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  • 1
    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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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 18 (1999), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Long-term field experiments at Abisko, Sweden, and Toolik Lake, Alaska, reveal both similarities and differences in response of contrasting Arctic ecosystems to changes in temperature, light, and nutrient availability. Five different ecosystems were manipulated for 5–15 years by increasing air temperature with greenhouses, by decreasing light with shading, and by increasing available N and P with fertilizers. The ecosystems at Abisko included evergreen-dominated heath and fellfield sites; at Toolik Lake they included wet sedge tundra, moist tussock tundra, and dry heath tundra. In all ecosystems, fertilizer treatment increased plant growth, production, and/or biomass. Plant responses to warming were smaller and occasionally nonsignificant, Responses to shading were generally nonsignificant after 3–6 years, although after 9 years the tussock tundra showed significant decreases in biomass. In general, the ecosystems at Abisko were less responsive to nutrients and more responsive to temperature than the ecosystems at Toolik Lake. Overall, though, the sites were quite similar in their responses to the perturbations, increasing our confidence in predictions of response to climate change over large areas based on small-area studies.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Ecologists have long been intrigued by the ways co-occurring species divide limiting resources. Such resource partitioning, or niche differentiation, may promote species diversity by reducing competition. Although resource partitioning is an important determinant of species diversity and ...
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Global warming is predicted to be most pronounced at high latitudes, and observational evidence over the past 25 years suggests that this warming is already under way. One-third of the global soil carbon pool is stored in northern latitudes, so there is considerable interest in understanding ...
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1432-1939
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The effects of fertilization on leaf longevity and leaf mortality in the Alaskan evergreen shrub, Ledum palustre (Ait.) Hult., were investigated in a field experiment. The fertilization treatments included N alone, P alone, N plus P, and N plus P plus K. After 5 years all treatments had the same effect on leaf longevity, decreasing life expectancy from about 2 years in controls to 1–1.5 years in the fertilized plants. In the NPK-fertilized plants, most of the decrease in leaf longevity was due to increased winter leaf mortality; fertilization actually decreased leaf losses during the growing season. The results are consistent with previous research suggesting that one function of overwintering evergreen leaves is to serve as nutrient storage organs, a function that is superfluous when nutrient supplies for new growth can be obtained from current uptake.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Oecologia 49 (1981), S. 362-365 
    ISSN: 1432-1939
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Effects of variable mineral nutrient status on evergreen leaf longevity were investigated in a field fertilization experiment, and by comparison of plants from several sites. The species studied was Ledum palustre spp. decumbens, with a normal leaf life expectancy of 2.06 years and a maximum leaf longevity of 4.5–5.0 years. Most leaf losses took place during the growing season, not during the winter. Fertilization increased leaf production but decreased leaf survivorship. Total number of leaves per stem was unchanged with fertilization. In a comparison among sites, there was a moderate negative correlation between plant N and P concentrations and leaf longevity. These intraspecific responses are similar to known interspecific changes along nutrient gradients, i.e. with high nutrient availability a vegetation should become more “deciduous” and less “evergreen”.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1435-0629
    Keywords: Key words: multiple-element limitation (MEL); biogeochemical model; climate change; plant competition; carbon–nitrogen interactions; nutrient use efficiency; relative growth rate; temperature; CO2.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: ABSTRACT Vegetation growth characteristics influence ecosystem biogeochemistry and must be incorporated in models used to project biogeochemical responses to climate variations. We used a multiple-element limitation model (MEL) to examine how variations in nutrient use efficiency (NUE) and net primary production to biomass ratio (nPBR) affect changes in ecosystem C stocks after an increase in temperature and atmospheric CO2. nPBR influences the initial rates of response, but the magnitude and direction of long-term responses are determined by NUE. MEL was used to simulate responses to climate change in communities composed of two species differing in nPBR and/or NUE. When only nPBR differed between the species, the high-nPBR species outgrew the low-nPBR species early in the simulations, but the shift in dominance was transitory because of secondary N limitations. High-NUE species were less affected by secondary N limitations and were therefore favored under elevated CO2. Increased temperature stimulated N release from soil organic matter (SOM) and therefore favored low-NUE species. The combined release from C and N limitation under the combination of increased temperature and elevated CO2 favored high-NUE species. High C:N litter from high-NUE species limited the N-supply rate from SOM, which favors the dominance of the high-NUE species in the short term. However, in the long term increased litter production resulted in SOM accumulation, which reestablished a N supply rate favorable to the reestablishment and dominance of the low-NUE species. Conditions then reverted to a state favorable to the high-NUE species.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2015-01-23
    Description: Fire frequency has dramatically increased in the tundra of northern Alaska, which has major implications for the carbon budget of the region and the functioning of these ecosystems that support important wildlife species. We investigated the post-fire succession of plant and soil carbon (C), nitrogen (N), and phosphorus (P) fluxes and stocks along a burn severity gradient in the 2007 Anaktuvuk River Fire scar in northern Alaska. Modeling results indicated that the early regrowth of post-fire tundra vegetation was limited primarily by its canopy photosynthetic potential, rather than nutrient availability, because of the initially low leaf area and relatively high inorganic N and P concentrations in soil. Our simulations indicated that the post-fire recovery of tundra vegetation was sustained predominantly by the uptake of residual inorganic N (i.e. in the remaining ash), and the redistribution of N and P from soil organic matter to vegetation. Although residual nutrients in ash were higher in the severe burn than the moderate burn, the moderate burn recovered faster because of the higher remaining biomass and consequent photosynthetic potential. Residual nutrients in ash allowed both burn sites to recover and exceed the unburned site in both aboveground biomass and production five years after the fire. The investigation of interactions among post-fire C, N, and P cycles has contributed to a mechanistic understanding of the response of tundra ecosystems to fire disturbance. Our study provided insight on how the trajectory of recovery of tundra from wildfire is regulated during early succession. # doi:10.1890/14-1921.1
    Print ISSN: 1051-0761
    Electronic ISSN: 1939-5582
    Topics: Biology
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  • 9
    Publication Date: 2017-01-05
    Description: Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by permission of Blackwell Publishing for personal use, not for redistribution. The definitive version was published in Journal of Ecology 93 (2005): 770-782, doi:10.1111/j.1365-2745.2005.01006.x.
