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...
| الحاوية / القاعدة: | Nature Communications |
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| المؤلفون الرئيسيون: | , , , , , , , , , , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Nature Portfolio
2018-09-01
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1038/s41467-018-06080-w |
