“…This crinoid fauna has no similarity with the fauna of South Africa (except by Ophiocrinus stangeri ), but has taxa associated with the eastern United States of America, and mainly Europe and northern Gondwana (Scheffler et al, 2013; Scheffler, 2015). Although elements that have similarity to Europe and northern Gondwana Old World Realm have long been known in other Devonian invertebrate groups of South America (e.g., Katzer, 1897, 1903, 1933; Clarke, 1913; Isaacson and Perry, 1977; Melo, 1985, 1988; Fonseca and Melo, 1987; Isaacson and Sablock, 1990; Fonseca, 2004; Carvalho and Ponciano, 2015; Távora et al, 2017), the Malvinokaffric fauna has always been considered to have great similarity throughout its distribution area, including southern Brazil, Bolivia, and South Africa (Boucot, 1971, 1988; Boucot and Racheboeuf, 1993). Therefore, these data suggest that: (1) the known crinoids are still a very small part of the actual class diversity in this period for South America; and/or (2) this class, unlike almost all other faunal groups of the Malvinokaffric Realm (e.g., trilobites, brachiopods, conulariids, bivalves, gastropods), has a high degree of endemism within each sedimentary basin, even among the typically Malvinokaffric basins.…”