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The Devonian system of New England, New South Wales, Australia



The Devonian system of New England, New South Wales, Australia



Pages 135-142 1967



The Devonian sequence of New England, Australia is essentially eugeosynclinal, the predominant rock types being pelagic or turbidite sediments of andesitic provenance. Interspersed limestones contain 8 or 9 coral and conodont faunas of early Gedinnian, late Emsian, Eifelian and Givetian ages. Famennian ammonoids and conodonts are known from higher in the succession. There is no faunal evidence for the presence of either Siegenian or Frasnian beds. Two unconformities have been recognised in the upper Devonian and it is possible that another unconformity (or disconformity) separates the Gedinnian and Emsian parts of the sequence.

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