Modern Sedimentation Patterns in Lake El'gygytgyn, NE Russia, Derived from Surface Sediment and Inlet Streams Samples V Wennrich University of Cologne

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Modern Sedimentation Patterns in Lake El'gygytgyn, NE Russia, Derived from Surface Sediment and Inlet Streams Samples V Wennrich University of Cologne University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers Faculty of Science, Medicine and Health 2013 Modern sedimentation patterns in Lake El'gygytgyn, NE Russia, derived from surface sediment and inlet streams samples V Wennrich University of Cologne Alexander Francke University of Wollongong, [email protected] A Dehnert Swiss Federal Nuclear Safety Inspectorate ENSI O Juschus Eberswalde University for Sustainable Development T Leipe Leibniz Institute For Baltic Sea Research See next page for additional authors Publication Details Wennrich, V., Francke, A., Dehnert, A., Juschus, O., Leipe, T., Vogt, C., Brigham-Grette, J., Minyuk, P. S., Melles, M. et al (2013). Modern sedimentation patterns in Lake El'gygytgyn, NE Russia, derived from surface sediment and inlet streams samples. Climate of the Past, 9 135-148. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Modern sedimentation patterns in Lake El'gygytgyn, NE Russia, derived from surface sediment and inlet streams samples Abstract Lake El'gygytgyn/NE Russia holds a continuous 3.58 Ma sediment record, which is regarded as the most long-lasting climate archive of the terrestrial Arctic. Based on multi-proxy geochemical, mineralogical, and granulometric analyses of surface sediment, inlet stream and bedrock samples, supplemented by statistical methods, major processes influencing the modern sedimentation in the lake were investigated. Grain-size parameters and chemical elements linked to the input of feldspars from acidic bedrock indicate a wind- induced two-cell current system as major driver of sediment transport and accumulation processes in Lake El'gygytgyn. The distribution of mafic ockr related elements in the sediment on the lake floor can be traced back to the input of weathering products of basaltic rocks in the catchment. Obvious similarities in the spatial variability of manganese and heavy metals indicate sorption or co-precipitation of these elements with Fe and Mn hydroxides and oxides. But the similar distribution of organic matter and clay contents might also point to a fixation to organic components and clay minerals. An enrichment of mercury in the inlet streams might be indicative of neotectonic activity around the lake. The er sults of this study add to the fundamental knowledge of the modern lake processes of Lake El'gygytgyn and its lake-catchment interactions, and thus, yield crucial insights for the interpretation of paleo-data from this unique archive. Disciplines Medicine and Health Sciences | Social and Behavioral Sciences Publication Details Wennrich, V., Francke, A., Dehnert, A., Juschus, O., Leipe, T., Vogt, C., Brigham-Grette, J., Minyuk, P. S., Melles, M. et al (2013). Modern sedimentation patterns in Lake El'gygytgyn, NE Russia, derived from surface sediment and inlet streams samples. Climate of the Past, 9 135-148. Authors V Wennrich, Alexander Francke, A Dehnert, O Juschus, T Leipe, C Vogt, J Brigham-Grette, P S. Minyuk, and Martin Melles This journal article is available at Research Online: http://ro.uow.edu.au/smhpapers/4887 Clim. Past, 9, 135–148, 2013 www.clim-past.net/9/135/2013/ Climate doi:10.5194/cp-9-135-2013 of the Past © Author(s) 2013. CC Attribution 3.0 License. Modern sedimentation patterns in Lake El’gygytgyn, NE Russia, derived from surface sediment and inlet streams samples V. Wennrich1, A. Francke1, A. Dehnert2, O. Juschus3, T. Leipe4, C. Vogt5, J. Brigham-Grette6, P. S. Minyuk7, M. Melles1, and El’gygytgyn Science Party 1University of Cologne, Institute for Geology and Mineralogy, Cologne, Germany 2Swiss Federal Nuclear Safety Inspectorate ENSI, Brugg, Switzerland 3Eberswalde University for Sustainable Development, Eberswalde, Germany 4Leibniz Institute for Baltic Sea Research Warnemuende, Marine Geology, Rostock, Germany 5University Bremen, Department of Geosciences, Crystallography/ZEKAM, Bremen, Germany 6University of Massachusetts, Department of Geosciences, Amherst, USA 7Russian Academy of Sciences, Northeast Interdisciplinary Scientific Research Institute, Magadan, Russia Correspondence to: V. Wennrich ([email protected]) Received: 27 April 2012 – Published in Clim. Past Discuss.: 1 June 2012 Revised: 19 October 2012 – Accepted: 10 December 2012 – Published: 22 January 2013 Abstract. Lake El’gygytgyn/NE Russia holds a continuous 1 Introduction 3.58 Ma sediment record, which is regarded as the most long- lasting climate archive of the terrestrial Arctic. Based on multi-proxy geochemical, mineralogical, and granulometric In spring 2009, the ICDP El’gygytgyn Drilling Project re- analyses of surface sediment, inlet stream and bedrock sam- covered the 318-m long lacustrine sediment record of Lake ples, supplemented by statistical methods, major processes El’gygytgyn in Chukotka, NE Russia (Melles et al., 2011, influencing the modern