Middle Miocene Southern Ocean Cooling and Antarctic Cryosphere Expansion

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
Published in:Science
Main Authors: Shevenell, Amelia E., Kennett, James P., Lea, David W.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2004
Subjects:
Antarctic
Pacific
Southern Ocean
Antarc*
Planktonic foraminifera
Online Access:http://dx.doi.org/10.1126/science.1100061
https://www.science.org/doi/pdf/10.1126/science.1100061
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Summary: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 eccentricity forcing and precedes Antarctic cryosphere expansion by ∼60 thousand years, suggesting the involvement of additional feedbacks during this interval of inferred low-atmospheric partial pressure of CO 2 ( p CO 2 ). Comparing SSTs and global carbon cycling proxies challenges the notion that episodic p CO 2 drawdown drove this major Cenozoic climate transition. SST, salinity, and ice-volume trends suggest instead that orbitally paced ocean circulation changes altered meridional heat/vapor transport, triggering ice growth and global cooling.

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