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• W2068886703 abstract "Research Article| October 01, 2004 FORAMINIFERAL BIOFACIES OF THE MIOCENE WARM TO COOL CLIMATIC TRANSITION IN THE PORT PHILLIP BASIN, SOUTHEASTERN AUSTRALIA Tiffany L. Gourley; Tiffany L. Gourley School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia Search for other works by this author on: GSW Google Scholar Stephen J. Gallagher Stephen J. Gallagher * School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia *Corresponding author E-mail: t.gourley@pgrad.unimelb.edu.au; sjgall@unimelb.edu.au Search for other works by this author on: GSW Google Scholar Author and Article Information Tiffany L. Gourley School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia Stephen J. Gallagher * School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia *Corresponding author E-mail: t.gourley@pgrad.unimelb.edu.au; sjgall@unimelb.edu.au Publisher: Cushman Foundation for Foraminiferal Research Received: 06 Jan 2003 Accepted: 24 Mar 2004 First Online: 03 Mar 2017 Online ISSN: 1943-264X Print ISSN: 0096-1191 © 2004 Journal of Foraminiferal Research Journal of Foraminiferal Research (2004) 34 (4): 294–307. https://doi.org/10.2113/34.4.294 Article history Received: 06 Jan 2003 Accepted: 24 Mar 2004 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Tiffany L. Gourley, Stephen J. Gallagher; FORAMINIFERAL BIOFACIES OF THE MIOCENE WARM TO COOL CLIMATIC TRANSITION IN THE PORT PHILLIP BASIN, SOUTHEASTERN AUSTRALIA. Journal of Foraminiferal Research 2004;; 34 (4): 294–307. doi: https://doi.org/10.2113/34.4.294 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract The Miocene marine sediments of the Torquay Group in the Port Phillip Basin of southeast Australia were deposited at a paleolatitude of at least 45°S. Nevertheless, the presence of subtropical larger foraminifers, plankton of the “Orbulina” bioseries and other biofacies signals testify to a time of global warmth and correspond to the “Miocene Climatic Optimum”. Throughout the Early Miocene to early Middle Miocene, bioclastic calcarenite of the Batesford Limestone was deposited in warm, subtropical and oligotrophic marine conditions in a high-energy inner-shelf (<70 m depth) environment. During the early Middle Miocene, a distinct change in foraminiferal assemblage accompanied the transition to deposition of finer-grained marl and silty clay of the Fyansford Formation. At this level, a significant increase in the abundance of infaunal and planktonic taxa indicates a shift to a low-energy, middle- to outer-shelf environment (50–100 m depth). The disappearance of the larger subtropical foraminifera and the shift to a foraminiferal assemblage dominated by cool-water upwelling indices later in the Middle Miocene, signal the onset of oceanic upwelling and climatic cooling as identified in other southern Australian Tertiary basins. This event can be correlated to a period of global climatic cooling and intensified oceanic circulation that occurred in response to expansion of the East and West Antarctic ice sheets during the Middle to Late Miocene. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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