Pliocene Warmth, Polar Amplification, and Stepped Pleistocene Cooling Recorded 
in NE Arctic Russia

Brigham-Grette, J.; Melles, M.; Minyuk, P.; Andreev, A.; Tarasov, P.; DeConto, R.; Koenig, S.; Nowaczyk, Norbert; Wennrich, V.; Rosén, P.; Haltia, E.; Cook, T.; Gebhardt, C.; Meyer-Jacob, C.; Snyder, J.; Herzschuh, U.

doi:10.1126/science.1233137

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Pliocene Warmth, Polar Amplification, and Stepped Pleistocene Cooling Recorded in NE Arctic Russia

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Brigham-Grette, J.
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Melles, M.
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Minyuk, P.
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Andreev, A.
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Tarasov, P.
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DeConto, R.
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Koenig, S.
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Nowaczyk, Norbert
5.2 Climate Dynamics and Landscape Evolution, 5.0 Earth Surface Processes, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Wennrich, V.
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Rosén, P.
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Haltia, E.
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Cook, T.
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Gebhardt, C.
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Meyer-Jacob, C.
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Snyder, J.
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Herzschuh, U.
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Citation

Brigham-Grette, J., Melles, M., Minyuk, P., Andreev, A., Tarasov, P., DeConto, R., Koenig, S., Nowaczyk, N., Wennrich, V., Rosén, P., Haltia, E., Cook, T., Gebhardt, C., Meyer-Jacob, C., Snyder, J., Herzschuh, U. (2013): Pliocene Warmth, Polar Amplification, and Stepped Pleistocene Cooling Recorded in NE Arctic Russia. - Science, 340, 6931, 1421-1427.
https://doi.org/10.1126/science.1233137

https://gfzpublic.gfz-potsdam.de/pubman/item/item_247076

Abstract

Understanding the evolution of Arctic polar climate from the protracted warmth of the middle Pliocene into the earliest glacial cycles in the Northern Hemisphere has been hindered by the lack of continuous, highly resolved Arctic time series. Evidence from Lake El’gygytgyn, NE Arctic Russia, shows that 3.6-3.4 million years ago, summer temperatures were ~8°C warmer than today when pCO2 was ~400 ppm. Multiproxy evidence suggests extreme warmth and polar amplification during the middle Pliocene, sudden stepped cooling events during the Pliocene-Pleistocene transition, and warmer than present Arctic summers until ~2.2 Ma, after the onset of Northern Hemispheric glaciation. Our data are consistent with sea-level records and other proxies indicating that Arctic cooling was insufficient to support large-scale ice sheets until the early Pleistocene.