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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
2829 °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
3334 °C (± 2 °C) during the middle Cretaceous hothouse. Uppermost Cenomanian tropical sea-surface temperatures may have been as much as 47 °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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