Stable isotope ecology of Miocene bovids from northern Greece and the ape/monkey turnover in the Balkans

作者：Merceron Gildas^*; Kostopoulos Dimitris S; de Bonis Louis; Fourel Francois; Koufos George D; Lecuyer Christophe; Martineau Francois

来源：Journal of Human Evolution, 2013, 65(2): 185-198.

DOI：10.1016/j.jhevol.2013.05.003

• Primates
• Europe
• Oxygen isotopes
• Carbon isotopes
• Ruminants
• Neogene

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 C-3 environments. However, the large range of delta C-13 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 degrees C and warmest monthly temperatures rose close to or above 20 degrees 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 delta O-18(p) 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.

• 出版日期2013-8