Anomalocaridids


"a picture of four red lines coming from the bottom right center on a tan rock"Anomalocaridids are one of the most charismatic groups of Cambrian animals. These swimming creatures were the largest Cambrian animals and were probably top-level predators. They had a dougnut shaped mouth (originally thought to be a jellyfish!) with two large grasping appendages on either side. For more information on anomalocaridids, visit the Smithsonian Institution's webpage about Anomalocaris.

We have chosen to group anomalocaridids with the arthropods on the basis of their sclerotized, segmented feeding appendages. While most paleontologists think that anomalocaridids are closely related to arthropods, some think that they represent a basal branch on the portion of the evolutionary tree containing the arthropods and therefore deserve their own phylum-level status.

Regardless of how one classifies anomalocaridids, they were remarkable animals and are well-represented in the Cambrian fossil record of Utah. While several genera of anomalocaridids have been described--especially from the Burgess Shale of British Columbia and the Chengjiang region of China--all specimens from Utah have been referred either to the genus Anomalocaris or the family Anomalocarididae.

Some have suggested that Pahvantia and Proboscicaris, both of which are classified here as bivalved arthropods, were actually parts of an anomalocaridid.

 

Gallery of Anomalocaridids

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




Anomalocaris sp. Whiteaves, 1892




a tan rock with red marks in the middle that stretch down the rock

KUMIP 314037. Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 1.1 in Briggs & Lieberman et al. (2008).

a yellow fish outline on a white and gray rock

KUMIP 314087. Wheeler Formation, House Range, Millard County, Utah. Figure 3.1 in Briggs & Lieberman et al. (2008).




Anomalocaris nathorsti (Walcott, 1911)




a close up of a gray rock with two gray marks that have long lines coming out of them

KUMIP 153093 (part, counterpart). Wheeler Formation, House Range, Millard County, Utah. Figure 1-4 in Conway Morris & Robison (1982).

a gray rock with a dark brown mark at the bottom that has pointy lines going up

KUMIP 153094. Wheeler Formation, House Range, Millard County, Utah. Figure 5 in Conway Morris & Robison (1982).

a close up of a gray rock with a yellow line with smaller lines coming out of it on the right side

KUMIP 204777 (part, counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 26.1a, 26.1b in Conway Morris & Robison (1988).

a close up of a gray rock with a red curved line that has a smaller line coming out and point to the left

KUMIP 204778 (part, counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah. Figure 26.2 in Conway Morris & Robison (1988).

a close up of a yellow rock with a black mark that has smaller lines pointing out to the left

KUMIP 204779 (part, counterpart). Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah.

a close up of a gray rock with a faded mark in the middle that looks like it is dripping down the rock

KUMIP 204780. Spence Shale Member of the Langston Formation, Wellsville Mountains, Box Elder County, Utah.

a close up of a gray rock with a black mark in the middle

KUMIP 204781 (part, counterpart). Wheeler Formation, House Range, Millard County, Utah. Figure 26.3 in Conway Morris & Robison (1988).

close up of the edge of a tan rock that has red lines pointing out of the middle with one large line in the middle

KUMIP 314095 (part, counterpart). Marjum Formation, House Range, Millard County, Utah.




Anomalocaridae gen. et sp. indet. (genus & species unknown)




a close up of a tan rock with a outline of a uncompleted circle with dark tan pointy lines coming out of the outline of the circle

KUMIP 314078 (part, counterpart). Wheeler Formation, House Range, Millard County, Utah. Figure 2.1 in Briggs & Lieberman et al. (2008).

a close up of a gray rock with a black mark in the middle that look like connected thick lines

KUMIP 314086 (part, counterpart). Wheeler Formation, House Range, Millard County, Utah. Figure 2.2 in Briggs & Lieberman et al. (2008).