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

Permafrost thaw can stimulate microbial decomposition and induce soil carbon (C) loss, potentially triggering a positive C-climate feedback. However, earlier observations have concentrated on bulk soil C dynamics upon permafrost thaw, with limited evidence involving soil C fractions. Here, we explor...

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Detalles Bibliográficos
Autores principales: Liu, Futing, Qin, Shuqi, Fang, Kai, Chen, Leiyi, Peng, Yunfeng, Smith, Pete, Yang, Yuanhe
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9424277/
https://www.ncbi.nlm.nih.gov/pubmed/36038568
http://dx.doi.org/10.1038/s41467-022-32681-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9424277/
https://www.ncbi.nlm.nih.gov/pubmed/36038568
http://dx.doi.org/10.1038/s41467-022-32681-7

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