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Noble Gases in the Sediments of Lake Van - Solute Transport and Palaeoenvironmental Reconstruction

dc.authorid Tomonaga, Yama/0000-0003-2871-8826
dc.authorid Gokdere, Aysegul Feray/0000-0002-3842-1711
dc.authorscopusid 16026037000
dc.authorscopusid 6506605535
dc.authorscopusid 55163647200
dc.authorscopusid 56264781700
dc.authorwosid Gökdere, Aysegul/Gwz-7043-2022
dc.authorwosid Tomonaga, Yama/Abg-9540-2020
dc.contributor.author Tomonaga, Yama
dc.contributor.author Brennwald, Matthias S.
dc.contributor.author Meydan, Aysegul F.
dc.contributor.author Kipfer, Rolf
dc.date.accessioned 2025-05-10T17:42:56Z
dc.date.available 2025-05-10T17:42:56Z
dc.date.issued 2014
dc.department T.C. Van Yüzüncü Yıl Üniversitesi en_US
dc.department-temp [Tomonaga, Yama; Brennwald, Matthias S.; Kipfer, Rolf] Eawag, Swiss Fed Inst Aquat Sci & Technol, CH-8600 Dubendorf, Switzerland; [Meydan, Aysegul F.] Yuzuncu Yil Univ, Dept Geol Engn, Van, Turkey; [Kipfer, Rolf] Swiss Fed Inst Technol, Inst Biogeochem & Pollutant Dynam, Zurich, Switzerland; [Kipfer, Rolf] Swiss Fed Inst Technol, Inst Geochem & Petrol, Zurich, Switzerland en_US
dc.description Tomonaga, Yama/0000-0003-2871-8826; Gokdere, Aysegul Feray/0000-0002-3842-1711 en_US
dc.description.abstract Sediment samples acquired in 2010 from the long cores of the International Continental Scientific Drilling Program (ICDP) PaleoVan drilling project on Lake Van for noble-gas analysis in the pore water allow determination of the local terrestrial He-gradient as a function of depth within a sediment column of more than 200 m. These measurements yield first insights into the physical transport mechanisms of terrigenic He through the uppermost part of unconsolidated lacustrine sediments overlying the continental crust. In line with our previous work on the spatial distribution of the terrigenic He release into Lake Van, we identify a high He concentration gradient in the uppermost 10 m of the sediment column. The He concentration gradient decreases below this depth down to approx. 160 m following in general the expectations of the modelling of radiogenic He production and transport in a sediment column with homogeneous fluid transport properties. Overall the in-situ radiogenic He production due to the decay of U and Th in the mineral phases of the sediments accounts for about 80% of the He accumulation. At approx. 190 m we observe a very high He concentration immediately below a large lithological unit characterised by strong deformations. We speculate that this local enrichment is the result of the lower effective diffusivities in the pore space that relate to the abrupt depositional history of this deformed unit. This particular lithological unit seems to act as a barrier that limits the transport of solutes in the pore space and hence might "trap" information on the past geochemical conditions in the pore water of Lake Van. The dissolved concentrations of atmospheric noble gases in the pore waters of the ICDP PaleoVan cores are used to geochemically reconstruct salinity on the time scale of 0-55 ka BP. Higher salinities in the pore water at a depth of about 20 m suggest a significantly lower lake level of Lake Van in the past. (C) 2014 Elsevier Ltd. All rights reserved. en_US
dc.description.sponsorship International Continental Scientific Drilling Program (ICDP); Deutsche Forschungsgemeinschaft (DFG); Swiss National Science Foundation (SNF) [20FI21_124972, 200021_124981, 200020_143340]; Scientific and Technological Research Council of Turkey (Tubitak); SNF; Marie Curie International Outgoing Fellowship, Project NoGOS [PIOF-GA-2012-332404]; Swiss National Science Foundation (SNF) [200020_143340, 20FI21_124972, 200021_124981] Funding Source: Swiss National Science Foundation (SNF) en_US
dc.description.sponsorship We would like to thank Urs Menet at ETH Zurich for the conception and realisation of the sediment squeezer used for the noble-gas sampling of the ICDP PaleoVan sediment cores. Thanks are also due to two anonymous reviewers for their valuable comments on the manuscript. We thank the PaleoVan team for support during the collection and sharing of data. The PaleoVan drilling campaign was funded by the International Continental Scientific Drilling Program (ICDP), the Deutsche Forschungsgemeinschaft (DFG), the Swiss National Science Foundation (SNF Grants 20FI21_124972, 200021_124981, and 200020_143340) and the Scientific and Technological Research Council of Turkey (Tubitak). The present work was supported by SNF (see the grants mentioned above) and a Marie Curie International Outgoing Fellowship (Contract No. PIOF-GA-2012-332404, Project NoGOS). en_US
dc.description.woscitationindex Science Citation Index Expanded
dc.identifier.doi 10.1016/j.quascirev.2014.09.005
dc.identifier.endpage 126 en_US
dc.identifier.issn 0277-3791
dc.identifier.issn 1873-457X
dc.identifier.scopus 2-s2.0-84909580967
dc.identifier.scopusquality Q2
dc.identifier.startpage 117 en_US
dc.identifier.uri https://doi.org/10.1016/j.quascirev.2014.09.005
dc.identifier.uri https://hdl.handle.net/20.500.14720/15710
dc.identifier.volume 104 en_US
dc.identifier.wos WOS:000345471400010
dc.identifier.wosquality Q1
dc.language.iso en en_US
dc.publisher Pergamon-elsevier Science Ltd en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.subject Icdp en_US
dc.subject Paleovan en_US
dc.subject Deep Drilling en_US
dc.subject Terrestrial He Emission en_US
dc.subject Palaeosalinity en_US
dc.title Noble Gases in the Sediments of Lake Van - Solute Transport and Palaeoenvironmental Reconstruction en_US
dc.type Article en_US

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