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...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:Nature Communications
المؤلفون الرئيسيون: Maria Winterfeld, Gesine Mollenhauer, Wolf Dummann, Peter Köhler, Lester Lembke-Jene, Vera D. Meyer, Jens Hefter, Cameron McIntyre, Lukas Wacker, Ulla Kokfelt, Ralf Tiedemann
التنسيق: مقال
اللغة:الإنجليزية
منشور في: Nature Portfolio 2018-09-01
الموضوعات:
الوصول للمادة أونلاين:https://doi.org/10.1038/s41467-018-06080-w