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

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

Abstract In the East Asian monsoon area, stalagmites generally record lower and higher oxygen isotope (δ18O) levels during warm humid interglacial and cold dry glacial periods, respectively. Here, we report unusually low stalagmite δ18O from the last glacial period (ca. 32.2–22.3 ka) in Fukugaguchi...

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Bibliographic Details
Main Authors: Shota Amekawa, Kenji Kashiwagi, Masako Hori, Tomomi Sone, Hirokazu Kato, Tomoyo Okumura, Tsai-Luen Yu, Chuan-Chou Shen, Akihiro Kano
Format: Article
Language:English
Published: SpringerOpen 2021-02-01
Series:Progress in Earth and Planetary Science
Subjects:
Stalagmite paleoclimatelogy
East Asian winter monsoon
Last glacial period
Japan Sea
Oxygen isotope ratio
Online Access:https://doi.org/10.1186/s40645-021-00409-8

Internet

https://doi.org/10.1186/s40645-021-00409-8

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