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Selkirkia

From Wikipedia, the free encyclopedia
Extinct genus of priapulid worms
For the plant genus, seeSelkirkia (plant).

Selkirkia
Temporal range:Cambrian Stage 3–Floian
Selkirkia columbia fossil from theBurgess Shale. FromSmith et al. (2015)[2]
Restoration ofSelkirkia columbia
Scientific classificationEdit this classification
Domain:Eukaryota
Kingdom:Animalia
Stem group:Priapulida (?)
Class:Archaeopriapulida
Family:Selkirkiidae
Conway Morris, 1977[1]
Genus:Selkirkia
Walcott, 1911
Species
  • S. columbia Conway Morris, 1977
  • S. elongata Luo & Hu, 1999
  • S. sinica Luo & Hu, 1999
  • S. spencei Resser, 1939
  • S. willoughbyi Conway Morris & Robison, 1986
  • S. tsering Nanglu 2024

Selkirkia is a genus of predatory,[3] tubicolouspriapulid worms known from the MiddleCambrianBurgess Shale, Ogygopsis Shale,Puncoviscana Formation[4] and the EarlyOrdovicianFezouata Formation.[5] 142 specimens ofSelkirkia are known from the GreaterPhyllopod bed, where they comprise 0.27% of the community.[6] 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 smallagnostid trilobites).[3] Whilst alive, the tubes were probably vertical, whereas trilobite-occupied tubes are horizontal.[3]

Morphology

[edit]

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

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Members ofCambrorhytium were originally described asSelkirkia before their identification as a separate genus.[7]

References

[edit]
  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 priapulidOttoia"(PDF).Palaeontology.58 (4):705–721.Bibcode:2015Palgy..58..705S.doi:10.1111/pala.12168.
  3. ^abcChatterton, B. D. E.; Collins, D. H.; Ludvigsen, R. (2003)."Cryptic behaviour in trilobites: Cambrian and Silurian examples from Canada, and other related occurrences". In Lane, P. D; Siveter, D. J;Fortey, R. A (eds.).Trilobites and Their Relatives. Special Papers in Palaeontology. Vol. 70.The Palaeontological Association. pp. 157–173.ISBN 978-0-901702-81-4.
  4. ^Aceñolaza, Florencio; Guillermo, Aceñolaza (2005)."La formación Puncoviscana y unidades estratigráficas vinculadas en el neoproterozoico - Cámbrico temprano del noroeste argentino"(PDF).Latin American Journal of Sedimentology and Basin Analysis (in Spanish).12 (2):65–87. Retrieved7 December 2015.
  5. ^Nanglu, Karma; Ortega-Hernández, Javier (March 2024)."Post-Cambrian survival of the tubicolous scalidophoran Selkirkia".Biology Letters.20 (3).doi:10.1098/rsbl.2024.0042.ISSN 1744-957X.PMID 38531414.
  6. ^Caron, Jean-Bernard; Jackson, Donald A. (October 2006). "Taphonomy of the Greater Phyllopod Bed community, Burgess Shale".PALAIOS.21 (5):451–65.Bibcode:2006Palai..21..451C.doi:10.2110/palo.2003.P05-070R.JSTOR 20173022.S2CID 53646959.
  7. ^SeeCambrorhytium.

External links

[edit]
Selkirkia


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