Response of carbon cycle to drier conditions in the mid-Holocene in central China
The effect of Asian summer monsoon hydrological changes on key biogeochemical processes remains poorly understood. Here, using a suite of biomarkers, the authors reconstruct palaeohydrological conditions during the Holocene and show that the peatland carbon cycle is strongly sensitive to paleohydrol...
Main Authors: | , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Nature Publishing Group
2018-04-01
|
Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-018-03804-w |