Anaerobic respiration pathways and response to increased substrate availability of Arctic wetland soils

Divergent soil biogeochemical conditions will determine the fate and pathways of labile carbon released during permafrost thaw, thereby influencing the production of greenhouse gas mixtures and radiative forcing of tundra soils.

Bibliographic Details
Published in:	Environmental Science: Processes & Impacts
Main Authors:	Philben, Michael, Zhang, Lijie, Yang, Ziming, Taş, Neslihan, Wullschleger, Stan D., Graham, David E., Gu, Baohua
Other Authors:	Oak Ridge National Laboratory
Format:	Article in Journal/Newspaper
Language:	English
Published:	Royal Society of Chemistry (RSC) 2020
Subjects:	permafrost Tundra
Online Access:	http://dx.doi.org/10.1039/d0em00124d http://pubs.rsc.org/en/content/articlepdf/2020/EM/D0EM00124D

Description
Summary:	Divergent soil biogeochemical conditions will determine the fate and pathways of labile carbon released during permafrost thaw, thereby influencing the production of greenhouse gas mixtures and radiative forcing of tundra soils.