Facies-Stratigraphic Distribution of Organic-Walled and Silicified Microfossils in the Early Billiyakh Basin (Lower Riphean, Anabar Uplift, Siberia)
- Авторлар: Petrov P.1, Sharma M.2, Vorob’eva N.1, Sergeev V.1
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Мекемелер:
- Geological Institute, Russian Academy of Sciences
- Birbal Sahni Institute of Palaeobotany
- Шығарылым: Том 53, № 8 (2019)
- Беттер: 867-872
- Бөлім: Article
- URL: https://journals.rcsi.science/0031-0301/article/view/168904
- DOI: https://doi.org/10.1134/S0031030119080161
- ID: 168904
Дәйексөз келтіру
Аннотация
The sedimentary succession of the Anabar Uplift (North Siberia) contains the Early Riphean abundant and diverse microfossil assemblages. The Ust-Il’ya and lower Kotuikan organic-walled assemblages of prokaryotic and eukaryotic microorganisms from open shelf facies reflect the level of the marine biosphere evolution in the early Mesoproterozoic. The silicified microbiotas of the upper subformations of Kotuikan and Yusmastakh formations are represented by prokaryotic cyanobacteria only.
Негізгі сөздер
Авторлар туралы
P. Petrov
Geological Institute, Russian Academy of Sciences
Email: sergeev-micro@rambler.ru
Ресей, Moscow, 119017
M. Sharma
Birbal Sahni Institute of Palaeobotany
Хат алмасуға жауапты Автор.
Email: sharmamukund1@rediffmail.com
Үндістан, Lucknow, 226007
N. Vorob’eva
Geological Institute, Russian Academy of Sciences
Email: sergeev-micro@rambler.ru
Ресей, Moscow, 119017
V. Sergeev
Geological Institute, Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: sergeev-micro@rambler.ru
Ресей, Moscow, 119017