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      Millennial-scale fluctuations in subtropical northwestern Atlantic surface ocean hydrography during the mid-Pleistocene : MILLENNIAL-SCALE SUBTROPICAL HYDROGRAPHY

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          A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates

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            An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677

            Ocean Drilling Program (ODP) Site 677 provided excellent material for high resolution stable isotope analysis of both benthonic and planktonic foraminifera through the entire Pleistocene and upper Pliocene. The oxygen isotope record is readily correlated with the SPECMAP stack (Imbrieet al.1984) and with the record from DSDP 607 (Ruddimanet al.1986) but a significantly better match with orbital models is obtained by departing from the timescale proposed by these authors below Stage 16 (620 000 years). It is the stronger contribution from the precession signal in the record from ODP Site 677 that provides the basis for the revised timescale. Our proposed modification to the timescale would imply that the currently adopted radiometric dates for the Matuyama–Brunhes boundary, the Jaramillo and Olduvai Subchrons and the Gauss–Matuyama boundary underestimate their true astronomical ages by between 5 and 7%.
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              Correlation between climate events in the North Atlantic and China during the last glaciation

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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                American Geophysical Union (AGU)
                08838305
                June 2004
                June 2004
                May 22 2004
                : 19
                : 2
                : n/a
                Affiliations
                [1 ]College of Marine Studies; University of Delaware; Lewes Delaware USA
                [2 ]Department of Earth and Environmental Sciences; University of Rochester; Rochester New York USA
                [3 ]Department of Earth Sciences; University of Southern California; Los Angeles California USA
                [4 ]Department of Geological Sciences; University of South Carolina; Columbia South Carolina USA
                Article
                10.1029/2003PA000990
                aacc46dd-6d0c-4b58-b93c-ad30d98a4433
                © 2004

                http://doi.wiley.com/10.1002/tdm_license_1.1

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