“…The present results update and refine, adding a third assemblage, the results previously described by Quiroz-Martínez et al [ 12 ]. Furthermore, polychaete assemblages distributed in the transitional region were different from the other sedimentary environments; this could be related to the high environmental variability of the transitional area, characterized by the transition from terrigenous to carbonated sediments, modulated by the Grijalva-Usumacinta plume and the oil extraction activities that affect the benthic fauna by reducing species diversity and richness [ 79 , 95 , 96 ]. Ecological research in the Southern Gulf of Mexico shows that “Nortes” and summer rains provoking high river run-off are the most important physical processes influencing large-scale benthic community structure across the carbonate and terrigenous shelves [ 45 , 47 , 90 , 97 – 99 ].…”