Input of easily available organic C and N stimulates microbial decomposition of soil organic matter in arctic permafrost soil.
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Nitrogen Fertilizer and Straw Applications Affect Uptake of 13C,15N-Glycine by Soil Microorganisms in Wheat Growth StagesThe decadal state of the terrestrial carbon cycle: Global retrievals of terrestrial carbon allocation, pools, and residence timesPlant-derived compounds stimulate the decomposition of organic matter in arctic permafrost soilsA simplified, data-constrained approach to estimate the permafrost carbon-climate feedbackMetagenomics Reveals Pervasive Bacterial Populations and Reduced Community Diversity across the Alaska Tundra EcosystemLinking soil microbial communities to vascular plant abundance along a climate gradient.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.Regional variation in the temperature sensitivity of soil organic matter decomposition in China's forests and grasslands.Microbial Community Dynamics in Soil Depth Profiles Over 120,000 Years of Ecosystem DevelopmentMicrobial carbon mineralization in tropical lowland and montane forest soils of Peru.Distinct summer and winter bacterial communities in the active layer of Svalbard permafrost revealed by DNA- and RNA-based analyses.Microbial control of soil organic matter mineralization responses to labile carbon in subarctic climate change treatments.Are variations in heterotrophic soil respiration related to changes in substrate availability and microbial biomass carbon in the subtropical forests?Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia.Contrasting above- and belowground organic matter decomposition and carbon and nitrogen dynamics in response to warming in High Arctic tundra.Experimentally increased nutrient availability at the permafrost thaw front selectively enhances biomass production of deep-rooting subarctic peatland species.Long-term in situ permafrost thaw effects on bacterial communities and potential aerobic respirationShort-term carbon input increases microbial nitrogen demand, but not microbial nitrogen mining, in a set of boreal forest soilsProperties and bioavailability of particulate and mineral-associated organic matter in Arctic permafrost soils, Lower Kolyma Region, RussiaAerobic respiration of mineral-bound organic carbon in a soilNitrogen availability regulates topsoil carbon dynamics after permafrost thaw by altering microbial metabolic efficiency
P2860
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P2860
Input of easily available organic C and N stimulates microbial decomposition of soil organic matter in arctic permafrost soil.
description
2014 nî lūn-bûn
@nan
2014年の論文
@ja
2014年論文
@yue
2014年論文
@zh-hant
2014年論文
@zh-hk
2014年論文
@zh-mo
2014年論文
@zh-tw
2014年论文
@wuu
2014年论文
@zh
2014年论文
@zh-cn
name
Input of easily available orga ...... ter in arctic permafrost soil.
@en
type
label
Input of easily available orga ...... ter in arctic permafrost soil.
@en
prefLabel
Input of easily available orga ...... ter in arctic permafrost soil.
@en
P2093
P2860
P50
P1476
Input of easily available orga ...... ter in arctic permafrost soil.
@en
P2093
Antje Gittel
Galina Zrazhevskaya
Georg Guggenberger
Hana Santrůčková
Jiří Bárta
Margarete Watzka
Nikolay Lashchinskiy
Norman Gentsch
Olga Rusalimova
Olga Shibistova
P2860
P304
P356
10.1016/J.SOILBIO.2014.04.014
P50
P577
2014-08-01T00:00:00Z