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Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the...

Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2031e698030d49fea21480095cb86a23

Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the Japan Sea during the last glacial period

About this item

Full title

Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the Japan Sea during the last glacial period

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

Journal title

Progress in earth and planetary science, 2021-02, Vol.8 (1), p.1-15, Article 18

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

More information

Scope and Contents

Contents

In the East Asian monsoon area, stalagmites generally record lower and higher oxygen isotope (δ
18
O) levels during warm humid interglacial and cold dry glacial periods, respectively. Here, we report unusually low stalagmite δ
18
O from the last glacial period (ca. 32.2–22.3 ka) in Fukugaguchi Cave, Niigata Prefecture, Japan, where a ma...

Alternative Titles

Full title

Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the Japan Sea during the last glacial period

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_2031e698030d49fea21480095cb86a23

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2031e698030d49fea21480095cb86a23

Other Identifiers

ISSN

2197-4284

E-ISSN

2197-4284

DOI

10.1186/s40645-021-00409-8

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