Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw

Based on observations from thermokarst-impacted sites on the Tibetan Plateau, the authors find substantial particulate organic carbon loss but stable mineral-associated organic carbon and enriched iron-bound organic carbon upon permafrost thaw.

Bibliographic Details
Published in:Nature Communications
Main Authors: Futing Liu, Shuqi Qin, Kai Fang, Leiyi Chen, Yunfeng Peng, Pete Smith, Yuanhe Yang
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2022
Subjects:
Science
Q
permafrost
Thermokarst
Online Access:https://doi.org/10.1038/s41467-022-32681-7
https://doaj.org/article/8ae8983bcc3d40a59a73428d27a079e8
Description
Summary:Based on observations from thermokarst-impacted sites on the Tibetan Plateau, the authors find substantial particulate organic carbon loss but stable mineral-associated organic carbon and enriched iron-bound organic carbon upon permafrost thaw.

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