History of the vegetation during the middle and late Wurm and the Holocene in the upper Ob valley [in Russian].

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dc.contributor.authorArkhipov, S A
dc.coverage.spatialLATITUDE: 55.000000 * LONGITUDE: 83.000000 * MINIMUM DEPTH, sediment/rock: 0.2000 m * MAXIMUM DEPTH, sediment/rock: 4.8000 m
dc.date.accessioned2019-11-13T04:45:52Z
dc.date.available2019-11-13T04:45:52Z
dc.date.issued2014-11-12
dc.formattext/tab-separated-values, 15 data points
dc.identifierhttps://doi.pangaea.de/10.1594/PANGAEA.838636
dc.identifierhttps://doi.org/10.1594/PANGAEA.838636
dc.identifier.citationArkhipov, S A; Votakh, M R (1973): History of the vegetation during the middle and late Wurm and the Holocene in the upper Ob valley [in Russian]. In: V.N. Saks (ed.) The Pleistocene of Siberia and neighboring regions. Nauka, Moscow, 130-143
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/6509
dc.language.isoen
dc.publisherPANGAEA
dc.relationArkhipov, S A; Votakh, M R (1973): History of the vegetation during the middle and late Wurm and the Holocene in the upper Ob valley [in Russian]. In: V.N. Saks (ed.) The Pleistocene of Siberia and neighboring regions. Nauka, Moscow, 130-143
dc.relation.isbasedonAnderson, Patricia M; Lozhkin, Anatoly V (2002): Late Quaternary vegetation and climate of Siberia and the Russian far east (Palynological and Radiocarbon Database). North East Science Center, Far East Branch, Russian Academy of Sciences, Magadan, Russia
dc.rightsCC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rightsAccess constraints: unrestricted
dc.subjectDEPTH, sediment/rock
dc.subjectKARGOPOL
dc.subjectKargopolovo
dc.subjectLithology/composition/facies
dc.subjectRussia
dc.titleHistory of the vegetation during the middle and late Wurm and the Holocene in the upper Ob valley [in Russian].
dc.title.alternativeLithology of sediment core KARGOPOL, Russia
dc.typeDataset

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