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Geology; April 2002; v. 30; no. 4; p. 299-302; DOI: 10.1130/0091-7613(2002)030<0299:JTTTIT>2.0.CO;2
© 2002 Geological Society of America
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Jiggling the tropical thermostat in the Cretaceous hothouse

Richard D. Norris1, Karen L. Bice1, Elizabeth A. Magno2 and Paul A. Wilson3

1 Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543-1541, USA
2 Department of Geology, Arizona State University, Tempe, Arizona 85287, USA
3 Southampton Oceanography Centre, School of Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK

Modern open-ocean sea-surface temperatures rarely exceed ~28–29 °C, and the same has been thought to represent a rough maximum for past tropical climates. However, new isotopic estimates from the uppermost Cenomanian in the tropical western North Atlantic suggest that mixed-layer temperatures reached ~33–34 °C (± 2 °C) during the middle Cretaceous hothouse. Uppermost Cenomanian tropical sea-surface temperatures may have been as much as 4–7 °C warmer than the highest modern mean annual temperatures. Such extreme conditions suggest that warm tropical oceans could have driven substantially intensified atmospheric heat transport near the Cenomanian-Turonian boundary. The tropical "thermostat" was set higher than today, challenging the hypothesis of tropical climate stability.

Key Words: temperature • Cretaceous • planktonic foraminifera • stable isotopes • Atlantic




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