Long-term warming restructures Arctic tundra without changing net soil carbon storage.
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Managing uncertainty in soil carbon feedbacks to climate changePlant-derived compounds stimulate the decomposition of organic matter in arctic permafrost soilsExperimental warming of a mountain tundra increases soil CO2 effluxes and enhances CH4 and N2O uptake at Changbai Mountain, ChinaLong-Term Warming Alters Carbohydrate Degradation Potential in Temperate Forest SoilsThree-decade long fertilization-induced soil organic carbon sequestration depends on edaphic characteristics in six typical croplandsClimatic change controls productivity variation in global grasslandsPlant functional types in Earth system models: past experiences and future directions for application of dynamic vegetation models in high-latitude ecosystems.Thermal adaptation of decomposer communities in warming soils.Climate change and geothermal ecosystems: natural laboratories, sentinel systems, and future refugia.Permafrost degradation stimulates carbon loss from experimentally warmed tundra.Invited review: climate change impacts in polar regions: lessons from Antarctic moss bank archives.Vegetation shift from deciduous to evergreen dwarf shrubs in response to selective herbivory offsets carbon losses: evidence from 19 years of warming and simulated herbivory in the subarctic tundra.Two decades of warming increases diversity of a potentially lignolytic bacterial community.Decadal warming causes a consistent and persistent shift from heterotrophic to autotrophic respiration in contrasting permafrost ecosystems.Long-term warming alters richness and composition of taxonomic and functional groups of arctic fungi.Experimental soil warming and cooling alters the partitioning of recent assimilates: evidence from a (14)C-labelling study at the alpine treeline.Stronger warming effects on microbial abundances in colder regions.Nitrogen availability increases in a tundra ecosystem during five years of experimental permafrost thaw.Winter precipitation and snow accumulation drive the methane sink or source strength of Arctic tussock tundra.Earlier snowmelt and warming lead to earlier but not necessarily more plant growth.Ecosystem nitrogen fixation throughout the snow-free period in subarctic tundra: effects of willow and birch litter addition and warming.Changes in composition and abundance of functional groups of arctic fungi in response to long-term summer warming.Quantifying global soil carbon losses in response to warming.A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphereClimate Change Across Seasons Experiment (CCASE): A new method for simulating future climate in seasonally snow-covered ecosystemsSoil bacterial community composition altered by increased nutrient availability in Arctic tundra soils.Climatic influences on wood anatomy and tree-ring features of Great Basin conifers at a new mountain observatory.Carbon-degrading enzyme activities stimulated by increased nutrient availability in Arctic tundra soils.Summer temperature increase has distinct effects on the ectomycorrhizal fungal communities of moist tussock and dry tundra in Arctic Alaska.Vascular plant abundance and diversity in an alpine heath under observed and simulated global changeClimate change and the permafrost carbon feedback.Distinct soil bacterial communities along a small-scale elevational gradient in alpine tundraMicrobial responses to southward and northward Cambisol soil transplantMicrobial control of soil organic matter mineralization responses to labile carbon in subarctic climate change treatments.Modeling long-term changes in tundra carbon balance following wildfire, climate change, and potential nutrient addition.A gradient of nutrient enrichment reveals nonlinear impacts of fertilization on Arctic plant diversity and ecosystem function.Alpine soil carbon is vulnerable to rapid microbial decomposition under climate cooling.Responses of lichen communities to 18 years of natural and experimental warming.Impacts of twenty years of experimental warming on soil carbon, nitrogen, moisture and soil mites across alpine/subarctic tundra communitiesSimple additive simulation overestimates real influence: altered nitrogen and rainfall modulate the effect of warming on soil carbon fluxes.
P2860
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P2860
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
description
2013 nî lūn-bûn
@nan
2013年の論文
@ja
2013年学术文章
@wuu
2013年学术文章
@zh
2013年学术文章
@zh-cn
2013年学术文章
@zh-hans
2013年学术文章
@zh-my
2013年学术文章
@zh-sg
2013年學術文章
@yue
2013年學術文章
@zh-hant
name
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@en
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@nl
type
label
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@en
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@nl
prefLabel
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@en
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@nl
P2093
P2860
P356
P1433
P1476
Long-term warming restructures Arctic tundra without changing net soil carbon storage.
@en
P2093
John C Moore
Joshua P Schimel
Rodney T Simpson
Seeta A Sistla
P2860
P2888
P304
P356
10.1038/NATURE12129
P407
P577
2013-05-15T00:00:00Z
P5875
P6179
1020759734