Palaeophragmodictya is an extinct genus of sponge-grade organisms from the Ediacaran Period. Originally interpreted as a hexactinellid sponge,[1] the organism also bears some coelomate characteristics, including bilateral symmetry.[2][3]

Palaeophragmodictya
Temporal range: Late Ediacaran, 558–555 Ma
Fossil of P. spinosa
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Porifera
Class: Hexactinellida
Order: Reticulosa
Genus: Palaeophragmodictya
Gehling & Rigby, 1996
Species
  • P. reticulata
    Gehling & Rigby, 1996
  • P. spinosa Serezhnikova, 2007

Morphology

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The organisms take the form of a rounded, dome-like bag, 7–68 mm in diameter, with an uneven margin. Radial grooves define sac-like compartments within the bag. The radial pattern has an element of bilateral symmetry. A stalk emerges from the central point of some specimens, at the top of the organism; in life, it probably extended into the water column. Ray-like filaments radiate outwards from the edge of the bag.[2] Some structures in the organism have been interpreted as spicules.[1][4]

Ecology

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The organisms have been interpreted as tall suspension feeders, reaching 10 cm or more up into the sea water above them.[1][5]

Original description

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The genus was originally considered to be a member of the Dictyospongiidae family (hexactinellia), and was among the first Precambrian sponges to be described.[1]

Distribution

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First found in the Pound group of Australia, fossils have also been recovered from the White Sea region of Russia.[2]

Other Sponge-Grade Ediacarans

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See also

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References

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  1. ^ a b c d Gehling, J. G.; Rigby, J. K. (1996), "Long expected sponges from the Neoproterozoic Ediacara fauna of South Australia", Journal of Paleontology, 70 (2): 185–195, Bibcode:1996JPal...70..185G, doi:10.1017/S0022336000023283, ISSN 0022-3360, JSTOR 1306383
  2. ^ a b c Serezhnikova, E. (2007), "Palaeophragmodictya spinosa sp. Nov., a bilateral benthic organism from the Vendian of the Southeastern White Sea Region", Paleontological Journal, 41 (4): 360–369, Bibcode:2007PalJ...41..360S, doi:10.1134/S0031030107040028, archived from the original on 2016-02-22, retrieved 2008-08-16
  3. ^ Botting, J. P. (2007), ""Cambrian" demosponges in the Ordovician of Morocco: Insights into the early evolutionary history of …", Geobios, 40 (6): 737–748, Bibcode:2007Geobi..40..737B, doi:10.1016/j.geobios.2007.02.006
  4. ^ Ivantsov, A. Y.; Malakhovskaya, Y. E.; Serezhnikova, E. A. (2004), "Some Problematic Fossils from the Vendian of the Southeastern White Sea Region" (PDF), Paleontological Journal, 38 (1): 1–9, archived from the original (PDF) on 2013-07-20
  5. ^ Yuan, X.; Xiao, S.; Parsley, R. L.; Zhou, C.; Chen, Z.; Hu, J. (2002), "Towering sponges in an Early Cambrian Lagerstätte: Disparity between nonbilaterian and bilaterian epifaunal tierers at the Neoproterozoic-Cambrian transition", Geology, 30 (4): 363–366, Bibcode:2002Geo....30..363Y, doi:10.1130/0091-7613(2002)030<0363:TSIAEC>2.0.CO;2, ISSN 0091-7613