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Nakalipithecus

Nakalipithecus is an extinct of great ape known from the early of , representing a key in understanding the divergence of extant African apes and humans. The type and only , N. nakayamai, was described based on fossils recovered from the Nakali Formation, including a right mandibular fragment preserving the first to third molars (M1–M3) as the (KNM-NA46400) and several isolated teeth comprising the hypodigm, such as an upper , canine, premolars, and additional molars. These remains, housed at the , date to 9.9–9.8 million years ago, within chronozone C5n.1n as determined by 40Ar-39Ar dating and magnetic polarity stratigraphy. The anatomy of Nakalipithecus nakayamai indicates a relatively large hominoid, with body size comparable to that of female or orangutans, based on dental dimensions. The features a well-developed inferior transverse extending to the mid-M1, with a thickness-to-height index of approximately 45% at M1. Dentally, it exhibits thick enamel, voluminous cusps, and reduced but marked cingula; the lower molars are mesiodistally elongated, with M3 larger than M2, while the upper canine is low-crowned with a prominent lingual cusplet. These traits show similarities to the contemporaneous ape Ouranopithecus macedoniensis (9.6–8.7 Ma) in overall size and some dental features, but N. nakayamai possesses less specialized characteristics, such as less inflated cusps and better-developed cingula, distinguishing it from earlier African hominoids like Proconsul and later forms like Samburupithecus. Phylogenetically, Nakalipithecus nakayamai is positioned near the last common ancestor of extant African great apes ( and chimpanzees) and humans, suggesting that the African and Eurasian great ape lineages had diverged by the early . Its discovery underscores a higher of large-bodied hominoids in during this interval, coinciding with the period of divergence between African apes and humans, and highlights the need for further fossil evidence to clarify intercontinental dispersals among apes. The Nakali site also yields other , contributing to a broader faunal assemblage that informs on .

Discovery and Naming

Discovery

The fossils of Nakalipithecus were excavated in 2005 at the Nakali site in central Kenya's Baringo District during paleontological surveys conducted by a joint Japanese-Kenyan expedition team led by Yutaka Kunimatsu of . The discovery occurred within the context of ongoing fieldwork initiated in 2002 to explore early faunas in the region. The specimen, cataloged as KNM-NA46400, comprises a right mandibular preserving the first through third molars (M1-M3). Accompanying the were 10 isolated , including premolars, molars, and a , all attributed to the same based on shared morphological features. These remains represent the primary evidence for the genus and were initially recognized as belonging to a great due to their large size and dental characteristics. Geologically, the specimens derive from (volcanic mudflow) deposits in the Upper Member of the Nakali Formation, a sequence of volcaniclastic sediments approximately 340 m thick divided into lower, middle, and upper units. The formation's age was established through , correlating the hominoid-bearing horizon to Chron C5n.1n, combined with biostratigraphic analysis of associated fauna, constraining the deposition to 9.9–9.8 million years ago. All Nakalipithecus fossils are housed and curated in the collections of the in , under the KNM (Kenya National Museums) designation.

The genus name Nakalipithecus is derived from "Nakali," the locality in where the fossils were discovered, combined with word pithekos, meaning "," to reflect the site's significance in identifying this great . The species name nakayamai honors the late Japanese geologist Katsuhiro Nakayama, who made key contributions to elucidating the geology of the Nakali Formation during the 2005 expedition. The was formally named and described in 2007 by Kunimatsu et al. in a publication in the Proceedings of the .

Taxonomy and Phylogeny

Classification

Nakalipithecus is classified within the domain Eukaryota, kingdom Animalia, phylum Chordata, class Mammalia, order Primates, suborder Haplorhini, infraorder Simiiformes, superfamily Hominoidea, and family Hominidae https://www.pnas.org/doi/10.1073/pnas.0706190104. Its subfamily placement remains incertae sedis, with ongoing debate regarding whether it represents a stem taxon to the Ponginae (orangutan clade) or Homininae (African ape and human clade) due to its mosaic of primitive and derived dental and cranial features https://www.pnas.org/doi/10.1073/pnas.0706190104. The genus Nakalipithecus is monotypic, containing only the single N. nakayamai, with no recognized https://www.pnas.org/doi/10.1073/pnas.0706190104. This was formally described in as a great based on a partial and associated teeth from the Nakali Formation in https://www.pnas.org/doi/10.1073/pnas.0706190104. A 2017 morphometric analysis of the lower fourth deciduous (dp4) further supports Nakalipithecus' affinities with hominoids, positioning it near the last common of , chimpanzees, and humans in morphospace and emphasizing its retention of primitive features shared with earlier apes https://doi.org/10.1016/j.crpv.2016.10.004. This study highlights phenotypic continuity with later hominoid lineages, reinforcing an origin for the great radiation https://doi.org/10.1016/j.crpv.2016.10.004. The debated subfamily assignment stems from Nakalipithecus' combination of primitive traits, such as less inflated cusps and well-developed cingula on molars, alongside derived features suggesting proximity to the African great ape and human https://www.pnas.org/doi/10.1073/pnas.0706190104. These mosaic characteristics complicate precise phylogenetic placement, with some interpretations favoring a basal position within rather than a clear affiliation to modern subfamilies https://doi.org/10.1016/j.crpv.2016.10.004.

