“…There were nevertheless large amounts of degraded p~gments which probably derived from the breakdown of autochthonous material. We have indeed detected many forms of phaeopigment a, which is consistent with findings of other studies concerning sediment (Brown et al 1981, Riaux-Gobin et al 1987, Klein et Riaux-Gobin 1991, Yacobi et al 1991. The 4 phaeophorbides, which represented about 7 5 % of total phaeopigments, are markers for macrobenthic deposit-feeding processes (Bianchi et al 1988(Bianchi et al , 1993 and more generally for metazoan grazing activity (Brown et al 1981, Welschmeyer & Lorenzen 1985, Abele-Oeschger et al 1992 Based on their order of elution and retention times, the 2 major phaeophorbides a-like:, and a-like, (accounting for about 50 % of total phaeophorbides) correspond very likely to the phaeophorbides a-like in Hawkins et al (1986) study and to phaeophorbides a, and a3 reported by Plante-Cuny et al (1993).…”