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  • Ecology-Handbooks, manuals, etc.  (1)
  • belowground respiration  (1)
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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Ecology-Handbooks, manuals, etc. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (365 pages)
    Edition: 1st ed.
    ISBN: 9783030713300
    Series Statement: Ecological Studies ; v.241
    DDC: 577.27
    Language: English
    Note: Intro -- Preface -- Contents -- 1: Ecosystem Collapse and Climate Change: An Introduction -- 1.1 Introduction -- 1.2 Defining Ecosystems Collapse -- 1.3 Observed Dynamics as They Occur -- 1.3.1 Polar and Boreal Ecosystems -- 1.3.2 Temperate and Semi-arid Ecosystems -- 1.3.3 Tropical and Temperate Coastal Ecosystems -- References -- Part I: Polar and Boreal Ecosystems -- 2: Ecosystem Collapse on a Sub-Antarctic Island -- 2.1 Background -- 2.2 The Collapse -- 2.2.1 Former State -- 2.2.2 Progression to the New State -- 2.2.3 Functional Changes -- 2.2.4 Context of the Change -- 2.3 Major Causes -- 2.4 Prognosis and Management Strategies -- 2.5 Wider Context -- References -- 3: Permafrost Thaw in Northern Peatlands: Rapid Changes in Ecosystem and Landscape Functions -- 3.1 Introduction -- 3.2 Current Distribution and Characteristics of Peatlands in the Northern Permafrost Region -- 3.2.1 Current Peatland Distribution and Major Regions -- 3.2.2 Peatland Characteristics Across Permafrost Zones -- 3.2.2.1 Peatlands in the Continuous Permafrost Zone -- 3.2.2.2 Peatlands in the Discontinuous Permafrost Zone -- 3.2.2.3 Peatlands in the Sporadic Permafrost Zone -- 3.3 Holocene Development of Peatlands in the Northern Permafrost Region -- 3.3.1 Timing and Mode of Peatland Initiation -- 3.3.2 Timing and Processes of Permafrost Aggradation -- 3.3.3 Holocene Carbon Accumulation in Permafrost Peatlands -- 3.4 Observed Peatland Change Associated with Permafrost Thaw -- 3.4.1 Peatland Change in the Continuous Permafrost Zone -- 3.4.2 Peatland Change in the Discontinuous and Sporadic Permafrost Zones -- 3.5 Implications of Permafrost Thaw -- 3.5.1 Hydrology and Water Quality -- 3.5.2 Ecology and Human Use -- 3.5.3 Carbon Cycling and Greenhouse Gas Exchange -- 3.5.4 Interactions Between Wildfire, Permafrost Thaw, and Peatland Carbon Balance -- 3.6 Conclusions. , References -- 4: Post-fire Recruitment Failure as a Driver of Forest to Non-forest Ecosystem Shifts in Boreal Regions -- 4.1 Introduction -- 4.2 Role of Fire in Boreal Forests -- 4.2.1 Post-fire Recruitment Dynamics -- 4.2.2 Post-fire Recruitment Failure -- 4.2.3 A Case Study of Post-fire Recruitment Failure in Southern Siberia -- 4.3 Drivers of Change in the Boreal Forest Zone -- 4.3.1 Climate Change -- 4.3.1.1 Climate Change and Increases in the Fire Regime -- 4.3.1.2 Climate Change and Decreased Ecosystem Resilience -- 4.3.2 Management and Human Influence -- 4.3.2.1 Forest Management and the Fire Regime -- 4.4 Measuring the Scale of the Problem -- 4.4.1 Disturbance Detection -- 4.4.2 Large-Scale Trends in Vegetation -- 4.4.3 Detecting Post-fire Recruitment Failure -- 4.4.4 Post-fire Recruitment Failure and the Prediction of Future Climate -- 4.5 Future Management -- References -- 5: A Paleo-perspective on Ecosystem Collapse in Boreal North America -- 5.1 Introduction -- 5.2 Ecosystem Collapse During the Late Pleistocene -- 5.2.1 Abrupt Climatic Changes -- 5.2.2 Human Disturbance -- 5.3 Ecosystem Building During Early- to Mid-Holocene -- 5.3.1 Creation of the Boreal Forest Environment -- 5.3.2 Peatland Expansion -- 5.3.3 Southern Conifer Forest and Insects -- 5.4 Ecosystem Collapse After the Mid-Holocene -- 5.4.1 Ecosystem Collapse in the Northern Part of the Boreal Forest -- 5.4.1.1 Climate-Fire Interactions -- 5.4.1.2 Collateral