CENOZOIC CONTOURITES IN THE EASTERN GREAT AUSTRALIAN BIGHT, OFFSHORE SOUTHERN AUSTRALIA: IMPLICATIONS FOR THE ONSET OF THE LEEUVVIN CURRENT

Thermohaline oceanic currents influence global heat transfer, controlling local and global variations in climate, biodiversity, and the terrestrial biosphere. Paleoceanographic studies typically use biostratigraphic and geochemical proxies to reconstruct the dynamics of these currents in Earth's ancient oceans, although seismic reflection data have also been successfully employed, most commonly in the North Atlantic Ocean. Here we use 2D seismic reflection data from the Ceduna Sub-basin, Great Australian Bight, offshore southern Australia, to describe middle Eocene to Recent contourites deposited in an overall carbonate-dominated succession. These deposits comprise large (100 m wavelength by up to 50 m tall) bedforms and deep (10-90 m), wide (up to 3 km) erosional scours. The scours are particularly well developed at one specific stratigraphic level, defining moats that encircle middle Eocene shield volcanoes, which formed syndcpositional bathy metric highs. We suggest that sediment erosion, transport, and deposition record middle Eocene initiation of the Leeuwin Current, one of the most important ocean currents in the southern hemisphere. Deepest seabed scouring occurs in the middle of the middle Eocene to Recent sequence, and may reflect middle Miocene waxing of the so-called proto-Leeuwin Current, possibly driven by changes in ocean circulation patterns caused by the Miocene Global Optimum. The results of this seismic reflection-based study are consistent with results derived from other paleoceanographic proxies, thereby highlighting the continued key role seismic reflection data have in understanding the occurrence, geographical distribution, and significance of ancient ocean currents.