Enigmatic Fossil Creature #5 from Cambrian Utah (Sidneyia?)

From a Burgess Shale-like Laggerstatte

Arthropoda Indet. (Sidneyia?)

Geological Time: Upper Middle Cambrian

Size: 63 mm long by 43 mm

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


Sidneyia Cambrian FossilDescription: Yet another of the fantastic fossils being uncovered in the Weeks Formation, this spiky arthropod looks to have its affinities with Sidneyia inexpectans, a large Burgess Shale arthropod named by C.D. Walcott for his son. It seems to have a more spiky carapace thanSidneyia Fossil Utah Sidneyia, but otherwise has many of the same features (see the reconstruction). Like Sidneyia, the gut contents seem hard shelled, perhaps the remains of trilobites. At any rate, seen here as a part/counterpart example, this is a most unusual and unique specimen.

SidneyiaThe 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.

Related: Soft-bodied Cambrian Explosion Biota from Utah

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).

click fossil pictures to enlarge


l Fossil Mall Home l Fossils Science Section l

Cambrian Explosion Fossils at Fossil Mall