Nature Communications (Sep 2018)
Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrost
Abstract
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 and ∆14C.