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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Tundra ecology-Alaska-North Slope. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (447 pages)
    Edition: 1st ed.
    ISBN: 9783662011454
    Series Statement: Ecological Studies ; v.120
    DDC: 574.5/2644/097987
    Language: English
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Plant ecophysiology -- Arctic regions. ; Vegetation and climate -- Arctic regions. ; Vegetation dynamics -- Arctic regions. ; Plants -- Effect of global warming on. ; Electronic books.
    Description / Table of Contents: The arctic region is predicted to experience the earliest and most pronounced global warming response to human-induced climatic change. This book synthesizes information on the physiological ecology of arctic plants, discusses how physiological processes influence ecosystem processes, and explores how climate warming will affect arctic plants, plant communities, and ecosystem processes. Key Features * Reviews the physiological ecology of arctic plants * Explores biotic controls over community and ecosystems processes * Provides physiological bases for predicting how the Arctic will respond to global climate change.
    Type of Medium: Online Resource
    Pages: 1 online resource (490 pages)
    Edition: 1st ed.
    ISBN: 9780323138420
    Series Statement: Physiological Ecology Series
    DDC: 581.5/2621
    Language: English
    Note: Front Cover -- Arctic Ecosystems in a Changing Climate: An Ecophysiological Perspective -- Copyright Page -- Table of Contents -- Contributors -- Preface -- Introduction -- Chapter 1. Arctic Plant Physiological Ecology: A Challenge for the Future -- I. Introduction -- II. Physiological Ecology and Ecosystem Studies -- III. Physiological Ecology in the Arctic -- IV. Climate Change: A Theme for Arctic Physiological Ecology -- References -- Part I: The Arctic System -- Chapter 2. Arctic Climate: Potential for Change under Global Warming -- I. Introduction -- II. Present-Day Climate -- III. The Greenhouse Effect -- IV. Climate Models -- V. Implications for Snow, Permafrost, and Ice -- VI. Implications for Ecosystems -- VII. Summary -- References -- Chapter 3. Arctic Hydrology and Climate Change -- I. Introduction -- II. Watershed Structure -- III. Watershed Processes -- IV. Impact of Climatic Warming on Watershed Structure -- V. Hydrologic Response of an Arctic Watershed to Global Warming -- VI. Summary -- Acknowledgments -- References -- Chapter 4. Circumpolar Arctic Vegetation -- I. Introduction -- II. Forest-Tundra -- III. Low Arctic -- IV. High Arctic -- V. Arctic Carbon Reserves -- VI. Arctic Climate Change and Vegetation Patterns -- VII. Summary -- Acknowledgments -- References -- Chapter 5. Phytogeographic and Evolutionary Potential of the Arctic Flora and Vegetation in a Changing Climate -- I. Introduction -- II. Status and History of the Arctic Flora -- III. History of the Tundra Vegetation on the Alaskan North Slope -- IV. History of the Subarctic Vegetation in Central Alaska -- V. Floristic Richness along Latitudinal Gradients -- VI. Warmer Climates and Future Migrations -- VII. Summary -- References -- Chapter 6. Plant Succession, Competition, and the Physiological Constraints of Species in the Arctic -- I. Introduction. , II. Arctic Landscapes -- III. Models of Succession -- IV. Succession in the Low Arctic -- V. Succession in the High Arctic -- VI. Plant Competition -- VII. Summary -- Acknowledgments -- References -- Part II: Carbon Balance -- Chapter 7. Effects of Global Change on the Carbon Balance of Arctic Plants and Ecosystems -- I. Introduction -- II. Current Net Ecosystem Carbon Storage and Flux -- III. Effects of Global Change on Photosynthesis and Net Primary Productivity -- IV. Expected Effects of Global Change on Net Ecosystem Carbon Flux -- V. Summary and Conclusions -- References -- Chapter 8. Photosynthesis, Respiration, and Growth of Plants in the Soviet Arctic -- I. Introduction -- II. Photosynthesis -- III. Respiration and Growth -- IV. Summary and Conclusions -- References -- Chapter 9. Phenology, Resource Allocation, and Growth of Arctic Vascular Plants -- I. Introduction -- II. Phenology, Allocation, and Storage -- III. Growth Rates and Productivity -- IV. Conclusions -- V. Summary -- References -- Chapter 10. The Ecosystem Role of Poikilohydric Tundra Plants -- I. Introduction -- II. The Ecosystem Role of Mosses and Lichens -- III. Community Interactions and Poikilohydric Plants -- IV. Carbon Flows a s an Indicator of the Ecosystem Role of Poikilohydric Plants -- V. Summary -- Acknowledgments -- References -- Chapter 11. Arctic Tree Line in a Changing Climate -- I. Introduction -- II. Environmental Correlates of Tree Line -- III. Physiological Processes -- IV. Soil Processes -- V. Life History -- VI. Future Scenarios -- VII. Summary -- Acknowledgments -- References -- Part III: Water and Nutrient Balance -- Chapter 12. Water Relations of Arctic Vascular Plants -- I. The Importance of Water Stress -- II. Unique Aspects of the Arctic Environment -- III. Factors Influencing Plant Water Relations. , IV. Interactions between Water Relations and Whole-Plant Function -- V. Scaling Up from Leaf to Canopy Processes -- VI. Water Relations, Global Climate Change, and Ecosystem Processes -- VII. Arctic Plant Water Relations and the Biosphere -- VIII. Summary -- References -- Chapter 13. Microbial Processes and Plant Nutrient Availability in Arctic Soils -- I. Introduction -- II. Microbial and Soil Processes -- III. Soil Nitrogen and Phosphorus Cycling in a Warmer Arctic Climate -- IV. Summary -- Acknowledgments -- References -- Chapter 14. Nitrogen Fixation in Arctic Plant Communities -- I. Introduction -- II. Nitrogen Fixation Rates and Their Biological Importance in Arctic Ecosystems -- III. Environmental Controls -- IV. Climate Change, Nitrogen Fixation, and Arctic Ecosystem Processes -- V. Summary -- Acknowledgments -- References -- Chapter 15. Nutrient Absorption and Accumulation in Arctic Plants -- I. Introduction -- II. Response of Tundra Plants to the Environment -- III. Species and Growth-Form Differences -- IV. Uptake in the Field -- V. Role of Nutrient Uptake in Ecosystem Processes -- VI. Climate Change and Plant Nutrient Absorption -- VII. Summary -- References -- Chapter 16. Nutrient Use and Nutrient Cycling in Northern Ecosystems -- I. Introduction -- II. Storage and Recirculation of Nutrients or Additional Uptake? -- III. Nutrient Losses from the Plant -- IV. Impact of Dominant Plant Species on Nutrient Cycles -- V. Climate Change and Nutrient Cycles in Tundra Ecosystems -- VI. Summary -- Acknowledgments -- References -- Part IV: Interactions -- Chapter 17. Response of Tundra Plant Populations to Climatic Change -- I. Introduction -- II. Life Histories of Tundra Plants -- III. Demography at the Modular Level: Implications for Productivity -- IV. Demography at the Individual Level: Implications for Ecosystem Change. , V. Ecological Genetic Variation, Plasticity, and Ecosystem Change -- VI. Summary and Conclusions -- References -- Chapter 18. Controls over Secondary Metabolite Production by Arctic Woody Plants -- I. Introduction -- II. Environmental Controls of Secondary Metabolite Production -- III. Responses of Secondary Metabolite Production to Climate Change -- IV. Replacement of Tundra by Taiga -- V. Summary -- Acknowledgments -- References -- Chapter 19. Tundra Grazing Systems and Climatic Change -- I. Introduction -- II. Tundra Grazing Systems -- III. Comparisons among Tundra Grazing Systems -- IV. Tundra Grazing Systems and Climatic Change -- V. Summary -- Acknowledgments -- References -- Chapter 20. Modeling the Response of Arctic Plants to Changing Climate -- I. Introduction -- II. Scales and Types of Models -- III. Arctic Plant Growth Models -- IV. Critique of Models -- V. The Paradox of Model Complexity -- VI. A Strategy for Future Modeling -- VII. Summary -- Acknowledgments -- References -- Part V: Summary -- Chapter 21. Arctic Plant Physiological Ecology in an Ecosystem Context -- I. Ecophysiology of Individual Processes -- II. Physiological Ecology in an Ecosystem Context -- III. Physiological Ecology and Climate Change -- IV. Conclusion -- References -- Index.
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  • 3
    Publication Date: 2017-06-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2009. This is the author's version of the work. It is posted here by permission of Blackwell for personal use, not for redistribution. The definitive version was published in Ecology Letters 12 (2009): E15-E18, doi:10.1111/j.1461-0248.2009.01332.x.
    Description: Hartley et al. question whether reduction in Rmass, under experimental warming, arises because of the biomass method. We show the method they treat as independent yields the same result. We describe why the substrate-depletion hypothesis cannot alone explain observed responses, and urge caution in the interpretation of the seasonal data.
    Description: This research was supported by the Office of Science (BER), U.S. Department of Energy, the Andrew W. Mellon Foundation and U.S. National Science Foundation grants to the Coweeta LTER program.
