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Deglacial and Holocene changes in Mediterranean Thermohaline Circulation: A joint perspective from Eastern and Western basins [INQUA 2023]
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The dominant arid climate conditions over the Mediterranean (Med) control water
properties and the formation processes of intermediate and deep water masses. Deep
convection cells occur in both the E- and W-Med basins and there are interconnected
through the intermediate waters mostly formed in the easternmost area of the Med. During
last deglaciation and Holocene periods both E- and W-Med had experienced periods of
major disruptions in deep convection. The last organic layer (ORL1) formed in the WMed
during the deglacial period and later the last sapropel (S1) in the E-Med. Both
enhanced productivity and enhanced stratification are regarded as the causes for the two
events but responding to different drivers, the deglacial freshening in the case of the
ORL1 and the African monsoon flooding for the S1.
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CACHO LASCORZ, Isabel, CATALÀ, Albert, PENA GONZÁLEZ, Leopoldo david, FRIGOLA FERRER, Jaime i., CAMPDERRÓS SERRA, Sara, INGLAVAGA, R., MARTÍN CLOSAS, Carles, TRIAS NAVARRO, Sergio, CHECA, Helena, DE LA FUENTE, María, MARGARITELLI, Giulia, PÉREZ-ASENSIO, José n. (josé noel), LIRER, Fabrizio. Deglacial and Holocene changes in Mediterranean Thermohaline Circulation: A joint perspective from Eastern and Western basins [INQUA 2023]. _Presentació a: XXII INQUA Congress 2023_. Roma (14-20 July). Session 133: Unravelling Mediterranean sensitivity to past rapid climate variability. Abstract ID. 5278 Oral presentation. [consulta: 25 de novembre de 2025]. [Disponible a: https://hdl.handle.net/2445/202104]