Here, wedescribe newtheropod materials (several isolated teeth, an axis, two caudal centra anda proximal left tibia) fromthe type locality of theBajada Colorada Formation (Lower Cretaceous, Berriasian-Valanginian).Although fragmentary, the recovered material shows a diverse association of meat-eating dinosaurs for this poorly undestood period of time. Three techniques were used to assess the phylogenetic position of the isolated teeth: multivariate (PCA), discriminant and phylogenetic analyses. The morphotypes 1, 2 and 3 (small non-recurved isolated crowns) were regarded as Theropoda indet.,as our analyses failed to supporta more precise classification. Two large almost complete ziphodont crowns, considered morphotype 4, were identified as belonging to megalosaurid tetanurans by phylogenetic, discriminantand multivariate analyses, thus likely representing the first record of this ancient family in South America, and the youngest worldwide. We refer the axis to a small abelisauroid ceratosaurian based on the following suite ofcharacters; long and pointed epipophyses,a pneumatic foramen in the centrum,the invaginated spinopostzygapophyseal lamina, and the anteroposteriorly long, dorsally convex, anddorsally/posteriorly unexpanded neural spine. The caudal centra can be referred to a theropod, and tentatively to Abelisauroidea, suggesting that theymay belong to the same taxon than that represented by the axis.The tibia lacks the incisura tibialis, presents a low, sharp and proximally positioned fibular crest,and has a deep lateral fossa, which islimited dorsally by a coarse, rounded in section and anteriorly directed crest.This combination of features allowsto refer it to a large abelisaurid. The Bajada Colorada dinosaur recordincludes so fara small abelisauroid, a large abelisaurid,aprobably medium to large megalosaurid tetanuran,diplodocid and dicraeosaurid sauropods. It shows some similarities with Middle and Upper Jurassic units in centralPatagonia, Africa and Portugal,suggesting that no significant dinosaur faunal turnover took place through the Jurassic-Cretaceous event inthe southern part of South America.