Stratigraphic correlation potential of the Ediacaran palaeopascichnids
DOI:
https://doi.org/10.3989/egeol.43588.557Keywords:
Orbisiana, Palaeopascichnus, Yelovichnus, Palaeopascichnida, Ediacaran, VendianAbstract
For more than forty years, palaeopascichnids represented an enigmatic group of macroscopic fossils, which are characterised by substantial differences in preservation leading to no consistent diagnosis for these organisms. Numerically abundant palaeopascichnid fossils are globally distributed in Ediacaran sequences of the East European Platform, Avalonia, South China, Siberia and Australia. In light of new perspective to reanimate the ‘Vendian’ as a formal upper series of the Ediacaran System, Palaeopascichnida is probably the only Ediacaran fossil group whose stratigraphic range spans almost the entire ‘Vendian Series’. Furthermore, it has been considered that palaeopascichnids are among the oldest known macro organisms with an agglutinated skeleton; its presence puts emphasis on this group in terms of Ediacaran biostratigraphy and geological correlation and paves the way for the reexamination of other skeletal palaeopascichnid-like fossils.
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Antcliffe, J.B.; Gooday, A.J. & Brasier, M.D. (2011). Testing the protozoan hypothesis for Ediacaran fossils: A developmental analysis of Palaeopascichnus. Palaeontology, 54: 1157-1175. https://doi.org/10.1111/j.1475-4983.2011.01058.x
Chistyakov, B.G.; Kalmykova, N.A.; Nesov, L.A. & Suslov, G.A. (1984). The occurrence of Vendian strata in the middle reaches of the Onega River and a possibility of tunicates (Tunicata: Chordata). existence in the Precambrian. Vestnik Leningradskogo Universiteta, Seriya Geologicheskaya, 6: 11-19 [in Russian].
Cope, J.C.W. (1982). Precambrian fossils of the Carmarthen area, Dyfed. Nature in Wales, 1 (2): 11-16.
Fedonkin, M.A. (1980). Vendian fauna in the north of the Russian Platform. In: The Vendian System: argumentation of historical geology and palaeontology (Sokolov, B.S. & Ivanovski, A.B.; Eds.), Nauka, Moscow, 112-117. [in Russian]
Gehling, J.G.; Droser, M.L.; Jensen, S. & Runnegar, B.N. (2005). Ediacara Organisms: Relating Form to Function. In: Evolving Form and Function: Fossils and Development: Proceedings of a symposium honouring Adolph Seilacher for his contributions to palaeontology in celebration of his 80th birthday (Briggs, D.E.G.; Ed.), Peabody Museum of Natural History, Yale University, 43-66.
Grazhdankin, D.V. & Maslov, A.V. (2015). The room for the Vendian in the International Chronostratigraphic Chart. Russian Geology and Geophysics, 56: 549-559. https://doi.org/10.1016/j.rgg.2015.03.007
Haines, P.W. (2001). Problematic fossils in the late Neoproterozoic Wonoka Formation, South Australia. Precambrian Research, 100: 97-108. https://doi.org/10.1016/S0301-9268(99)00070-4
Ivantsov, A.Yu. (2017). Finds of Ediacaran-type fossils in Vendian deposits of the Yudoma Group, eastern Siberia. Doklady Earth Sciences, 472: 143-146. https://doi.org/10.1134/S1028334X17020131
Jensen, S.; Högström, A.E.S.; Høyberget, M.; Meinhold, G.; McIlroy, D.; Ebbestad, J.O.R.; Taylor, W.L.; Agic, H. & Palacios, T. (2018). New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of Varanger Ice Age. Canadian Journal of Earth Sciences, 55: 1253-1261. https://doi.org/10.1139/cjes-2018-0035
Kolesnikov, A.V.; Marusin, V.V.; Nagovitsin, K.E.; Maslov, A.V. & Grazhdankin, D.V. (2015). Ediacaran biota in the aftermath of the Kotlinian Crisis: Asha Group of the South Urals. Precambrian Research, 263: 59-78. https://doi.org/10.1016/j.precamres.2015.03.011
Kolesnikov, A.V.; Rogov, V.I.; Bykova, N.V.; Danelian, T.; Clausen, S.; Maslov, A.V. & Grazhdankin, D.V. (2018a). The oldest skeletal macroscopic organism Palaeopascichnus linearis. Precambrian Research, 316: 24-37. https://doi.org/10.1016/j.precamres.2018.07.017
Kolesnikov, A.V.; Liu, A.G.; Danelian, T. & Grazhdankin, D. (2018b). A reassessment of the problematic Ediacaran genus Orbisiana Sokolov 1976. Precambrian Research, 316: 197-205. https://doi.org/10.1016/j.precamres.2018.08.011
Kolesnikov, A.V. & Bobkov, N.I. (2019). Revisiting the age of the Asha Group in the South Urals. Estudios Geológicos 75(2): e103. https://doi.org/10.3989/egeol.43590.558
Narbonne, G.M.; Myrow, P.M.; Landing, E. & Anderson, M.M. (1987). A candidate stratotype for the Precambrian-Cambrian boundary, Fortune Head, Burin Peninsula, south-eastern Newfoundland. Canadian Journal of Earth Sciences, 24: 1277-1293. https://doi.org/10.1139/e87-124
Palij, V.M. (1976). Remains of soft-bodied animals and trace fossils from the Upper Precambrian and Lower Cambrian of Podolia. In: Palaeontology and stratigraphy of Upper Precambrian and Lower Cambrian of southeast East European Platform (Schul'ga, P.L.; Ed.), Naukova dumka, Kiev, 63-76. [in Russian]
Parcha, S.K. & Pandey, S. (2011). Ichnofossils and their significance in the Cambrian successions of the Parahio Valley in the Spiti Basin, Thethys Himalaya, India. Journal of Asian Earth Sciences, 42: 1097-1116. https://doi.org/10.1016/j.jseaes.2011.04.028
Seilacher, A.; Grazhdankin, D. & Legouta, A. (2003). Ediacaran biota: the dawn of animal life on the shadow of giant protists. Paleontological Research, 7 (1): 43-54. https://doi.org/10.2517/prpsj.7.43
Yuan, X.; Chen, Z.; Xiao, S.; Zhou, C. & Hua, H. (2011). An early Ediacaran assemblage of macroscopic and morphologically differentiated eukaryotes. Nature, 470: 390-393. https://doi.org/10.1038/nature09810 PMid:21331041
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