Effects of Forest Collapse -- 5.4.1.3 Extensive Collapse of Woodlands During the Little Ice Age -- 5.4.1.4 Wetland Ecosystem Collapse -- 5.4.1.5 Changing Water Levels of Subarctic Lakes and Rivers -- 5.4.2 Ecosystem Collapse in the Southern Part of the Boreal Forest -- 5.4.2.1 Shift of Closed-Crown Forests to Woodlands -- 5.4.2.2 Microclimatic Signatures of Closed-Crown Forests and Woodlands. , 5.5 Present Post-Little Ice Age Warming and Ecosystem Collapse and Recovery -- 5.5.1 Tree Line Advance, Regeneration and Consolidation of Pre-existing Forests of the Forest-Tundra Ecotone -- 5.5.2 Shrubification of the Northern Part of the Boreal Biome -- 5.5.3 Collapse and Recovery of Wetland and Riparian Ecosystems -- 5.6 Lessons Learned from the Past to Anticipate the Future -- References -- Part II: Temperate and Semi-arid Ecosystems -- 6: The 2016 Tasmanian Wilderness Fires: Fire Regime Shifts and Climate Change in a Gondwanan Biogeographic Refugium -- 6.1 Introduction -- 6.2 The 2016 Wilderness Fires -- 6.2.1 2016 Fire Impacts on A. cupressoides Populations -- 6.3 Persistence of A. cupressoides Under Climate Change -- 6.4 Broader Ecological Impacts -- 6.5 Anthropocene Management Responses -- 6.6 Conclusions -- References -- 7: Climate-Induced Global Forest Shifts due to Heatwave-Drought -- 7.1 Overview of Forest Mortality Episodes at the Global Scale -- 7.2 Causes of Forest Mortality by Drought -- 7.3 Historical Perspective of Forest Shifts -- 7.4 Abrupt Forest Mortality Events and Ecosystem Trajectory -- 7.4.1 General Trends -- 7.4.2 Cases of Forest Collapse and Its Relation with Management -- 7.5 Enhancing Resilience -- 7.5.1 Water Demand Strategy -- 7.5.2 Population and Biodiversity-Based Strategies -- 7.5.3 Disturbance Regime-Based Strategy: Wildfires -- 7.6 Future Prognosis of Forest Collapse -- 7.7 Conclusion -- References -- 8: Extreme Events Trigger Terrestrial and Marine Ecosystem Collapses in the Southwestern USA and Southwestern Australia -- 8.1 Introduction -- 8.1.1 Progressively Intense Ecological Stresses: From Drought to Warming to Heatwaves -- 8.1.2 Legacy Effects, Disturbance Interactions, and Order of Events -- 8.1.3 Ecosystem Collapses in Southwestern Australia and the USA -- 8.2 Southwestern USA Case Study. , 8.2.1 Terrestrial Drivers and Ecosystem Responses in the Southwestern USA -- 8.2.2 Marine Drivers and Ecosystem Responses in Southwestern USA -- 8.3 Southwestern Australian Case Study -- 8.3.1 Terrestrial Drivers and Ecosystem Responses in Southwestern Australia -- 8.3.2 Marine Drivers and Ecosystem Responses in Southwestern Australia -- 8.4 Ecological Implications -- 8.4.1 Prognosis for the Future -- 8.5 Managing Ecosystem Collapse and Future Research -- References -- Part III: Tropical and Temperate Coastal Ecosystems -- 9: Processes and Factors Driving Change in Mangrove Forests: An Evaluation Based on the Mass Dieback Event in Australia´s Gulf... -- 9.1 Introduction -- 9.2 Dynamic Processes Influencing Tidal Wetlands and Mangroves -- 9.2.1 Level 1: Global Setting of Tidal Wetlands: Site Geomorphology, Sea Level and Climate -- 9.2.2 Level 2: Composition of Dominant Vegetation Types of Tidal Wetlands: Regional Influences of Temperature and Rainfall -- 9.2.3 Level 3: Sustainable Turnover and Replenishment of Mangrove Forests: Small-Scale, Natural Disturbance Driving Forest Re-... -- 9.2.4 Level 4: Severe Drivers of Change and Replacement of Tidal Wetland Habitat: Large-Scale Disturbance-Recovery Dynamics In... -- 9.3 Climate and Natural Drivers of Key Environmental Changes Along Mangrove Shorelines -- 9.3.1 Shoreline Erosion and Seafront Retreat: Severe Storms, Sea Level Rise -- 9.3.2 Estuarine Bank Erosion: Flood Events, Sea Level Rise -- 9.3.3 Terrestrial Retreat: Upland Erosion, Sea Level Rise -- 9.3.4 Saltpan