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来自埃塞俄比亚中新世的首个类人猿及狭鼻小目动物肘部的进化

First hominoid from the Miocene of Ethiopia and the evolution of the catarrhine elbow.

作者信息

Richmond B G, Fleagle J G, Kappelman J, Swisher C C

机构信息

Smithsonian Institution, Washington, DC 20560, USA.

出版信息

Am J Phys Anthropol. 1998 Mar;105(3):257-77. doi: 10.1002/(SICI)1096-8644(199803)105:3<257::AID-AJPA1>3.0.CO;2-P.

Abstract

The first known fossil ape from the early-middle Miocene of Fejej, Ethiopia, is described here. The specimen, FJ-18SB-68, is a partial ulna from a locality dated by 40Ar/39Ar and paleomagnetic methods to a minimum age of 16.18 MYA. Compared to a variety of extant and fossil ulnae, FJ-18SB-68 is most similar to Turkanapithecus, Proconsul, and Pliopithecus, and appears to have been an arboreal quadruped with substantial forearm rotational mobility. Among the extant ulnae, canonical variates analysis successfully discriminates platyrrhines from catarrhines and within the latter, cercopithecoids from hominoids. Basal catarrhines (e.g., Aegyptopithecus) are platyrrhine-like in their morphology. Two basic trends appear to evolve from this generalized template: one with less mobile and more habitually pronated forearms, as seen in living and fossil cercopithecoids (including Victoriapithecus and Paracolobus), and another with greater forearm rotational mobility in fossil and modern hominoids. Primitive Miocene apes, including Proconsul, Turkanapithecus, and FJ-18SB-68, share with extant hominoids a more laterally positioned and laterally facing radial notch and an incipient trochlear keel. This morphology, along with a large insertion area for m. brachialis, suggests a departure from the more habitually pronated hand posture of monkeys and may indicate greater climbing abilities in these arboreally quadrupedal apes. Later Miocene apes, such as Oreopithecus and Dryopithecus share additional morphological features with hominoids, indicating considerable suspensory and climbing capabilities.

摘要

本文描述了来自埃塞俄比亚费杰伊中新世早期-中期的首个已知化石猿。标本FJ-18SB-68是一根尺骨的一部分,该地点通过40Ar/39Ar和古地磁方法测定的最小年龄为1618万年前。与各种现存和化石尺骨相比,FJ-18SB-68与图尔卡纳猿、原康修尔猿和上新猿最为相似,似乎是一种具有较大前臂旋转灵活性的树栖四足动物。在现存尺骨中,典型变量分析成功地区分了阔鼻猴类和狭鼻猴类,在狭鼻猴类中,又区分了猕猴类和类人猿。基部狭鼻猴(如埃及猿)在形态上类似阔鼻猴。从这个一般模板似乎演化出两种基本趋势:一种是前臂灵活性较低且更习惯旋前,如现存和化石猕猴类(包括维多利亚古猿和副疣猴);另一种是化石和现代类人猿的前臂旋转灵活性更大。包括原康修尔猿、图尔卡纳猿和FJ-18SB-68在内的中新世早期原始猿与现存类人猿有共同特征,即桡骨切迹更侧向定位且朝向外侧面,以及初期的滑车嵴。这种形态,连同肱肌的大附着区域,表明与猴子更习惯旋前的手部姿势不同,可能意味着这些树栖四足猿具有更强的攀爬能力。晚中新世的猿,如奥氏猿和森林古猿与类人猿有更多共同形态特征,表明它们具有相当强的悬吊和攀爬能力。

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