# name
A sedimentological insight into the deglacial reorganization of the Mediterranean thermohaline circulation

# metadata.dc.description.abstract[].value
During the last deglaciation and early Holocene significant oceanographic changes have been observed
in both western and eastern Mediterranean basins. Post glacial sea level rise strongly reduced the
northwestern overturning cell from 14.5 to 9 ka BP, which favored the formation of an organic rich layer in
the Alboran Sea. Increased river runoff in the east-Med enhanced water column stratification leading to the
formation of Sapropel 1 between 10.8-6.1 ka BP. Although asynchronous and triggered by independent
mechanisms, these basin-scale oceanographic changes had a profound impact on the water exchange
between both basins and the Mediterranean thermohaline circulation, and consequently, in the amount
and properties of Mediterranean waters exported to the north Atlantic region.
Our grain-size and geochemical records show coetaneous decrease/increase from cores at deep/
intermediate levels of the west-Med confirming a major reduction of deep water currents in the deepest
part of the basin related to the post glacial sea level rise, while increased intensity of currents at
intermediate levels. These results likely suggest a significant change in the water masses properties
during the deglaciation that would favored formation of intermediate water. On the other hand, the
sedimentological records from an Ionian Sea sediment core show enhanced deep water currents during
the first phase of the deglaciation, and a very marked reduction in the 10.8-7.5 ka time-interval, coinciding
with the Sapropel 1 formation.
Our results show that intermediate levels circulation was reinforced in both eastern and western
Mediterranean basins during the first phase of the deglaciation likely suggesting a major export of
intermediate water masses from the eastern to the western basin. Finally, the strong stratification leading
formation of the Sapropel 1 produced a major reduction of deep water ventilation in the eastern basin that
could also affect westward export of intermediate waters.

# metadata.dc.relation.ispartof[].value
Resum del pòster presentat a: 14th International Conference on Paleoceanography (ICP14). 29 August-2 September 2022. Bergen. (Poster Abstracts Topic 2: Ocean Circulation and its Variability - P2-027)

# metadata.dc.rights[].value
cc by-nc-nd (c) Frigola Ferrer, Jaime I. et al., 2023

# metadata.dc.source[].value
Comunicacions a congressos (Dinàmica de la Terra i de l'Oceà)

# metadata.dc.title[].value
A sedimentological insight into the deglacial reorganization of the Mediterranean thermohaline circulation