Project description:Pleistocene Pongo teeth show substantial variation in size and morphology, fueling taxonomic debates about the paleodiversity of the genus. We investigated prominent features of the enamel-dentine-junction junction (EDJ) – phylogenetically informative internal structures – of 71 fossil Pongo lower molars from various sites by applying geometric morphometrics and conducted paleoproteomic analyses from enamel proteins to attempt to identify extinct orangutan species. Forty-three orangutan lower molars representing Pongo pygmaeus and Pongo abelii were included for comparison. The shape of the EDJ was analyzed by placing five landmarks on the tip of the main dentine horns, and 142 semilandmarks along the marginal ridges connecting the dentine horns. Paleoproteomic analyses were conducted on 15 teeth of Late Pleistocene Pongo using high-resolution tandem mass spectrometry. The geometric morphometric results show variations in EDJ shape regarding aspects of the height and position of the dentine horns and connecting ridges. Despite the issue of molar position and sample size, modern molars are distinguished from fossil counterparts by their elongated tooth outline and narrowly positioned dentine horns. Proteomic results show that neither a distinction of P. pygmaeus and P. abelii, nor a consistent allocation of fossil specimens to extant species is feasible. Based on the EDJ shape, the (late) Middle to Late Pleistocene Pongo samples from Vietnam share the same morphospace, supporting the previous allocation to P. devosi, although substantial overlap with Chinese fossils could also indicate close affinities with P. weidenreichi. The hypothesis that both species represent one chronospecies cannot be ruled out. Two fossil specimens, one from Tam Hay Marklot (Laos, Late Pleistocene), and another from Sangiran (Java, Early to Middle Pleistocene), along with some specimens within the Punung sample (Java), exhibit affinities with Pongo abelii. The Punung fossils might represent a mix of early Late Pleistocene and later specimens (terminal Pleistocene to Holocene) related to modern Pongo. The taxonomy and phylogeny of the complete Punung sample needs to be further investigated.
Project description:These are the additional files that were not already in public repositories for this manuscript. These samples are negative ionization mode, organic matter metabolomics datasets from many distinct environments, including global cropland; dryland; late Pleistocene-aged permafrost; temperate and tropical forest soils; rivers and lakes; and ocean DOM.
Project description:Hominin relationships and their dispersal throughout Eurasia during the Early and Middle Pleistocene are highly debated. The relationships between Early and Middle Pleistocene hominins, like Homo antecessor and Homo erectus, and hominin species that dominate the Late Pleistocene fossil record, like Homo sapiens, Neanderthals and Denisovans, are unclear. Here, we obtain enamel proteomes from Homo antecessor (Atapuerca, Spain) and Homo erectus (Dmanisi, Georgia), two key fossil assemblages that have a central role in models of Pleistocene hominin morphology, dispersal, and divergence. We recover endogenous ancient proteomes from the Atapuerca and Dmanisi hominins. In addition, our proteomic data indicates that the sampled Homo antecessor molar derives from a male hominin through amelogenin protein sexing. Our data includes preserved in vivo phosphorylation and enamel proteome proteolytic digestion.