2010
DOI: 10.1016/j.dsr2.2009.08.018
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Introduction: Cold-Water Coral communities in the Mediterranean Sea

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Cited by 16 publications
(7 citation statements)
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“…Only recently have focused research programs (e.g. APLABES, [28] , EU-FP6 HERMES, EU-FP7 HERMIONE, and EU-FP7 CoralFISH) promoted international oceanographic expeditions using the latest generation of acoustic devices, Remotely Operated Vehicles (ROVs), and manned submersibles in order to systematically explore the Mediterranean Sea’s deep seabed. As a result of such programs, the occurrence of VMEs has been revealed (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Only recently have focused research programs (e.g. APLABES, [28] , EU-FP6 HERMES, EU-FP7 HERMIONE, and EU-FP7 CoralFISH) promoted international oceanographic expeditions using the latest generation of acoustic devices, Remotely Operated Vehicles (ROVs), and manned submersibles in order to systematically explore the Mediterranean Sea’s deep seabed. As a result of such programs, the occurrence of VMEs has been revealed (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Sampling was carried out in April 2010, in the Santa Maria di Leuca (SML) coral province (Ionian Sea; Central Mediterranean) (Figure 1) Taviani et al 2005;Corselli 2010), during a research cruise on board the R/V (Research Vessel) Minerva I, within the EU 7FP CoralFISH project. The first findings (Stations BT47 and BT64; Table I) were carried out by means of an epibenthic sledge with a fixed iron opening of 3.8 m by 0.46 m and a mesh size of 0.5 cm.…”
Section: Methodsmentioning
confidence: 99%
“…). During the APLABES project, (Corselli ) an area of 800 km 2 was mapped by means of multibeam sonar, between 200 and 1300 m in depth. This area includes (i) a broad eastern sector, influenced by mass‐transport deposition, with a very complex hummocky sea floor consisting of widespread mound‐like reliefs, (ii) a central ridge where drift sedimentation has been recognised by documenting the action of contour currents from the northeast and (iii) prominent fault‐scarps to the west, where widespread erosion processes are evident from the emergence of stiff and/or hardened older sediments (Savini & Corselli ; Fig.…”
Section: Introductionmentioning
confidence: 99%