The First Data on Isotope-Carbon Stratigraphy of the Asselian and Sakmarian of the Lower Permian of the Northern Verkhoyanie

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Abstract

For the first time in the North-East of Russia, changes in the values of δ13Соrg in the lower part of the Permian were detected, obtained in the Kubalakh section of the lower reaches of the Lena River and integrated with biostratigraphic data. A comparison with isotope-carbon trends identified in the Asselian and Sakmarian of the Southern Urals is proposed. Based on the established sequence of negative shifts of the carbon isotopic composition of organic matter, it is concluded that the boundary of Carboniferous and Permian in the Kubalakh section is located below the beds opened in the section and there is an 80 m break in the outcrop. The first data independent of biostratigraphic and paleontological constructions have been obtained on the Late Asselian age of the Tuora-Sis Formation containing the ammonoid association with Bulunites, the stage belonging of which has been debated for many decades. The chronostratigraphic indefinite interval between the Asselian and Samarian to the upper parts of the Jakutoproductus lenensis Beds has been significantly reduced. The data obtained indicate that the continuation of work on the chemostratigraphy of stable carbon isotopes has good prospects for substantiating the stage division and interregional correlation of the Lower Permian deposits in the Verkhoyanie.

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About the authors

V. I. Makoshin

Diamond and Precious Metal Geology Institute of the Siberian Branch of the Russian Academy of Sciences

Author for correspondence.
Email: makoshin_89@mail.ru
Russian Federation, Yakutsk

R. V. Kutygin

Diamond and Precious Metal Geology Institute of the Siberian Branch of the Russian Academy of Sciences; Kazan Federal University

Email: makoshin_89@mail.ru
Russian Federation, Yakutsk; Kazan

A. S. Byakov

Shilo North-East Interdisciplinary Scientific Research Institute of the Far East Branch of the Russian Academy of Sciences

Email: makoshin_89@mail.ru
Russian Federation, Magadan

B. I. Gareev

Kazan Federal University

Email: makoshin_89@mail.ru
Russian Federation, Kazan

A. N. Kilyasov

Diamond and Precious Metal Geology Institute of the Siberian Branch of the Russian Academy of Sciences

Email: makoshin_89@mail.ru
Russian Federation, Yakutsk

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2. Fig. 1. Location of the Kubalakh section, obn. 10R2

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3. Fig. 2. Kubalakh section of the Upper Paleozoic in the area of the Kubalakh Creek mouth, Obn. 10R2

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4. Fig. 3. Comparison of δ13Corg variation in Assel-Sakmar sediments of the Kubalakh section of the Northern Verkhoyany with isotope-carbon trends of the stratotypic locality of the Ural Division. From left to right: Kubalakhsky section (Obn. 10R2), distribution of brachiopods and ammonoids in it, biostratigraphic subdivision, variation in the carbon isotope composition of organic matter in the section and comparison with the variation of δ13Ccarb values in the Asselian and Sakmarian stages of the Southern Urals: 1 - mudstone, 2 - siltstone m/z, 3 - siltstone k/z, 4 - sandstone, 5 - limestone, 6 - conglomerate, 7 - nodules, 8 - ammonoids, 9 - brachiopods, 10 - invertebrate finds by number of specimens: units, up to ten, more than ten, 11 - double negative shift of δ13C values, the horizontal stroke indicates the position of the Asselian-Sakmarian boundary established by conodonts [13]; I, II - two variants of fixation of the double negative shift of δ13C values in the Kubalakh section; Gzh. , As., Sak., Ar. - Gzhelian, Asselian, Sakmarian and Artinskian stages, K. - Kygyltassic horizon, Sakh. - Sakhalin Formation; * with specification of boundaries based on carbon isotope data

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