Comparison of estimates of pelagic biomass. G. PriedeImants Aksel BergstadOdd I. MillerPeter VecchioneMichael GebrukAndrey FalkenhaugTone S. M. BillettDavid CraigJessica C. DaleAndrew A. ShieldsMark H. TilstoneGavin T. SuttonTracey J. GoodayAndrew E. InallMark O. B. JonesDaniel Martinez-VicenteVictor M. MenezesGui NiedzielskiTomasz SigurðssonÞorsteinn RotheNina RogachevaAntonina H. S. AltClaudia BrandTimothy AbellRichard S. BrierleyAndrew J. CousinsNicola CrockardDeborah Rus HoelzelA. HøinesÅge B. LetessierTom F. ReadJane ShimmieldTracy J. CoxMartin K. GalbraithJohn D. M. GordonJohn HortonTammy NeatFrancis LorancePascal 2013 <p>Open circles are data from the BIOTRANS station at 47°N, 20°W east of the MAR <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0061550#pone.0061550-Roe1" target="_blank">[42]</a>. The grey line is based on data from 31°17′N 25°24′ W over the Madeira Plain <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0061550#pone.0061550-Webb1" target="_blank">[43]</a>. The solid black line is the theoretical relationship derived from integrating the CoML global trend for benthic biomass as shown in <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0061550#pone-0061550-g012" target="_blank">Figure 12</a>.</p>