Geochemistry of the Bottom Sediments of Lake Peyungda, Tunguska Nature Reserve, and Paleoclimatic Reconstructions of the Arctic Territories of Eastern Siberia

Lake Peyungda contains annually layered bottom sediments (varves), which make it possible to build a reliable age model for the entire depth of the core. An age model was refined over the last century based on the presence of a layer of anomalous thickness associated with the fall of the Tunguska co...

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Published in:	Geochemistry international Vol. 62; no. 5; pp. 520 - 528
Main Authors:	Novikov, V. S., Darin, A. V., Babich, V. V., Darin, F. A., Rogozin, D. Yu
Format:	Journal Article
Language:	English
Published:	Moscow Pleiades Publishing 01.05.2024 Springer Springer Nature B.V
Subjects:	Aluminum Arctic zone Bottom sediments Chemical composition Climate Core sampling Depth Earth and Environmental Science Earth Sciences Epoxy resins Geochemistry Lakes Nature reserves Radiation Sediment Sedimentation & deposition Sediments Sediments (Geology) Temperature Thickness Transfer functions Varves Weather Arctic region Siberia Russia micro-XRF geochemistry bottom sediments Evenkia temperature reconstructions Tunguska Cosmic Body Lake Peyungda synchrotron radiation
ISSN:	0016-7029, 1556-1968
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Abstract	Lake Peyungda contains annually layered bottom sediments (varves), which make it possible to build a reliable age model for the entire depth of the core. An age model was refined over the last century based on the presence of a layer of anomalous thickness associated with the fall of the Tunguska cosmic body (TCB) in June 1908. The results of scanning µXRF-SI (elemental analysis along core depth) were used for comparison with regional average annual weather observation data over the time span of 1895–2000 to create a transfer function: average annual temperature as a function of the elemental composition of the dated layer of bottom sediment. Approximation of the obtained function to the depth of core sampling made it possible to reconstruct changes in regional temperature over the time interval of the last millennium with an annual time resolution. Comparison of the obtained reconstruction with literature data on reconstructions for the Arctic region over the past 1000 years shows the presence of general trends and extremes, which confirms the reliability of the obtained results.
AbstractList	Lake Peyungda contains annually layered bottom sediments (varves), which make it possible to build a reliable age model for the entire depth of the core. An age model was refined over the last century based on the presence of a layer of anomalous thickness associated with the fall of the Tunguska cosmic body (TCB) in June 1908. The results of scanning µXRF-SI (elemental analysis along core depth) were used for comparison with regional average annual weather observation data over the time span of 1895–2000 to create a transfer function: average annual temperature as a function of the elemental composition of the dated layer of bottom sediment. Approximation of the obtained function to the depth of core sampling made it possible to reconstruct changes in regional temperature over the time interval of the last millennium with an annual time resolution. Comparison of the obtained reconstruction with literature data on reconstructions for the Arctic region over the past 1000 years shows the presence of general trends and extremes, which confirms the reliability of the obtained results.
Audience	Academic
Author	Darin, A. V. Babich, V. V. Novikov, V. S. Darin, F. A. Rogozin, D. Yu
Author_xml	– sequence: 1 givenname: V. S. surname: Novikov fullname: Novikov, V. S. email: novikovvs@igm.nsc.ru organization: Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences – sequence: 2 givenname: A. V. surname: Darin fullname: Darin, A. V. organization: Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences – sequence: 3 givenname: V. V. surname: Babich fullname: Babich, V. V. organization: Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences – sequence: 4 givenname: F. A. surname: Darin fullname: Darin, F. A. organization: Siberian Ring Photon Source Center for the Collective Use, Institute of Catalysis, Siberian Branch, Russian Academy of Sciences – sequence: 5 givenname: D. Yu surname: Rogozin fullname: Rogozin, D. Yu organization: Institute of Biophysics, Siberian Branch, Russian Academy of Sciences
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Cites_doi	10.1134/S1028334X20060045 10.1038/srep00609 10.1134/S1995425515040022 10.1038/nature09051 10.1007/s00382-013-1701-4 10.1016/j.gloplacha.2011.03.004 10.24057/2071-9388-2014-7-1-16-29 10.3103/S106287381302010X 10.1016/j.accre.2023.06.003 10.1016/j.quaint.2009.02.005 10.1016/j.rgg.2011.03.008 10.1046/j.1365-2699.2000.00432.x 10.3103/S106287381911008X 10.1134/S1028334X23600044 10.1177/0959683608098952 10.1007/s10933-007-9119-9 10.1134/S0001433821010114 10.3354/cr01112 10.1007/978-3-662-103135_7 10.1007/1-4020-21224 10.1038/ngeo1797
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Copyright	Pleiades Publishing, Ltd. 2024. ISSN 0016-7029, Geochemistry International, 2024, Vol. 62, No. 5, pp. 520–528. © Pleiades Publishing, Ltd., 2024. COPYRIGHT 2024 Springer Pleiades Publishing, Ltd. 2024.
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Snippet	Lake Peyungda contains annually layered bottom sediments (varves), which make it possible to build a reliable age model for the entire depth of the core. An...
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SubjectTerms	Aluminum Arctic zone Bottom sediments Chemical composition Climate Core sampling Depth Earth and Environmental Science Earth Sciences Epoxy resins Geochemistry Lakes Nature reserves Radiation Sediment Sedimentation & deposition Sediments Sediments (Geology) Temperature Thickness Transfer functions Varves Weather
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Title	Geochemistry of the Bottom Sediments of Lake Peyungda, Tunguska Nature Reserve, and Paleoclimatic Reconstructions of the Arctic Territories of Eastern Siberia
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Volume	62
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