Lithology of sediment core ENTARNOY, Russia
Cobertura |
LATITUDE: 59.000000 * LONGITUDE: 78.333333 * MINIMUM DEPTH, sediment/rock: 0.8500 m * MAXIMUM DEPTH, sediment/rock: 5.8000 m |
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Data(s) |
12/11/2014
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Formato |
text/tab-separated-values, 15 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.838584 doi:10.1594/PANGAEA.838584 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
Anderson, 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 Arkhipov, SA; Levina, TP; Panychev, VA (1980): Palynological characteristics of two Holocene peats from the middle and lower Ob River valley [in Russian]. In: V.N. Saks (ed.) Paleopalynology of Siberia. Nauka, Moscow, 123-127 Neishtadt, Mark Ilich (1976): About environmental changes in middle taiga of western Siberia during the Holocene [in Russian]. In: E.D. Zaklinskaya and M.I. Neishtadt (eds.) Palynology of the USSR. Nauka, Moscow, 156-161 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; ENTARNOY; Entarnoye; Lithology/composition/facies; Russia |
Tipo |
Dataset |