Biology:Selkirkia

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Short description: Extinct genus of priapulid worms

Selkirkia
Temporal range: Cambrian Stage 3–Middle Cambrian
Selkirkia columbia ROM63131.jpg
Selkirkia columbia fossil from the Burgess Shale. From Smith et al. (2015)[2]
Selkirkia columbia Restoration.png
Restoration of Selkirkia columbia
Scientific classification e
Domain: Eukaryota
Kingdom: Animalia
Stem group: Priapulida (?)
Class: Archaeopriapulida
Family: Selkirkiidae
Conway Morris, 1977[1]
Genus: Selkirkia
Walcott, 1911
Species
  • Selkirkia columbia Conway Morris, 1977
  • Selkirkia elongata Luo & Hu, 1999
  • Selkirkia sinica Luo & Hu, 1999
  • Selkirkia spencei Resser, 1939
  • Selkirkia willoughbyi Conway Morris & Robison, 1986

Selkirkia is a genus of predatory,[3] tubicolous priapulid worms known from the Middle Cambrian Burgess Shale, Ogygopsis Shale and Puncoviscana Formation.[4] 142 specimens of Selkirkia are known from the Greater Phyllopod bed, where they comprise 0.27% of the community.[5] In the Burgess Shale, 20% of the tapering, organic-walled tubes are preserved with the worm inside them, whereas the other 80% are empty (or sometimes occupied by one or more small agnostid trilobites).[3] Whilst alive, the tubes were probably vertical, whereas trilobite-occupied tubes are horizontal.[3]

Morphology

Selkirkia had a body divisible into a proboscis towards the anterior of a trunk enclosed by a tube. The proboscis would have been partially invertable and was armed with several spinules and spines, decreasing size distally overall. It was controlled by at least two sets of anterior retractor muscles. Immediately behind the proboscis was the trunk, smooth for the most part but lined with papillae towards the anterior. Surrounding the trunk was the tube, which way very finely annulated (4 annulations per 0.1 millimeters).

History

Members Cambrorhytium were originally described as Selkirkia before their identification as a separate genus.[6]

References

  1. Conway Morris, S (1977). "Fossil priapulid worms". Special Papers in Palaeontology 20. 
  2. Smith, M. R.; Harvey, T. H. P.; Butterfield, N. J. (2015). "The macro- and microfossil record of the Cambrian priapulid Ottoia". Palaeontology 58 (4): 705–721. doi:10.1111/pala.12168. Bibcode2015Palgy..58..705S. http://dro.dur.ac.uk/18218/1/18218.pdf. 
  3. 3.0 3.1 3.2 Template:Chatterton 2003
  4. Aceñolaza, Florencio; Guillermo, Aceñolaza (2005). "La formación Puncoviscana y unidades estratigráficas vinculadas en el neoproterozoico - Cámbrico temprano del noroeste argentino" (in es). Latin American Journal of Sedimentology and Basin Analysis 12 (2): 65–87. http://www.scielo.org.ar/pdf/lajsba/v12n2/v12n2a02.pdf. Retrieved 7 December 2015. 
  5. Caron, Jean-Bernard; Jackson, Donald A. (October 2006). "Taphonomy of the Greater Phyllopod Bed community, Burgess Shale". PALAIOS 21 (5): 451–65. doi:10.2110/palo.2003.P05-070R. Bibcode2006Palai..21..451C. 
  6. See Cambrorhytium.

External links

Wikidata ☰ Q27438907 entry