    Description: In the northern foothills of the Brooks Range, Alaska, moist non-acidic tundra dominates more recently deglaciated upland landscapes, whereas moist acidic tundra dominates older upland landscapes. In previous studies, experimental fertilization of moist acidic tussock tundra greatly increased the abundance and productivity of the deciduous dwarf shrub Betula nana. However, this species is largely absent from moist non-acidic tundra. These two common upland tundra community types exhibited markedly different responses to fertilization with nitrogen and phosphorus. In moist acidic tundra, cover of deciduous shrubs (primarily B. nana) increased after only 2 years, and by 4 years vascular biomass and above-ground net primary productivity (ANPP) had increased significantly, almost entirely because of Betula. In moist non-acidic tundra, both biomass and ANPP were again significantly greater, but no single species dominated the response to fertilization. Instead, the effect was due to a combination of several small, sometimes statistically non-significant responses by forbs, graminoids and prostrate deciduous shrubs. The different growth form and species' responses suggest that fertilization will cause carbon cycling through plant biomass to diverge in these two tundra ecosystems. Already, production of new stems by apical growth has increased relative to leaf production in acidic tundra, whereas the opposite has occurred in non-acidic tundra. Secondary stem growth has also increased as a component of primary production in acidic tundra, but is unchanged in non-acidic tundra. Thus, fertilization will probably increase carbon sequestration in woody biomass of B. nana in acidic tundra, while increasing carbon turnover (but not storage) of non-woody species in non-acidic tundra. These results indicate that nutrient enrichment can have very different consequences for plant communities that occur on different geological substrates, because of differences in composition, even though they share the same regional species pool. Although the specific edaphic factors that maintain compositional differences in this case are unknown, variation in soil pH and related variability in soil nutrient availability may well play a role.
    Description: This research was supported by a collaborative grant from the National Science Foundation (OPP-9902695 to S.E.H. and OPP-9902721 to L.G.) and by the Arctic LTER (DEB-9810222).
    Keywords: Alaska ; Arctic ; Betula nana ; Fertilization ; Moist acidic tundra ; Moist non-acidic tundra ; Net primary production ; Nitrogen ; pH ; Phosphorus
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
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  • 10
    Publication Date: 2022-05-25
    Description: Author's draft titled: Carbon sequestration in terrestrial ecosystems under elevated CO2 and temperature : role of dissolved organic versus inorganic nitrogen loss
    Description: Author Posting. © The Authors, 2004. This is the author's version of the work. It is posted here by permission of Ecological Society of America for personal use, not for redistribution. The definitive version was published in Ecological Applications 15 (2005): 71–86, doi:10.1890/03-5303
    Description: We used a simple model of carbon–nitrogen (C–N) interactions in terrestrial ecosystems to examine the responses to elevated CO2 and to elevated CO2 plus warming in ecosystems that had the same total nitrogen loss but that differed in the ratio of dissolved organic nitrogen (DON) to dissolved inorganic nitrogen (DIN) loss. We postulate that DIN losses can be curtailed by higher N demand in response to elevated CO2, but that DON losses cannot. We also examined simulations in which DON losses were held constant, were proportional to the amount of soil organic matter, were proportional to the soil C:N ratio, or were proportional to the rate of decomposition. We found that the mode of N loss made little difference to the short-term (〈60 years) rate of carbon sequestration by the ecosystem, but high DON losses resulted in much lower carbon sequestration in the long term than did low DON losses. In the short term, C sequestration was fueled by an internal redistribution of N from soils to vegetation and by increases in the C:N ratio of soils and vegetation. This sequestration was about three times larger with elevated CO2 and warming than with elevated CO2 alone. After year 60, C sequestration was fueled by a net accumulation of N in the ecosystem, and the rate of sequestration was about the same with elevated CO2 and warming as with elevated CO2 alone. With high DON losses, the ecosystem either sequestered C slowly after year 60 (when DON losses were constant or proportional to soil organic matter) or lost C (when DON losses were proportional to the soil C:N ratio or to decomposition). We conclude that changes in long-term C sequestration depend not only on the magnitude of N losses, but also on the form of those losses.
    Description: This work was funded, in part, by the National Science Foundation (DEB 0108960 and DEB 0089585) and in part by the USGS Global Change Research Program.
    Keywords: Carbon–nitrogen interactions ; Carbon sequestration ; Dissolved inorganic nitrogen ; Dissolved organic nitrogen ; Ecosystem models ; Global climate change ; Carbon–nitrogen interactions ; Terrestrial ecosystems
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
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