Palaeopascichnida is a proposed group, which includes all known elongated, agglutinating organisms from the Ediacaranperiod. The term was first used in 2009 by Grazhdankin & Maslov.
Palaeopascichnids are agglutinating organisms, which primarily composed of globular or sausage-shaped chambers, with occasional branches seen in a majority of specimens.[3]
They were originally described as trace fossils, but further studies found this to not be the case, due to the branching of the fossils and some also being disarticulated, with chambers found separated from the rest of the body.[3] Some studies have even suggested a probably foraminiferan affinity for the palaeopascichnids.[4][5]
↑Grazhdankin, D. V.; Maslov, A. V. (June 2009). "Sequence stratigraphy of the upper Vendian of the East European Craton". Doklady Earth Sciences. 426 (1): 517–521. doi:10.1134/S1028334X09040011.
12Grazhdankin, Dmitriy (March 2014). "Patterns of Evolution of the Ediacaran Soft-Bodied Biota". Journal of Paleontology. 88 (2): 269–283. doi:10.1666/13-072.
↑Seilacher, Adolf; Grazhdankin, Dmitri; Legouta, Anton (2003). "Ediacaran biota: The dawn of animal life in the shadow of giant protists". Paleontological Research. 7 (1): 43–54. doi:10.2517/prpsj.7.43.
↑Kolesnikov, Anton V; Rogov, Vladimir I; Bykova, Natalia V; Danelian, Taniel; Clausen, Sébastien; Maslov, Andrey V; Grazhdankin, Dmitriy V (2018). "The oldest skeletal macroscopic organism Palaeopascichnus linearis". Precambrian Research. 316: 24–37. Bibcode:2018PreR..316...24K. doi:10.1016/j.precamres.2018.07.017. S2CID134885946.
↑Fedonkin, M. A. (1981). Keller, B. M. (ed.). "White Sea biota of Vendian: Precambrian non-skeletal fauna in the Russian Platform North". Transactions of the Geological Institute. 342. Moscow: Nauka: 1–100.
↑Palij, V.M. (1976). "Ostatki besskeletnoy fauny i sledy zhiznedeyatel'nosti iz otlozheniy verkhnego dokembriya i nizhnego kembriya Podolii" [Remains of the diskeletal fauna and traces of life activity from the deposits of the Upper Precambrian and the lower Cambrian of Podilia]. Paleontologiya i stratigrafiya verkhnego dokembriya i nizhnego paleozoya yugo-zapada Vostochno-Yevropeyskoy platformy[Paleontology and Stratigraphy of the Upper Precambrian and the Lower Paleozoic of the Southwest of the Eastern European Platform] (in Russian). Kiev: Naukova Dumka. pp.63–77.
↑Högström, AES; Jensen, S; Palacios, T; Ebbestad, JOR (2013). "New information on the Ediacaran-Cambrian transition in the Vesteranda Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils". Norwegian Journal of Geology. 93: 95–106.
↑Yan, Y.; Jiang, C.; Zhang, S.; Du, S.; and Bi, Z. (1992). "Research of the Sinian System in the region of western Zhejiang, northern Jiangxi, and southern Anhui provinces". Bull. Nanjing Inst. Geol. Mineral Res. Supplementary Issue 12. Chinese Acad. Geol. Sci.: 1–105.{{cite journal}}: CS1 maint: multiple names: authors list (link)
↑Becker-Kerber, Bruno; Paim, Paulo Sergio Gomes; Chemale Junior, Farid; Girelli, Tiago Jonatan; da Rosa, Ana Lucia Zucatti; Albani, Abderrazak El; Osés, Gabriel Ladeira; Prado, Gustavo M.E.M.; Figueiredo, Milene; Simões, Luiz Sérgio Amarante; Pacheco, Mírian Liza Alves Forancelli (August 2020). "The oldest record of Ediacaran macrofossils in Gondwana (~563 Ma, Itajaí Basin, Brazil)". Gondwana Research. 84: 211–228. doi:10.1016/j.gr.2020.03.007.
↑Pinto, André Jorge; Álvarez-Lloret, Pedro; Callegari, Ivan; Scharf, Andreas (July 2025). "An Ediacaran trace-like body fossil of a Palaeopascichnus specimen from Oman under 3D micro-tomography". Facies. 71 (3). doi:10.1007/s10347-025-00705-5.
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