Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrost
Permafrost-derived carbon (C) may have been an additional source of greenhouse gases during the last glacial-interglacial transition. Here the authors show that ancient C from degrading permafrost was mobilised during phases of rapid sea-level rise, partially explaining changes in atmospheric CO2 an...
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| Asıl Yazarlar: | , , , , , , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2018-09-01
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| Seri Bilgileri: | Nature Communications |
| Konular: | |
| Online Erişim: | https://doi.org/10.1038/s41467-018-06080-w |
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