Skip to content
Surf Wiki
Save to docs
general/burgess-shale-fossils

From Surf Wiki (app.surf) — the open knowledge base

Ancalagon minor

Extinct species of priapulid worm


Extinct species of priapulid worm

|†A. minor|(Walcott, 1911) Conway Morris, 1977 (type)}}

  • Ottoia minor Walcott 1911

Ancalagon minor is an extinct priapulid worm known from the Cambrian Burgess Shale.

Because it superficially resembles the modern-day internal parasites known as the acanthocephalids or "spiny-headed worms," A. minor was once thought to be, or once thought to resemble the hypothetical free-living ancestor of acanthocephalids. Two specimens of Ancalagon are known from the Greater Phyllopod bed, where they comprise

Along with the other Cambrian worms such as Ottoia, Selkirkia, Louisella, Fieldia, Scolecofurca, and Lecythioscopa, the organism may fall into a clade termed "Archaeopriapulida," a stem group to the Priapulids proper. However, the morphological similarity of these organisms to their modern cousins is remarkable, especially for the Burgess Shale. A phylogenetic analysis does not provide a great deal of resolution to the relationships between these basal worms.

Etymology

The generic name is a homage to the dragon Ancalagon of J.R.R. Tolkien's Middle-earth legendarium, in reference to the worm's prominent rows of hooks on its proboscis. The species was previously placed in the genus Ottoia, as Ottoia minor, but was removed by Simon Conway Morris, who noted morphological differences.

Morphology

Ancalagon had a slender, cyndrical, radially symmetric body averaging 6 centimeters in length. Its proboscis was armed with circum-oral hooks at the anterior. There were about 10 of these hooks, equal in size and with prominent bases. Directly posterior was an unarmed space, followed by posteriorly directed spinose hooks. The trunk is annulated with 0.2 to 0.25 millimeter spacing, and carried rows of setae possibly performing sensory functions. The apparent absence of retractor muscles correlates with ''Ancalagon'''s inability to significantly invert its proboscis. The organism was probably a burrowing predator.

References

References

  1. "Fossil priapulid worms". Special Papers in Palaeontology.
  2. Haaramo, Mikko. (2003). "Scalidophora – †palaeoscolecids, priapulids, mud dragons and brush heads".
  3. (1979). "The Burgess Shale (Middle Cambrian) Fauna". Annual Review of Ecology and Systematics.
  4. (1982). "The Origins and Evolution of the Acanthocephala". Biological Reviews.
  5. (October 2006). "Taphonomy of the Greater Phyllopod Bed community, Burgess Shale". PALAIOS.
  6. (1983). "Class Seticoronaria and Phylogeny of the Phylum Priapulida". Zoologica Scripta.
  7. (2004). "Anatomy and lifestyles of Early Cambrian priapulid worms exemplified by Corynetis and Anningvermis from the Maotianshan Shale (SW China)". Lethaia.
  8. Wills, M. A.. (1 April 1998). "Cambrian and Recent Disparity: the Picture from Priapulids". Paleobiology.
  9. "Ancalagon minor".
  10. Whittington, H.B.. (1911). "Middle Cambrian Annelids". Cambrian Geology and Paleontology.
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

Want to explore this topic further?

Ask Mako anything about Ancalagon minor — get instant answers, deeper analysis, and related topics.

Research with Mako

Free with your Surf account

Content sourced from Wikipedia, available under CC BY-SA 4.0.

This content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.

Report