Dental microwear of bovids from the Pliocene-Pleistocene transition in the lower Awash Valley, Ethiopia

IF 2.6 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
A.G. Kirkpatrick , I.A. Lazagabaster , J.R. Robinson , J. Rowan , C.J. Campisano , K.E. Reed , J.R. Scott , P.S. Ungar
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Abstract

Ethiopian fossil sites in the Lee Adoyta basin at Ledi-Geraru and the Maka'amitalu basin at Hadar straddle the Pliocene-Pleistocene transition and have both yielded fossil hominins attributed to early Homo. Faunal remains at these sites hold potential for providing insights into the ecological backdrop of the transition between these epochs in the lower Awash Valley and, by extension, the environments associated with the first appearance of Homo in the fossil record. Herbivore guild composition, ecomorphological study, and isotope analyses suggest that compared with paleoenvironments at earlier sites in the lower Awash, those in the Lee Adoyta basin and at Maka'amitalu had higher abundances of tropical grasses and sedges relative to browse plants. Here we bring another proxy to bear on the environments of the Lee Adoyta basin and Maka'amitalu associated with early Homo, dental microwear texture analysis. Dental microwear has been shown to separate grazing from browsing bovids and, because food choice reflects availability, can by extension provide insights into habitat. We employ texture analysis to infer the diets of bovid individuals from the Lee Adoyta basin (n = 13) and Maka'amitalu (n = 6) that preserve antemortem microwear. High-resolution replicas were scanned with a white-light confocal profiler and texture complexity and anisotropy were calculated for each surface and compared with baseline data for an extant sample of grazers, browsers, and mixed feeders. Values for bovids from the two sites do not differ from one another. Both samples have high anisotropy and low complexity, suggesting a graze-dominated diet and wide availability of grasses at both sites. These results are consistent with conclusions derived from other proxies.
埃塞俄比亚下阿瓦什河谷上新世-更新世过渡时期牛科动物牙齿微磨损
埃塞俄比亚在Ledi-Geraru的Lee Adoyta盆地和Hadar的Maka'amitalu盆地的化石遗址跨越了上新世-更新世的过渡时期,都发现了属于早期人属的化石。这些地点的动物遗骸有可能为了解阿瓦什河谷下游这些时代之间过渡的生态背景提供洞见,进而为化石记录中与人类首次出现相关的环境提供洞见。草食动物群落组成、生态形态研究和同位素分析表明,与阿瓦什河下游早期遗址相比,Lee Adoyta盆地和Maka'amitalu的古环境中热带禾草和莎草的丰度高于食草植物。在此,我们引入了另一个代理来研究与早期人类相关的Lee Adoyta盆地和Maka'amitalu的环境,即牙齿微磨损结构分析。牙齿微磨损已被证明可以区分放牧和浏览的牛科动物,因为食物选择反映了可用性,可以进一步提供对栖息地的了解。我们采用结构分析来推断来自Lee Adoyta盆地(n = 13)和Maka'amitalu (n = 6)的牛类个体的饮食,这些个体保存了生前的微磨损。用白光共聚焦剖面仪扫描高分辨率复制品,计算每个表面的纹理复杂性和各向异性,并与现有食草动物、浏览器和混合喂食动物样本的基线数据进行比较。两个站点的bovid值彼此没有差异。这两个样本都具有高各向异性和低复杂性,表明两个地点的饲料以食草为主,草的可用性很广。这些结果与从其他代理得出的结论一致。
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来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
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