Pollen and grainsize records and element composition of cores from the Wangdongyang peatland, southeast China ...

Our results reveals a warm and wet climate from 8000-2000 cal a BP and this was followed by a cooler and drier climate since ~2000 cal a BP. We identified a cooler and drier climate during 7500-7240 cal a BP and this abrupt cooling event have occurred earlier in the southeast relative to the north o...

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Bibliographic Details
Main Authors: Zhao, Lin, Ma, Chunmei, Wen, Zhenming, Ye, Wei, Shang, Guangchun, Tang, Lingyu
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2020
Subjects:
Climate change
East Asian summer monsoon
the abrupt climate event
Vegetation dynamics
Core
North Atlantic
Online Access:https://dx.doi.org/10.1594/pangaea.922889
https://doi.pangaea.de/10.1594/PANGAEA.922889
Description
Summary:Our results reveals a warm and wet climate from 8000-2000 cal a BP and this was followed by a cooler and drier climate since ~2000 cal a BP. We identified a cooler and drier climate during 7500-7240 cal a BP and this abrupt cooling event have occurred earlier in the southeast relative to the north of China. Solar activity and the influx of meltwater to the North Atlantic were the likely triggers for this abrupt climatic event. ...

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