Also known as "top 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.
• bed-level stratigraphic resolution
Environment/lithology: submarine fan; conglomeratic, cherty/siliceous wackestone and siltstone
Size class: macrofossils
Preservation: trace
Collection methods: chemical, mechanical,
• The specimens were collected in 1967 and 1968 by K. D. Corbett and are presently housed in the Geology Department, University of Tasmania (UT). The top faunal horizon has the richest amount of fossils of the three stratigraphic faunal groupings. All of the 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 8087: authorized by Mark Patzkowsky, entered by Phil Borkow on 19.06.2000
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Artiopoda | |
Pseudagnostus sp. Jaekel 1909 | |
Micragnostus sp.1 Howell 1935 | |
Brachiopoda | |
Brachiopoda indet. Cuvier 1805 represents an acrotretid, different than that found in the bottom fauna.
| |
Lingulata | |
| |
unclassified | |
Porifera indet. Grant 1836 |