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|a A 12-Million-Year Temperature History of the Tropical Pacific Ocean |h [electronic resource] |y English. |
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|a 1200 New York Avenue NW, Washington, DC 20005 : |b American Association for the Advancement of Science, |c 2014-04-04. |
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|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
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|a The appearance of permanent El Niño–like conditions prior to 3 million years ago is founded
on sea-surface temperature (SST) reconstructions that show invariant Pacific warm pool
temperatures and negligible equatorial zonal temperature gradients. However, only a few SST
records are available, and these are potentially compromised by changes in seawater chemistry,
diagenesis, and calibration limitations. For this study, we establish new biomarker-SST records
and show that the Pacific warm pool was ~4°C warmer 12 million years ago. Both the warm
pool and cold tongue slowly cooled toward modern conditions while maintaining a zonal
temperature gradient of ~3°C in the late Miocene, which increased during the Plio-Pleistocene.
Our results contrast with previous temperature reconstructions that support the supposition of a permanent El Niño–like state. |
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|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15042503/00001 |y Click here for full text |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/04/25/03/00001/FI15042503_thm.jpg |