The Mount Stephen trilobite beds (UNSM locality 14s)[1] are a series of fossil strata on Mount Stephen, British Columbia that contain exceptionally preserved fossil material. Part of the same stratigraphic unit as the Burgess Shale deposit, many non-mineralized parts (such as anomalocarid claws, sponges, and trilobite legs) are preserved; in addition, a high density of trilobite fossils is present.
A high density of trilobites are present at the trilobite beds.
The trilobite beds
The trilobite beds were the first Burgess shale locality to be discovered.[2]
The richness of fossils in the Field area was first identified by workers associated with the construction of the Trans-Canada railway, which had (somewhat controversially) been routed through the Kicking Horse valley.[3] Richard McConnell, of the Geological Survey of Canada, was pointed to the beds by a railway worker whilst mapping the geology around the railway line in September 1886.[4] Several unusual fossils were subsequently described from this site, including sponges, worms,[5] and the appendages of the unusual Anomalocaris, identified at that time as the bodies of crabs.[6] These fossils prompted Charles Doolittle Walcott to make forays into the area, and led to his discovery of the Walcott Quarry on Fossil Ridge.
^Collins, D. (July 1, 2009). "A Brief History of Field Research on the Burgess Shale". In Caron, Jean-Bernard; Rudkin, David (eds.). A Burgess Shale Primer—History, Geology and Research Highlights. The Burgess Shale Consortium. pp. 15–32. ISBN978-0-9812885-0-5.
^Matthew, G.F. (1899). "Studies on Cambrian Faunas, No. 3.—Upper Cambrian Fauna, Mount Stephen, British Columbia.—The Trilobites and Worms". Philosophical Transactions of the Royal Society. 5: 39–68.
^Whiteaves, J.F. (October 1892). "Description of a new genus and species of Phyllocarid crustacean from the Middle Cambrian of Mount Stephen, B.C.". The Canadian Record of Science. 5 (4).