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The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds. / Shurygin, B. N.; Dzyuba, O. S.

в: Russian Geology and Geophysics, Том 56, № 4, 01.04.2015, стр. 652-662.

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

Harvard

Shurygin, BN & Dzyuba, OS 2015, 'The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds', Russian Geology and Geophysics, Том. 56, № 4, стр. 652-662. https://doi.org/10.1016/j.rgg.2015.03.013

APA

Shurygin, B. N., & Dzyuba, O. S. (2015). The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds. Russian Geology and Geophysics, 56(4), 652-662. https://doi.org/10.1016/j.rgg.2015.03.013

Vancouver

Shurygin BN, Dzyuba OS. The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds. Russian Geology and Geophysics. 2015 апр. 1;56(4):652-662. doi: 10.1016/j.rgg.2015.03.013

Author

Shurygin, B. N. ; Dzyuba, O. S. / The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds. в: Russian Geology and Geophysics. 2015 ; Том 56, № 4. стр. 652-662.

BibTeX

@article{407967a74ae54b5592eb7b2680244ebc,
title = "The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds",
abstract = "There is no international consensus regarding the GSSP for the Berriasian, the basal stage of the Cretaceous System. Any of the events discussed by the international expert community can be regarded as a marker of the Jurassic/Cretaceous boundary: a phylogenetic change of taxa, paleomagnetic reversal, or isotopic excursion. However, the problem of identification of this level in Boreal sections can be solvedonly using a combination of data obtained by paleontological and nonpaleontological methods of stratigraphy (bio-, chemo-, magnetostratigraphy, etc.). With any of the accepted markers, the Jurassic/Cretaceous boundary in Siberian sections will be within the upper part of the regional Bazhenovo Horizon. The least interval of the uncertainty of the position of this boundary in Siberian sections will be ensured by the selection of one of two markers: biostratigraphic (base of the Pseudosubplanites grandis Subzone) or magnetostratigraphic (base of the M18r magnetozone).",
keywords = "Biostratigraphy, Chemostratigraphy, Cretaceous, Jurassic, Lithostratigraphy, Magnetostratigraphy, Siberia",
author = "Shurygin, {B. N.} and Dzyuba, {O. S.}",
year = "2015",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2015.03.013",
language = "English",
volume = "56",
pages = "652--662",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "4",

}

RIS

TY - JOUR

T1 - The Jurassic/Cretaceous boundary in northern Siberia and Boreal-Tethyan correlation of the boundary beds

AU - Shurygin, B. N.

AU - Dzyuba, O. S.

PY - 2015/4/1

Y1 - 2015/4/1

N2 - There is no international consensus regarding the GSSP for the Berriasian, the basal stage of the Cretaceous System. Any of the events discussed by the international expert community can be regarded as a marker of the Jurassic/Cretaceous boundary: a phylogenetic change of taxa, paleomagnetic reversal, or isotopic excursion. However, the problem of identification of this level in Boreal sections can be solvedonly using a combination of data obtained by paleontological and nonpaleontological methods of stratigraphy (bio-, chemo-, magnetostratigraphy, etc.). With any of the accepted markers, the Jurassic/Cretaceous boundary in Siberian sections will be within the upper part of the regional Bazhenovo Horizon. The least interval of the uncertainty of the position of this boundary in Siberian sections will be ensured by the selection of one of two markers: biostratigraphic (base of the Pseudosubplanites grandis Subzone) or magnetostratigraphic (base of the M18r magnetozone).

AB - There is no international consensus regarding the GSSP for the Berriasian, the basal stage of the Cretaceous System. Any of the events discussed by the international expert community can be regarded as a marker of the Jurassic/Cretaceous boundary: a phylogenetic change of taxa, paleomagnetic reversal, or isotopic excursion. However, the problem of identification of this level in Boreal sections can be solvedonly using a combination of data obtained by paleontological and nonpaleontological methods of stratigraphy (bio-, chemo-, magnetostratigraphy, etc.). With any of the accepted markers, the Jurassic/Cretaceous boundary in Siberian sections will be within the upper part of the regional Bazhenovo Horizon. The least interval of the uncertainty of the position of this boundary in Siberian sections will be ensured by the selection of one of two markers: biostratigraphic (base of the Pseudosubplanites grandis Subzone) or magnetostratigraphic (base of the M18r magnetozone).

KW - Biostratigraphy

KW - Chemostratigraphy

KW - Cretaceous

KW - Jurassic

KW - Lithostratigraphy

KW - Magnetostratigraphy

KW - Siberia

UR - http://www.scopus.com/inward/record.url?scp=84927951131&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.03.013

DO - 10.1016/j.rgg.2015.03.013

M3 - Article

AN - SCOPUS:84927951131

VL - 56

SP - 652

EP - 662

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 25830312