Data set on sedimentology, palaeoecology and chronology of Middle to Late Pleistocene deposits on the Taimyr Peninsula, Arctic RussiaShow others and affiliations
2019 (English)In: Data in Brief, E-ISSN 2352-3409, Vol. 25, p. 1-35, article id 104267Article in journal (Refereed) Published
Abstract [en]
This Data in Brief paper contains data (including images) from Quaternary sedimentary successions investigated along the Bol'shaya Balakhnya River and the Luktakh-Upper Taimyra-Logata river system on southern Taimyr Peninsula, NW Siberia (Russia). Marine foraminifera and mollusc fauna composition, extracted from sediment samples, is presented. The chronology (time of deposition) of the sediment successions is reconstructed from three dating methods; (i) radiocarbon dating of organic detritus (from lacustrine/fluvial sediment) and molluscs (marine sediment) as finite ages (usually <42 000 years) or as non-finite ages (>42 000-48 000 years) on samples/sediments beyond the radiocarbon dating limit; (ii) Electron Spin Resonance (ESR) dating on marine molluscs (up to ages >400 000 years); (iii) Optically Stimulated Luminescence (OSL) dating, usually effective up to 100-150 0000 years. Terrestrial Cosmogenic Nuclide (TCN) exposure dating has been applied to boulders resting on top of moraine ridges (Ice Marginal Zones). See (Moller et al., 2019) (doi.org/10.1016/j.earscirev.2019.04.004) for interpretation and discussion of all data. (c) 2019 The Author(s). Published by Elsevier Inc. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
Place, publisher, year, edition, pages
Elsevier, 2019. Vol. 25, p. 1-35, article id 104267
Keywords [en]
Taimyr, Glacial sedimentology, Glacial history, Kara Sea ice sheet, OSL dating, ESR dating, TCN dating
National Category
Earth and Related Environmental Sciences
Research subject
Environmental Science, Paleoecology
Identifiers
URN: urn:nbn:se:lnu:diva-90329DOI: 10.1016/j.dib.2019.104267ISI: 000495104500290PubMedID: 31388521Scopus ID: 2-s2.0-85069853250OAI: oai:DiVA.org:lnu-90329DiVA, id: diva2:1374219
2019-11-292019-11-292025-02-07Bibliographically approved