Reduced quantity and quality of SOM along a thaw sequence on the Tibetan Plateau

Carbon (C) release from thawing permafrost is potentially the largest climate feedback from terrestrial ecosystems. However, the magnitude of this feedback remains highly uncertain, partly due to the limited understanding of how abrupt permafrost thaw (e.g. permafrost collapse) alters soil organic m...

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Autores principales:	Futing Liu, Leiyi Chen, Benjamin W. Abbott, Yunping Xu, Guibiao Yang, Dan Kou, Shuqi Qin, Jens Strauss, Yinghui Wang, Beibei Zhang, Yuanhe Yang
Formato:	Artigo
Lenguaje:	Inglês
Publicado:	IOP Publishing 2018-01-01
Colección:	Environmental Research Letters
Materias:	carbon cycle climate feedback upland permafrost SOM quality abrupt thaw
Acceso en línea:	https://doi.org/10.1088/1748-9326/aae43b
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