Evolutionary paleoecology of European rhinocerotids across the Oligocene-Miocene transition

Manon Hullot, Celine Martin, Cecile Blondel, Damien Becker, Gertrud E Roessner
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Abstract

The Oligocene-Miocene transition witnessed great environmental and faunal changes, but its drivers and consequences on mammals remain poorly understood. Rhinocerotoids are among the most affected taxa, reflected by great taxonomical (extinction of all non-rhinocerotids) and morphological (e.g., more mediportal forms) changes observed during this interval. However, potential associated changes in ecology have not been explored. Here, we investigated the paleoecology of 10 rhinocerotid species coming from 15 localities across Western and Central Europe and ranging from Mammal Paleogene reference level 28 to Mammal Neogene zone 3. We explored evolutionary trends for their diet, physiology, and habitat via dental wear, hypoplasia, body mass estimates, and stable isotopy. Our results (isotopy, dental wear) suggest that all rhinocerotids studied were C3 feeders, whether browsing or mixed-feeding, but niche partitioning was assumed at some localities: distinct dietary preferences and/or habitats were highlighted at Gaimersheim, Ulm-Westtangente, and Rickenbach, whereas a potential competition for the resources or different niche partitioning strategies (body mass, feeding height) are hypothesized at others localities (La Milloque, Thezels, Paulhiac). We reconstructed similar warm conditions at all localities except Gaimersheim, but found greater variations in precipitation. Indeed, a clear shift in delta13CCO3, enamel values was noticed at the end of the Oligocene, consistent with climatic changes (Mi-1) and vegetation modifications reported at that time. Despite these great changes, the prevalence of hypoplasia was low (< 10 %) to moderate (< 20 %) except at some localities (Pappenheim, Rickenbach, Engehalde) and for some species (Brachydiceratherium aurelianense and B. lamilloquense). Teleoceratines were particularly affected, suggesting a potential phylogenetic effect. Fourth milk molars and third molars were the most affected loci, indicating stresses around birth and environmental stresses respectively. Body mass co-variated with hypoplasia prevalence, indicating that larger species might be more susceptible to stresses and environmental changes. The tracking of rhinocerotids paleoecological preferences during the Oligocene-Miocene revealed several changes in diet and habitat (temperature, precipitation, vegetation) consistent with global changes during this period.
跨越渐新世-中新世过渡时期的欧洲犀牛古生态进化论
渐新世-中新世过渡见证了环境和动物群的巨大变化,但人们对其驱动因素和对哺乳动物的影响仍然知之甚少。犀牛类是受影响最大的类群之一,在这一时期观察到的分类学(所有非犀牛类灭绝)和形态学(如更多的中腹部形态)的巨大变化反映了这一点。然而,与之相关的潜在生态学变化尚未得到探讨。在这里,我们研究了来自西欧和中欧 15 个地点的 10 个犀牛类物种的古生态学,其范围从哺乳动物古近纪参考水平 28 到哺乳动物新近纪 3 区不等。我们通过牙齿磨损、牙齿缺损、体重估算和稳定同位素研究,探索了它们的饮食、生理和栖息地的进化趋势。我们的研究结果(同位素、牙齿磨损)表明,所研究的所有犀牛类都是C3食性动物,不论是食草还是混合食草,但在某些地方,我们假定了生态位的划分:在盖默斯海姆、乌尔姆-韦斯特唐根特和里肯巴赫,我们发现了不同的食性偏好和/或栖息地,而在其他地方(拉米洛克、泰泽尔斯、保尔希亚克),我们假定了潜在的资源竞争或不同的生态位划分策略(体重、食草高度)。除盖默斯海姆外,我们在所有地点重建了类似的温暖条件,但发现降水量的变化更大。事实上,在渐新世末期,delta13CCO3、珐琅值发生了明显变化,这与当时报道的气候变化(Mi-1)和植被变化相一致。尽管发生了这些巨大的变化,但除一些地方(帕彭海姆、里肯巴赫、恩格哈尔德)和一些物种(Brachydiceratherium aurelianense 和 B. lamilloquense)外,牙釉质发育不全的发生率很低(10%)到中等(20%)。Teleoceratines 尤其受到影响,这表明可能存在系统发育的影响。第四乳臼齿和第三臼齿是受影响最大的位点,这分别表明了出生时的压力和环境压力。体重与臼齿发育不全的发生率存在共变关系,表明体型较大的物种可能更容易受到压力和环境变化的影响。在渐新世-中新世期间对犀牛古生态偏好的追踪显示了饮食和栖息地(温度、降水、植被)的一些变化,这些变化与这一时期的全球变化一致。
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