Inorganic geochemistry data from Lake El'gygytgyn sediments: marine isotope stages 6–11

• Main Authors: P. S. Minyuk, V. Y. Borkhodoev, V. Wennrich
• Format: Article
• Language: English
• Published: Copernicus Publications 2014-03-01
• Series: Climate of the Past
• Online Access: http://www.clim-past.net/10/467/2014/cp-10-467-2014.pdf

Geochemical analyses were performed on sediments recovered by deep drilling at Lake El'gygytgyn in central Chukotka, northeastern Russia (67°30' N; 172°05' E). Major and rare element concentrations were determined using X-ray fluorescence spectroscopy (XRF) on the < 250 μm fraction from 617 samples dated to ca. 440 and 125 ka, which approximates marine isotope stages (MIS) 11 to 6. The inorganic geochemistry indicates significant variations in elemental composition between glaciations and interglaciations. Interglacial sediments are characterized by high contents of SiO₂, Na₂O, CaO, K₂O, and Sr and are depleted in Al₂O₃, Fe₂O₃, TiO₂, and MgO. An extreme SiO₂ enrichment during MIS 11.3 and 9.3 was caused by an enhanced flux of biogenic silica (BSi). The geochemical structure of MIS 11 shows similar characteristics as seen in MIS 11 records from Lake Baikal (southeastern Siberia) and Antarctic ice cores, thereby arguing for the influence of global forcings on these records. High sediment content of TiO₂, Fe₂O₃, MgO, Al₂O₃, LOI, Ni, Cr, and Zr typifies glacial stages, with the most marked increases during MIS 7.4 and 6.6. Reducing conditions during glacial times are indicated by peaks in the Fe₂O₃ content and coinciding low Fe₂O₃/MnO ratios. This conclusion also is supported by P₂O₅ and MnO enrichment, indicating an increased abundance of authigenic, fine-grained vivianite. Elemental ratios (CIA, CIW, PIA, and Rb/Sr) indicate that glacial sediments are depleted in mobile elements, like Na, Ca, K and Sr. This depletion was caused by changes in the sedimentation regime and thus reflects environmental changes.