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Archive · collection · 2020

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

Listed in PANGAEA

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.

Description

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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Where it is published

Catalogue records · 1

Topics

Provenance · 1 source records, 7 field assertions
SourceKeyLast seenRaw
PANGAEAoai:pangaea.de:doi:10.1594/PANGAEA.92288915 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · PANGAEAconnector:pangaea@1.0.0
concepts[field].local:field:earth-environmentalmapping · PANGAEAconnector:pangaea@1.0.0
descriptionsource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/description
licensesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/rights
publication_datesource · PANGAEAconnector:pangaea@1.0.0
spatialsource · PANGAEAconnector:pangaea@1.0.0
titlesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/title