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

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Main Authors: Zhao, Lin, Ma, Chunmei, Wen, Zhenming, Ye, Wei, Shang, Guangchun, Tang, Lingyu
Format: Dataset Open Access
Language:en
Published: PANGAEA 2020
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author Zhao, Lin
Ma, Chunmei
Wen, Zhenming
Ye, Wei
Shang, Guangchun
Tang, Lingyu
author_facet Zhao, Lin
Ma, Chunmei
Wen, Zhenming
Ye, Wei
Shang, Guangchun
Tang, Lingyu
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_922889
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Pollen and grainsize records and element composition of cores from the Wangdongyang peatland, southeast China
Zhao, Lin
Ma, Chunmei
Wen, Zhenming
Ye, Wei
Shang, Guangchun
Tang, Lingyu
Climate change; Core; CORE; East Asian summer monsoon; South China; the abrupt climate event; Vegetation dynamics; Wangdongyang_WDY1; Wangdongyang_WDY2
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.
title Pollen and grainsize records and element composition of cores from the Wangdongyang peatland, southeast China
topic Climate change; Core; CORE; East Asian summer monsoon; South China; the abrupt climate event; Vegetation dynamics; Wangdongyang_WDY1; Wangdongyang_WDY2
url https://doi.org/10.1594/PANGAEA.922889