Nature, ISSN 0028-0836, 06/2012, Volume 486, Issue 7401, pp. 52 - 58
Localized ecological systems are known to shift abruptly and irreversibly from one state to another when they are forced across critical thresholds. Here we...
BIODIVERSITY | TRANSFORMATION | LATE-QUATERNARY VEGETATION | REGIME SHIFTS | EARLY-WARNING SIGNALS | MULTIDISCIPLINARY SCIENCES | HUMAN APPROPRIATION | CLIMATE-CHANGE | INTERACTION STRENGTH | EXTINCTION | DIVERSITY LOSS | Models, Theoretical | Environmental Monitoring | Animals | Ecosystem | Humans | Human Activities | Earth (Planet) | Forecasting | Climate Change - statistics & numerical data | Earth | Environmental aspects | Biosphere | Observations | Analysis | Power marketers | Lawn & garden services | Outsourcing | Budgets | State employees
BIODIVERSITY | TRANSFORMATION | LATE-QUATERNARY VEGETATION | REGIME SHIFTS | EARLY-WARNING SIGNALS | MULTIDISCIPLINARY SCIENCES | HUMAN APPROPRIATION | CLIMATE-CHANGE | INTERACTION STRENGTH | EXTINCTION | DIVERSITY LOSS | Models, Theoretical | Environmental Monitoring | Animals | Ecosystem | Humans | Human Activities | Earth (Planet) | Forecasting | Climate Change - statistics & numerical data | Earth | Environmental aspects | Biosphere | Observations | Analysis | Power marketers | Lawn & garden services | Outsourcing | Budgets | State employees
Journal Article
Ecology Letters, ISSN 1461-023X, 04/2011, Volume 14, Issue 4, pp. 373 - 379
Ecology Letters (2011) 14: 373–379 Global vegetation models predict that boreal forests are particularly sensitive to a biome shift during the 21st century....
global warming | productivity | drought | Boreal forests | high latitudes | remote sensing | NDVI | evergreen forests | tree rings | Productivity | Tree rings | Evergreen forests | High latitudes | Global warming | Drought | Remote sensing | FIRE DISTURBANCE | CARBON | NORTHERN ALASKA | TREE GROWTH | BOREAL FOREST | CLIMATE-CHANGE | SATELLITE DATA | INTERIOR ALASKA | ECOLOGY | ECOSYSTEMS | VEGETATION | Climate Change | Droughts | Picea - growth & development | Ecosystem | History, 20th Century | Alaska | Trees - growth & development | Biomes | Dendroclimatology | Industrial productivity | Analysis | Humanities and Social Sciences | Archaeology and Prehistory
global warming | productivity | drought | Boreal forests | high latitudes | remote sensing | NDVI | evergreen forests | tree rings | Productivity | Tree rings | Evergreen forests | High latitudes | Global warming | Drought | Remote sensing | FIRE DISTURBANCE | CARBON | NORTHERN ALASKA | TREE GROWTH | BOREAL FOREST | CLIMATE-CHANGE | SATELLITE DATA | INTERIOR ALASKA | ECOLOGY | ECOSYSTEMS | VEGETATION | Climate Change | Droughts | Picea - growth & development | Ecosystem | History, 20th Century | Alaska | Trees - growth & development | Biomes | Dendroclimatology | Industrial productivity | Analysis | Humanities and Social Sciences | Archaeology and Prehistory
Journal Article
Ecosphere, ISSN 2150-8925, 08/2016, Volume 7, Issue 8, pp. e01410 - n/a
Forests near the lower limit of montane tree cover are expected to be particularly vulnerable to warming climate, potentially converting to non‐forest for...
