Stratigraphic correlation potential of the Ediacaran palaeopascichnids
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 Edi...
| Published in: | Estudios Geológicos |
|---|---|
| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Consejo Superior de Investigaciones Científicas
2019
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| Online Access: | http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995 https://doi.org/10.3989/egeol.43588.557 |
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ftjegeologicos:oai:estudiosgeologicos.revistas.csic.es:article/995 |
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Orbisiana Palaeopascichnus Yelovichnus Palaeopascichnida Ediacaran Vendian Paleopasciquínidos Ediacárico Véndico |
| spellingShingle |
Orbisiana Palaeopascichnus Yelovichnus Palaeopascichnida Ediacaran Vendian Paleopasciquínidos Ediacárico Véndico Kolesnikov, A. V. Stratigraphic correlation potential of the Ediacaran palaeopascichnids |
| topic_facet |
Orbisiana Palaeopascichnus Yelovichnus Palaeopascichnida Ediacaran Vendian Paleopasciquínidos Ediacárico Véndico |
| description |
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. Durante más de cuarenta años, los paleopasciquínidos han representado un grupo enigmático de fósiles macroscópicos, caracterizados por diferencias sustanciales en la conservación, lo que no conduce a un diagnóstico consistente de estos organismos. Los fósiles de paleopasciquínidos se encuentran distribuidos globalmente en las secuencias ediacáricas de la Plataforma de Europa Oriental, Avalonia, China meridional, Siberia y Australia. A la luz de una nueva perspectiva para reanimar el “Véndico” como una serie superior formal del Sistema Ediacárico, los paleopasciquínidos son probablemente el único grupo fósil ediacárico cuyo rango estratigráfico abarca casi toda la “Serie del Véndico”. Además, se ha considerado que los paleopasciquínidos se encuentran entre los macroorganismos más antiguos conocidos con un esqueleto aglutinado; su presencia enfatiza este grupo en términos de bioestratigrafía y correlación geológica ediacárica y allana el camino para la reexaminación de otros fósiles esqueléticos de tipo paleopasciquínido. |
| format |
Article in Journal/Newspaper |
| author |
Kolesnikov, A. V. |
| author_facet |
Kolesnikov, A. V. |
| author_sort |
Kolesnikov, A. V. |
| title |
Stratigraphic correlation potential of the Ediacaran palaeopascichnids |
| title_short |
Stratigraphic correlation potential of the Ediacaran palaeopascichnids |
| title_full |
Stratigraphic correlation potential of the Ediacaran palaeopascichnids |
| title_fullStr |
Stratigraphic correlation potential of the Ediacaran palaeopascichnids |
| title_full_unstemmed |
Stratigraphic correlation potential of the Ediacaran palaeopascichnids |
| title_sort |
stratigraphic correlation potential of the ediacaran palaeopascichnids |
| publisher |
Consejo Superior de Investigaciones Científicas |
| publishDate |
2019 |
| url |
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995 https://doi.org/10.3989/egeol.43588.557 |
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ENVELOPE(-56.866,-56.866,-64.300,-64.300) |
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Fósiles |
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Fósiles |
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Arctic Siberia |
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Arctic Siberia |
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Estudios Geológicos; Vol. 75 No. 2 (2019); e102 Estudios Geológicos; Vol. 75 Núm. 2 (2019); e102 1988-3250 0367-0449 10.3989/egeol.16728 |
| op_relation |
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995/1239 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995/1240 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995/1241 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 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995 doi:10.3989/egeol.43588.557 |
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ftjegeologicos:oai:estudiosgeologicos.revistas.csic.es:article/995 2023-05-15T14:28:22+02:00 Stratigraphic correlation potential of the Ediacaran palaeopascichnids Potencial de correlación estratigráfica de los paleopasciquínidos del Ediacárico Kolesnikov, A. V. 2019-12-30 text/html application/pdf application/xml http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995 https://doi.org/10.3989/egeol.43588.557 eng eng Consejo Superior de Investigaciones Científicas http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995/1239 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995/1240 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995/1241 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 http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/995 doi:10.3989/egeol.43588.557 Derechos de autor 2019 Consejo Superior de Investigaciones Científicas (CSIC) https://creativecommons.org/licenses/by/4.0 CC-BY Estudios Geológicos; Vol. 75 No. 2 (2019); e102 Estudios Geológicos; Vol. 75 Núm. 2 (2019); e102 1988-3250 0367-0449 10.3989/egeol.16728 Orbisiana Palaeopascichnus Yelovichnus Palaeopascichnida Ediacaran Vendian Paleopasciquínidos Ediacárico Véndico info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed article Artículo revisado por pares 2019 ftjegeologicos https://doi.org/10.3989/egeol.43588.557 https://doi.org/10.3989/egeol.16728 https://doi.org/10.1016/S0301-9268(99)00070-4 https://doi.org/10.1134/S1028334X17020131 2020-12-13T10:08:29Z 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. Durante más de cuarenta años, los paleopasciquínidos han representado un grupo enigmático de fósiles macroscópicos, caracterizados por diferencias sustanciales en la conservación, lo que no conduce a un diagnóstico consistente de estos organismos. Los fósiles de paleopasciquínidos se encuentran distribuidos globalmente en las secuencias ediacáricas de la Plataforma de Europa Oriental, Avalonia, China meridional, Siberia y Australia. A la luz de una nueva perspectiva para reanimar el “Véndico” como una serie superior formal del Sistema Ediacárico, los paleopasciquínidos son probablemente el único grupo fósil ediacárico cuyo rango estratigráfico abarca casi toda la “Serie del Véndico”. Además, se ha considerado que los paleopasciquínidos se encuentran entre los macroorganismos más antiguos conocidos con un esqueleto aglutinado; su presencia enfatiza este grupo en términos de bioestratigrafía y correlación geológica ediacárica y allana el camino para la reexaminación de otros fósiles esqueléticos de tipo paleopasciquínido. Article in Journal/Newspaper Arctic Siberia Estudios Geológicos (E-Journal) Fósiles ENVELOPE(-56.866,-56.866,-64.300,-64.300) Estudios Geológicos 75 2 102 |