(Table 1) Oxygen isotope composition and comparison between ages and sea surface temperature from sediment core KH-79-3_L-3
The Japan Sea experienced bottom water anoxia at the last glacial maximum (LGM) since it is surrounded by four shallow straits, the sill depths of which are close to, or shallower than, the drop in sea level (~120 m) that occurred then. A distinctive negative d18O excursion of planktonic foraminifer...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2001
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.802169 https://doi.org/10.1594/PANGAEA.802169 |