Variability in above- and belowground carbon stocks in a Siberian larch watershed

Permafrost soils store between 1330 and 1580 Pg carbon (C), which is 3 times the amount of C in global vegetation, almost twice the amount of C in the atmosphere, and half of the global soil organic C pool. Despite the massive amount of C in permafrost, estimates of soil C storage in the high-latitu...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Webb, Elizabeth E., Heard, Kathryn, Natali, Susan M., Bunn, Andrew G., Alexander, Heather D., Berner, Logan T., Kholodov, Alexander, Loranty, Michael M., Schade, John D., Spektor, Valentin, Zimov, Nikita
Format: Text
Language:English
Published: 2018
Subjects:
Ice
Online Access:https://doi.org/10.5194/bg-14-4279-2017
https://www.biogeosciences.net/14/4279/2017/