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. 2014 Apr 30;9(4):e95839. doi: 10.1371/journal.pone.0095839

Figure 1. Locations of the study sites sampled with imaging technology (ROVs, manned submersible, towed camera systems) and trawling.

Figure 1

A-B.B  =  Algero-Balearic Basin (W. Med.), A.S  =  Anton Dohrn Seamount, B.C  =  Blanes Canyon (NW Med.), C.C  =  Cascais Canyon, C.S  =  Condor Seamount, Calabrian Slope & Basin  =  C.S&B, Crete-Rhodes Ridge  =  C.R.R, D&E.C  =  Dangeard & Explorer Canyons, D.M  =  Darwin Mounds, G.L.C  =  Gulf of Lion canyons (NW Med.), G.L  =  Gulf of Lion, G.C  =  Guilvinec Canyon, H.B  =  Hatton Bank, H.IV  =  HAUSGARTEN, station IV, J.S =  Josephine Seamount, L.C =  Lisbon Canyon, N.C  =  Nazaré Canyon, N.C-G  =  North Charlie Gibbs Fracture Zone, N-E.F.C  =  North-East Faroe-Shetland Channel, N.F.C  =  North Faroe-Shetland Channel, N.W =  Norwegian margin, P.D.M  =  Pen Duick Alpha/Beta Mound, R.B  =  Rockall Bank, Ros.B  =  Rosemary Bank, S.C  =  Setúbal Canyon, S.C-G  =  South Charlie Gibbs Fracture Zone, W.C  =  Whittard Canyon, W.M.S  =  Western Mediterranean slope, W-T.R  =  Wyville-Thomson Ridge.