-PALEOICHTHYOFAUNA OF THE PIMENTEIRA FORMATION (DEVONIAN), PARNAÍBA BASIN, PI, BRAZIL. The Pimenteira Formation extends through the east border of the Parnaíba Basin and corresponds to the Middle and Upper Devonian (Eifelian-Frasnian). This formation possesses as characteristic fauna an invertebrate association composed mostly of gastropods, brachiopods and trilobites. However, there are also rare vertebrate remains, normally isolated and poorly preserved. The vertebrate fauna have been studied since the middle of the twentieth century and until then, had not shown a considerable taxonomic variety, only comprising Ctenacanthus and Machaeracanthus spines. In this study, besides discussing the fossil fish material already known for this formation, we describe new fossil remains, including the description of: a new Machaeracanthus spine; the first spines of climatiiform acanthodians, one related to Ptomacanthus and the other to Climatius enodicosta; an Antarctilamna-like spine; and fragments of Ctenacanthus kegeli. Lastly, we present the possible first record of Placodermi for the Pimenteira Formation and the Parnaíba Basin. These occurrences expand considerably the vertebrate faunal composition of the Pimenteira Formation and helps to understand the connections among South American basins during the Devonian, due to the similarity between the Pimenteira Formation and other South American fossiliferous formations, especially those of Bolivia.