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Tommotian (Lower Cambrian) stratigraphy and fossil fauna communities in the Kiya River section (Kuznetsk Alatau). / Korovnikov, I. V.; Tokarev, D. A.; Novozhilova, N. V. et al.

In: Russian Geology and Geophysics, Vol. 59, No. 2, 01.02.2018, p. 186-192.

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Korovnikov IV, Tokarev DA, Novozhilova NV, Terleev AA. Tommotian (Lower Cambrian) stratigraphy and fossil fauna communities in the Kiya River section (Kuznetsk Alatau). Russian Geology and Geophysics. 2018 Feb 1;59(2):186-192. doi: 10.1016/j.rgg.2018.01.015

Author

Korovnikov, I. V. ; Tokarev, D. A. ; Novozhilova, N. V. et al. / Tommotian (Lower Cambrian) stratigraphy and fossil fauna communities in the Kiya River section (Kuznetsk Alatau). In: Russian Geology and Geophysics. 2018 ; Vol. 59, No. 2. pp. 186-192.

BibTeX

@article{5064208f9723469f813af316510c9650,
title = "Tommotian (Lower Cambrian) stratigraphy and fossil fauna communities in the Kiya River section (Kuznetsk Alatau)",
abstract = "The lower Ust{\textquoteright}-Kundat Formation has been studied in detail in a section along the Kiya River (Kuznetsk Alatau, Altai-Sayan folded area). The section was deposited during the Tommotian stage and is a stratotype for the Lower Cambrian Ust{\textquoteright}-Kundat sequence comprising several members of the Ust{\textquoteright}-Kundat Formation. Member 2 contains newly discovered and previously known species of archaeocyathids near its top found stratigraphically lower than the oldest known archaeocyathan assemblage of the Nochoroicyathus mariinskii biozone. The found archaeocyaths cannot be dated precisely and may have either Tommotian or Atdabanian ages. Small shelly fossils from the same section cover a large stratigraphic range as well. The findings call for updating the age of the upper Ust{\textquoteright}-Kundat sequence and the Tommotian upper boundary in the regional stratigraphy of the Altai-Sayan folded area.",
keywords = "Altai-Sayan folded area, archaeocyatha, small shelly fossils, stratigraphy, Tommotian Stage",
author = "Korovnikov, {I. V.} and Tokarev, {D. A.} and Novozhilova, {N. V.} and Terleev, {A. A.}",
note = "Publisher Copyright: {\textcopyright} 2018",
year = "2018",
month = feb,
day = "1",
doi = "10.1016/j.rgg.2018.01.015",
language = "English",
volume = "59",
pages = "186--192",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "2",

}

RIS

TY - JOUR

T1 - Tommotian (Lower Cambrian) stratigraphy and fossil fauna communities in the Kiya River section (Kuznetsk Alatau)

AU - Korovnikov, I. V.

AU - Tokarev, D. A.

AU - Novozhilova, N. V.

AU - Terleev, A. A.

N1 - Publisher Copyright: © 2018

PY - 2018/2/1

Y1 - 2018/2/1

N2 - The lower Ust’-Kundat Formation has been studied in detail in a section along the Kiya River (Kuznetsk Alatau, Altai-Sayan folded area). The section was deposited during the Tommotian stage and is a stratotype for the Lower Cambrian Ust’-Kundat sequence comprising several members of the Ust’-Kundat Formation. Member 2 contains newly discovered and previously known species of archaeocyathids near its top found stratigraphically lower than the oldest known archaeocyathan assemblage of the Nochoroicyathus mariinskii biozone. The found archaeocyaths cannot be dated precisely and may have either Tommotian or Atdabanian ages. Small shelly fossils from the same section cover a large stratigraphic range as well. The findings call for updating the age of the upper Ust’-Kundat sequence and the Tommotian upper boundary in the regional stratigraphy of the Altai-Sayan folded area.

AB - The lower Ust’-Kundat Formation has been studied in detail in a section along the Kiya River (Kuznetsk Alatau, Altai-Sayan folded area). The section was deposited during the Tommotian stage and is a stratotype for the Lower Cambrian Ust’-Kundat sequence comprising several members of the Ust’-Kundat Formation. Member 2 contains newly discovered and previously known species of archaeocyathids near its top found stratigraphically lower than the oldest known archaeocyathan assemblage of the Nochoroicyathus mariinskii biozone. The found archaeocyaths cannot be dated precisely and may have either Tommotian or Atdabanian ages. Small shelly fossils from the same section cover a large stratigraphic range as well. The findings call for updating the age of the upper Ust’-Kundat sequence and the Tommotian upper boundary in the regional stratigraphy of the Altai-Sayan folded area.

KW - Altai-Sayan folded area

KW - archaeocyatha

KW - small shelly fossils

KW - stratigraphy

KW - Tommotian Stage

UR - http://www.scopus.com/inward/record.url?scp=85044448464&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.01.015

DO - 10.1016/j.rgg.2018.01.015

M3 - Article

AN - SCOPUS:85044448464

VL - 59

SP - 186

EP - 192

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 2

ER -

ID: 12214457