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Chondrichthyans from the Lower Carboniferous of Yakutia, Russia. / Ivanov, A. O.

в: Paleontological Journal, Том 52, № 7, 01.12.2018, стр. 697-706.

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

Harvard

Ivanov, AO 2018, 'Chondrichthyans from the Lower Carboniferous of Yakutia, Russia', Paleontological Journal, Том. 52, № 7, стр. 697-706. https://doi.org/10.1134/S0031030118070055

APA

Ivanov, A. O. (2018). Chondrichthyans from the Lower Carboniferous of Yakutia, Russia. Paleontological Journal, 52(7), 697-706. https://doi.org/10.1134/S0031030118070055

Vancouver

Ivanov AO. Chondrichthyans from the Lower Carboniferous of Yakutia, Russia. Paleontological Journal. 2018 Дек. 1;52(7):697-706. https://doi.org/10.1134/S0031030118070055

Author

Ivanov, A. O. / Chondrichthyans from the Lower Carboniferous of Yakutia, Russia. в: Paleontological Journal. 2018 ; Том 52, № 7. стр. 697-706.

BibTeX

@article{2e70abce1fba4f2ab1f78eb3c96b1dfb,
title = "Chondrichthyans from the Lower Carboniferous of Yakutia, Russia",
abstract = "Abstract: Teeth of Cladodoides cf. wildungensis (Jaekel), fin spines of Ctenacanthus cf. angulatus Newberry et Worthen and Ctenacanthus sp. occur in the Lower Carboniferous Emyaksin Formation of the Vilyui River, Yakutia, Vilyui Syneclise, eastern part of the Siberian Platform. The assemblage includes widespread chondrichthyan taxa, along with endemic sarcopterygian fishes. The systematic position of Cladodoides is discussed. Their teeth possess some features characteristic of stethacanthids and ctenacanthids.Cladodoides is probably the basal taxon of cladodontomorph sharks.",
keywords = "Chondrichthyes, Lower Carboniferous, Russia, Yakutia",
author = "Ivanov, {A. O.}",
year = "2018",
month = dec,
day = "1",
doi = "10.1134/S0031030118070055",
language = "English",
volume = "52",
pages = "697--706",
journal = "Paleontological Journal",
issn = "0031-0301",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "7",

}

RIS

TY - JOUR

T1 - Chondrichthyans from the Lower Carboniferous of Yakutia, Russia

AU - Ivanov, A. O.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - Abstract: Teeth of Cladodoides cf. wildungensis (Jaekel), fin spines of Ctenacanthus cf. angulatus Newberry et Worthen and Ctenacanthus sp. occur in the Lower Carboniferous Emyaksin Formation of the Vilyui River, Yakutia, Vilyui Syneclise, eastern part of the Siberian Platform. The assemblage includes widespread chondrichthyan taxa, along with endemic sarcopterygian fishes. The systematic position of Cladodoides is discussed. Their teeth possess some features characteristic of stethacanthids and ctenacanthids.Cladodoides is probably the basal taxon of cladodontomorph sharks.

AB - Abstract: Teeth of Cladodoides cf. wildungensis (Jaekel), fin spines of Ctenacanthus cf. angulatus Newberry et Worthen and Ctenacanthus sp. occur in the Lower Carboniferous Emyaksin Formation of the Vilyui River, Yakutia, Vilyui Syneclise, eastern part of the Siberian Platform. The assemblage includes widespread chondrichthyan taxa, along with endemic sarcopterygian fishes. The systematic position of Cladodoides is discussed. Their teeth possess some features characteristic of stethacanthids and ctenacanthids.Cladodoides is probably the basal taxon of cladodontomorph sharks.

KW - Chondrichthyes

KW - Lower Carboniferous

KW - Russia

KW - Yakutia

UR - http://www.scopus.com/inward/record.url?scp=85059853661&partnerID=8YFLogxK

U2 - 10.1134/S0031030118070055

DO - 10.1134/S0031030118070055

M3 - Article

AN - SCOPUS:85059853661

VL - 52

SP - 697

EP - 706

JO - Paleontological Journal

JF - Paleontological Journal

SN - 0031-0301

IS - 7

ER -

ID: 38439106