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Predictive habitat modeling of Cold Water Coral Distribution in the Bari Canyon (Adriatic Sea) with Hydrodynamic variables. Federica Foglini1 Annaëlle BARGAIN2, Lorenzo Angeletti, Davide Bonaldo, Marie-Claire FABRI2, , Marco Taviani 2 1 LER PAC, IFREMER, La Seyne Sur Mer, France. ISMAR–CNR, Bologna, Italy. Madrepora oculata and Lophelia pertusa are the two main species of cold-water coral (CWC) found in the Mediterranean Canyons. These Hexacoralia (Scleractinia) are important biodiversity hotspots, providing habitat and resources for many species, including commercial fishes. However, CWC ecosystems are especially vulnerable (Freiwald, 2004) and suffer from many physical damages, particularly anthropogenic impacts from fishery activities (Fabri et al. 2014). Therefore, they have been identified as sensitive habitat, being priority species for management and protection measures by The General Fisheries Commission foe the Mediterranean (GFCM, 200a). However, the Mediterranean CWC distribution is still unknown compared to the one in the Atlantic Ocean (Freiwald et al. 2009) and factors controlling their repartition are still not entirely understood. The Bari Canyon is located along the South Western Adriatic Margin and represents the main sediment conduit active since the last glacial interval (Trincardi et al., 2007). It is the main path for the North Adriatic dense Water cascading and represents the main biodiversity hotspot for CWC habitats in the Adriatic Sea. The objective of this study is to combine several parameters to describe the environmental conditions in favor of CWC settlement: (1) CWC observations, extracted from georeferenced underwater video films, (2) eco-geographic variables (EGVs) derived from high resolution bathymetry (collected by an autonomous underwater vehicle), (3) reflectivity from the multibeam (4) hydrodynamic data (based on ROMS for ocean currents, coupled with SWAN within the COAWST modelling system). Habitat suitability models have been used to identify the main eco-geographical variables explaining CWC distribution. Presence-only models (MaxEnt and ENFA) but also presence-absence model (GLMs) have been used and compared. The models pointed out slope, rugosity, water density (salinity and temperature) and maximum current to be the main explaining factors for CWC distribution. These results have been used to produce habitat suitability maps useful for the assessment of potential habitat extent for deep sea environment also in the framework of the Marine Strategy framework directive (MSFD).