Standard

The occurrence of Dickinsonia in non-marine facies. / Bobkov, N. I.; Kolesnikov, A. V.; Maslov, A. V. и др.

в: Estudios Geologicos, Том 75, № 2, e096, 01.01.2019.

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

Harvard

Bobkov, NI, Kolesnikov, AV, Maslov, AV & Grazhdankin, DV 2019, 'The occurrence of Dickinsonia in non-marine facies', Estudios Geologicos, Том. 75, № 2, e096. https://doi.org/10.3989/EGEOL.43587.551

APA

Bobkov, N. I., Kolesnikov, A. V., Maslov, A. V., & Grazhdankin, D. V. (2019). The occurrence of Dickinsonia in non-marine facies. Estudios Geologicos, 75(2), [e096]. https://doi.org/10.3989/EGEOL.43587.551

Vancouver

Bobkov NI, Kolesnikov AV, Maslov AV, Grazhdankin DV. The occurrence of Dickinsonia in non-marine facies. Estudios Geologicos. 2019 янв. 1;75(2):e096. doi: 10.3989/EGEOL.43587.551

Author

Bobkov, N. I. ; Kolesnikov, A. V. ; Maslov, A. V. и др. / The occurrence of Dickinsonia in non-marine facies. в: Estudios Geologicos. 2019 ; Том 75, № 2.

BibTeX

@article{559286595f2443c483d9946c0147171a,
title = "The occurrence of Dickinsonia in non-marine facies",
abstract = "Dickinsonia in the central Urals occurs in a succession transitional from marginal marine to non-marine. Even within this sequence Dickinsonia appears to be restricted to the least marine facies interpreted as a coastal lagoon surrounded by tidal flats. Another puzzling aspect is the complete absence of other Ediacaran taxa that are usually found together with Dickinsonia in other fossil localities. In fact, the Sinii Kamen Member of the Cherny Kamen Formation yielded an assemblage of Ediacaran macrofossils including aspidellamorph and mawsonitomorph holdfasts, frondomorphs, palaeopascichnids, and concentric ring structures of microbial origin; however, fossils of Dickinsonia have never been found in this association.",
keywords = "Continental environments, Dickinsonia, Ediacaran, Soft-bodied metazoan, soft-bodied metazoan, continental environments",
author = "Bobkov, {N. I.} and Kolesnikov, {A. V.} and Maslov, {A. V.} and Grazhdankin, {D. V.}",
year = "2019",
month = jan,
day = "1",
doi = "10.3989/EGEOL.43587.551",
language = "English",
volume = "75",
journal = "Estudios Geologicos",
issn = "0367-0449",
publisher = "CSIC Consejo Superior de Investigaciones Cientificas",
number = "2",

}

RIS

TY - JOUR

T1 - The occurrence of Dickinsonia in non-marine facies

AU - Bobkov, N. I.

AU - Kolesnikov, A. V.

AU - Maslov, A. V.

AU - Grazhdankin, D. V.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - Dickinsonia in the central Urals occurs in a succession transitional from marginal marine to non-marine. Even within this sequence Dickinsonia appears to be restricted to the least marine facies interpreted as a coastal lagoon surrounded by tidal flats. Another puzzling aspect is the complete absence of other Ediacaran taxa that are usually found together with Dickinsonia in other fossil localities. In fact, the Sinii Kamen Member of the Cherny Kamen Formation yielded an assemblage of Ediacaran macrofossils including aspidellamorph and mawsonitomorph holdfasts, frondomorphs, palaeopascichnids, and concentric ring structures of microbial origin; however, fossils of Dickinsonia have never been found in this association.

AB - Dickinsonia in the central Urals occurs in a succession transitional from marginal marine to non-marine. Even within this sequence Dickinsonia appears to be restricted to the least marine facies interpreted as a coastal lagoon surrounded by tidal flats. Another puzzling aspect is the complete absence of other Ediacaran taxa that are usually found together with Dickinsonia in other fossil localities. In fact, the Sinii Kamen Member of the Cherny Kamen Formation yielded an assemblage of Ediacaran macrofossils including aspidellamorph and mawsonitomorph holdfasts, frondomorphs, palaeopascichnids, and concentric ring structures of microbial origin; however, fossils of Dickinsonia have never been found in this association.

KW - Continental environments

KW - Dickinsonia

KW - Ediacaran

KW - Soft-bodied metazoan

KW - soft-bodied metazoan

KW - continental environments

UR - http://www.scopus.com/inward/record.url?scp=85075990250&partnerID=8YFLogxK

U2 - 10.3989/EGEOL.43587.551

DO - 10.3989/EGEOL.43587.551

M3 - Article

AN - SCOPUS:85075990250

VL - 75

JO - Estudios Geologicos

JF - Estudios Geologicos

SN - 0367-0449

IS - 2

M1 - e096

ER -

ID: 22573355