“…The specimens described here were sampled from two horizons within the La Luna Formation: one from the Aguada Member (Cementos Andinos Quarry, Trujillo state) and the other from just above the contact between the Maraca Formation (Cogollo Group) and the La Luna Formation (La Luna Quarry, Zulia state). While a Cenomanian age was proposed for the Aguada Member based on foraminifera and ammonites (Renz, 1959), the presence of horizons of Cenomanian age in the Maracaibo Basin, from which the La Luna Quarry samples originate, has been controversial (Dot et al, 2015;Erlich et al, 1999;Renz, 1982). The two sampled localities have distinct (and rich) anacoracid composition but they share two taxa: M. saskatchewanensis and A. karsteni.…”