Miocene Climate Transitions in the Southwest Pacific, Tasmania: Interpretations Based on Calcareous Nannofossils

• Other Authors: Roessig, Kristeen Lynn McGonigal. (authoraut), Wise, Sherwood W. (professor directing dissertation), Iverson, Richard (outside committee member), Lundberg, Neil (committee member), Wang, Yang (committee member), Donoghue, Joseph (committee member), Department of Earth, Ocean and Atmospheric Sciences (degree granting department), Florida State University (degree granting institution)
• Format: Text
• Language: English
• Published: Tallahassee, Florida: Florida State University 2007
• Subjects: Oceanography; Atmospheric sciences; Meteorology; Antarctic; Southern Ocean; The Antarctic; East Antarctic Ice Sheet; Shackleton; Pacific; New Zealand; Cape Roberts; Malone; Kennett; Antarc*; Antarctica; Ice Sheet
• Online Access: https://diginole.lib.fsu.edu/islandora/object/fsu%3A180830/datastream/TN/view/Miocene%20Climate%20Transitions%20in%20the%20Southwest%20Pacific,%20Tasmania.jpg

The tectonic separation of Australia from Antarctica is a key constraint on the development of the Antarctic Circumpolar Current (ACC) during the Cenozoic. The ACC plays a critical role in global climate thermally isolating Antarctica and its initiation is hypothesized to have crossed a critical global climate boundary resulting in initial Antarctic ice sheet growth (Kennett, Houtz et al., 1975; Exon, Kennett, Malone et al., 2001). The relatively shallow Tasmanian Gateway is one of the few places in the Southern mid to high latitudes where fairly complete, carbonate-rich sequences can be drilled detailing development of the ACC. The upper Oligocene and Miocene sediments recovered by Ocean Drilling Program (ODP) Leg 189 are rare when compared to other Southern Ocean drilling sites in terms of biotic richness and continuous sedimentation through the Miocene (Exon, Kennett, Malone et al., 2001). The Miocene has been characterized as a warm interval with significant cooling taking place in the middle Miocene with the permanent emplacement of the East Antarctic Ice Sheet (EAIS) (Shackleton and Kennett, 1975). Evidence for periods of ice sheet growth and decay prior to the mid-Miocene permanent emplacement of the EAIS include deep-sea oxygen isotope records (Miller et al., 1987) correlated with major sequence boundaries (Haq et al., 1987) and glacimarine sediments deposited on the Antarctic margin (Cape Roberts Science Team, 1999; Roberts et al., 2003). Climatic conditions fluctuated in the early Miocene peaking in warmth at the mid-Miocene Climatic Optimum (~16Ma). A major shift in the stable isotope records at ~14 Ma marks a significant phase of ice growth on Antarctica (Kennett and Shackleton, 1975). This cooling trend continued and by the middle/late Miocene the development of oceanic fronts was well established in the Tasmanian and New Zealand sectors of the Southern Ocean (Exon, Kennett, Malone et al., 2001; Nelson and Cooke, 2001). This dissertation interprets the calcareous nannofossil assemblage data, coupled ...