Where: New South Wales, Australia (35.4° S, 150.4° E: paleocoordinates 70.4° S, 162.3° E)

• coordinate based on nearby landmark

• small collection-level geographic resolution

When: Wandrawandian Formation, Roadian (272.3 - 268.8 Ma)

• Brachiopods suggest the Echinalosia davidi or E. discinia zone, correlated with the upper part of APP3.3 to APP4.1 palynomorph zone (Briggs, 1998). There are no direct radiometric constraints on APP3.3, although the top of the underlying APP3.2 is around 271.6 Ma (Laurie et al., 2016), placing it near the Kungurian-Roadian boundary or in the lower Roadian. Strata in Western Australia assigned to APP4.1 yielded U-Pb ages of 269.25 Ma or younger, constraining the upper boundary of APP3.3 to the late Roadian. As a result, APP3.3 appears to fall entirely within the Roadian. The top of APP4.1 is likely late Wordian, constrained by earliest Capitanian radiometric dates in the lower part of APP4.2 (Laurie et al., 2016). The Broughton Formation, higher in the Sydney Basin succession, also yields an early Capitanian radiometric date (262.51 Ma) from its uppermost part (Metcalfe et al., 2015). Therefore upper parts of the formation are possibly early Wordian in age, but a Roadian age is assigned in the Ulladulla area.

• group of beds-level stratigraphic resolution

Environment/lithology: prodelta; lithified mudstone

Size class: macrofossils

Collection methods: peel or thin section,

Primary reference: C. M. Reid. 2003. Permian Bryozoa of Tasmania and New South Wales: systematics and their use in Tasmanian biostratigraphy. Association of Australasian Palaeontologists, Memoir 28:1-133 [D. Bottjer/C. Powers]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 97266: authorized by Matthew Clapham, entered by Matthew Clapham on 21.07.2010

Creative Commons license: CC BY (attribution)