sedimentation in the lake were inves- 2012; Fig. 1). Long high-resolution lake sediment records tigated. Grain-size parameters and chemical elements linked are known to well document regional hydrologic and cli- to the input of feldspars from acidic bedrock indicate a wind- matic responses to atmospheric changes (Brigham-Grette et induced two-cell current system as major driver of sediment al., 2007a), and therefore are valuable archives of climate and transport and accumulation processes in Lake El’gygytgyn. environmental changes (e.g. Allen et al., 1999; Gasse et al., The distribution of mafic rock related elements in the sed- 2011; Cohen, 2012). Given their often continuous sediment iment on the lake floor can be traced back to the input of sequences, large and old lake basins play an important role weathering products of basaltic rocks in the catchment. Ob- in collecting sedimentological information providing a conti- vious similarities in the spatial variability of manganese and nental signature to couple with the marine realm. Thus, these heavy metals indicate sorption or co-precipitation of these el- lakes help to close gaps in the knowledge on land–ocean in- ements with Fe and Mn hydroxides and oxides. But the sim- teractions through time. Nevertheless, the profound interpre- ilar distribution of organic matter and clay contents might tation of proxy data derived from lake sediment records re- also point to a fixation to organic components and clay min- quires an in-depth knowledge of the lake-specific modern bi- erals. An enrichment of mercury in the inlet streams might ological and sedimentological processes and their controlling be indicative of neotectonic activity around the lake. The factors (e.g. Vogel et al., 2010; Viehberg et al., 2012). results of this study add to the fundamental knowledge of Lake El’gygytgyn represents a unique site, because it the modern lake processes of Lake El’gygytgyn and its lake- holds the most long-lasting climate archive of the terres- catchment interactions, and thus, yield crucial insights for the trial Arctic (Melles et al., 2011, 2012), reaching back to the interpretation of paleo-data from this unique archive. time of meteorite impact event 3.58 Ma ago (Layer, 2000). Furthermore, the basin was never overcome by large Ceno- zoic continental ice-masses (Glushkova, 2001; Glushkova Published by Copernicus Publications on behalf of the European Geosciences Union. 136 V. Wennrich et al.: Modern sedimentation patterns in Lake El’gygytgyn tigated (e.g. Cremer and Wagner, 2003; Cremer et al., 2005; a 70°N Arctic Ocean Nolan and Brigham-Grette, 2007; Nolan et al., 2002; Fe- SIBERIA ALASKA dorov et al., 2012), and a variety of modern to sub-recent sample sets were taken for study (Melles et al., 2005). Lake El‘gygytgyn 60°N Bering Here, we present the combined results of a multi-proxy 180° 150°E Sea 150°W and statistical approach to enhance the understanding of the b modern sedimentation of Lake El’gygytgyn by analyzing a 1 set of surface sediment and inlet streams samples, as well 2 560 as hand samples from the surrounding bedrock. The major 540520 3 500 goal of this study is to provide information concerning the 4 dominant sedimentation patterns in the lake controlled by 5 climate-driven transport processes, bedrock geology, post- -170 6 depositional processes, but possibly also influenced by tec- -160 7 tonic activity. In combination with recent climatologic and 8 -150 hydrologic data (Nolan, 2012; Fedorov et al., 2012), these findings will enhance our understanding of fundamental in- 9 lake processes, and thus, form an important basis for the in- 10 terpretation of the Lake El’gygytgyn paleo-record extending 11 to 3.58 Ma. 12 0 1 2 3 4 5 km 2 Study site Fig. 1. (a) Map showing the locationFigure of1 Lake El’gygytgyn in the western Beringian Arctic, (b) geological map of the El’gygytgyn Lake El’gygytgyn (67◦300 N, 172◦050 E, 492 m a.s.l.; Fig. 1) impact impact crater illustrating the major stratigraphic units (mod- is located within the Anadyr Mountain Range in central ified after Nowaczyk et al., 2002) and major fault systems (compiled Chukotka/ Far East Russian Arctic. Today, the roughly cir- after Belyi and Belaya, 1998; Belyi and Raikevich, 1994) in the lake cular lake has a diameter of ∼ 12 km and a maximum wa- catchment, bathymetric contour lines in the lake (modified after Be- ter depth of 175 m (Nolan and Brigham-Grette, 2007; Melles lyi, 2001), and locations of lake floor and bedrock samples used in et al., 2007), filling the deepest part of the ∼ 18-km wide this study as well as of ICDP site 5011-1.; (1) Koekvun’ Formation (basalt, andesite-basalt, tuff, tuff-breccia, sandstone, tuff-siltstone), El’gygytgyn impact crater (Gurov et al., 2007). With a sur- 2 (2) Ergyvaam Formation (ignimbrite, tuff), (3) Pykarvaam Forma- face area of ∼ 110 km , the lake is fed by 50 ephemeral 2 tion (ignimbrite, tuff), (4) Voron’in Formation (ignimbrite, tuff), (5) streams draining a watershed area of 293 km defined by the dykes, stocks, and sills of subvolcanic rocks, (6) flood plain de- crater rim (Nolan et al., 2002; Fig.
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