condition dependent in young females. Reproductive success of older females was not affected by either weather or individual parameters. This suggests that older and experienced females can better deal with adverse conditions.
To examine if beneficial weather conditions are linked to a large body size, I investigated the effect of ambient temperatures during the growing season on body size. I found that higher ambient temperatures during summer led to larger individuals, however, only in the northern population. In the on average colder North, warmer summers may benefit juvenile growth by reducing thermoregulatory costs and increasing prey abundance, whereas in the general warmer South, this effect might not be visible or relevant. When I analyzed the link between body size and survival, I revealed that larger adult females have higher survival rates. Given the fact, that a large body size is a response to beneficial early life conditions, this demonstrates the impact of early life conditions on long lasting fitness effects.
The results of my research lead to the assumption that warmer ambient temperatures have positive effects on Natterer’s bats, both during winter and summer. However, increased activity in response to rising winter temperatures, as expected under climate change scenarios, could be a serious thread for hibernating bats, if food availability does not increase in the same amount as bat activity. During summer, warmer temperatures may have positive effects on juvenile development in northern regions, but this effect could be negative in more southern regions by exceeding heat tolerance and resulting in water stress. This research highlights, that investigating periods of weather sensitivity on a finer time scale and also in a spatial context is of crucial importance to gain a better understanding for mechanisms leading to the impacts of weather on fitness.
Recent climate change has affected the forest system comprehensively. Northern hemisphere elevational treelines are considered as a key environment for monitoring the effects of current anthropogenic climate change. Moreover, trees from these areas are also widely employed in paleo-climate reconstructions. The stability of the tree growth climate relationship under current scenario is crucial for all tree ring based climate researches. It is important to investigate how trees respond to this rapid environmental change at altitudinal treelines. Tree cores from 21 treeline sites of three species (Pinus tabulaeformis, Picea crassifolia, and Sabina przewalskii) from Northeastern Tibetan have been conducted in this thesis. The instable correlations between tree growth and climate are the general response pattern of trees from all study sites in NE Tibetan Plateau. Picea crassifolia shows the most instable response to climate factors (mean monthly temperature and total monthly precipitation). Pinus tabulaeformis and Sabina przewalskii just showed instable and divergent responses to their main limiting climate factors but no clear trend was found which is limited by the few sample sites. Corresponding to divergent responses of Picea crassifolia to mean monthly temperature, most radial growth of Picea crassifolia were inhibited by this climate change type drought, only few trees within same sites grew faster due to temperature increasing during recent decades. The divergence response mainly started in last 30 years in six of eleven sample sites over the Northeastern Tibetan Plateau. North-westerly drier sites showed a large percentage of trees per site with a negative correlation to temperature and mostly southerly moister sites showed more mixed responses with both negatively and positively responding trees within site. Concurrent with the regional pattern, low elevation sites show mostly negative correlations with temperature and high elevation sites show more mixed responses. As the hydrothermal conditions of the investigation area changed to a drier and warmer combination, drought stress on tree growth have been intensifying over time and expanding spatially from the middle to most of our study area during the last half century. The Picea crassifolia tree growth climate relationship conducted on an elevational gradient with four different levels from upper treeline to lower treeline at the NE Tibetan Plateau. Results show that upper treeline trees show divergent growth trends and divergent responses in recent decades. Trees from lower treeline show a strengthening drought stress signal over time and no divergent growth trends within sites. This potential ecological reaction of tree populations to changing environmental conditions shows an implications for using trees to reconstruct climate, since the indiscriminate use of tree ring data from sites showing opposite responses to increasing warming could cause mis-calibration of tree ring based climate reconstructions, and over- or underestimation of carbon sequestration potential in biogeochemical models. The physiological response of Sabina przewalskii tree growth to major limiting climate factors based on the Vaganov-Shashkin (VS) model indicated that precipitation during the early growing season, especially in May and June, has significant effect on tree growth, while temperature mainly affects tree growth by warming-induced drought and by extending the growing season in the NE Tibetan Plateau. Under current and projected climate scenarios, modeling results predict an increase in radial growth of Sabina przewalskii around the Qaidam Basin, with the potential outcome that regional forests will increase their capacity to sequester carbon. However, most Picea crassifolia trees growing at lower elevations than Sabina przewalskii might be continue stressed by the warming induced drought and might decrease radial growth in future.