FIRST DETAILED RECORD δ13 Corg. IN PERMIAN MUDSTONES OF THE TASKAN BASIN (OMULEVKA BLOCK): A REFLECTION OF BIOSPHERIC EVENTS IN NORTHEAST ASIA

A. S. Biakov; Бяков А. С.; I. L. Vedernikov; Ведерников И. Л.; N. A. Goryachev; Горячев Н. А.; B. I. Gareev; Гареев Б. И.

doi:10.31857/S2686739723601199

FIRST DETAILED RECORD δ13 Corg. IN PERMIAN MUDSTONES OF THE TASKAN BASIN (OMULEVKA BLOCK): A REFLECTION OF BIOSPHERIC EVENTS IN NORTHEAST ASIA

Authors: Biakov A.S.¹, Vedernikov I.L.¹, Goryachev N.A.¹, Gareev B.I.²
Affiliations:
1. N.A. Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch, Russian Academy of Sciences
2. Kazan Federal University
Issue: Vol 513, No 1 (2023)
Pages: 33-38
Section: ГЕОЛОГИЯ
URL: https://journals.rcsi.science/2686-7397/article/view/232966
DOI: https://doi.org/10.31857/S2686739723601199
EDN: https://elibrary.ru/LEDFUC
ID: 232966

Cite item

Full Text

Open Access
Restricted Access

Access granted
Restricted Access

Subscription Access

Abstract
About the authors
References
Supplementary files
Statistics

Abstract

For the first time, a detailed record of the δ13Сorg value has been obtained in Permian mudstones of the Taskan Basin (Omulevka block, Northeast Asia), covering the interval from the Upper Kungurian, Roadian, Wordian, Capitanian, and Lower Wuchiapingian stages. The value of δ13 Corg. varies from –23.81‰ (middle Kungurian) to –26.97‰ (lower part of the Wuchiapingian). Three negative excursions of the δ13 Corg. value are clearly distinguished in the section – in the upper part of the Kungurian Stage of the Lower Permian, in the lower part of the Capitanian and at the boundary of the Capitanian – Wuchiapingian stages. These excursions are in good agreement with the episodes of mass extinctions established by us earlier (Biakov, 2012) and are most likely associated with periods of activity of island-arc magmatism in the region during the Permian.

Keywords

δ¹³С_оrg., chemostratigraphy, negative excursions, biospheric events, extinctions, Permian, Northeast Asia

