THE OLDEST TRACE FOSSILS IN ASSOCIATION WITH EDIACARA-TYPE BIOTA IN THE UPPER VENDIAN OF THE SOUTH URALS

Мұқаба

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

Trace fossils and palaeopascichnids have been studied from the Basa Formation of the Vendian Asha Group of the South Urals (southwestern periphery of the Suleiman Anticline, Shubino quarry in the Ust’-Katav city, Chelyabinsk Region. The general morphology and preservation of ichnofossils was shown to be similar to the Late Vendian-Early Cambrian subhorizontal bilobate burrows of Didymaulichnus. The paleontological remains were found to be confined to extremely shallow depositional settings and located stratigraphically below the volcanic tuff layer, the zircon from which has a U–Pb isotopic age of 578 ± 7 Ma. Until now, the first occurrence of trace fossils and the associated “Agronomic Revolution” were thought to be timed to the interval of ~560–550 Ma. Our results show that mobile benthos and biological mixing of sediments may have occurred 20–30 Ma earlier and support the hypothesis that the onset of the first “Agronomic Revolution” and the “Cambrian Explosion” were not significantly coincident in time.

Авторлар туралы

A. Kolesnikov

Geological Institute of the Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: kolesnikov@ginras.ru
Russian, Moscow

V. Desiatkin

Geological Institute of the Russian Academy of Sciences

Email: kolesnikov@ginras.ru
Russian, Moscow

V. Terekhova

Geological Institute of the Russian Academy of Sciences

Email: kolesnikov@ginras.ru
Russian, Moscow

V. Pan’kov

Geological Institute of the Russian Academy of Sciences

Email: kolesnikov@ginras.ru
Russian, Moscow

A. Maslov

Geological Institute of the Russian Academy of Sciences

Email: kolesnikov@ginras.ru
Russian, Moscow

Әдебиет тізімі

  1. Wood R., Liu A.G., et al. Integrated records of environmental change and evolution challenge the Cambrian Explosion // Nat. Ecol. Evol. 2019. V. 3. P. 528–538.
  2. Mángano M.G., Buatois L.A. Decoupling of body-plan diversification and ecological structuring during the Ediacaran–Cambrian transition: evolutionary and geobiological feedbacks // Proc. Royal Soc. B. 2014. V. 281. 20140038.
  3. Seilacher A. Biomat-related lifestyles in the Precambrian // Palaios. 1999. V. 14. P. 86–93.
  4. Mángano M.G., Buatois L.A. The Cambrian revolutions: Trace-fossil record, timing, links and geobiological impact // Earth-Sci. Rev. 2017. V. 173. P. 96–108.
  5. Seilacher A., Pfluger F. From biomats to benthic agriculture: A biohistoric revolution / Biostabilization of Sediments // Bibliotheks- und Informationssystem der Carl von Ossietzky Universität Oldenburg, Oldenburg, 1994. P. 97–105.
  6. Seilacher A., Buatois L.A., et al. Trace fossils in the Ediacaran-Cambrian transition: Behavioral diversification, ecological turnover and environmental shift // Palaeogeogr. Palaeoclim. Palaeoecol. 2005. V. 227. P. 323–356.
  7. Liu A.G., McIlroy D., et al. First evidence for locomotion in the Ediacara biota from the 565 Ma Mistaken Point Formation, Newfoundland // Geology. 2010. V. 38 (2). P. 123–126.
  8. Беккер Ю.Р. Молассы докембрия. Л.: Недра, 1988, 288 с.
  9. Беккер Ю.Р. О выделении бакеевских отложений в стратотипическом разрезе рифея // Известия Академии наук СССР. Серия геологическая. 1975. № 6. С. 125–129.
  10. Беккер Ю.Р. Молассы докембрия. Л.: Недра, 1988. 288 с.
  11. Kolesnikov A., Desiatkin V. Taxonomy and palaeoenvironmental distribution of palaeopascichnids // Geological Magazine. 2022. V. 159. P. 1175–1191.
  12. Гражданкин Д.В., Марусин В.В. и др. Котлинский горизонт на Южном Урале // ДАН. 2011. Т. 440. № 2. С. 201–206.
  13. Levashova N.M., Bazhenov M.L., et al. Paleogeography of Baltica in the Ediacaran: Paleomagnetic and geochronological data from the clastic Zigan Formation, South Urals // Precambrian Research. 2013. V. 236. P. 16–30.
  14. Kolesnikov A.V., Marusin V.V., et al. Ediacaran biota in the aftermath of the Kotlinian Crisis: Asha Group of the South Urals // Precambrian Research. 2015. V. 263. P. 59–78.
  15. Зайцева Т.С., Кузнецов А.Б. и др. Основание венда на Южном Урале: Rb–Sr возраст глауконитов бакеевской свиты // Стратиграфия. Геологическая корреляция. 2019. Т. 27. № 5. С. 82–96.
  16. Разумовский А.А., Новиков И.А. и др. Древнейшие вендские ископаемые северной Евразии: U–Pb-изотопный возраст басинской свиты (ашинская серия, Южный Урал) // ДАН. 2020. Т. 495. № 2. С. 3–8.
  17. Рязанцев А.В., Разумовский А.А. и др. Возраст вулканических туфов в разрезах басинской и зиганской свит ашинской серии венда (эдиакария) на Южном Урале: результаты U–Th–Pb (SIMS и LA-ICP-MS) датирования акцессорного циркона // Доклады Российской АН. Науки о Земле. 2023. Т. 508. № 1. С. 68–78.
  18. Jensen S., Mens K. Trace fossils Didymaulichnus cf. tirasensis and Monomorphicus isp. From the Estonian Lower Cambrian, with a discussion of the early Cambrian ichnocoenoses of Baltica // Proc. Estonian Acad. Sci. Geol. 2001. V. 50 (2). P. 75–85.
  19. Seilacher A. Trace fossil analysis. Berlin: Springer-Verlag, 2007. 226 p.
  20. Chen Z., Zhou C., et al. Trace fossil evidence for Ediacaran bilaterian animals with complex behaviour // Precambrian Research. 2013. V. 224. P. 690–701.

Қосымша файлдар

Қосымша файлдар
Әрекет
1. JATS XML
2.

Жүктеу (4MB)
3.

Жүктеу (5MB)
4.

Жүктеу (8MB)
5.

Жүктеу (5MB)

© А.В. Колесников, В.Д. Десяткин, В.А. Терехова, В.Н. Паньков, А.В. Маслов, 2023