Analysis of the middle Miocene climate transition from different Holes of IODP Site 321-U1337
The middle Miocene climate transition (MMCT) is characterized by an abrupt 1‰ increase in benthic foraminiferal oxygen isotopes at ca. 13.8 Ma, marking expansion of the Antarctic Ice Sheet and transition of Earth's climate to a cooler, relatively stable glacial state. Also occurring during this...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2018
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.893203 https://doi.org/10.1594/PANGAEA.893203 |