title: Stable isotope ecology of Miocene bovids from Northern Greece and the ape/monkey turnover in the Balkans.
abstract: Eurasia was home to a great radiation of hominoid primates during the Miocene. All were extinct by the end of the Miocene in Western Eurasia. Here, we investigate the hypothesis of climate and vegetation changes at a local scale when the cercopithecoid Mesopithecus replaced the hominoid Ouranopithecus along the Axios River, Greece. Because they are herbivorous and were much more abundant than primates, bovids are preferred to primates to study climate change in the Balkans as a cause of hominoid extinction. By measuring carbon stable isotope ratios of bovid enamel, we conclude that Ouranopithecus and Mesopithecus both evolved in pure C3 environments. However, the large range of δ(13)C values of apatite carbonate from bovids combined with their molar microwear and mesowear patterns preclude the presence of dense forested landscapes in northern Greece. Instead, these bovids evolved in rather open landscapes with abundant grasses in the herbaceous layer. Coldest monthly estimated temperatures were below 10°C and warmest monthly temperatures rose close to or above 20°C for the two time intervals. Oxygen isotope compositions of phosphate from bulk samples did not show significant differences between sites but did show between-species variation within each site. Different factors influence oxygen isotope composition in this context, including water provenience, feeding ecology, body mass, and rate of amelogenesis. We discuss this latter factor in regard to the high intra-tooth variations in δ(18)Op reflecting important amplitudes of seasonal variations in temperature. These estimations fit with paleobotanical data and differ slightly from estimations based on climate models. This study found no significant change in climate before and after the extinction of Ouranopithecus along the Axios River. However, strong seasonal variations with relatively cold winters were indicated, conditions quite usual for extant monkeys but unusual for great apes distributed today in inter-tropical regions.
authors.affiliation: IPEPH UMR 7262 CNRS, Université de Poitiers, France. gildas.merceron@univ-poitiers.fr
authors.forename: Gildas
authors.initials: G
authors.lastname: Merceron
authors.forename: Dimitris S
authors.initials: DS
authors.lastname: Kostopoulos
authors.forename: Louis de
authors.initials: Ld
authors.lastname: Bonis
authors.forename: François
authors.initials: F
authors.lastname: Fourel
authors.forename: George D
authors.initials: GD
authors.lastname: Koufos
authors.forename: Christophe
authors.initials: C
authors.lastname: Lécuyer
authors.forename: François
authors.initials: F
authors.lastname: Martineau
mesh_terms: D000818:Animals; D063368:Balkan Peninsula; D044822:Biodiversity; D005075:Biological Evolution; D002247:Carbon Isotopes / Q000032:analysis; D051079:Catarrhini / Q000502:physiology*; D057231:Climate Change; D004032:Diet; D017753:Ecosystem; D005580:Fossils; D006115:Greece; D010103:Oxygen Isotopes / Q000032:analysis; D010163:Paleontology; D012418:Ruminants / Q000502:physiology*; D014070:Tooth / Q000737:chemistry
chemical_list: D002247:Carbon Isotopes; D010103:Oxygen Isotopes
keywords: Carbon isotopes; Europe; Neogene; Oxygen isotopes; Primates; Ruminants