Temporal range: Middle Cambrian
|Reconstruction of Haplophrentis|
Haplophrentis is a genus of tiny shelled hyolithid which lived in the Cambrian Period. Its shell was long and conical, with the open end protected by an operculum, from which two fleshy arms called helens protruded at the sides. These arms served to elevate the opening of the shells above the sea floor, acting like stilts.
Mature Haplophrentis ranged in length between 2–6 cm, H, reesi being larger than H. carinatus. Juveniles could of course be smaller. It is distinguished from Hyolithes by the presence of a longitudinal septum on the middle of the inner surface of the top of the shell.
Its soft anatomy comprises 12(H. carinatus) to 16 (H. reesi) tentacles attached to a horseshoe-shaped lophophorre. A pair of wide structures of uncertain function extend along the length of the conical shell. A larval shell is attached to the shell apex.
The soft anatomy of Haplophrentis was key to establishing the hyoliths as members of the Lophophorata, the group containing brachiopods and phoronids.
186 specimens of Haplophrentis are known from the Greater Phyllopod bed, where they comprise 0.35% of the community. It is also known from several specimens in the Spence Shale, and occurs prolifically at the Marble Canyon locality. Many specimens at Stanley Glacier display soft tissue well.
- "Haplophrentis carinatus". Burgess Shale Fossil Gallery. Virtual Museum of Canada. 2011.
- "Haplophrentis". Smithsonian Institution.
- Babcock, L. E.; Robison, R. A. (1988). "Taxonomy and paleobiology of some Middle Cambrian Scenella (Cnidaria) and Hyolithids (Mollusca) from western North America" (PDF). University of Kansas Paleontological Contributions. 121: 1–22. ASIN B00071LPJW. hdl:1808/3638. OCLC 19610612.
- Moysiuk, Joseph; Smith, Martin R.; Caron, Jean-Bernard (2017). "Hyoliths are Palaeozoic lophophorates". Nature. 541 (7637): 394. doi:10.1038/nature20804.
- 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. JSTOR 20173022.
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