Diversity dynamics of echinoderms and evolution of marine communities

A compound analysis of two global paleontological databases (Sepkoski??s database (SDB) and The Paleobiology Database) allowed the recognition of a number of previously undescribed trends in the evolution of the phylum Echinodermata. Paleozoic echinoderms, dominated by sessile epibenthic filter feeders, played an important role in benthic communities, especially in the Ordovician and Carboniferous. Paleozoic echinoderms typically showed an increased rate of genus renewal, which significantly decreases in the Meso-Cenozoic. After the P-T crisis the echinoderms became dominated by motile taxa, while the role of infaunal forms increased. During the global turnover in the benthic communities at the K-T boundary, which was accompanied by a sharp increase in the mean alpha-diversity, many marine organisms became inhabitants of much richer (compared to the Mesozoic) communities. However, of all echinoderms, this trend is observed only in crinoids. In contrast to most large taxa, echinoderms do not show positive correlation between the duration of genera and alpha-diversity of communities, which included these genera. During the Phanerozoic the geographical distribution of echinoderms showed a sharp paleolatitudinal gradient, i.e., each period was characterized by one paleolatitudinal zone with the maximum diversity of echinoderms, and the diversity rapidly decreasing to the north and to the south of this zone. The zone of the maximum diversity of echinoderms, like of entire marine biota, during the Phanerozoic gradually moved from the tropics of the southern hemisphere to the middle latitudes of the northern hemisphere.