2.8 Million Years of Arctic Climate Change from Lake El’gygytgyn, NE Russia

Crater Core The high-northern latitudes of the Arctic have an important influence on climate and constitute a region with a unique array of complex feedbacks that make it difficult to understand the workings of its climate. Melles et al. (p. 315 , published online 21 June) developed a 2.8-million-ye...

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Bibliographic Details
Published in:Science
Main Authors: Melles, Martin, Brigham-Grette, Julie, Minyuk, Pavel S., Nowaczyk, Norbert R., Wennrich, Volker, DeConto, Robert M., Anderson, Patricia M., Andreev, Andrei A., Coletti, Anthony, Cook, Timothy L., Haltia-Hovi, Eeva, Kukkonen, Maaret, Lozhkin, Anatoli V., Rosén, Peter, Tarasov, Pavel, Vogel, Hendrik, Wagner, Bernd
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2012
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Online Access:http://dx.doi.org/10.1126/science.1222135
https://www.science.org/doi/pdf/10.1126/science.1222135
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Summary:Crater Core The high-northern latitudes of the Arctic have an important influence on climate and constitute a region with a unique array of complex feedbacks that make it difficult to understand the workings of its climate. Melles et al. (p. 315 , published online 21 June) developed a 2.8-million-year record of Arctic climate, using a sediment core from a lake in northeastern Russia that was formed more than 3.5 million years ago by a meteorite impact. Pronounced glacial episodes began 2.6 million years ago but did not achieve orbital pacing for another 700,000 years.