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...

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Bibliographic Details
Main Authors: Carter, Samantha Cassie, Griffith, Elizabeth M, Penman, Donald E
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.893203
https://doi.org/10.1594/PANGAEA.893203