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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/58263
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dc.contributor.authorCamens, Aaron Bruceen
dc.contributor.authorWells, R. T.en
dc.date.issued2009en
dc.identifier.citationJournal of Vertebrate Paleontology, 2009; 29(3):863-869en
dc.identifier.issn0272-4634en
dc.identifier.urihttp://hdl.handle.net/2440/58263-
dc.description.abstractThe first Pliocene marsupial fossil trackways from Australia are described. The trackways, attributed to Euowenia grata (De Vis) (Diprotodontoidea, Marsupialia), occur in the middle Pliocene Tirari Formation, Warburton River, northern South Australia. The trackways were formed as the animals made their way across a soft claypan. Pad impressions, subsequently infilled by a gypsum-cemented clay, indicate how weight was distributed within the pes.en
dc.description.statementofresponsibilityAaron Camens and Rod Wellsen
dc.language.isoenen
dc.publisherSoc Vertebrate Paleontologyen
dc.rights© 2009 by the Society of Vertebrate Paleontologyen
dc.titleDiprotodontid footprints from the Pliocene of Central Australiaen
dc.typeJournal articleen
dc.contributor.schoolSchool of Earth and Environmental Sciencesen
dc.identifier.doi10.1671/039.029.0316en
Appears in Collections:Earth and Environmental Sciences publications

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