Evolutionary Relationships

Nakalipithecus nakayamai is hypothesized to represent a stem great ape positioned close to the last common ancestor of the extant African great apes (gorillas, chimpanzees, and humans). Its dental morphology, including thick-enameled molars and low-crowned canines, aligns it with early members of the African ape-human clade (AAH), suggesting it predates and potentially contributes to the divergence of these lineages around 10–8 million years ago (Ma). Phylogenetic analyses place Nakalipithecus within the hominine clade, distinct from the pongine (orangutan) lineage, reinforcing its role in the early radiation of African hominoids. However, a 2023 phylogenetic analysis positions it as a stem hominid outside the crown Hominidae, highlighting the ongoing debate. The exhibits notable similarities to macedoniensis from (dated ~9.6–8.7 Ma), including comparable body size and certain craniodental features, leading to proposals of a taxon relationship or an ancestral-descendant link. However, Nakalipithecus retains more traits, such as less inflated cusps and better-developed cingula on its teeth, indicating it may serve as an precursor to this Eurasian form. A 2017 morphometric analysis of the lower fourth premolar (dp4) further supports closer affinities to apes than to Eurasian taxa like Sivapithecus, with Nakalipithecus showing morphology that bridges early Miocene forms to later hominines. Shared dental characteristics with Chororapithecus abyssinicus from (~10 Ma), such as large, thick-enameled molars, imply an early diversification of great ape lineages, potentially including the gorilla-chimpanzee split. Both taxa highlight a previously underdocumented diversity of hominoids in , challenging earlier models favoring Eurasian origins for the AAH . Nakalipithecus carries implications for "" dispersals among Miocene hominoids, potentially representing an African migrant that gave rise to Eurasian apes like via vicariance events driven by climate-induced between ~10–7 Ma. Its older age and basal features relative to European counterparts support an African source for these dispersals, coinciding with the expansion of open woodlands and savannas across . This scenario underscores Nakalipithecus as a key node in the biogeographic history of great apes.

Anatomy

Craniodental Morphology

The mandibular corpus of Nakalipithecus nakayamai is robust but less so than that of most Eurasian Miocene hominoids, such as Ouranopithecus and Sivapithecus, with a height of approximately 44 mm and thickness of 19.8 mm at the level of M1, yielding a thickness/height index of about 45%. The symphysis exhibits moderate eversion, a well-developed inferior transverse torus that extends to the mid-M1, and moderate symphyseal torsion. A superior transverse torus is moderately developed, and the lateral aspect of the corpus is vertical below M1, transitioning to a more oblique orientation posteriorly. The canines are small and low-crowned, with subtle inferred from size variation; for example, the upper canine (KNM-NA 47594) measures 10.7 mm mesiodistally by 10.5 mm buccolingually. It features a prominent lingual cingulum and a large lingual cusplet, with light wear indicating functionality in a frugivorous context. Lower canines, though not preserved, are expected to show similar low-crown morphology based on overall dental proportions. The premolars display elongated forms with distinct features; the P3s (e.g., KNM-NA 46423: 12.4 mm MD × 8.2 mm BL; KNM-NA 46431: 9.3 mm MD × 11.1 mm BL) are semitriangular in occlusal outline, exhibiting weak bilateral compression, a wide distal fovea, and a prominent lingual cingulum. The P4s (e.g., KNM-NA 46424: 10.4 mm MD × 14.0 mm BL; KNM-NA 46430: 9.5 mm MD × 11.9 mm BL) are broader, with voluminous cusps positioned peripherally, large distal foveae, and oblique wear facets suggesting shearing capabilities. Both premolar types show thin enamel relative to molars and moderate development of accessory structures. The molars are quadrate and relatively flat, with low, massive cusps, thick , a flat dentine/ junction, and reduced but marked cingula; the M1s (e.g., KNM-NA 46400: 15.6 mm MD × 14.0 mm BL; KNM-NA 47591: 12.4 mm MD × 13.4 mm BL) are slightly smaller than M2 (KNM-NA 46400: 16.2 mm MD × 15.8 mm BL), while M3s are the largest and mesiodistally elongated (e.g., KNM-NA 46400: 19.5 mm MD × 15.1 mm BL). patterns on the molars indicate heavy attrition on buccal cusps of M1–M2, with preserved lingual relief, and spacious occlusal basins. The lower fourth (dp4, KNM-NA 46435: 11.4 mm MD × 9.4 mm BL) retains features, including massive low cusps, a broad distal fovea, and a weakly developed buccal cingulum with small depressions at the protoconid base. The overall dental arcade is parabolic, with postcanine teeth arranged in a gently diverging row, representing an intermediate between more V-shaped patterns and the U-shaped arcs of modern hominoids. These craniodental traits, including thick and reduced cingula, align Nakalipithecus with basal great apes.

