Sedimentary evolution and environmental history of Lake Van (Turkey) over the past 600 000 years. Issue 6 (5th May 2014)

• Record Type: Journal Article
• Authors: Stockhecke, Mona; Sturm, Michael; Brunner, Irene; Schmincke, Hans‐Ulrich; Sumita, Mari; Kipfer, Rolf; Cukur, Deniz; Kwiecien, Ola; Anselmetti, Flavio S.; Ariztegui, Daniel
• Is Part Of: Sedimentology. Volume 61:Issue 6(2014)
• Page Start: 1830
• Page End: 1861
• Publication Date: 2014-05-05
• Subjects: Sedimentology -- Periodicals; 552.5
• DOI: 10.1111/sed.12118
• Languages: English
• ISSNs: 0037-0746

Abstract

<abstract abstract-type="main" id="sed12118-abs-0001"> <title>Abstract</title> <p>The lithostratigraphic framework of Lake Van, eastern Turkey, has been systematically analysed to document the sedimentary evolution and the environmental history of the lake during the past <italic>ca</italic> 600 000 years. The lithostratigraphy and chemostratigraphy of a 219 m long drill core from Lake Van serve to separate global climate oscillations from local factors caused by tectonic and volcanic activity. An age model was established based on the climatostratigraphic alignment of chemical and lithological signatures, validated by <sup>40</sup>Ar/<sup>39</sup>Ar ages. The drilled sequence consists of <italic>ca</italic> 76% lacustrine carbonaceous clayey silt, <italic>ca</italic> 2% fluvial deposits, <italic>ca</italic> 17% volcaniclastic deposits and 5% gaps. Six lacustrine lithotypes were separated from the fluvial and event deposits, such as volcaniclastics (<italic>ca</italic> 300 layers) and graded beds (<italic>ca</italic> 375 layers), and their depositional environments are documented. These lithotypes are: (i) graded beds frequently intercalated with varved clayey silts reflecting rising lake levels during the terminations; (ii) varved clayey silts reflecting strong seasonality and an intralake oxic–anoxic boundary, for example, lake‐level highstands during interglacials/interstadials; (iii) CaCO<sub>3</sub>‐rich banded sediments which are representative of a lowering of the oxic–anoxic boundary, for example, lake level decreases during glacial inceptions; (iv) CaCO<sub>3</sub>‐poor banded and mottled clayey silts reflecting an oxic–anoxic boundary close to the sediment–water interface, for example, lake‐level lowstands during glacials/stadials; (v) diatomaceous muds were deposited during the early beginning of the lake as a fresh water system; and (vi) fluvial sands and gravels indicating the initial flooding of the lake basin. The recurrence of lithologies (i) to (iv) follows the past five glacial/interglacial cycles. A 20 m thick disturbed unit reflects an interval of major tectonic activity in Lake Van at <italic>ca</italic> 414 ka <sc>bp</sc>. Although local environmental processes such as tectonic and volcanic activity influenced sedimentation, the lithostratigraphic pattern and organic matter content clearly reflect past global climate changes, making Lake Van an outstanding terrestrial archive of unprecedented sensitivity for the reconstruction of the regional climate over the last 600 000 years.</p> </abstract>