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Cited by 574

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Middle Miocene Southern Ocean Cooling and Antarctic Cryosphere Expansion

Shevenell, Amelia E., Kennett, James P., Lea, David W.·2004·Science

Abstract

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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Crossref · 10.1126/science.1100061

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Metadata

Authors
Shevenell, A. E., Kennett, J. P., & Lea, D. W.
Venue
Science
Published
2004-09-17
Volume
305
Issue
5691
Pages
1766-1770
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2070511571
Cited by
574
References
1
FWCI
10.65
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Middle Miocene Southern Ocean Cooling and Antarctic Cryosphere Expansion. https://app.cochat.ai/papers/10.1126/science.1100061
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Shevenell, A. E., Kennett, J. P., & Lea, D. W. (2004). Middle Miocene Southern Ocean Cooling and Antarctic Cryosphere Expansion. Science. https://doi.org/10.1126/science.1100061

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.