References

Бяков А.С., Horacek M., Горячев Н.А., Ведерников И.Л., Захаров Ю.Д. Первая детальная запись δ13 Соrg. в пограничных пермо-триасовых отложениях Колымо-Омолонского региона (Северо-Восток Азии) // ДАН. 2017. Т. 474. № 3. С. 347–350.
Бяков А.С., Прокопьев А.В., Кутыгин Р.В., Ведерников И.Л., Будников И.В. Геодинамические обстановки формирования пермских седиментационных бассейнов Верхояно-Колымской складчатой области // Отечественная геология. 2005. № 5. С. 81–85.
Бяков А.С., Ведерников И.Л., Колесов Е.В. Предварительные результаты изучения пермских отложений юга Омулёвского блока (Северо-Восток Азии) // Геология, география и биологическое разнообразие Северо-Востока России: Мат-лы Дальневост. регион. конф., посв. памяти А.П. Васьковского. Магадан: СВНЦ ДВО РАН, 2006. С. 71–75.
Ishikawa T., Ueno Y., Shu D., Li Y., Han J., Guo J., Yoshida N., Komiya T. Irreversible change of the oceanic carbon cycle in the earliest Cambrian: high-resolution organic and inorganic carbon chemostratigraphy in the Three Gorges area, South China // Precambrian Res. 2013. V. 225. P. 190–208.
Svensen H., Planke S., Malthe-Sørenssen A., Jamtveit B., Myklebust R., Eidem T.R., Rey S.S. Release of methane from a volcanic basin as a mechanism for initial Eocene global warming // Nature. 2004. V. 429. P. 542–545.
Grard A., Francois L.M., Dessert C., Dupre B., Godderis Y. Basaltic volcanism and mass extinction at the Permo-Triassic boundary: environmental impact and modeling of the global carbon cycle // Earth Planet. Sci. Let. 2005. V. 234. P. 207–221.
Zhang B.L., Wignall P.B., Yao S.P., Hu W.X., Liu B. Collapsed upwelling and intensified euxinia in response to climate warming during the Capitanian (Middle Permian) mass extinction // Gondwana Res. 2021. V. 89. P. 31–46.
Chen J., Xu Y. Establishing the link between Permian volcanism and biodiversity changes: Insights from geochemical proxies // Gondwana Res. 2019. V. 75. P. 68–96.
Bryan S. Environmental impact of silicic magmatism in large igneous province events / Large igneous provinces: driver of global environmental and biotic changes. Ernst R., Dickson A., Bekker A., eds. Geoph. Monogr. Ser. № 255. Washington: AGU and Wiley, 2021. P. 133–152.
Chen J., Xu Y. Permian large igneous provinces and their paleoenvironmental effects / Large igneous provinces: driver of global environmental and biotic changes. Ernst R., Dickson A., Bekker A., eds. Geoph. Monogr. Ser. № 255. Washington: AGU and Wiley, 2021. P. 417–434.
Zhang H., Zhang F.F., Chen J.B., Erwin D.H., Syverson D.D., Ni P., et al. Felsic volcanism as a factor driving the end-Permian mass extinction // Sci. Adv. 2021. V. 7. № 47. Eabh1390. https://doi.org/10.1126/sciadv.abh1390
Бяков А.С. Пермские биосферные события на Северо-Востоке Азии // Стратиграфия. Геол. корреляция. 2012. № 2. С. 88–100.
Zhang B.L., Yao S.P., Mills B.J.W., Wignall P.B., Hu W.X., Liu B., Ren Y.L., Li L.L., Shi G. Middle Permian organic carbon isotope stratigraphy and the origin of the Kamura Event // Gondwana Res. 2020. V. 79. P. 217–232.
Решения Третьего межведомственного регионального стратиграфического совещания по докембрию, палеозою и мезозою Северо-Востока России (Санкт-Петербург, 2002) / Ред. Т.Н. Корень, Г.В. Котляр. СПб: Изд-во ВСЕГЕИ, 2009. 268 с. + CDR.
Бяков А.С., Ведерников И.Л., Акинин В.В. Пермские диамиктиты Северо-Востока Азии и их вероятное происхождение // Вестник СВНЦ ДВО РАН. 2010. № 1. С. 14–24.
Брынько И.В., Ползуненков Г.О., Бяков А.С., Ведерников И.Л. Первые результаты U-Pb SHRIMP датирования цирконов из кепитенских (средняя пермь) отложений Омолонского массива (Северо-Восток России) // Тихоокеанская геология. 2021. Т. 40. № 1. С. 77–86.
Davydov V.I., Biakov A.S., Crowley J.L., Schmitz M.D., Isbell J.L., Vedernikov I.L. Middle Permian U-Pb zircon ages of the “glacial” deposits of the Atkan Formation, Ayan-Yuryakh anticlinorium, Magadan province, NE Russia: Their significance for global climatic interpretations // Gondwana Res. 2016. V. 38. P. 74–85.
Kaiho K., Chen Z.-Q., Ohashi T., Arinobu T., Sawada K., Cramer B.S. A negative carbon isotope anomaly associated with the earliest Lopingian (Late Permian) mass extinction // Palaeogeogr., Palaeoclimatol., Palaeoecol. 2005. V. 223. P. 172–180.
Bond D.P.G., Wignall P.B., Joachimski M.M., Sun Y., Savov I., Grasby S.E., Beauchamp B., Blomeier D.P.G. An abrupt extinction in the Middle Permian (Capitanian) of the Boreal Realm (Spitsbergen) and its link to anoxia and acidification // GSA Bulletin, 2015. https://doi.org/10.1130/B31216.1
Davydov V.I., Biakov A.S., Schmitz M.D., Silantiev V.V. Radioisotopic calibration of the Guadalupian Series: review and updates // Earth-Sci. Rev. 2018. V. 176. P. 222–240.