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IRMNG taxon details

Dickinsoniamorpha †

11934106  (urn:lsid:irmng.org:taxname:11934106)

Retallack, 2016
accepted
Order
Proarticulata † · unaccepted (alternative name (approximate synonym))

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marine, brackish, fresh, terrestrial
fossil only
Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   
Taxonomic remark Spelled Dickinsoniomorpha (error or intentional?) in Retallack & Broz, 2020. Affinities unclear; according to Retallack &...  
Taxonomic remark Spelled Dickinsoniomorpha (error or intentional?) in Retallack & Broz, 2020. Affinities unclear; according to Retallack & Broz, 2020, Dickinsonia [hence: Dickinsoniamorpha] has in the past been considered as (1) lichenised glomeromycotan fungus (Retallack 1994, 2007, 2015b), (2) xenophyophoran protist (Zhuravlev 1993; Seilacher et al. 2005), (3) stem metazoan between sponges and cnidarians (Brasier 2004, Hoekzema et al. 2017; Evans et al. 2017; Dunn et al. 2018), (4) cnidarian sea jelly (Sprigg 1947; Harrington and Moore 1956), (5) cnidarian anemone (Valentine 1992), (6) polychaete worm (Wade 1972; Runnegar 1982), (7) annelid worm (Conway Morris 1979; Evans et al. 2019a), (8) turbellarian flatworm (Termier & Termier 1968, Fedonkin 1981), or (9) placozoan (Sperling and Vinther 2010).  [details]
IRMNG (2024). Dickinsoniamorpha †. Accessed at: https://irmng.org/aphia.php?p=taxdetails&id=11934106 on 2024-04-30
Date
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by
2024-01-31 18:00:36Z
created

original description Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   

basis of record Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   

taxonomy source Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   

name verified source Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   

current name source Retallack, G. J.; Broz, A. P. (2020). <i>Arumberia</i> and other Ediacaran–Cambrian fossils of central Australia. <em>Historical Biology.</em> 33(10): 1964-1988., available online at https://doi.org/10.1080/08912963.2020.1755281
note: as Dickinsoniamorpha (slightly different spelling) [details]   

extant flag source Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   

habitat flag source Retallack, G. J. (2016). Ediacaran fossils in thin-section. <em>Alcheringa: An Australasian Journal of Palaeontology.</em> 40(4): 583-600., available online at https://doi.org/10.1080/03115518.2016.1159412 [details]   
From other sources
Taxonomic remark Spelled Dickinsoniomorpha (error or intentional?) in Retallack & Broz, 2020. Affinities unclear; according to Retallack & Broz, 2020, Dickinsonia [hence: Dickinsoniamorpha] has in the past been considered as (1) lichenised glomeromycotan fungus (Retallack 1994, 2007, 2015b), (2) xenophyophoran protist (Zhuravlev 1993; Seilacher et al. 2005), (3) stem metazoan between sponges and cnidarians (Brasier 2004, Hoekzema et al. 2017; Evans et al. 2017; Dunn et al. 2018), (4) cnidarian sea jelly (Sprigg 1947; Harrington and Moore 1956), (5) cnidarian anemone (Valentine 1992), (6) polychaete worm (Wade 1972; Runnegar 1982), (7) annelid worm (Conway Morris 1979; Evans et al. 2019a), (8) turbellarian flatworm (Termier & Termier 1968, Fedonkin 1981), or (9) placozoan (Sperling and Vinther 2010).  [details]

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