Onset and Role of the Antarctic Circumpolar Current.

• Published in: Paleoceanography
• Main Authors: Barker, P., Filippelli, G., Florindo, F., Martin, E., Scher, H.
• Other Authors: Barker, P.; Church St., Great Gransden, SG19 3AF, UK, Filippelli, G.; Dept of Geology, Indiana Univ.-Purdue Univ. Indianapolis (IUPUI), Indianopolis, IN 46202-5132 USA, Florindo, F.; Istituto Nazionale di Geofisica e Vulcanologia. Via di Vigna Murata 605, 00143 Rome, Italy, Martin, E.; Dept of Geological Sciences, Univ. of Florida, Gainesville, FL 32611-2120, USA, Scher, H.; Dept of Earth & Environmental Sciences, Univ. of Rochester, Rochester NY 14611, USA, Church St., Great Gransden, SG19 3AF, UK, Dept of Geology, Indiana Univ.-Purdue Univ. Indianapolis (IUPUI), Indianopolis, IN 46202-5132 USA, Istituto Nazionale di Geofisica e Vulcanologia. Via di Vigna Murata 605, 00143 Rome, Italy, Dept of Geological Sciences, Univ. of Florida, Gainesville, FL 32611-2120, USA, Dept of Earth & Environmental Sciences, Univ. of Rochester, Rochester NY 14611, USA
• Format: Manuscript
• Language: English
• Published: 2006
• Subjects: Antarctic; 03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatology; The Antarctic; Antarc*
• Online Access: http://hdl.handle.net/2122/2184

The major role for the ACC, as inferred in the past, is to have caused or stabilised full Antarctic glaciation. This role has since been questioned, and other hypothesised roles are relatively minor. Using a “smoking gun” assumption, determination of the time of onset of an ACC will resolve uncertainties in its role, and constrain the importance of ocean circulation to climate. To this end, we summarise all published estimates of ACC onset. The time of onset, of shallow circulation or deep, is extremely uncertain, whether based on tectonic studies or the interpretation of changes in the sediment record. Two potential final barriers to circumpolar flow have been identified; south of Tasmania and south of South America. The former is wellconstrained by tectonics and marine geology to before 32 Ma for a deep gap, with a shallow gap in place by 35.5 Ma at the latest. These ages fit nicely with the onset of full Antarctic glaciation at 33-34 Ma, although some workers deny the causality. Estimates of the time of opening of the latter range very widely, whether based on tectonics or sedimentary geology, from as recently as 6 Ma to as early as 41 Ma, with the gap depth uncertain also. Resolution of the tectonics-based uncertainties by additional survey being most probably both timeconsuming and inconclusive, and the geological estimates being open to alternative interpretations, we define an optimal strategy for additional sampling and measurement, designed to resolve the time of onset much more certainly, possibly also resolving between deep and shallow opening, and thereby constraining the ACC role. Sample sites would have to be close to likely final barriers, to avoid extraneous influence, and within modern zones of ACC influence, ideally would form a depth transect, and would have continuous, mixed terrigenous and biogenic sections. A wide range of carefully-selected parameters would be measured at each. Submitted open