Abstract

Research subject. Main problems of the General Stratigraphic Scale (GSS) of the Upper Precambrian including uncertainties in the hierarchy of subdivisions are analyzed.Results.Prospects for detailing the Upper Precambrian GSS are discussed, along with questions of its correlation with International Chronostratigraphic Chart (ICSC) and establishing the lower boundaries of chronostratigraphic subdivisions. The importance of unifying the existing views is emphasized.Conclusions.It is proposed to carry out the following reforms of GSS: to abolish Acrothemes / Acrons; to approve the Proterozoic (as well as the Archean) as an Eonotheme / Eon; to minimize the use of terms “Upper Proterozoic” and “Lower Proterozoic”; to assign the Riphean and Vendian to the rank of Erathem / Era (while preserving the status of the Vendian as a System / Period); to consider Burzyanian, Yurmatinian, Karatavian and Arshinian as Systems / Periods of the Riphean. Attention is focused on the Upper Riphean-Vendian interval. The lower boundary of the Upper Riphean (Karatavian) was proposed to establish according to the first appearance of theTrachyhystrichosphaera sp.microfossils. Then, the Terminal Riphean (Arshinian) lower boundary should be traced to the base of the tillites formed during the global Sturtian glaciation (which approximately corresponds to the base of the Cryogenian in ICSC). Apparently, the Vendian lower boundary may be raised to the level of the top of the Gaskiers tillites, as the deposits of the last major glaciation in the Precambrian. The indicated proposals are substantiated. It is necessary to form work groups to develop solutions.

Highlights

  • It is proposed to carry out the following reforms of General Stratigraphic Scale (GSS): to abolish Acrothemes / Acrons; to approve the Proterozoic as an Eonotheme / Eon; to minimize the use of terms “Upper Proterozoic” and “Lower Proterozoic”; to assign the Riphean and Vendian to the rank of Erathem / Era; to consider Burzyanian, Yurmatinian, Karatavian and Arshinian as Systems / Periods of the Riphean

  • Attention is focused on the Upper Riphean-Vendian interval

  • The Terminal Riphean (Arshinian) lower boundary should be traced to the base of the tillites formed during the global Sturtian glaciation

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Summary

Источник финансирования

Работа выполнена в рамках темы No АААА-А18-118053090044-1 госзадания ИГГ УрО РАН. Upper Precambrian General Stratigraphic Scale of Russia: Main problems and proposals for improvement. Main problems of the General Stratigraphic Scale (GSS) of the Upper Precambrian including uncertainties in the hierarchy of subdivisions are analyzed. Prospects for detailing the Upper Precambrian GSS are discussed, along with questions of its correlation with International Chronostratigraphic Chart (ICSC) and establishing the lower boundaries of chronostratigraphic subdivisions. The lower boundary of the Upper Riphean (Karatavian) was proposed to establish according to the first appearance of the Trachyhystrichosphaera sp. The Terminal Riphean (Arshinian) lower boundary should be traced to the base of the tillites formed during the global Sturtian glaciation. (2021) Upper Precambrian General Stratigraphic Scale of Russia: Main problems and proposals for improvement. Funding information The studies were carried out in accordance with the State Contract No AAAA A18-118053090044-1

ПРОБЛЕМЫ ОБЩЕЙ СТРАТИГРАФИЧЕСКОЙ ШКАЛЫ ВЕРХНЕГО ДОКЕМБРИЯ
Иерархия стратонов ОСШ
Граница протерозоя и фанерозоя
ПРЕДЛОЖЕНИЯ ПО СОВЕРШЕНСТВОВАНИЮ ОСШ ВЕРХНЕГО ДОКЕМБРИЯ
Иерархия стратонов
Взаимоотношения рифея и венда
Граница среднего и верхнего рифея
СПИСОК ЛИТЕРАТУРЫ
Full Text
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