Research output: Contribution to journal › Article › peer-review
Biostratigraphy and Sedimentary Settings of the Middle Devonian Succession of the Yuryung-Tumus Peninsula, Khatanga Gulf of the Laptev Sea. / Sennikov, N. V.; Shcherbanenko, T. A.; Varaksina, I. V. et al.
In: Stratigraphy and Geological Correlation, Vol. 26, No. 3, 01.05.2018, p. 267-282.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Biostratigraphy and Sedimentary Settings of the Middle Devonian Succession of the Yuryung-Tumus Peninsula, Khatanga Gulf of the Laptev Sea
AU - Sennikov, N. V.
AU - Shcherbanenko, T. A.
AU - Varaksina, I. V.
AU - Izokh, N. G.
AU - Sobolev, E. S.
AU - Yazikov, A. Yu
PY - 2018/5/1
Y1 - 2018/5/1
N2 - The age of the Paleozoic sedimentary successions of the Yuryung-Tumus Peninsula in the Khatanga Gulf is determined as Middle Devonian, late Eifelian, and the beginning of the early Givetian on the basis of the study of brachiopods, ammonoids, nautiloids, bactritoids, gastropods, and conodonts, and in the terminology of the standard conodont succession, these deposits are not older than the late Eifelian Tortodus kockelianus Zone, but include the terminal Eifelian Polygnathus ensensis Zone and the first Givetian Polygnathus hemiansatus Zone and are no younger than the beginning of the early Givetian Polygnathus varcus Zone. The Middle Devonian sedimentary successions of the Yuryung-Tumus Peninsula show the level of the global sedimentary Kačak Event. The areas of distribution of the Devonian sedimentary deposits in the Yuryung-Tumus Peninsula in the Khatanga Gulf should be considered as one of the fragments of the regional geological structures of a remote (isolated?) region of the Taymyr Fold System rather than a component of the structures of the northern Siberian Platform.
AB - The age of the Paleozoic sedimentary successions of the Yuryung-Tumus Peninsula in the Khatanga Gulf is determined as Middle Devonian, late Eifelian, and the beginning of the early Givetian on the basis of the study of brachiopods, ammonoids, nautiloids, bactritoids, gastropods, and conodonts, and in the terminology of the standard conodont succession, these deposits are not older than the late Eifelian Tortodus kockelianus Zone, but include the terminal Eifelian Polygnathus ensensis Zone and the first Givetian Polygnathus hemiansatus Zone and are no younger than the beginning of the early Givetian Polygnathus varcus Zone. The Middle Devonian sedimentary successions of the Yuryung-Tumus Peninsula show the level of the global sedimentary Kačak Event. The areas of distribution of the Devonian sedimentary deposits in the Yuryung-Tumus Peninsula in the Khatanga Gulf should be considered as one of the fragments of the regional geological structures of a remote (isolated?) region of the Taymyr Fold System rather than a component of the structures of the northern Siberian Platform.
KW - ammonoids
KW - brachiopods
KW - conodonts
KW - Devonian
KW - global Kačak Event
KW - Yuryung-Tumus Peninsula
KW - global Kacak Event
UR - http://www.scopus.com/inward/record.url?scp=85048251062&partnerID=8YFLogxK
U2 - 10.1134/S0869593818030103
DO - 10.1134/S0869593818030103
M3 - Article
AN - SCOPUS:85048251062
VL - 26
SP - 267
EP - 282
JO - Stratigraphy and Geological Correlation
JF - Stratigraphy and Geological Correlation
SN - 0869-5938
IS - 3
ER -
ID: 13925074