Where: Queensland, Australia (21.5° S, 148.5° E: paleocoordinates 57.8° S, 146.0° E)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Moonlight Sandstone Member (Blenheim Formation), Wordian to Wordian (266.9 - 259.5 Ma)
• Presence of Terrakea brachythaera suggests an age within the E. runnegari/E. wassi zone, correlated with APP4.2 palynomorph zone (Briggs, 1998). The APP4.2 zone was constrained as late Wordian to mid-Wuchiapingian age by U-Pb dating in Laurie et al. (2016). In the Sydney Basin, these species are common in the Broughton Formation, dated as older than early Capitanian (a sample 2 m below the top yielded a radiometric date of 262.51 Ma in Metcalf et al., 2015). As a result, a Wordian-Capitanian age is assigned here.
• group of beds-level stratigraphic resolution
Environment/lithology: coastal; lithified sandstone
Size class: macrofossils
Primary reference: B. Runnegar. 1965. The bivalves Megadesmus Sowerby and Astartila Dana from the Permian of eastern Australia. Journal of the Geological Society of Australia 12(2):227-252 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 85041: authorized by Matthew Clapham, entered by Matthew Clapham on 22.11.2008
Creative Commons license: CC BY (attribution)
Taxonomic list
Strophomenata | |
Terrakea brachythaera2 Morris 1845 | |
"Echinalosia cf. runnegari" = Glabauria runnegari2
"Echinalosia cf. runnegari" = Glabauria runnegari2 Briggs 1998 | |
Rhynchonellata | |
"Spirifer duodecimcostatus" = Glendonia duodecimcostata1
"Spirifer duodecimcostatus" = Glendonia duodecimcostata1 M'Coy 1847 | |
Bivalvia | |
| |
"Megadesmus grandis" = Megadesmus (Cleobis) grandis
"Megadesmus grandis" = Megadesmus (Cleobis) grandis Dana 1847 clam |