Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing

被引：0

作者：

Jonathan P. LaRiviere

A. Christina Ravelo

Allison Crimmins

Petra S. Dekens

Heather L. Ford

Mitch Lyle

Michael W. Wara

机构：

[1] University of California,Ocean Sciences Department

[2] Texas A&M University,Department of Oceanography

[3] Present addresses: US Environmental Protection Agency,undefined

[4] Climate Change Division,undefined

[5] Washington DC 20460,undefined

[6] USA (A.C.); Department of Geosciences,undefined

[7] San Francisco State University,undefined

[8] San Francisco,undefined

[9] California 94132,undefined

[10] USA (P.S.D.); Freeman Spogli Institute for International Studies,undefined

[11] Stanford Law School,undefined

[12] Stanford,undefined

[13] California 94305,undefined

[14] USA (M.W.W.).,undefined

来源：

Nature | 2012年 / 486卷

关键词：

D O I：

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学科分类号：

摘要：

Measurements from several ocean cores reveal that ocean warmth persisted throughout the late Miocene epoch despite CO2 levels of only 200–350 p.p.m.v., probably driven by a deep thermocline that isolated climate responses from CO2 variations.

引用

页码：97 / 100

页数：3

共 50 条

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