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      Data report: late Eocene-early Oligocene ostracods at IODP Site U1411, off Newfoundland, North Atlantic

      Proceedings of the IODP
      Integrated Ocean Drilling Program

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          Abstract

          At the present, typical North Atlantic Deep Water ostracod faunas are characterized by the dominance of Krithe species and the association with Henryhowella and Poseidonamicus. The fauna may have originated during the Eocene–Oligocene. Because there are only a few taxonomic studies on Eocene–Oligocene ostracod taxa in the North Atlantic deep-sea sediments, the ostracod taxa are poorly understood. Here I report and illustrate 23 taxa from the upper Eocene–lower Oligocene sediments at Integrated Ocean Drilling Program Site U1411 in the North Atlantic Ocean and describe the taxa systematically.

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          Review and revision of Cenozoic tropical planktonic foraminiferal biostratigraphy and calibration to the geomagnetic polarity and astronomical time scale

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            Evolution of Atlantic thermohaline circulation: Early Oligocene onset of deep-water production in the North Atlantic

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              Impact of Antarctic Circumpolar Current development on late Paleogene ocean structure.

              Global cooling and the development of continental-scale Antarctic glaciation occurred in the late middle Eocene to early Oligocene (~38 to 28 million years ago), accompanied by deep-ocean reorganization attributed to gradual Antarctic Circumpolar Current (ACC) development. Our benthic foraminiferal stable isotope comparisons show that a large δ(13)C offset developed between mid-depth (~600 meters) and deep (>1000 meters) western North Atlantic waters in the early Oligocene, indicating the development of intermediate-depth δ(13)C and O(2) minima closely linked in the modern ocean to northward incursion of Antarctic Intermediate Water. At the same time, the ocean's coldest waters became restricted to south of the ACC, probably forming a bottom-ocean layer, as in the modern ocean. We show that the modern four-layer ocean structure (surface, intermediate, deep, and bottom waters) developed during the early Oligocene as a consequence of the ACC.
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                Author and article information

                Journal
                10.2204/iodp.proc.342.2014
                Proceedings of the IODP
                Integrated Ocean Drilling Program
                1930-1014
                02 March 2018
                Article
                10.2204/iodp.proc.342.206.2018
                1bad32a3-fe5a-4b54-8b55-0957cbae9980

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History

                Earth & Environmental sciences,Oceanography & Hydrology,Geophysics,Chemistry,Geosciences

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