Where: South Australia, Australia (30.0° S, 135.0° E: paleocoordinates 16.3° N, 166.0° W)
• local area-level geographic resolution
When: Moorowie Formation, Botomian (516.0 - 512.9 Ma)
• Equivalent to the Flinders Range of South Australia. Deposited during transgressive and highstand phases of the sequence showing transition from non marine to marine of a young seaway.
• formation-level stratigraphic resolution
Environment/lithology: shallow subtidal; lithified, bioturbated, calcareous wackestone
Preservation: original calcite, replaced with calcite, replaced with phosphate
Collection methods: peel or thin section,
• Specimens are spherulitic clustes or parallel calcite fibers, but mostly clusters of calcite crystallites (original).
Primary reference: J. E. Sorauf and M. Savarese. 1995. A Lower Cambrian coral from South Australia. Palaeontology 38(4):757-770 [M. Patzkowsky/P. Borkow/J. Alroy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 8094: authorized by Mark Patzkowsky, entered by Phil Borkow on 19.06.2000
Creative Commons license: CC BY (attribution)
Taxonomic list
Epiphyton | |
Epiphyton sp. Bornemann 1886 | |
Anthozoa | |
Flindersipora bowmani Lafuste et al. 1991 | |
Hormogoneae | |
Girvanella sp. Nicholson and Etheridge 1878 | |
Renalcis | |
Renalcis sp. Vologdin 1932 |