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Indonesian Throughflow Variability on Sub-OrbitalTimescales during Marine Isotope Stage 3:Geochemical Aspects.
Zuraida, Rina (2011) Indonesian Throughflow Variability on Sub-OrbitalTimescales during Marine Isotope Stage 3:Geochemical Aspects. (PhD/ Doctoral thesis), Christian-Albrechts-Universität, Kiel, Germany, 207 pp.
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Abstract
This thesis examines variability of the Indonesian Throughflow (ITF) and factors controlling its variability during Marine Isotope Stage 3 (~24–62 ka B.P.). Proxy records from Cores MD01-2378 (mixing zone between ITF and Indian Ocean waters) and 185 SO185-18460 (ITF) are developed and examined. The main objectives of this study are (1) to detect the amplitude and frequency of changes in surface and thermocline temperature and 18O within the main ITF outflow during MIS 3, (2) to test the hypothesis that a slow down in thermohaline circulation during stadials reduces the cool and fresh ITF thermocline flow, (3) to test modeling predictions that a reduction in ITF thermocline flow during stadials alters hydrographic profiles in the eastern Indian Ocean and leads to a warmer and saltier tropical Indian Ocean, and (4) to assess linkages between high latitude and tropical climate evolution.
Document Type: | Thesis (PhD/ Doctoral thesis) |
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Thesis Advisor: | Kuhnt, Wolfgang and Nürnberg, Dirk |
Keywords: | Indonesian Throughflow; Mg/Ca Thermometry; MIS3; Indonesischer Durchstrom; Mg/Ca Thermometrie; MIS3 |
Research affiliation: | OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography Kiel University |
Expeditions/Models/Experiments: | |
Date Deposited: | 22 Mar 2024 11:59 |
Last Modified: | 14 Aug 2024 13:30 |
URI: | https://oceanrep.geomar.de/id/eprint/60133 |
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