    Keywords: Acclimation ; Adaptation ; Soil respiration ; Thermal biology ; Temperature ; Carbon cycling ; Climate change ; Climate warming ; Microbial community ; CO2
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here by permission of Blackwell for personal use, not for redistribution. The definitive version was published in Ecology Letters 11 (2008): 1316-1327, doi:10.1111/j.1461-0248.2008.01251.x.
    Description: In the short-term heterotrophic soil respiration is strongly and positively related to temperature. In the long-term its response to temperature is uncertain. One reason for this is because in field experiments increases in respiration due to warming are relatively short-lived. The explanations proposed for this ephemeral response include depletion of fast-cycling, soil carbon pools and thermal adaptation of microbial respiration. Using a 〉15 year soil warming experiment in a mid-latitude forest, we show that the apparent ‘acclimation’ of soil respiration at the ecosystem scale results from combined effects of reductions in soil carbon pools and microbial biomass, and thermal adaptation of microbial respiration. Mass specific respiration rates were lower when seasonal temperatures were higher, suggesting that rate reductions under experimental warming likely occurred through temperature-induced changes in the microbial community. Our results imply that stimulatory effects of global temperature rise on soil respiration rates may be lower than currently predicted.
    Description: This research was supported by the Office of Science (BER), U.S. Department of Energy and the Andrew W. Mellon Foundation.
    Keywords: Acclimation ; Adaptation ; Soil respiration ; Thermal biology ; Temperature ; Carbon cycling ; Climate change ; Climate warming ; Microbial community ; CO2
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 6
    Publication Date: 2022-05-26
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 11 (2016): 034014, doi:10.1088/1748-9326/11/3/034014.
    Description: As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased production of Arctic and boreal biomass; however, the lack of robust estimates of net carbon balance increases the risk of further overshooting international emissions targets. Precise empirical or model-based assessments of the critical factors driving carbon balance are unlikely in the near future, so to address this gap, we present estimates from 98 permafrost-region experts of the response of biomass, wildfire, and hydrologic carbon flux to climate change. Results suggest that contrary to model projections, total permafrost-region biomass could decrease due to water stress and disturbance, factors that are not adequately incorporated in current models. Assessments indicate that end-of-the-century organic carbon release from Arctic rivers and collapsing coastlines could increase by 75% while carbon loss via burning could increase four-fold. Experts identified water balance, shifts in vegetation community, and permafrost degradation as the key sources of uncertainty in predicting future system response. In combination with previous findings, results suggest the permafrost region will become a carbon source to the atmosphere by 2100 regardless of warming scenario but that 65%–85% of permafrost carbon release can still be avoided if human emissions are actively reduced.
    Description: This work was supported by the National Science Foundation ARCSS program and Vulnerability of Permafrost Carbon Research Coordination Network (grants OPP-0806465, OPP-0806394, and 955713) with additional funding from SITES (Swedish Science Foundation), Future Forest (Mistra), and a Marie Curie International Reintegration Grant (TOMCAR-Permafrost #277059) within the 7th European Community Framework Programme.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 7
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: We use a spatially explicit landscape model to investigate the potential role of rainfall on shrub–grass transitions in the Jornada Basin of southern New Mexico during the past century. In long-term simulations (1915–1998) along a 2700 m transect running from a dry lake bed to the foothills of a small mountain, we test two hypotheses: (i) that wetter winters and drier summers may have facilitated shrub encroachment in grasslands, and (ii) that increases in large precipitation events may have increased soil water recharge at deeper layers, thus favoring shrub establishment and growth. Our model simulations generally support the hypothesis that wetter winters and drier summers may have played a key role, but we are unable to reproduce the major shifts from grass- to shrub-domination that occurred in this landscape during the early part of the 1900s; furthermore, the positive shrub response to wetter winters and drier summers was only realized subsequent to the drought of 1951–1956, which was a relatively short ‘window of opportunity’ for increased shrub establishment and growth. Our simulations also generally support the hypothesis that an increase in the number of large precipitation events may also have favored shrub establishment and growth, although these results are equivocal, depending upon what constitutes a ‘large’ event and the timing of such events. We found complex interactions among (i) the amount/seasonality of rainfall, (ii) its redistribution in the landscape via run-on and runoff, (iii) the depth of the soil water recharge, and (iv) subsequent water availability for the growth and reproduction of shrubs vs. herbaceous plants at various landscape positions. Our results suggest that only a mechanistic understanding of these interactions, plus the role of domestic cattle grazing, will enable us to elucidate fully the relative importance of biotic vs. abiotic factors in vegetation dynamics in this semiarid landscape.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1432-1939
    Keywords: Key words Elevated CO2 ; Secondary compounds ; Carbon-nutrient balance ; Pinus taeda
