Dryopithecus fontani

Abstract: A well-preserved 11.8-million-years-old lower face attributed to the seminal taxon Dryopithecus fontani (Primates, Hominidae) from the Catalan site ACM/C3-Ae of the Hostalets de Pierola area (Valles-Penedes Basin, Catalonia, NE Spain) is described. The new data indicate that D. fontani is distinct at the genus level from Late Miocene European taxa previously attributed to Dryopithecus, which are here reassigned to Hispanopithecus. The new facial specimen also suggests that D. fontani and the Middle Miocene Pierolapithecus catalaunicus are not synonymous. Anatomical and morphometric analyses further indicate that the new specimen shows a combination of lower facial features-hitherto unknown in Miocene hominoids-that resembles the facial pattern of Gorilla, thus providing the first nondental evidence of gorilla-like lower facial morphology in the fossil record. Considering the current evidence, the gorilla-like facial pattern of D. fontani is inferred to be derived relative to previously known stem hominids, and might indicate that this taxon is either an early member of the Homininae or, alternatively, a stem hominid convergent with the lower facial pattern of Gorilla. The biogeographic implications of both alternatives are discussed. This new finding in the Hostalets de Pierola section reinforces the importance of this area for understanding the elusive question of the Middle Miocene origin and early radiation of great apes.

Abstract: On the basis of industrial computed tomography, relative enamel thickness (RET) is computed in three Middle Miocene (ca 11.9–11.8 Ma) hominoids from Abocador de Can Mata (Valles-Penedes Basin, Catalonia, Spain): Pierolapithecus catalaunicus from BCV1 and Anoiapithecus brevirostris from C3-Aj, interpreted as stem hominids; and Dryopithecus fontani from C3-Ae of uncertain phylogenetic affinities. Pierolapithecus displays an average RET value of 19.5, Anoiapithecus of 18.6 and Dryopithecus of 10.6. The thick-enamelled condition of Pierolapithecus and Anoiapithecus is also characteristic of afropithecids, including the more derived kenyapithecins from the early Middle Miocene of Eurasia (Griphopithecus and Kenyapithecus). Given the presence of other dentognathic and craniofacial similarities, thick enamel may be interpreted as a symplesiomorphy of the Hominidae (the great ape and human clade), which would have been later independently modified along several lineages. Given the correlation between thick enamel and hard-object feeding, our results suggest that thick enamel might have been the fundamental adaptation that enabled the out-of-Africa dispersal of great-ape ancestors and their subsequent initial radiation throughout Eurasia. The much thinner enamel of Dryopithecus is difficult to interpret given phylogenetic uncertainties, being either a hominine synapomorphy or a convergently developed feature.

Abstract: The hominoid right partial humerus IPS4334, from the middle Miocene (MN 8) of Castell de Barbera (Valles-Penedes Basin, Catalonia, Spain), is described. It preserves the mid-distal portion of the shaft until the proximal margins of the radial and coronoid fossae, as well as the proximal portion of the olecranon fossa; the capitulum, the trochlea and the two epicondyles are missing. Although morphological comparisons are restricted, available evidence indicates that IPS4334 is more derived towards the modern hominoid condition than the Klein Hadersdorf specimen attributed to Griphopithecus (ca. 13–14 Ma), thus being most similar (except for its larger size and greater robusticity) to the presumably juvenile specimen of Dryopithecus fontani from Saint Gaudens in France (ca. 11–12 Ma). On the basis of shaft measurements and allometric regressions derived for extant hominoids, a body mass estimate around 50 kg is derived for IPS4334. Morphological similarities with the Saint Gaudens specimen, together with the large body mass estimate, suggest a tentative attribution of IPS4334 to cf. D. fontani, which is the largest hominoid taxon so far recorded from the Valles-Penedes Basin. The larger size and higher robusticity of IPS4334 as compared to the Saint Gaudens specimen might be explained by the juvenile status of the latter and/or sexual dimorphism. When both specimens are considered together with a partial femur from Abocador de Can Mata, D. fontani emerges as a less suspensory ape than the late Miocene Hispanopithecus, the locomotor repertoire of the former emphasizing climbing, but still displaying a significant quadrupedal component. Am J Phys Anthropol, 2011. © 2010 Wiley-Liss, Inc.