Ordovician stratigraphy of the Junee-Narromine Volcanic Belt in central New South Wales, Australia: conodont studies and regional correlations.

This contribution reviews the newly revised biostratigraphy of Middle-Upper Ordovician marine shelf successions from the Junee-Narromine Volcanic Belt in central New South Wales, based on conodont studies from four areas covering the northern, central and southern sectors of the Belt. Seven conodont biozones ranging from the middle Darriwilian (Histiodella holodentata-Eoplacognathus pseudoplanus Biozone) to the lower Katian (Taoqupognathus blandus Biozone) are recognized in the Billabong Creek Formation exposed in the Gunningbland area. This includes the first known biostratigraphic succession in Australia that extends continuously from the middle Darriwilian to the basal Sandbian. These new data are crucial for a better understanding of the geological evolution of this region in central New South Wales, and for the enhanced cor-relation of Ordovician rocks throughout the Macquarie Volcanic Province, which hosts substantial porphyry Cu-Au mineral deposits.

Automated summary

This paper reviews the newly revised biostratigraphy of Middle-Upper Ordovician marine shelf successions in central New South Wales, focusing on the Junee-Narromine Volcanic Belt. Seven conodont biozones were recognized in the Billabong Creek Formation, extending from the middle Darriwilian to the lower Katian. These findings provide crucial information for understanding the geological evolution of the region and correlating Ordovician rocks in the Macquarie Volcanic Province, which contains significant mineral deposits.