Miocene Stable Isotope Record: A Detailed Deep Pacific Ocean Study and Its Paleoclimatic Implications

Deep Sea Drilling Project site 289 in the western equatorial Pacific has yielded an extremely detailed record of the carbon and oxygen isotopic changes in the Miocene deep ocean. The isotopic record reflects major changes in paleoclimate and paleoceanography, probably dominated by a major phase of A...

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Bibliographic Details
Published in:Science
Main Authors: Woodruff, Fay, Savin, Samuel M., Douglas, Robert G.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1981
Subjects:
Online Access:http://dx.doi.org/10.1126/science.212.4495.665
https://www.science.org/doi/pdf/10.1126/science.212.4495.665
Description
Summary:Deep Sea Drilling Project site 289 in the western equatorial Pacific has yielded an extremely detailed record of the carbon and oxygen isotopic changes in the Miocene deep ocean. The isotopic record reflects major changes in paleoclimate and paleoceanography, probably dominated by a major phase of Antarctic ice-cap growth. The transition from a relatively unglaciated world to one similar to today occurred between 16.5 × 10 6 and 13 × 10 6 years before the present, with the greatest change occurring between approximately 14.8 × 10 6 and 14.0 × 10 6 years before the present.