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

• Published in: Climate of the Past
• Main Authors: Frank, U., Nowaczyk, Norbert, Minyuk, Pavel, Vogel, Hendrik, Rosen, Peter, Melles, Martin
• Format: Article in Journal/Newspaper
• Language: English
• Published: Institutionen för ekologi, miljö och geovetenskap 2013
• Subjects: Geology; Geologi; Meteorology and Atmospheric Sciences; Meteorologi och atmosfärforskning; Arctic; Chukotka; Chukotka Peninsula; Climate change; Magnetic susceptibility
• Online Access: http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-81025; https://doi.org/10.5194/cp-9-1559-2013

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 (delta O-18) stack LR04 (Lisiecki and Raymo, 2005) and the summer insolation at 67.5 degrees N, with the extended Lake El'gygytgyn parameter records of magnetic susceptibility (kappa(LF)), 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.