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Lower Permian brachiopods from Wasp Head Formation, Sydney Basin, southeastern Australia

Cisterna,GA and Shi,GR 2014, Lower Permian brachiopods from Wasp Head Formation, Sydney Basin, southeastern Australia, Journal of Paleontology, vol. 88, no. 3, pp. 531-544, doi: 10.1666/13-004.

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Title Lower Permian brachiopods from Wasp Head Formation, Sydney Basin, southeastern Australia
Author(s) Cisterna,GA
Shi,GR
Journal name Journal of Paleontology
Volume number 88
Issue number 3
Start page 531
End page 544
Total pages 14
Publisher BioOne
Place of publication Washington, DC
Publication date 2014-05
ISSN 0022-3360
Keyword(s) Science & Technology
Life Sciences & Biomedicine
Paleontology
Bueno-Aires province
Summary Although there is a generally accepted framework for the Permian marine biogeography of Australia, significant uncertainties remain concerning the temporal biogeographical changes closely related to the timing of Permian glacial-interglacial events. Several recent studies along these research lines demonstrate the importance of a reliable high-resolution biostratigraphical timescale for paleobiogeographical and paleoclimatic reconstructions. This paper provides, for the first time, a full taxonomic and biostratigraphical study of the brachiopod fauna from the Wasp Head Formation, southern Sydney Basin, southeastern Australia. The fauna is associated with deposits of the first Permian glacial interval suggested for eastern Australia. Three brachiopod assemblages are recognized. The lower and middle assemblages contain scarce brachiopods although associated bivalves are comparatively more common. Despite very low diversity and low abundance, these two brachiopod assemblages contain characteristic species of the Strophalosia concentrica and Strophalosia subcircularis brachiopod zones, both considered of late Asselian age. The third assemblage, occurring in the uppermost part of the formation, contains more brachiopods than bivalves and is referred to early Sakmarian in age. The species diversity and stratigraphic occurrences of the brachiopod assemblages in relation to sedimentary facies suggest that the lower two assemblages may represent an intra-glacial interval while the younger third assemblage, characterized by abundant occurrences of Trigonotreta and Tomiopsis species, accompanied by the bivalve Eurydesma, is more indicative of a post-glacial benthic marine fauna comparable to coeval brachiopod faunas found elsewhere in Gondwana. © 2014, The Paleontological Society.
Language eng
DOI 10.1666/13-004
Field of Research 059999 Environmental Sciences not elsewhere classified
Socio Economic Objective 960305 Ecosystem Adaptation to Climate Change
HERDC Research category C1 Refereed article in a scholarly journal
Copyright notice ©2014, BioOne
Persistent URL http://hdl.handle.net/10536/DRO/DU:30067944

Document type: Journal Article
Collections: Faculty of Science, Engineering and Built Environment
School of Life and Environmental Sciences
Centre for Integrative Ecology
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Created: Mon, 01 Dec 2014, 10:22:30 EST

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