Hyolithids

HyolithidsHyoliths are an extinct group of animals that had cone shaped shells.  They lived from the Cambrian to the Permian, but were most diverse and abundant during the Cambrian.  Most paleontologists think that they lived on the sea-floor, did not move around much, and fed on organic material in the sediment (deposit feeders).  Many paleontologists agree that hyoliths are related to mollusks, though the closeness of this relationship remains in dispute.

Three species of hyolithids known from the Cambrian of Utah include:

Many specimens are well-preserved and show the distinctive cone-shaped shell, the operculum (a “trap-door” that covered the front end of the animal), and the paired spines called “helens”, which are thought to have been used for stabilization on the sea-floor.

Gallery of Hyolithids

Note: Marks on all scale bars are centimeters (cm).

 

Haplophrentis reesei Babcock & Robison, 1988

KUMIP 204339 (Holotype). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figures 5.2 and 6.5 in Babcock & Robison (1988).

KUMIP204339

 

KUMIP 204340 (Paratype). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figures 5.1 and 6.4 inBabcock & Robison (1988) .

KUMIP204340

 

KUMIP 204341 (Paratype; part and counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figures 5.3 and 6.6 in Babcock & Robison (1988).

KUMIP204341AKUMIP204341B

 

KUMIP 204342 (Paratype; operculum only). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 5.4 in Babcock & Robison (1988).

KUMIP204342

 

KUMIP 204343 (Paratypes; two specimens). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 1.1 in Babcock & Robison (1988).

KUMIP204343

 

KUMIP 204352 (Paratype). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 1.2 in Babcock & Robison (1988).

KUMIP204352

 

KUMIP 204383 (Paratype; part and counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figures 5.5 and 6.1 in Babcock & Robison (1988).

KUMIP204383AKUMIP204383B

 

KUMIP 204384 (Paratype; part and counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figures 5.6 and 6.3 in Babcock & Robison (1988).

KUMIP204384AKUMIP204384B

 

"Hyolithes" idahoensis Resser, 1938

KUMIP 204345. Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 9.2 in Babcock & Robison (1988).

KUMIP204345

 

KUMIP 204346 (operculum only). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 9.3 in Babcock & Robison (1988).

KUMIP204346

 

KUMIP 204385 (Part and counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figures 9.1a and 9.1b in Babcock & Robison (1988).

KUMIP204385AKUMIP204385B

 

"Hyolithes" comptus Howell, 1946

KUMIP 204344. Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 8 in Babcock & Robison (1988).

KUMIP204344

 

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