|Author||Mccave, I. N.|
|Subject Domain (in DDC)||Computer science, information & general works ♦ Data processing & computer science|
|Subject Keyword||Southwest Pacific Gateway ♦ Deep Pacific Source Modified ♦ Southwest Pacific Gatewayleg ♦ Acc-dwbc System ♦ Wind-driven Antarctic Circumpolar Current ♦ Latitudinal Range ♦ Excellent Stratigraphic Record ♦ Sediment Drift East ♦ Understanding World Oceanic ♦ Southern Ocean Neogene Paleohydrography ♦ 32-20 Ma ♦ Sedimentary Sequence ♦ South America ♦ Deep Western Boundary Current ♦ Pacific Dwbc ♦ High-priority Problem ♦ Neogene Sediment ♦ Plate Movement ♦ Water Depth ♦ Dwbc Erosion ♦ Modern Acc-dwbc ♦ Deep Antarctic Bottom Water ♦ Dsdp Drilling ♦ Previous Hydraulic Piston Core Site ♦ First Deep-water Oceanic Gap ♦ World Ocean ♦ Related Water Mass ♦ Earth Climate ♦ Late Oligocene ♦ Seven Southwest Pacific ♦ Large Region ♦ Southwest Pacific Ocean History ♦ New Zealand Microcontinental Plateau ♦ Climatic History|
|Abstract||The circulation of cold, deep Antarctic Bottom Water (AABW) is one of the controlling factors in Earth’s climate. Today, 40 % of this water enters the world ocean through the Southwest Pacific Gateway as a thermohaline driven Deep Western Boundary Current (DWBC). South of 46°S, the DWBC is coupled with the wind-driven Antarctic Circumpolar Current (ACC). Understanding the evolution of the Pacific DWBC is fundamental to understanding world oceanic and climatic histories. The ACC-DWBC system has evolved since the late Oligocene (32-20 Ma), when plate movements created the first deep-water oceanic gaps south of Australia and South America. An excellent stratigraphic record of these events, and of the development of the modern ACC-DWBC, occurs in sediment drifts east of the New Zealand microcontinental plateau. Seven Southwest Pacific drill sites are proposed to reconstruct the stratigraphy, paleohydrography, and dynamics of the DWBC and related water masses. The proposed sites comprise a transect of water depths from 320 m to 4460 m, and span a latitudinal range from 39°S to 51°S. Only one previous hydraulic piston core site is located in this large region (Deep Sea Drilling Project [DSDP] Site 594), and earlier DSDP drilling (Sites 275-276) occurred at sites where Neogene sediment is largely missing due to DWBC erosion. Consequently, our knowledge of Southwest Pacific ocean history, and of the development of the ACC-DWBC system, is extremely poor. Coring during Leg 181 will provide the sedimentary sequences needed to study a range of high-priority problems in Southern Ocean Neogene paleohydrography, sedimentology, paleoclimatology, and micropaleontology.|
|Educational Role||Student ♦ Teacher|
|Age Range||above 22 year|
|Education Level||UG and PG ♦ Career/Technical Study|
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