CORDIS Project
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This project investigates past ocean salinity changes using deep-sea foraminifers to understand their role in climate dynamics. It aims to establish a new proxy for paleosalinity and explore the Mediterranean Outflow Water's impact on historical climate shifts.
Heat and salt are major components of the thermohaline circulation of the global conveyor belt as they regulate the masses of water bodies and and hence ocean-climate dynamics.
The thermohaline circulation (THC) has played a significant role in the past climate extremes such as the onset of the Northern Hemisphere Glaciation.
Although the temperature component of the THC can be extracted applying various methods such as foraminiferal magnesium/calcium thermometry and alkenone thermometry, salini…
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