Department of Anthropology, Stony Brook University, Stony Brook, New York, USA.
Department of Anthropology and Archaeology, University of Calgary, Calgary, Alberta, Canada.
Am J Biol Anthropol. 2022 Oct;179(2):261-275. doi: 10.1002/ajpa.24594. Epub 2022 Jul 24.
Hominoid fossils are abundant at early Miocene fossil sites in the Lothidok Range, located directly west of Lake Turkana in northern Kenya. The West Turkana Miocene Project (WTMP) has worked in the Lothidok Range since 2008 with the goal of further elucidating the paleobiology of the hominoids through the recovery of new specimens and detailed documentation of their paleoecological context. To date our research has focused largely on the Kalodirr and Moruorot Site Complexes, both radiometrically dated to ~17.5-16.8 Ma.
Our ongoing fieldwork at the Kalodirr Site Complex resulted in the discovery of new dentognathic specimens of the three previously identified species of fossil hominoids-Turkanapithecus kalakolensis, Simiolus enjiessi, and Afropithecus turkanensis.
A new mandible and an isolated M of T. kalakolensis from Kalodirr further clarify the lower molar morphology of the species and permit identification of KNM-MO 1 as a mandible of T. kalakolensis. A new mandible of S. enjiessi provides evidence of the relative proportions of the first and second lower molars. A new male specimen of A. turkanensis shows unusual P morphology that may be a developmental anomaly or a previously unknown morphological variant.
An improved understanding of the lower molar morphology of T. kalakolensis further strengthens its identification as a nyanzapithecine. Our new specimens and subsequent re-identification of existing collections makes it clear that all three Lothidok hominoids are known from both the Moruorot and Kalodirr Site Complexes. The Lothidok Range holds great promise for further documenting hominoid evolution.
在肯尼亚北部图尔卡纳湖以西的洛蒂多克山脉的早中新世化石遗址中,有大量的人科化石。自 2008 年以来,西图尔卡纳人猿化石项目(WTMP)一直在洛蒂多克山脉工作,目标是通过回收新标本并详细记录其古生态背景,进一步阐明人科动物的古生物学。迄今为止,我们的研究主要集中在卡洛迪尔和莫鲁罗特遗址群,这两个遗址都经过放射性测年,时间约为 1750-1680 万年前。
我们在卡洛迪尔遗址群的持续野外工作中发现了三种已鉴定的化石人科动物——图尔卡纳原康修尔猿、西莫伊索利斯和非洲南猿图尔卡纳种——的新齿列和齿骨标本。
卡洛迪尔发现的新下颌骨和孤立的 T. kalakolensis 的 M 代表了该物种的下臼齿形态进一步得到了明确,并使 KNM-MO 1 被鉴定为 T. kalakolensis 的下颌骨。新的 S. enjiessi 下颌骨提供了第一和第二下臼齿相对比例的证据。新的 A. turkanensis 雄性标本显示出不寻常的 P 形态,这可能是一种发育异常或以前未知的形态变异。
对 T. kalakolensis 下臼齿形态的更好理解进一步加强了它作为 Nyanzapithecus 的鉴定。我们的新标本以及随后对现有标本的重新鉴定,清楚地表明洛蒂多克的三种人科动物都来自莫鲁罗特和卡洛迪尔遗址群。洛蒂多克山脉有很大的潜力进一步记录人科动物的进化。