Seminar: Alexander Piotrowski (University of Cambridge). Can deep ocean circulation pathways and strength be reconstructed using marine sediment dispersion?
Jaeger 1 Seminar Room Research School of Earth Sciences, 142 Mills Rd, Acton, ACT, AustraliaOcean circulation plays a key role in the Earth’s climate system because surface ocean currents transport heat and deep ocean water masses can sequester carbon dioxide from the atmosphere. Geochemical proxies measured on carbonate foraminifera picked from marine sediments have been widely utilized to reconstruct past ocean changes. However, it is difficult to use the... View Article