This study analyzed conodont elements retrieved from Mocambo Carbonates, marine portion of the Piauí Formation, Parnaíba Basin, Northeast Brazil, West Gondwana. This manuscript aims i) to update the conodont fauna and, ii) to refine the biostratigraphic and paleoecological data of the marine portion, according to new conodont occurrences. The description of the conodont species Diplognathodus orphanus, Idiognathodus incurvus and Adetognathus lautus, suggests a late Bashkirian age. In addition, the presence of adults and juvenile Diplognathodus orphanus and Idiognathodus incurvus, as well as fern sporangia, ostracods, benthic foraminifers, and fish teeth, indicate a very shallow marine platform, of neritic tidal facies. The Mocambo Carbonates are traditionally recognized as Pennsylvanian in age, and thus, with our conodont contribution is refined to late Bashkirian. Paleoecologically, this sequence is interpreted as very shallow marine facies. We also correlate the marine carbonate sequence of the Piauí Formation, Parnaíba Basin, with the marine shallow waters from the Itaituba Formation, Amazonas Basin. This is well-positioned with international biozones from North America, China and Europe, allowing the correlation of the Piauí marine portion with the transgressive-regressive epicontinental Itaituba-Piauí Sea in Northwest South America, Western Gondwana, during the Late Paleozoic.