A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
about
The origin, source, and cycling of methane in deep crystalline rock biosphereA simplified, data-constrained approach to estimate the permafrost carbon-climate feedbackPermafrost collapse alters soil carbon stocks, respiration, CH4 , and N2O in upland tundra.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.Heterogeneity of carbon loss and its temperature sensitivity in East-European subarctic tundra soils.Warming of subarctic tundra increases emissions of all three important greenhouse gases - carbon dioxide, methane, and nitrous oxide.Are variations in heterotrophic soil respiration related to changes in substrate availability and microbial biomass carbon in the subtropical forests?Determinants of carbon release from the active layer and permafrost deposits on the Tibetan Plateau.Temperature effects on net greenhouse gas production and bacterial communities in arctic thaw ponds.Microbial community dynamics in soil aggregates shape biogeochemical gas fluxes from soil profiles - upscaling an aggregate biophysical model.Greenhouse gas released from the deep permafrost in the northern Qinghai-Tibetan Plateau.Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change.Potential carbon emissions dominated by carbon dioxide from thawed permafrost soilsPathways of anaerobic organic matter decomposition in tundra soils from Barrow, AlaskaSoil incubations reproduce field methane dynamics in a subarctic wetlandVariability in the sensitivity among model simulations of permafrost and carbon dynamics in the permafrost region between 1960 and 2009Redox dynamics in the active layer of an Arctic headwater catchment; examining the potential for transfer of dissolved methane from soils to stream waterModeling CO2 emissions from Arctic lakes: Model development and site-level studyMethane emissions proportional to permafrost carbon thawed in Arctic lakes since the 1950sLimited contribution of permafrost carbon to methane release from thawing peatlandsAdding stable carbon isotopes improves model representation of the role of microbial communities in peatland methane cycling
P2860
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P2860
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
description
2015 nî lūn-bûn
@nan
2015 թուականի Յունուարին հրատարակուած գիտական յօդուած
@hyw
2015 թվականի հունվարին հրատարակված գիտական հոդված
@hy
2015年の論文
@ja
2015年論文
@yue
2015年論文
@zh-hant
2015年論文
@zh-hk
2015年論文
@zh-mo
2015年論文
@zh-tw
2015年论文
@wuu
name
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@ast
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@en
type
label
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@ast
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@en
prefLabel
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@ast
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@en
P2093
P2860
P50
P356
P1476
A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.
@en
P2093
Anthony David McGuire
Hana Šantrůčková
Massimo Lupascu
Merritt R Turetsky
Susan M Natali
Taniya Roy Chowdhury
Victoria L Sloan
P2860
P356
10.1111/GCB.12875
P50
P577
2015-01-24T00:00:00Z