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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 4 | Copyright

Special issue: Initial results from lake El'gygytgyn, western Beringia: first...

Clim. Past, 9, 1559-1569, 2013
https://doi.org/10.5194/cp-9-1559-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 22 Jul 2013

Research article | 22 Jul 2013

A 350 ka record of climate change from Lake El'gygytgyn, Far East Russian Arctic: refining the pattern of climate modes by means of cluster analysis

U. Frank1, N. R. Nowaczyk1, P. Minyuk2, H. Vogel3, P. Rosén4, and M. Melles3 U. Frank et al.
  • 1Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Section 5.2 – Paleoclimate and Landscape evolution, 14473 Potsdam, Germany
  • 2North-East Interdisciplinary Science Research Institute, FEB RAS, 685000 Magadan, Russia
  • 3Institute of Geology and Mineralogy, University of Cologne, 50674 Cologne, Germany
  • 4Climate Impacts Research Centre (CIRC), Umeå University, 98107 Abisko, Sweden

Abstract. Rock magnetic, biochemical and inorganic records of the sediment cores PG1351 and Lz1024 from Lake El'gygytgyn, Chukotka peninsula, Far East Russian Arctic, were subject to a hierarchical agglomerative cluster analysis in order to refine and extend the pattern of climate modes as defined by Melles et al. (2007). Cluster analysis of the data obtained from both cores yielded similar results, differentiating clearly between the four climate modes warm, peak warm, cold and dry, and cold and moist. In addition, two transitional phases were identified, representing the early stages of a cold phase and slightly colder conditions during a warm phase. The statistical approach can thus be used to resolve gradual changes in the sedimentary units as an indicator of available oxygen in the hypolimnion in greater detail. Based upon cluster analyses on core Lz1024, the published succession of climate modes in core PG1351, covering the last 250 ka, was modified and extended back to 350 ka. Comparison to the marine oxygen isotope (δ18O) stack LR04 (Lisiecki and Raymo, 2005) and the summer insolation at 67.5° N, with the extended Lake El'gygytgyn parameter records of magnetic susceptibility (κLF), total organic carbon content (TOC) and the chemical index of alteration (CIA; Minyuk et al., 2007), revealed that all stages back to marine isotope stage (MIS) 10 and most of the substages are clearly reflected in the pattern derived from the cluster analysis.

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