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“Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы). / Kuz'min, A. V.; Yatskov, S. V.; Orlov, A. N.; Ivanov, A. O.

в: Paleontologicheskii Zhurnal, № 3, 01.12.1997.

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

Harvard

Kuz'min, AV, Yatskov, SV, Orlov, AN & Ivanov, AO 1997, '“Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы).', Paleontologicheskii Zhurnal, № 3.

APA

Kuz'min, A. V., Yatskov, S. V., Orlov, A. N., & Ivanov, A. O. (1997). “Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы). Paleontologicheskii Zhurnal, (3).

Vancouver

Kuz'min AV, Yatskov SV, Orlov AN, Ivanov AO. “Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы). Paleontologicheskii Zhurnal. 1997 Дек. 1;(3).

Author

Kuz'min, A. V. ; Yatskov, S. V. ; Orlov, A. N. ; Ivanov, A. O. / “Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы). в: Paleontologicheskii Zhurnal. 1997 ; № 3.

BibTeX

@article{a218f321c4f24ab78ec6c4bb79a763de,
title = "“Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы).",
abstract = "The faunistic complex of the Domanik Formation of Southern Timan is characterized by primary development of the planctonic forms and almost complete absence of benthos, that makes it significantly different from the faunistic assemblages from the underlying and overlying deposits, being formed in depth similar conditions. Changes in structure of ostracods, ammonoids, conodonts and some other faunistic groups assemblages at the boundary of the Domanik and underlying Ust-Yarega Formations are considered. Critical factors in reorganization of faunistic assemblages are the changes in the basin bottom relief, such as topographical isolation of deep-water areas from the shallow-water sedimentation zone, formation of anoxic conditions at the depressions bottom and periodic inflow of silicic acid in the bottom water layers.",
keywords = "Ammonoids, Conodonts, Devonian, Ichthyofauna, Lower Frasnian, Ostracods, Russian Platform, South Timan",
author = "Kuz'min, {A. V.} and Yatskov, {S. V.} and Orlov, {A. N.} and Ivanov, {A. O.}",
year = "1997",
month = dec,
day = "1",
language = "русский",
journal = "ПАЛЕОНТОЛОГИЧЕСКИЙ ЖУРНАЛ",
issn = "0031-031X",
publisher = "Издательство {"}Наука{"}",
number = "3",

}

RIS

TY - JOUR

T1 - “Доманиковый кризис” в развитии фауны франского морского бассейна на Южном Тимане (северо-востока Русской платформы).

AU - Kuz'min, A. V.

AU - Yatskov, S. V.

AU - Orlov, A. N.

AU - Ivanov, A. O.

PY - 1997/12/1

Y1 - 1997/12/1

N2 - The faunistic complex of the Domanik Formation of Southern Timan is characterized by primary development of the planctonic forms and almost complete absence of benthos, that makes it significantly different from the faunistic assemblages from the underlying and overlying deposits, being formed in depth similar conditions. Changes in structure of ostracods, ammonoids, conodonts and some other faunistic groups assemblages at the boundary of the Domanik and underlying Ust-Yarega Formations are considered. Critical factors in reorganization of faunistic assemblages are the changes in the basin bottom relief, such as topographical isolation of deep-water areas from the shallow-water sedimentation zone, formation of anoxic conditions at the depressions bottom and periodic inflow of silicic acid in the bottom water layers.

AB - The faunistic complex of the Domanik Formation of Southern Timan is characterized by primary development of the planctonic forms and almost complete absence of benthos, that makes it significantly different from the faunistic assemblages from the underlying and overlying deposits, being formed in depth similar conditions. Changes in structure of ostracods, ammonoids, conodonts and some other faunistic groups assemblages at the boundary of the Domanik and underlying Ust-Yarega Formations are considered. Critical factors in reorganization of faunistic assemblages are the changes in the basin bottom relief, such as topographical isolation of deep-water areas from the shallow-water sedimentation zone, formation of anoxic conditions at the depressions bottom and periodic inflow of silicic acid in the bottom water layers.

KW - Ammonoids

KW - Conodonts

KW - Devonian

KW - Ichthyofauna

KW - Lower Frasnian

KW - Ostracods

KW - Russian Platform

KW - South Timan

UR - http://www.scopus.com/inward/record.url?scp=1842690045&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:1842690045

JO - ПАЛЕОНТОЛОГИЧЕСКИЙ ЖУРНАЛ

JF - ПАЛЕОНТОЛОГИЧЕСКИЙ ЖУРНАЛ

SN - 0031-031X

IS - 3

ER -

ID: 36073025