Body Size and

The body size of Nakalipithecus nakayamai has been estimated solely from dental and dimensions, as no postcranial skeletal elements are available for analysis. The (KNM-NA 46400), presumed to represent a based on the of an associated upper , is similar in dental size to and orangutans. These assessments derive from mandibular robusticity metrics, such as a body of approximately 44 mm and thickness of 19.8 mm at the M1 level (yielding a thickness/ of ≈45%), and tooth dimensions. Dental metrics further indicate moderate levels of in N. nakayamai. For instance, variation in third molar (M3) crown areas—where isolated specimens are ≈70% the size of the holotype M3—implies a size difference of around 30% between presumed sexes, serving as a proxy for overall dimorphism that is less extreme than the ≈50% size disparity observed in modern gorillas (Gorilla gorilla). dimensions support this pattern, with the low-crowned, buccolingually broad upper (10.7 mm mesiodistal length, 10.5 mm buccolingual breadth) of the consistent with a , and inferred showing a 20–30% size increase based on comparable ratios in related hominoids. This estimated size positions N. nakayamai as a medium- to large-bodied great ape, likely adapted for a mix of arboreal and possibly more terrestrial behaviors akin to extant pongines and hominines, though direct locomotor evidence is lacking.

Paleobiology

Habitat and Paleoecology

Nakalipithecus nakayamai inhabited the Upper Nakali Beds of the Nakali Formation in north-central , located along the eastern margin of the Valley. These deposits, dated to approximately 9.9–9.8 million years ago, consist primarily of volcanic mudflow sediments indicative of lakeside and riverine environments influenced by rift-related tectonic activity. This tectonic setting, part of the broader System, promoted rapid sediment accumulation and local hydrological variations, shaping a dynamic during the early . The paleoenvironment at Nakali featured seasonal sclerophyllous evergreen woodlands dominated by vegetation, reflecting a warm and humid climate typical of the before a broader transition to drier conditions across between approximately 10 and 7 million years ago. Stable isotope analyses of herbivore confirm the prevalence of plants, suggesting a more forested setting compared to contemporaneous sites like the Samburu Hills, where grasslands were emerging. This woodland habitat supported browsers such as early black rhinoceroses (Diceros spp.), highlighting a of closed-canopy forests interspersed with open areas. The associated fauna from the Upper Nakali Beds includes a diverse mammalian assemblage, featuring suids such as Nyanzachoerus nakaliensis, hippopotamids like Kenyapotamus coryndonae, proboscideans, and various , with no evidence of direct ecological competitors to Nakalipithecus among large . This community coexisted with early bovids, indicating a mixed forest-savanna mosaic where Nakalipithecus likely occupied the niche of a mid-level browser, foraging in the of sclerophyllous woodlands. The faunal composition underscores a wetter, resource-rich transitional within the Pikermian , influenced by regional rift dynamics.

Diet and Behavior

Nakalipithecus nakayamai exhibited a mixed diet inferred from its dental morphology, featuring thick enamel and low, voluminous cusps on the molars that supported consumption of both soft vegetation, such as fruits and leaves, and harder items like nuts and seeds. This configuration indicates primarily folivorous habits with a supplementary hard-object feeding component, though less specialized for abrasive foods compared to contemporaneous Eurasian hominoids like Ouranopithecus. Locomotion in Nakalipithecus is inferred to have involved arboreal , with potential terrestrial elements, based on its estimated body mass comparable to that of female or orangutans and the robusticity of the , consistent with the generalized great bauplan; however, no postcranial fossils are available to confirm these traits directly. Social behavior likely included unimale polygynous grouping akin to modern , as suggested by high intraspecific variation in third molar crown size (approximately 70% relative to the ), indicative of that correlates with polygynous mating systems in extant s. Territorial displays were probably mediated by honing, evidenced by the mesial honing facet on the upper , a feature shared with other hominoids for .

References

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    A new Late Miocene great ape from Kenya and its implications for ...
    Here we describe a new genus of great ape (Nakalipithecus nakayamai gen. et sp. nov.) recently discovered from the early Late Miocene of Nakali, Kenya.
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    A second hominoid species in the early Late Miocene fauna of ...
    As the presently available material for Nakalipithecus is comprised of a single mandibular fragment with heavily worn molars and a handful of isolated teeth, ...
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    New apes fill the gap - PNAS
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    A morphometric mapping analysis of lower fourth deciduous ...
    August–September 2017, ... One of the fossil materials that is available for Nakalipithecus and Ouranopithecus is the lower fourth deciduous premolar (dp4).
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