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001        FI15042503_00001
005        20171019170458.0
006        m^^^^^o^^d^^^^^^^^
007        cr^^n^---ma^mp
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245 00 |a A 12-Million-Year Temperature History of the Tropical Pacific Ocean |h [electronic resource] |y English.
260        |a 1200 New York Avenue NW, Washington, DC 20005 : |b American Association for the Advancement of Science, |c 2014-04-04.
506        |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.
520 2    |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.
533        |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.
650        |a Temperature.
651        |a Pacific Ocean.
700 1    |a Zhang, Yige.
700 1    |a Pagani, Mark.
700 1    |a Liu, Zhonghui.
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15042503/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/04/25/03/00001/FI15042503_thm.jpg
997        |a Sea Level Rise


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