lower‐montane forest | Rocky Mountains | ecotone | wildfire | Douglas‐fir | Greater Yellowstone Ecosystem | treeline | Pseudotsuga menziesii | climate change | UNITED-STATES | NATIONAL-PARK | BOREAL FOREST | lower-montane forest | CLIMATE-CHANGE | Douglas-fir | CONIFER REGENERATION | SUB-ALPINE FORESTS | GREATER YELLOWSTONE | SOUTHWESTERN MONTANA | ECOLOGY | LANDSCAPE PATTERNS | Wildfires | Forests | Biogeography | Forest & brush fires | Forest ecosystems | Forest fires | National parks | 21st century | Climate change | Hypotheses | Vegetation cover | Treeline | Vegetation | Montane environments | Parks & recreation areas
lower‐montane forest | Rocky Mountains | ecotone | wildfire | Douglas‐fir | Greater Yellowstone Ecosystem | treeline | Pseudotsuga menziesii | climate change | UNITED-STATES | NATIONAL-PARK | BOREAL FOREST | lower-montane forest | CLIMATE-CHANGE | Douglas-fir | CONIFER REGENERATION | SUB-ALPINE FORESTS | GREATER YELLOWSTONE | SOUTHWESTERN MONTANA | ECOLOGY | LANDSCAPE PATTERNS | Wildfires | Forests | Biogeography | Forest & brush fires | Forest ecosystems | Forest fires | National parks | 21st century | Climate change | Hypotheses | Vegetation cover | Treeline | Vegetation | Montane environments | Parks & recreation areas
Journal Article
Nature, ISSN 0028-0836, 2001, Volume 413, Issue 6856, pp. 591 - 596
All ecosystems are exposed to gradual changes in climate, nutrient loading, habitat fragmentation or biotic exploitation. Nature is usually assumed to respond...
Leerstoelgroep Aquatische ecologie en waterkwaliteitsbeheer | Aquatic Ecology and Water Quality Management | Aquatische Ecologie en Waterkwaliteitsbeheer | WIMEK | GRAZING SYSTEMS | SAHEL | PHASE-SHIFTS | MANAGEMENT | MULTIDISCIPLINARY SCIENCES | MULTIPLE STABLE STATES | DYNAMICS | ARABIAN PENINSULA | SHALLOW LAKES | VEGETATION | CLIMATE | Trees | Oceans and Seas | Animals | Stochastic Processes | Models, Biological | Ecosystem | Cnidaria | Conservation of Natural Resources | Fresh Water | Desert Climate | Changes | Climate change | Ecosystems | Habitats
Leerstoelgroep Aquatische ecologie en waterkwaliteitsbeheer | Aquatic Ecology and Water Quality Management | Aquatische Ecologie en Waterkwaliteitsbeheer | WIMEK | GRAZING SYSTEMS | SAHEL | PHASE-SHIFTS | MANAGEMENT | MULTIDISCIPLINARY SCIENCES | MULTIPLE STABLE STATES | DYNAMICS | ARABIAN PENINSULA | SHALLOW LAKES | VEGETATION | CLIMATE | Trees | Oceans and Seas | Animals | Stochastic Processes | Models, Biological | Ecosystem | Cnidaria | Conservation of Natural Resources | Fresh Water | Desert Climate | Changes | Climate change | Ecosystems | Habitats
Journal Article
Science, ISSN 0036-8075, 6/2008, Volume 320, Issue 5884, pp. 1768 - 1771
Spatial fingerprints of climate change on biotic communities are usually associated with changes in the distribution of species at their latitudinal or...
Climate change | Population ecology | Marine ecology | Mountain forests | Reports | Climate models | Ecology | Global warming | Plants | Species | Topographical elevation | UPHILL SHIFTS | FINGERPRINTS | RESPONSES | MARGIN | ALPINE PLANTS | MULTIDISCIPLINARY SCIENCES | EXTENT | BUTTERFLIES | CLIMATE-CHANGE | GLOBAL CHANGE | RANGE | Geography | Trees | Climate | Temperature | Plant Development | Time Factors | Ecosystem | Europe | Environment | Biodiversity | Altitude | Environmental aspects | Altitudes | Forest flora | Research | Vegetation and climate | Distribution | Biogeography | Forests | Botany | Life Sciences | Cellular Biology
Climate change | Population ecology | Marine ecology | Mountain forests | Reports | Climate models | Ecology | Global warming | Plants | Species | Topographical elevation | UPHILL SHIFTS | FINGERPRINTS | RESPONSES | MARGIN | ALPINE PLANTS | MULTIDISCIPLINARY SCIENCES | EXTENT | BUTTERFLIES | CLIMATE-CHANGE | GLOBAL CHANGE | RANGE | Geography | Trees | Climate | Temperature | Plant Development | Time Factors | Ecosystem | Europe | Environment | Biodiversity | Altitude | Environmental aspects | Altitudes | Forest flora | Research | Vegetation and climate | Distribution | Biogeography | Forests | Botany | Life Sciences | Cellular Biology
Journal Article
Quaternary Science Reviews, ISSN 0277-3791, 10/2015, Volume 125, pp. 117 - 130
Late Quaternary climate variability in the southern African subtropics is still only poorly resolved, with significant complexity and apparent contradictions...
