Cenozoic paleoceanographic changes of the South Pacific from seismic reflection data

• Main Author: Horn, Michael
• Format: Thesis
• Language: unknown
• Published: Staats und Universitätsbibliotek Bremen 2015
• Subjects: Antarctic; The Antarctic; East Antarctic Ice Sheet; Pacific; New Zealand; Bounty Trough; Antarc*; Ice Sheet
• Online Access: https://epic.awi.de/id/eprint/37832/; https://epic.awi.de/id/eprint/37832/1/Diss_Michael_Horn_zum_Publizieren.pdf; http://nbn-resolving.de/urn:nbn:de:gbv:46-00104423-12; https://hdl.handle.net/10013/epic.45471; https://hdl.handle.net/10013/epic.45471.d001

The Thermohaline Circulation (THC) in the world oceans is closely coupled with earth climate. With reconstructions of past oceanic conditions and comparisons with past climate conditions this coupling can be better understood. This in turn allows to provide better boundary conditions on ocean-climate coupling for forecasting models. However, the paleoceanographic setup is far from being completely revealed. One of the largest areas of the world oceans poorly surveyed is the South Pacific Ocean. The present ocean currents that transport deep cold water into the South Pacific are the Antarctic Circumpolar Current (ACC) and two northward setting flows directly influenced by the ACC, the Deep Western Boundary Current (DWBC) or western limb close to New Zealand and an eastern limb above the western flank of the East Pacific Rise (EPR). Understanding changes of this current system is important for reconstructions of past climates and the Antarctic Glaciation history. At present the reconstructed paleoceanographic history of the South Pacific is limited to ACC and DWBC at the western margin of the Southwest Pacific Basin and only reveals changes back to the Eocene/Oligocene boundary. This thesis presents new multichannel seismic reflection data surveying two regions at the eastern and western margin in the Southwest Pacific Basin. The objective is the identification and characterization of deep current derived sediment deposits in the South Pacific. The investigation covers the whole Cenozoic and thus provides indications for paleoceanographic changes due to East Antarctic Ice Sheet build-up prior to 34 Ma. Furthermore the study helps to fill a data gap in the open Pacific Ocean between New Zealand and South America and presents the first evidence for paleoceanographic changes in this poorly explored area. East of New Zealand at the Bounty Trough mouth a sediment drift indicates the onset of a deep cold current originating from the South Pacific Ocean around the Cretaceous/Palaeocene boundary. This current prevailed ...