Interpretation of the 231Pa/230Th paleocirculation proxy: New water-column measurements from the southwest Indian Ocean |
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| Institution: | 1. Micropaleontology Laboratory, CSIR-National Institute of Oceanography, Dona Paula 403004, Goa, India;2. Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee 247667, India;1. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA;2. Department of Earth and Environmental Sciences, Columbia University, New York, NY, USA;3. Department of Ocean Sciences, University of California, Santa Cruz, CA 95064, USA;4. Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA;5. Institute of Global Environmental Change, Xi''an Jiaotong University, Xi''an, China |
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| Abstract: | Measurements of 231Pa, 230Th and 232Th concentrations have been made on five water-column profiles along the western margin of the Madagascar and Mascarene Basins in the southern Indian Ocean. These measurements help to fill a significant gap in the global coverage of water-column 232Th, 230Th and 231Pa data. 232Th concentrations vary, but generally increase with depth, suggesting higher particle loading in deeper waters, and the presence of a significant dissolved fraction of 232Th. 230Th concentrations increase with depth, and profiles are similar to the average of existing data from other regions. 231Pa concentrations, on the other hand, show significant depth structure, apparently reflecting the various water masses sampled at this location. The modified remnants of North Atlantic Deep Water are found at a depth of ≈ 2000 m and exhibit elevated 231Pa concentrations exported from the South Atlantic. Antarctic Intermediate and Bottom Waters have lower 231Pa, probably due to scavenging onto opal particles during transit from the Southern Ocean. The differences between water masses raises a question: which water mass is important in controlling the 231Pa/230Th ratio in underlying sediments? A simple one-dimensional model is used to demonstrate that the 230Th and 231Pa exported to sea-floor sediments last equilibrates with waters close to the seafloor (within ≈ 1000 m), rather than averaging the whole water column. These findings suggest that 231Paxs/230Thxs in sediments provides information primarily about deep-water masses. In this region, sedimentary records will therefore provide information about the past flow of Antarctic Bottom Water into the Indian Ocean. Interpretation of data from other regions, such as the North Atlantic where this proxy has most successfully been applied, requires careful consideration of regional oceanography and knowledge of the composition of the water masses being investigated. |
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