ITCZ | Insolation forcing | Quaternary | Climate reconstruction | Southern Africa | Pollen | Palaeoclimatology | Holocene | East Africa | LATE QUATERNARY | PAST 25,000 YEARS | SAVANNA BIOME | GEOGRAPHY, PHYSICAL | GEOSCIENCES, MULTIDISCIPLINARY | HIGH-RESOLUTION | ROCK HYRAX MIDDENS | HOLOCENE CLIMATE-CHANGE | WINTER RAINFALL ZONE | VEGETATION DYNAMICS | LATE PLEISTOCENE | EARTHS ORBITAL PARAMETERS | Interglacial periods | Climate | Precipitation variability | Rain and rainfall | Environmental Sciences | Global Changes
ITCZ | Insolation forcing | Quaternary | Climate reconstruction | Southern Africa | Pollen | Palaeoclimatology | Holocene | East Africa | LATE QUATERNARY | PAST 25,000 YEARS | SAVANNA BIOME | GEOGRAPHY, PHYSICAL | GEOSCIENCES, MULTIDISCIPLINARY | HIGH-RESOLUTION | ROCK HYRAX MIDDENS | HOLOCENE CLIMATE-CHANGE | WINTER RAINFALL ZONE | VEGETATION DYNAMICS | LATE PLEISTOCENE | EARTHS ORBITAL PARAMETERS | Interglacial periods | Climate | Precipitation variability | Rain and rainfall | Environmental Sciences | Global Changes
Journal Article
Functional Ecology, ISSN 0269-8463, 04/2018, Volume 32, Issue 8, pp. 1959 - 1971
1. Herbivory can drive vegetation into different states of productivity and community composition, and these changes may be stable over time due to historical...
Global environmental change | Eco-evolutionary dynamics | international | alternative state, herbivory, historical contingency, legacy effects, plant–soil feedback, Rangifer tarandus, reindeer husbandry, vegetation composition | historical contingency | legacy effects | vegetation composition | Rangifer tarandus | reindeer husbandry | herbivory | plant–soil feedback | alternative state | METAANALYSIS | ARBUSCULAR MYCORRHIZAL FUNGI | GRASSLAND | DEFOLIATION | COMMUNITIES | ECOSYSTEM PROCESSES | COEXISTENCE | PRODUCTIVITY | ECOLOGY | plant-soil feedback | Caribou | Reindeer | Ecosystem components | Communities | Radiation | Positive feedback | Contingency | Soil conditions | Feedback | Milking | Nutrients | Species | Community composition | Plants (botany) | Landscape | Plant communities | Herbivory | Nitrogen | Plant populations | Soils | Soil stabilization | Plant growth | Vegetation | Vegetation changes | Nutrient availability | Herbivores | Herding | Tundra | Biological Sciences | Ecology | Naturvetenskap | Biologiska vetenskaper | lternative state | Rangifer randus | Natural Sciences | Ekologi
Global environmental change | Eco-evolutionary dynamics | international | alternative state, herbivory, historical contingency, legacy effects, plant–soil feedback, Rangifer tarandus, reindeer husbandry, vegetation composition | historical contingency | legacy effects | vegetation composition | Rangifer tarandus | reindeer husbandry | herbivory | plant–soil feedback | alternative state | METAANALYSIS | ARBUSCULAR MYCORRHIZAL FUNGI | GRASSLAND | DEFOLIATION | COMMUNITIES | ECOSYSTEM PROCESSES | COEXISTENCE | PRODUCTIVITY | ECOLOGY | plant-soil feedback | Caribou | Reindeer | Ecosystem components | Communities | Radiation | Positive feedback | Contingency | Soil conditions | Feedback | Milking | Nutrients | Species | Community composition | Plants (botany) | Landscape | Plant communities | Herbivory | Nitrogen | Plant populations | Soils | Soil stabilization | Plant growth | Vegetation | Vegetation changes | Nutrient availability | Herbivores | Herding | Tundra | Biological Sciences | Ecology | Naturvetenskap | Biologiska vetenskaper | lternative state | Rangifer randus | Natural Sciences | Ekologi
Journal Article
Proceedings of the National Academy of Sciences of the United States of America, ISSN 0027-8424, 2/2015, Volume 112, Issue 5, pp. 1458 - 1463
We document changes in forest structure between historical (1930s) and contemporary (2000s) surveys of California vegetation through comparisons of tree...
