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来自希腊马其顿中新世晚期沉积物中的马其顿原康修尔猿(灵长目,人猿总科)的乳下齿列。

The deciduous lower dentition of Ouranopithecus macedoniensis (Primates, Hominoidea) from the late Miocene deposits of Macedonia, Greece.

作者信息

Koufos George D, de Bonis Louis

机构信息

Department of Geology, Laboratory of Geology and Palaeontology, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece.

出版信息

J Hum Evol. 2004 Jun;46(6):699-718. doi: 10.1016/j.jhevol.2004.03.007.

Abstract

Two mandibular fragments with associated milk teeth assigned to the late Miocene hominoid primate Ouranopithecus macedoniensis are analyzed. The fossils, which belong to a single individual, were found in the Vallesian locality of "Ravin de la Pluie" of the Axios Valley (Macedonia, Greece). The material is described here and compared with extant and extinct hominoids, allowing assessment of the evolutionary trends in the deciduous lower dentition within the Hominoidea. Hylobatids represent the more primitive pattern. Gorilla is slightly more derived than hylobatids, but less derived than Pongo and Pan, the latter being the most derived. With relatively smaller deciduous canines and more molarized deciduous premolars, Ouranopithecus is more derived than both Pan and Gorilla. Among the fossil hominoids, Proconsul, representing the primitive condition, has a very simple dp(3)and a dp(4)that has a trigonid that is taller than the talonid and which lacks a hypoconulid. Griphopithecus is more derived than Proconsul in having a dp(4) with a lower trigonid, a hypoconulid, and a less oblique cristid obliqua. Australopithecus and Paranthropus possess a similar morphology to that of Homo, while Ardipithecus appears to be more primitive than the latter genera. Ouranopithecus has a more derived lower milk dentition than Proconsul and Griphopithecus, but less derived than Australopithecus and Paranthropus. The comparison of the lower milk dentition of Ouranopithecus confirms our previous conclusions suggesting that this fossil hominoid shares derived characters with Australopithecus and Homo.

摘要

对两块带有乳齿的下颌骨碎片进行了分析,这些碎片属于晚中新世类人猿灵长目动物马其顿原康修尔猿。这些化石来自同一个体,发现于希腊马其顿阿西奥斯河谷“Ravin de la Pluie”的瓦勒西安期地层。本文对该材料进行了描述,并与现存和已灭绝的类人猿进行了比较,从而评估类人猿下乳齿列的进化趋势。长臂猿代表了更为原始的模式。大猩猩比长臂猿稍为进化,但比猩猩和黑猩猩进化程度低,后两者是进化程度最高的。马其顿原康修尔猿的乳齿犬齿相对较小,乳前磨牙更为臼齿化,比黑猩猩和大猩猩都更为进化。在化石类人猿中,代表原始状态的原康修尔猿有非常简单的dp(3)和dp(4),其三角座比跟座高,且没有下后尖。希腊古猿比原康修尔猿更为进化,其dp(4)的三角座较低,有下后尖,斜嵴也不那么倾斜。南方古猿和傍人具有与现代人相似的形态,而地猿似乎比后两者更为原始。马其顿原康修尔猿的下乳齿列比原康修尔猿和希腊古猿更为进化,但比南方古猿和傍人进化程度低。对马其顿原康修尔猿下乳齿列的比较证实了我们之前的结论,即这种化石类人猿与南方古猿和现代人共有一些衍生特征。

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