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Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia. / Kuzmina, O. B.; Kuzmin, D. V.; Shurygin, B. N.

в: Doklady Earth Sciences, Том 474, № 2, 01.06.2017, стр. 620-623.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Kuzmina, OB, Kuzmin, DV & Shurygin, BN 2017, 'Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia', Doklady Earth Sciences, Том. 474, № 2, стр. 620-623. https://doi.org/10.1134/S1028334X17060204

APA

Kuzmina, O. B., Kuzmin, D. V., & Shurygin, B. N. (2017). Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia. Doklady Earth Sciences, 474(2), 620-623. https://doi.org/10.1134/S1028334X17060204

Vancouver

Kuzmina OB, Kuzmin DV, Shurygin BN. Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia. Doklady Earth Sciences. 2017 июнь 1;474(2):620-623. doi: 10.1134/S1028334X17060204

Author

Kuzmina, O. B. ; Kuzmin, D. V. ; Shurygin, B. N. / Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia. в: Doklady Earth Sciences. 2017 ; Том 474, № 2. стр. 620-623.

BibTeX

@article{c5d65413c25849b293cead7157947bff,
title = "Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia",
abstract = "Palynological (dinocysts) and geochemical data were compared for the first time for Paleogene sediments of borehole no. 8 (settlement of Russkaya Polyana, Omsk oblast). The layers with a concentrated amount of dinocysts of the genus Pseudokomewuia (20.5% of the palynocomplex) are characterized by higher contents of Fe, P, Ti, Nb, Ta, and W. The microphytoplankton bloom (an analog of the present-day red tides) in the late Oligocene Turtas Lake–Sea was probably caused by a greater contribution of nutrient substances from the continent during the transgression of this basin. Comparative analysis of the geochemical features of marine and continental Paleogene sediments from borehole no. 8 showed that the Turtas basin was either freshwater or had brackish water.",
author = "Kuzmina, {O. B.} and Kuzmin, {D. V.} and Shurygin, {B. N.}",
year = "2017",
month = jun,
day = "1",
doi = "10.1134/S1028334X17060204",
language = "English",
volume = "474",
pages = "620--623",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia

AU - Kuzmina, O. B.

AU - Kuzmin, D. V.

AU - Shurygin, B. N.

PY - 2017/6/1

Y1 - 2017/6/1

N2 - Palynological (dinocysts) and geochemical data were compared for the first time for Paleogene sediments of borehole no. 8 (settlement of Russkaya Polyana, Omsk oblast). The layers with a concentrated amount of dinocysts of the genus Pseudokomewuia (20.5% of the palynocomplex) are characterized by higher contents of Fe, P, Ti, Nb, Ta, and W. The microphytoplankton bloom (an analog of the present-day red tides) in the late Oligocene Turtas Lake–Sea was probably caused by a greater contribution of nutrient substances from the continent during the transgression of this basin. Comparative analysis of the geochemical features of marine and continental Paleogene sediments from borehole no. 8 showed that the Turtas basin was either freshwater or had brackish water.

AB - Palynological (dinocysts) and geochemical data were compared for the first time for Paleogene sediments of borehole no. 8 (settlement of Russkaya Polyana, Omsk oblast). The layers with a concentrated amount of dinocysts of the genus Pseudokomewuia (20.5% of the palynocomplex) are characterized by higher contents of Fe, P, Ti, Nb, Ta, and W. The microphytoplankton bloom (an analog of the present-day red tides) in the late Oligocene Turtas Lake–Sea was probably caused by a greater contribution of nutrient substances from the continent during the transgression of this basin. Comparative analysis of the geochemical features of marine and continental Paleogene sediments from borehole no. 8 showed that the Turtas basin was either freshwater or had brackish water.

UR - http://www.scopus.com/inward/record.url?scp=85024098467&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17060204

DO - 10.1134/S1028334X17060204

M3 - Article

AN - SCOPUS:85024098467

VL - 474

SP - 620

EP - 623

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25830203