Sea surface temperature reconstruction for the middle Miocene Southern Ocean

Magnesium/calcium data from Southern Ocean planktonic foraminifera demonstrate that high-latitude (~55°S) southwest Pacific sea surface temperatures (SSTs) cooled 6° to 7°C during the middle Miocene climate transition (14.2 to 13.8 million years ago). Stepwise surface cooling is paced by eccentricit...

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Bibliographic Details
Main Authors: Shevenell, Amelia E, Kennett, James P, Lea, David W
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.772059
https://doi.org/10.1594/PANGAEA.772059