UPPER VENDIAN NEMAKIT-DALDYNIAN STAGE ON THE SIBERIAN PLATFORM

A recent revision of the volume and the age of the Nemakit-Daldynian Stage of the Upper Vendian articulated its comprehensive (bio- and chemostratigraphic) characteristic. This stage includes strata ranging from the first appearance of unequivocal anabaritids (approximately 539 Ma) to the base of the Nochoroicyathus sunnaginicus Assemblage Zone of the Lower Cambrian Tommotian Stage (530 Ma). In addition to the characteristic assemblages of small shelly fossils (SSF), this stratigraphic interval is defined by specific changes in the trace fossil assembalges and by variations of carbon isotope composition in carbonates. Using the established criteria, this study evaluates the completeness of the Nemakit-Daldynian Stage in its type locality (western Anabar Uplift) and in other sections of the Siberian Platform (eastern Anabar Uplift, Olenek Uplift, Kharaulakh Uplift, Uchur-Maya Region, Patom Basin, Baikal area, Irkutsk Cis-Sayans Uplift, Biryusa Cis-Sayans Uplift, southern Yenisei Ridge, northern Yenisei Ridge, Turukhansk Uplift, Igarka Uplift, and inner regions of the Platform).

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Publication Details

Journal
Russian Geology and Geophysics
Published
2025-10-14
DOI
https://doi.org/10.2113/rgg20254911
Primary Topic
Geological Studies and Exploration
Type
article
Field-Weighted Citation Impact
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article

UPPER VENDIAN NEMAKIT-DALDYNIAN STAGE ON THE SIBERIAN PLATFORM

Vasiliy V. Marusin
Russian Geology and Geophysics
Geological Studies and Exploration
article

UPPER VENDIAN NEMAKIT-DALDYNIAN STAGE ON THE SIBERIAN PLATFORM

Vasiliy V. Marusin
article en

Abstract

A recent revision of the volume and the age of the Nemakit-Daldynian Stage of the Upper Vendian articulated its comprehensive (bio- and chemostratigraphic) characteristic. This stage includes strata ranging from the first appearance of unequivocal anabaritids (approximately 539 Ma) to the base of the Nochoroicyathus sunnaginicus Assemblage Zone of the Lower Cambrian Tommotian Stage (530 Ma). In addition to the characteristic assemblages of small shelly fossils (SSF), this stratigraphic interval is defined by specific changes in the trace fossil assembalges and by variations of carbon isotope composition in carbonates. Using the established criteria, this study evaluates the completeness of the Nemakit-Daldynian Stage in its type locality (western Anabar Uplift) and in other sections of the Siberian Platform (eastern Anabar Uplift, Olenek Uplift, Kharaulakh Uplift, Uchur-Maya Region, Patom Basin, Baikal area, Irkutsk Cis-Sayans Uplift, Biryusa Cis-Sayans Uplift, southern Yenisei Ridge, northern Yenisei Ridge, Turukhansk Uplift, Igarka Uplift, and inner regions of the Platform).

Russian Geology and GeophysicsVol. 66(11)
Novosibirsk State University (RU), Institute of Petroleum Geology and Geophysics (RU)
Siberian Branch, Russian Academy of Sciences, Russian Science Foundation, Lomonosov Moscow State University, Institut Pierre-Gilles de Gennes, Russian Academy of Sciences
Openalex Percentile: Top 60%
Geological Studies and Exploration
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UPPER VENDIAN NEMAKIT-DALDYNIAN STAGE ON THE SIBERIAN PLATFORM — Vasiliy V. Marusin · Russian Geology and Geophysics (2025) | TGRS Research Map | TGRS