Journal
GEOLOGY
Volume 36, Issue 3, Pages 251-254Publisher
GEOLOGICAL SOC AMER, INC
DOI: 10.1130/G24584A.1
Keywords
Eocene; Oligocene; climate; ice sheets; temperature; Cenozoic
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Funding
- Natural Environment Research Council [NE/B503225/1, NE/E007902/1] Funding Source: researchfish
- NERC [NE/E007902/1] Funding Source: UKRI
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The Eocene-Oligocene (E-O) climate transition (ca. 34 Ma) marks a period of Antarctic ice growth and a major step from early Cenozoic greenhouse conditions toward today's glaciated climate state. The transition is represented by an increase in deep-sea benthic foraminiferal oxygen isotope (delta O-18) values occurring in two main steps that reflect the temperature and delta O-18 of seawater. Existing benthic Mg/Ca paleotemperature records do not display a cooling across the transition, possibly reflecting a saturation state effect on benthic foraminiferal Mg/Ca ratios at deep-water sites. Here we present data from exceptionally well preserved foraminifera deposited well above the calcite compensation depth that provide the first proxy evidence for an similar to 2.5 degrees C ocean cooling associated with the ice growth. This permits interpretation of E-O delta O-18 records without invoking Northern Hemisphere continental-scale ice.
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