Thawing permafrost increases old soil and autotrophic respiration in tundra: partitioning ecosystem respiration using δ(13) C and ∆(14) C.
about
Thermal acclimation of shoot respiration in an Arctic woody plant species subjected to 22 years of warming and altered nutrient supply.The unseen iceberg: plant roots in arctic tundra.Decadal warming causes a consistent and persistent shift from heterotrophic to autotrophic respiration in contrasting permafrost ecosystems.Permafrost collapse alters soil carbon stocks, respiration, CH4 , and N2O in upland tundra.Vascular plants promote ancient peatland carbon loss with climate warmingCoupled long-term summer warming and deeper snow alters species composition and stimulates gross primary productivity in tussock tundra.Nonlinear CO2 flux response to 7 years of experimentally induced permafrost thaw.The impacts of climate change and human activities on biogeochemical cycles on the Qinghai-Tibetan Plateau.Differential physiological responses to environmental change promote woody shrub expansionThe subzero microbiome: microbial activity in frozen and thawing soils.Beyond simple linear mixing models: process-based isotope partitioning of ecological processes.Contrasting above- and belowground organic matter decomposition and carbon and nitrogen dynamics in response to warming in High Arctic tundra.Microbial functional diversity covaries with permafrost thaw-induced environmental heterogeneity in tundra soil.Experimentally increased nutrient availability at the permafrost thaw front selectively enhances biomass production of deep-rooting subarctic peatland species.Microbial network, phylogenetic diversity and community membership in the active layer across a permafrost thaw gradient.Diurnal characteristics of ecosystem respiration of alpine meadow on the Qinghai-Tibetan Plateau: implications for carbon budget estimation.Understory vegetation mediates permafrost active layer dynamics and carbon dioxide fluxes in open-canopy larch forests of northeastern Siberia.High-quality eddy-covariance CO2 budgets under cold climate conditionsTransitions in Arctic ecosystems: Ecological implications of a changing hydrological regimeObservations of 14 CO2 in ecosystem respiration from a temperate deciduous forest in Northern WisconsinAnnual patterns and budget of CO2flux in an Arctic tussock tundra ecosystemModel-based analysis of environmental controls over ecosystem primary production in an alpine tundra dry meadowComparison of plant litter and peat decomposition changes with permafrost thaw in a subarctic peatlandTundra is a consistent source of CO2 at a site with progressive permafrost thaw during 6 years of chamber and eddy covariance measurements
P2860
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P2860
Thawing permafrost increases old soil and autotrophic respiration in tundra: partitioning ecosystem respiration using δ(13) C and ∆(14) C.
description
2012 nî lūn-bûn
@nan
2012 թուականի Նոյեմբերին հրատարակուած գիտական յօդուած
@hyw
2012 թվականի նոյեմբերին հրատարակված գիտական հոդված
@hy
2012年の論文
@ja
2012年論文
@yue
2012年論文
@zh-hant
2012年論文
@zh-hk
2012年論文
@zh-mo
2012年論文
@zh-tw
2012年论文
@wuu
name
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@ast
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@en
type
label
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@ast
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@en
prefLabel
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@ast
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@en
P2860
P921
P356
P1476
Thawing permafrost increases o ...... ion using δ(13) C and ∆(14) C.
@en
P2093
Caitlin E Hicks Pries
Kathryn G Crummer
P2860
P304
P356
10.1111/GCB.12058
P577
2012-11-29T00:00:00Z