Tegert Formation, Lower Silurian, southern Rocky Mountains, southeastern British Columbia
Trilobites:
Paracybantyx tegartensis Norford, 1994
Songkania sp. Norford, 1994
Scotoharpes sp. Norford, 1994
Radiurus avalanchensis Chatterton and Perry, 1984
Youngia sp. 1 Norford, 1994
Youngia sp. 2 Norford, 1994
Wallacia hendersoni Norford, 1994
Podowrinella rossi Norford, 1994 (also in the Beaverfoot Fm.)
indet. lichid Norford, 1994
?Kettneraspis sp. Norford, 1994
Eophacops aff. E. marklandensis = Podowrinella rossi
Encrinurus sp. (of Norford, 1962) = Wallacia hendersoni
Cheirurus cf. C. niagarensis (of Norford, 1962) = Radiurus avalanchensis
Comments:
The Tegert Formation outcrops in the western Ranges of the Rocky Mountains near Radium, British Columbia. Almost all known outcrops are in Canada's Rocky Mountain Parks, so collecting is forbidden. The Tegert Formation consists mainly of argillaceous limestone and shale and occurs locally beneath the sub-Devonian unconformity. Fossils include: graptolites, conodonts, and benthic macrofossils (trilobites, brachiopods, echinoderm fragments, also rare corals, gastropods, cephalopods, and conularids). The age is Late Telychian (Late Llandovery). The trilobite fauna is named after the two most prominent genera - the Podowrinella-Radiurus Fauna. Ten species of trilobites have been recorded (Norford, 1994).
References:
Norford,
B. S. (1994) Biostratigraphy and
trilobite fauna of the Lower Silurian Tegart Formation, southeastern British
Columbia. In Contributions to Canadian Paleontology, Geological Survey of
Canada, Bulletin 479, p. 13-47.
Western
Trilobites Association Home: |