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Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai. / Sennikov, N. V.; Timokhin, A. V.; Lykova, E. V.

в: Russian Geology and Geophysics, Том 58, № 6, 01.06.2017, стр. 711-726.

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

Harvard

Sennikov, NV, Timokhin, AV & Lykova, EV 2017, 'Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai', Russian Geology and Geophysics, Том. 58, № 6, стр. 711-726. https://doi.org/10.1016/j.rgg.2016.03.019

APA

Sennikov, N. V., Timokhin, A. V., & Lykova, E. V. (2017). Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai. Russian Geology and Geophysics, 58(6), 711-726. https://doi.org/10.1016/j.rgg.2016.03.019

Vancouver

Sennikov NV, Timokhin AV, Lykova EV. Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai. Russian Geology and Geophysics. 2017 июнь 1;58(6):711-726. doi: 10.1016/j.rgg.2016.03.019

Author

Sennikov, N. V. ; Timokhin, A. V. ; Lykova, E. V. / Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai. в: Russian Geology and Geophysics. 2017 ; Том 58, № 6. стр. 711-726.

BibTeX

@article{58d7bc593cb64f36a713ed8cebe2ca85,
title = "Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai",
abstract = "A biostratigraphic analysis of the Middle Ordovician reference sections of northeastern Gorny Altai is carried out. We study complexes of pelagic graptolites and benthic trilobites from the Dapingian–Darriwilian Tuloi and Karasu Formations. For the first time for the Late Paleozoic sedimentary basins of Siberia, lithofacies and biofacies analyses of the sedimentary successions and associated paleobiota are applied to estimation of the depths of the shelf basin and the remoteness of its particular parts from the shoreline. Proposed reconstructions are based on a complex analysis of lithology and thickness of the successions and the structure of associated complexes of pelagic organisms, graptolites (including evaluation of the population density and dominating taxa). Herein we appraise the bioindicator potential of the benthic trilobite paleocommunities.",
keywords = "biofacies and lithofacies analyses, Gorny Altai, graptolites, Ordovician, paleobasin depth, trilobites, FAUNA, ZONATION, ECOLOGY, OSTRACODES, LITHOFACIES",
author = "Sennikov, {N. V.} and Timokhin, {A. V.} and Lykova, {E. V.}",
year = "2017",
month = jun,
day = "1",
doi = "10.1016/j.rgg.2016.03.019",
language = "English",
volume = "58",
pages = "711--726",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "6",

}

RIS

TY - JOUR

T1 - Depth differentiation of the Middle Ordovician graptolite and trilobite complexes of Gorny Altai

AU - Sennikov, N. V.

AU - Timokhin, A. V.

AU - Lykova, E. V.

PY - 2017/6/1

Y1 - 2017/6/1

N2 - A biostratigraphic analysis of the Middle Ordovician reference sections of northeastern Gorny Altai is carried out. We study complexes of pelagic graptolites and benthic trilobites from the Dapingian–Darriwilian Tuloi and Karasu Formations. For the first time for the Late Paleozoic sedimentary basins of Siberia, lithofacies and biofacies analyses of the sedimentary successions and associated paleobiota are applied to estimation of the depths of the shelf basin and the remoteness of its particular parts from the shoreline. Proposed reconstructions are based on a complex analysis of lithology and thickness of the successions and the structure of associated complexes of pelagic organisms, graptolites (including evaluation of the population density and dominating taxa). Herein we appraise the bioindicator potential of the benthic trilobite paleocommunities.

AB - A biostratigraphic analysis of the Middle Ordovician reference sections of northeastern Gorny Altai is carried out. We study complexes of pelagic graptolites and benthic trilobites from the Dapingian–Darriwilian Tuloi and Karasu Formations. For the first time for the Late Paleozoic sedimentary basins of Siberia, lithofacies and biofacies analyses of the sedimentary successions and associated paleobiota are applied to estimation of the depths of the shelf basin and the remoteness of its particular parts from the shoreline. Proposed reconstructions are based on a complex analysis of lithology and thickness of the successions and the structure of associated complexes of pelagic organisms, graptolites (including evaluation of the population density and dominating taxa). Herein we appraise the bioindicator potential of the benthic trilobite paleocommunities.

KW - biofacies and lithofacies analyses

KW - Gorny Altai

KW - graptolites

KW - Ordovician

KW - paleobasin depth

KW - trilobites

KW - FAUNA

KW - ZONATION

KW - ECOLOGY

KW - OSTRACODES

KW - LITHOFACIES

UR - http://www.scopus.com/inward/record.url?scp=85020297313&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.03.019

DO - 10.1016/j.rgg.2016.03.019

M3 - Article

AN - SCOPUS:85020297313

VL - 58

SP - 711

EP - 726

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 6

ER -

ID: 9639929