Scouring: Pan Erosion, Sea Level Rise -- 9.3.5 Depositional Gain: Flood Events, Sea Level Rise -- 9.3.6 Severe Storm Damage: Mangrove Dieback, Cyclonic Winds, Large Waves -- 9.3.7 Light Gaps: Lightning Strikes, Herbivore Attacks, Mini Tornados. , 9.3.8 Zonal Retreat: Local-Scale Patterns of Single, Dual and Triple Zones of Concurrent Upper Zone Dieback -- 9.4 The Synchronous, Large-Scale Mass Dieback of Mangroves in Australia´s Remote Gulf of Carpentaria -- Box. Mangrove Diversity in the Area of Mass Dieback of Mangroves -- 9.4.1 Likely Causal Factors Observed Along the Impacted Shoreline -- 9.4.2 Linking Specific Factors with the Dieback Event -- 9.4.3 Did Human-Induced Climate Change Play a Role in the 2015-2016 Dieback of Mangroves? -- 9.5 Current Recommendations for Management Strategies -- 9.6 A Regional Mitigation and Monitoring Strategy for Tidal Wetlands -- 9.7 Vulnerability of Impacted Shorelines with Key Risks and Consequences -- References -- 10: Recurrent Mass-Bleaching and the Potential for Ecosystem Collapse on Australia´s Great Barrier Reef -- 10.1 Introduction -- 10.2 Considering the Criteria for Collapse of Coral Reefs -- 10.3 Background Trends on the Great Barrier Reef -- 10.4 Climate Change and Mass Coral Bleaching -- 10.5 Is the Great Barrier Reef Collapsing? -- 10.6 Recasting Conservation Goals for Coral Reefs -- References -- 11: Sliding Toward the Collapse of Mediterranean Coastal Marine Rocky Ecosystems -- 11.1 Introduction -- 11.2 Marine Heatwaves and Mass Mortality Events in the Mediterranean -- 11.2.1 Sea Surface Thermal Stress Signals in the Cold Northern Mediterranean Areas -- 11.2.2 Subsurface Thermal Stress Signals in the Cold NW Mediterranean -- 11.2.2.1 Subsurface MHWs Amplification -- 11.3 Immediate Impacts, Sublethal Effects, and Recovery of Habitat-Forming Gorgonians from Mass Mortalities Events -- 11.3.1 Immediate Impacts and Sublethal Effects of Mass Mortality Events -- 11.3.1.1 Immediate Impacts -- 11.3.1.2 Sublethal Effects with Long-Term Consequences -- 11.3.2 Recovery Trajectories. , Box 11.1 Description of Demographic and Genetic Features of Octocorals.
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  • 2
    ISSN: 1573-5036
    Keywords: belowground respiration ; ecosystem carbon balance ; enhanced atmospheric [CO2] ; root symbionts ; root turnover ; soil carbon accumulation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract We undertake a synthesis of the most relevant results from the presentations at the meeting “Plant-Soil Carbon Below-Ground: The Effects of Elevated CO2” (Oxford-UK, September 1995), many of which are published in this Special Issue. Below-ground responses to elevated [CO2] are important because the capacity of soils for long-term carbon sequestration. We draw the following conclusions: (i) several ecosystems exposed to elevated [CO2] showed sustained increased CO2 uptake at the plot level for many years. A few systems, however, showed complete down-regulation of net CO2 uptake after several years of elevated [CO2] exposure; (ii) under elevated [CO2], a greater proportion of fixed carbon is generally allocated below-ground, potentially increasing the capacity of below-ground sinks; and (iii) some of the increased capacity of these sinks may lead to increased long-term soil carbon sequestration, although strong evidence is still lacking. We highlight the need for more soil studies to be undertaken within ongoing ecosystem-level experiments, and suggest that while some key experiments already established should be maintained to allow long term effects and feedbacks to take place, more research effort should be directed to mechanisms of soil organic matter stabilization.
    Type of Medium: Electronic Resource
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