Anomalocaris nathorsti Fossil from Utah

a terror of the cambrian seas

Anomalocaris cf nathorsti

Geological Time: Upper Middle Cambrian

Size: 25 mm long by 14 mm across

Fossil Site: House Range, Weeks Formation, Millard County, Utah


AnomalocarisDescription: This is most of the thorax of the “Terror Of The Cambrian”, Anomalocaris saron, seen here in the first example I have had. The members of this group of enigmatic creatures are known from Asia, Australia, Europe, and North America, and are thought by many to be closely allied with the Arthropda, a position not held by all researchers. Several have been described from Utah, notably a 50 mm partial specimen of A nathorsti from the Marjum Formation, but they are far more rare Anomalocaristhan those from Chengjiang or the Burgess Shale. The central gut trace is present, as well as indications of the lateral lobes. This is the first example I have had, and I do not expect it will remain posted for long.

The House Range of Utah has several formations that exhibit Burgess Shale-like preservation of soft tissues, and yield fossils of creatures closely allied with the Burgess Shale biota. Interestingly, the formations are normally found in alternating biofacies. Some are rich in trilobites lacking soft bodied organisms, while adjacent ones lack trilobites but preserve soft bodied organisms in the form of kerogenized carbon films. Gaines (2004) has studied the taphonomy of House Range soft tissue preservation, hypothesizing a taphonomic pathway much like the Burgess Shale with delayed decay facilitating rapid diagenesis in an anoxic zone lacking benthic bioturbators. While soft bodied organisms are far rarer and generally not so exquisitely preserved as in the Burgess Shale, some scientists believe the House Range biota might be even more diverse. Many fossils found are enigmatic as to their taxonomic placement. Unfortunately, the numerous sites are much understudied, while mining operations are resulting in wholesale destruction of a potentially rich portion of the Cambrian fossil record.

References:

  • Briggs D.E.G., and R.A. Robison. 1984. Exceptionally preserved non trilobite arthropods and Anomalocaris from the Middle Cambrian of Utah. University of Kansas Paleontological Contributions, Paper 111:1-24.
  • Gaines, Robert R.; Kennedy, Martin J. Droser, Mary L. 2004. A new hypothesis for organic preservation of Burgess Shale taxa in the middle Cambrian Wheeler Formation, House Range, Utah. Palaeo, 220:193-205.
  • House Range Fossils: Wheeler Shale, Marjum Formation, and Weeks Formation, The Virtual Fossil Museum (www.fossilmuseum.net).

Also see a putative Anomalocaris nathorsti Fossil from the older Wheeler Formation.

click fossil pictures to enlarge

 
 

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