Mid-Pliocene shifts in ocean overturning circulation and the onset of Quaternary-style climates

Sarnthein, Michael, Bartoli, G., Prange, M., Schmittner, A., Schneider, Birgit, Weinelt, Mara, Andersen, Nils and Garbe-Schönberg, Dieter (2009) Mid-Pliocene shifts in ocean overturning circulation and the onset of Quaternary-style climates Climate of the Past, 5 (2). pp. 269-283.

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Abstract

A major tipping point of Earth's history occurred during the mid-Pliocene: the onset of major Northern-Hemisphere Glaciation (NHG) and of pronounced, Quaternary-style cycles of glacial-to-interglacial climates, that contrast with more uniform climates over most of the preceding Cenozoic and continue until today (Zachos et al., 2001). The severe deterioration of climate occurred in three steps between 3.2 Ma (warm MIS K3) and 2.7 Ma (glacial MIS G6/4) (Lisiecki and Raymo, 2005). Various models (sensu Driscoll and Haug, 1998) and paleoceanographic records (intercalibrated using orbital age control) suggest clear linkages between the onset of NHG and the three steps in the final closure of the Central American Seaways (CAS), deduced from rising salinity differences between Caribbean and the East Pacific. Each closing event led to an enhanced North Atlantic meridional overturning circulation and this strengthened the poleward transport of salt and heat (warmings of +2-3 degrees C) (Bartoli et al., 2005). Also, the closing resulted in a slight rise in the poleward atmospheric moisture transport to northwestern Eurasia (Lunt et al., 2007), which probably led to an enhanced precipitation and fluvial run-off, lower sea surface salinity (SSS), and an increased sea-ice cover in the Arctic Ocean, hence promoting albedo and the build-up of continental ice sheets. Most important, new evidence shows that the closing of the CAS led to greater steric height of the North Pacific and thus doubled the low-saline Arctic Throughflow from the Bering Strait to the East Greenland Current (EGC). Accordingly, Labrador Sea IODP Site 1307 displays an abrupt but irreversible EGC cooling of 6 degrees C and freshening by similar to 2 psu from 3.25/3.16-3.00 Ma, right after the first but still reversible attempt of closing the CAS.

Document Type: Article
Keywords: northern-hemisphere glaciationatlantic region panama uplift late neogene nordic seas ice greenland pacific ma intensification
Research affiliation: OceanRep > The Future Ocean - Cluster of Excellence
Kiel University > Faculty of Mathematics and Natural Sciences > Institute of Geosciences
Kiel University > Other > Leibniz-Laboratory for Radiometric Dating and Isotope Research
Kiel University
Refereed: Yes
ISSN: 1814-9324
Projects: Future Ocean
Date Deposited: 11 Feb 2011 12:14
Last Modified: 19 Apr 2013 12:30
URI: http://eprints.uni-kiel.de/id/eprint/9692

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