Sources and characteristics of terrestrial carbon in Holocene-scale sediments of the East Siberian Sea
Thawing of permafrost carbon (PF-C) due to climate warming can remobilise considerable amounts of terrestrial carbon from its long-term storage to the marine environment. PF-C can be then be buried in sediments or remineralised to CO<sub>2</sub> with implications for the carbon–climate feedback....
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| Principais autores: | , , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Copernicus Publications
2017-09-01
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| coleção: | Climate of the Past |
| Acesso em linha: | https://www.clim-past.net/13/1213/2017/cp-13-1213-2017.pdf |
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