Climatic water deficit | Forest | Historical ecology | Global change | VEGETATION MORTALITY | climatic water deficit | forest | WESTERN UNITED-STATES | MULTIDISCIPLINARY SCIENCES | SPECIES OPTIMUM ELEVATIONS | CLIMATE-CHANGE | WATER-BALANCE | YOSEMITE-NATIONAL-PARK | SEVERE DROUGHT | historical ecology | global change | SIERRA-NEVADA | MIXED-CONIFER FORESTS | DRIVE DOWNHILL SHIFTS | Forests | Biomass | California | History, 21st Century | Biodiversity | History, 20th Century | Observations | Forest dynamics | Biological Sciences
Climatic water deficit | Forest | Historical ecology | Global change | VEGETATION MORTALITY | climatic water deficit | forest | WESTERN UNITED-STATES | MULTIDISCIPLINARY SCIENCES | SPECIES OPTIMUM ELEVATIONS | CLIMATE-CHANGE | WATER-BALANCE | YOSEMITE-NATIONAL-PARK | SEVERE DROUGHT | historical ecology | global change | SIERRA-NEVADA | MIXED-CONIFER FORESTS | DRIVE DOWNHILL SHIFTS | Forests | Biomass | California | History, 21st Century | Biodiversity | History, 20th Century | Observations | Forest dynamics | Biological Sciences
Journal Article
Ecology, ISSN 0012-9658, 09/2014, Volume 95, Issue 9, pp. 2504 - 2513
We test the validity of applying the alternative stable state paradigm to account for the landscape-scale forest/non-forest mosaic that prevails in temperate...
forest | paleoecology | regime shift | Tasmania | fire | non-forest | alternative stable states | Australia | hysteresis | Moorlands | Taxa | Marine ecology | Vegetation | Temperate rain forests | Forest ecology | Pollen | Wetland ecology | Forest hydrology | Forest fires | Alternative stable states | Fire | Forest | Regime shift | Non-forest | Paleoecology | Hysteresis | SOUTHWEST TASMANIA | MOORLAND | REGIMES | POLLEN-VEGETATION RELATIONSHIPS | ORGANIC SOILS | COMMUNITY | ECOLOGY | SCALE | IMPACTS | ECOSYSTEMS | Vegetation zones | Research | Fires
forest | paleoecology | regime shift | Tasmania | fire | non-forest | alternative stable states | Australia | hysteresis | Moorlands | Taxa | Marine ecology | Vegetation | Temperate rain forests | Forest ecology | Pollen | Wetland ecology | Forest hydrology | Forest fires | Alternative stable states | Fire | Forest | Regime shift | Non-forest | Paleoecology | Hysteresis | SOUTHWEST TASMANIA | MOORLAND | REGIMES | POLLEN-VEGETATION RELATIONSHIPS | ORGANIC SOILS | COMMUNITY | ECOLOGY | SCALE | IMPACTS | ECOSYSTEMS | Vegetation zones | Research | Fires
Journal Article