Massive remobilization of permafrost carbon during post-glacial warming

Recent hypotheses, based on atmospheric records and models, suggest that permafrost carbon (PF-C) accumulated during the last glaciation may have been an important source for the atmospheric CO(2) rise during post-glacial warming. However, direct physical indications for such PF-C release have so fa...

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Detalles Bibliográficos
Autores principales: Tesi, T., Muschitiello, F., Smittenberg, R. H., Jakobsson, M., Vonk, J. E., Hill, P., Andersson, A., Kirchner, N., Noormets, R., Dudarev, O., Semiletov, I., Gustafsson, Ö
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5141343/
https://www.ncbi.nlm.nih.gov/pubmed/27897191
http://dx.doi.org/10.1038/ncomms13653

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5141343/
https://www.ncbi.nlm.nih.gov/pubmed/27897191
http://dx.doi.org/10.1038/ncomms13653

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