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dc.contributor.authorOlden, Liam J.
dc.contributor.supervisorMilo Barhamen_US
dc.contributor.supervisorJane Cunneenen_US
dc.date.accessioned2020-12-01T07:50:07Z
dc.date.available2020-12-01T07:50:07Z
dc.date.issued2020en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/81908
dc.description.abstract

Stromatolites from the northern Perth Basin, Western Australia, purported to be associated with the End Permian mass extinction (EPME), were re-examined through several new sites over an expanded 24 km2. New lithological relationships show the stromatolites are intimately associated with a clastic sequence and formed within a fluvio-lacustrine setting. A revised mid to late Permian age is proposed for the stromatolites, disassociated from the EPME. Stromatolite microstructures representing remnant skeletal cyanobacteria are exceptionally preserved throughout.

en_US
dc.publisherCurtin Universityen_US
dc.titleMid Phanerozoic stromatolites in the Northern Perth Basin: Understanding their evolution and occurrenceen_US
dc.typeThesisen_US
dcterms.educationLevelMResen_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US
curtin.contributor.orcidOlden, Liam J. [0000-0002-0198-1547]en_US


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