IPEPH UMR 7262 CNRS, Université de Poitiers, France.
J Hum Evol. 2013 Aug;65(2):185-98. doi: 10.1016/j.jhevol.2013.05.003. Epub 2013 Jul 16.
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.
欧亚大陆在中新世时期是灵长类动物的辐射中心。所有的灵长类动物在中新世末期都在西欧亚大陆灭绝了。在这里,我们研究了在希腊 Axios 河沿岸,狨猴 Mesopithecus 取代人猿 Ouranopithecus 时,当地规模的气候和植被变化的假说。因为它们是食草动物,而且比灵长类动物多得多,所以在研究巴尔干半岛的气候变化导致人猿灭绝时,牛科动物比灵长类动物更受欢迎。通过测量牛科动物牙釉质的碳稳定同位素比值,我们得出结论,Ouranopithecus 和 Mesopithecus 都是在纯 C3 环境中进化而来的。然而,牛科动物的磷灰石碳酸盐的 δ(13)C 值范围很大,再加上它们的臼齿微磨损和中磨损模式,排除了希腊北部存在茂密森林景观的可能性。相反,这些牛科动物在草本层中草类丰富的开阔景观中进化而来。两个时间段估计的最冷月份温度都低于 10°C,最热月份温度接近或高于 20°C。来自大块样品的磷酸盐的氧同位素组成在不同地点之间没有显著差异,但在每个地点内都显示出种间变异。在这种情况下,不同的因素影响氧同位素组成,包括水的来源、食性、体重和牙釉质形成的速度。我们讨论了后一个因素,因为牙齿内部 δ(18)Op 的变化很大,反映了温度季节性变化的重要幅度。这些估计与古植物学数据相符,与基于气候模型的估计略有不同。本研究在 Axios 河沿岸的 Ouranopithecus 灭绝前后都没有发现气候有显著变化。然而,研究结果表明,冬季相对寒冷的季节变化较大,这对于现存的猴子来说是很常见的条件,但对于今天分布在热带地区的大型猿类来说却很不寻常。