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 of China. Solar activity and the influx of meltwater to the North Atlantic were the likely triggers for this abrupt climatic event.

Data and Resources

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Cite this as

Zhao, Lin, Ma, Chunmei, Wen, Zhenming, Ye, Wei, Shang, Guangchun, Tang, Lingyu (2020). Dataset: Pollen and grainsize records and element composition of cores from the Wangdongyang peatland, southeast China. https://doi.org/10.1594/PANGAEA.922889

DOI retrieved: 2020

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.922889
Author Zhao, Lin
Given Name Lin
Family Name Zhao
More Authors
Ma, Chunmei
Wen, Zhenming
Ye, Wei
Shang, Guangchun
Tang, Lingyu
Source Creation 2020
Publication Year 2020
Resource Type application/zip - filename: Zhao-etal_2020
Subject Areas
Name: BiologicalClassification

Name: Paleontology

Related Identifiers
Title: Vegetation dynamics and their response to Holocene climate change derived from multi-proxy records from Wangdongyang peat bog in southeast China
Identifier: https://doi.org/10.1007/s00334-021-00852-z
Type: DOI
Relation: References
Year: 2021
Source: Vegetation History and Archaeobotany
Authors: Zhao Lin , Ma Chunmei , Wen Zhenming , Ye Wei , Shang Guangchun , Tang Lingyu .