| Summary: | The Atlantic Meridional Overturning Circulation (AMOC) plays a central role in the northward distribution of heat. It is a key mechanism in the climatic system that needs to be further understood. Most studies focused on surface or deep water conditions. Relatively little is known about the role of subsurface, thermocline and intermediate waters, where heat uptake and/or transport occur. Our aim is to give a better representation of the hydrography during the past by reconstructing the upper water column from surface to intermediate waters. Understanding of how changes in the upper water masses properties is crucial for determining the role of oceanic heat distribution involved in the AMOC and is the main objective of this PhD project. The Western Tropical Atlantic is a sensitive oceanic region connected with surface and intermediate waters that flow from the Southern Hemisphere into the North Atlantic and a deep water mass from the Northern Hemisphere. This region is unique in identifying the upper limb pathway of the AMOC and associated water masses. In this context, using sediment cores from depth transects is therefore crucial for estimating not only the magnitude of change but, particularly the orientation of water mass distribution change. Seven coring sites have been retrieved that fall along a depth transect extending from 600 to 1000 m water depth. Main strategy is to use different planktonic species having different depth habitat to reconstruct the upper surface to about 200-400 m water depth, and furthermore benthic species from depth of the coring sites to reconstruct water mass changes further below to 1000 m. The PhD project has two major objectives. The first is to calibrate and validate relationship between Mg/Ca ratio and temperature in benthic foraminiferal shells. Mg/Ca ratio in several benthic foraminifer species from core-tops were analysed to develop Mg/Ca calibrations over the 0-6 degrees Celsius temperature range in the Atlantic Ocean (Paper I). Apart from temperature, other factors may ...
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