The attribution of osteological remains of a bird discovered in Preceramic deposits at Nemocón IV rockshelter (Sabana de Bogotá, Colombia) to Ara sp. (macaws) is confirmed through osteological and morphometrical analyses. Thirteen bones were recovered from two adjacent, arbitrary excavation levels; and are considered the remains of a single individual because of the rarity of the taxon, their similar size and taphonomic alteration, and the presence of paired elements. Radiocarbon dating of the macaw reveals it comes from the ninth millennium cal BP, the oldest date recorded from Nemocón IV. Paleoenvironmental data suggest that, during the deposition of the Preceramic levels at Nemocón IV, climatic conditions were close to those of today. The modern range of the macaws is outside these climatic parameters, and all modern Ara species are allochthonous to the Sabana de Bogotá, indicating the archaeological macaw was also allochthonous in Preceramic times. Analysis of the remains shows the macaw was not dismembered, so it is unlikely that it was used as food. Early conquest records indicate macaws were traded and maintained outside their natural ranges as pets, as a source of feathers, for use in rituals, or for a combination of uses.

Six vertebrae (one cervical, three articulated thoracic, and two lumbar) and an incomplete thoracic neural spine from a new late Pleistocene site at Anolaima, Cundinamarca, Colombia, are attributed to the extinct gomphothere (Elephantoidea, Proboscidea) Notiomastodon platensis. The preserved bones exhibit a range of alterations, including porosities, piercings, hollows, and deep bone lesions on the spinous process and the neural arch; asymmetrical zygapophyseal articulations; and osteoarthritic lesions. Diet, behaviour, ecological aspects, selective pressures, and disease have the potential to affect the bones, so the study of individual variations and palaeopathology provides important information for understanding aspects of the life of extinct organisms. Osteological anomalies in the Anolaima gomphothere are interpreted as the result of nutritional deficiencies in essential minerals caused by environmental stresses, possibly related to the palaeoenvironmental instability that characterized the late Pleistocene and that coincides with the age of the fossils. Excessive biomechanical loading on already weakened bones from locomotion through the uneven, upland terrain of the Anolaima region may have contributed to the pathologies. This palaeopathological analysis is the first for Colombian megafauna, and thereby broadens our knowledge of the health conditions of South American gomphotheres.