Also known as "bottom fauna", Singing Creek Formation, Denison Range, Tasmania - Jago 1987
Where: Tasmania, Australia (43.0° S, 147.0° E: paleocoordinates 43.0° S, 147.0° E)
• local area-level geographic resolution
When: Proceratopyge cryptica + Stigmatoa diloma trilobite zone, Singing Creek Formation, Maentwrogian (497.0 - 496.8 Ma)
• Stratigraphically equivalent fossils are found elsewhere in the Adamsfield Trough. The bottom faunal horizon is 185-240m above the base of the Singing Formation. bottom faunal horizon
• group of beds-level stratigraphic resolution
Environment/lithology: submarine fan; lithified, conglomeratic, cherty/siliceous wackestone and siltstone
Size class: macrofossils
Collection methods: chemical, mechanical,
• The specimens were collected in 1967-1968 by K.D. Corbett and are presently housed in the Geology Department, University of Tasmania (UT). All specimens have undergone tectonic distortion.
Primary reference: J. B. Jago. 1987. Idamean (Late Cambrian) trilobites from the Denison Range, south-west Tasmania. Palaeontology 30(2):207-231 [M. Patzkowsky/P. Borkow/J. Alroy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 8084: authorized by Mark Patzkowsky, entered by Phil Borkow on 19.06.2000
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Trilobita | |
Eugonocare sp. Whitehouse 1939 trilobite | |
"Dokimocephalidae indet." = Dokimokephalidae
"Dokimocephalidae indet." = Dokimokephalidae Kobayashi 1935 trilobite | |
Proceratopyge sp. Wallerius 1895 trilobite | |
Artiopoda | |
Micragnostus sp.2 Howell 1935 | |
Pseudagnostus idalis n. sp., Denagnostus corbetti n. gen. n. sp.
Pseudagnostus idalis n. sp. Opik 1967
Denagnostus corbetti n. gen. n. sp. | |
Brachiopoda | |
| |
Strophomenata | |
Billingsella sp. Hall and Clarke 1892 |