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract We examined the extent to which carbon investment into secondary compounds in loblolly pine (Pinus taeda L.) is changed by the interactive effect of elevated CO2 and N availability and whether differences among treatments are the result of size-dependent changes. Seedlings were grown for 138 days at two CO2 partial pressures (35 and 70 Pa CO2) and four N solution concentrations (0.5, 1.5, 3.5, and 6.5 mmol l−1 NO3NH4) and concentrations of total phenolics and condensed tannins were determined four times during plant development in primary and fascicular needles, stems and lateral and tap roots. Concentrations of total phenolics in lateral roots and condensed tannins in tap roots were relatively high regardless of treatment. In the smallest seedlings secondary compound concentrations were relatively high and decreased in the initial growth phase. Thereafter condensed tannins accumulated strongly during plant maturation in all plant parts except in lateral roots, where concentrations did not change. Concentrations of total phenolics continued to decrease in lateral roots while they remained constant in all other plant parts. At the final harvest plants grown at elevated CO2 or low N availability showed increased concentrations of condensed tannins in aboveground parts. The CO2 effect, however, disappeared when size differences were adjusted for, indicating that CO2 only indirectly affected concentrations of condensed tannins through accelerating growth. Concentrations of total phenolics increased directly in response to low N availability and elevated CO2 in primary and fascicular needles and in lateral roots, which is consistent with predictions of the carbon-nutrient balance (CNB) hypothesis. The CNB hypothesis is also supported by the strong positive correlations between soluble sugar and total phenolics and between starch and condensed tannins. The results suggest that predictions of the CNB hypothesis could be improved if developmentally induced changes of secondary compounds were included.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1432-1939
    Keywords: Anaerobic ; Biomass partitioning ; Eriophorum ; Growth ; Nutrient stress
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract In arctic tundra soil, oxygen depletion associated with soil flooding may control plant growth either directly through anoxia or indirectly through effects on nutrient availability. This study was designed to evaluate whether plant growth and physiology of two arctic sedge species are more strongly controlled by the direct or indirect effects of decreased soil aeration. Eriophorum angustifolium and E. vaginatum, which originate from flooded and well-drained habitats, respectively, were grown in an in situ transplant garden at two levels of soil oxygen, nitrogen, and phosphorus availability over two growing seasons. In both species, N addition had a stronger effect on growth and biomass allocation than P addition or soil oxygen depletion. Net photosynthesis and carbohydrate concentrations were relatively insensitive to changes in these factors. Biomass reallocated from shoots to below-ground parts in response to limited N supply was equally divided between roots (nutrient acquisition) and perennating rhizomes (storage tissue formation) in E. angustifolium. E. Vaginatum only increased its allocation to rhizomes. In the flood-tolerant E. angustifolium, growth was improved by soil anoxia and biomass allocation among plant parts was not significantly affected. Contrary to our initial hypothesis, whole-plant growth in E. vaginatum improved in flooded soils; however, it only did so when N availability was high. Under low N availability growth in flooded soils was reduced by 20% compared to growth in the aerobic environment. Reduced biomass allocation to rhizomes and thus to storage potential under anaerobic conditions may reduce long-term survival of E. vaginatum in flooded habitats.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1432-1939
    Keywords: Canopy structure ; Coordination ; Nitrogen allocation ; Optimization ; Photosynthesis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract It has long been observed that leaf nitrogen concentrations decline with depth in closed canopies in a number of plant communities. This phenomenon is generally believed to be related to a changing radiation environment and it has been suggested by some researchers that plants allocate nitrogen in order to optimize total whole canopy photosynthesis. Although optimization theory has been successfully utilized to describe a variety of physiological and ecological phenomena, it has some shortcomings that are subject to criticism (e.g., time constraints, oversimplifications, lack of insights, etc.). In this paper we present an alternative to the optimization theory of plant canopy nitrogen distribution, which we term coordination theory. We hypothesize that plants allocate nitrogen to maintain a balance between two processes, each of which is dependent on leaf nitrogen content and each of which potentially limits photosynthesis. These two processes are defined as Wc, the Rubiscolimited rate of carboxylation, and Wj, the electron transport-limited rate of carboxylation. We suggest that plants allocate nitrogen differentially to, leaves in different canopy layers in such a way that Wc and Wj remain roughly balanced. In this scheme, the driving force for the allocation of nitrogen within a canopy is the difference between the leaf nitrogen content that is required to bring Wc and Wj into balance and the current nitrogen content. We show that the daily carbon assimilation of a canopy with a nitrogen distribution resulting from this internal coordination of Wc and Wj is very similar to that obtained using optimization theory.
    Type of Medium: Electronic Resource
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