A high resolution and quasi-zonal transect of dissolved Ba in the Mediterranean Sea

• D_Ba is investigated along a high resolution and quasi-zonal transect in the MedSea.
• The D_Ba content ranges from 38 to 85 nmol kg− 1 with local deep D_Ba maxima reaching up to 172 nmol kg− 1.
• The water column is largely undersaturated with respect to barite (0.2 < SI < 0.6).
• The D_Ba distribution is impacted by the large-scale Mediterranean circulation and biogeochemical processes.
• Local changes in the D_Ba patterns may be the key to better constrain the C dynamics in the MedSea.

The dissolved barium (D_Ba) data set for the Mediterranean Sea is here expanded with data from a large-scale transect sampled in April 2011 (M84/3 cruise) at high resolution. A total of 833 seawater samples have been analyzed for D_Ba. Over the basin the D_Ba content ranges from 38 to 85 nmol kg− 1 with local deep D_Ba maxima reaching up to 172 nmol kg− 1. Deep D_Ba maxima are associated with near bottom waters influenced by benthic processes and brine waters. The water column is largely undersaturated with respect to barite (BaSO4, the main phase of particulate biogenic barium P_Ba), with water column barite saturation state ranging between 0.2 and 0.6 over the basin. This new D_Ba dataset shows that the general zonal distribution of D_Ba is impacted by the large-scale Mediterranean circulation, as evidenced by the Levantine Intermediate Water zonal and meridional progression as well as by the eastward flow of surface Atlantic Water. However biogeochemical processes are also at play, as suggested by an elevated D_Ba content of deep waters and by local lower D_Ba contents in intermediate waters. These features could be attributed to active cycling between the particulate and dissolved Ba phases. Since P_Ba barite has been recognized in previous studies as a proxy for particulate organic carbon remineralization at intermediate depths, the significance of local changes in the water column D_Ba patterns may be the key to better constrain the Ba and carbon dynamics in the Mediterranean Sea.