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Lewis JE, Ward CV, Kimbel WH, Kidney CL, Brown FH, Quinn RL, Rowan J, Lazagabaster IA, Sanders WJ, Leakey MG, Leakey LN. A 4.3-million-year-old Australopithecus anamensis mandible from Ileret, East Turkana, Kenya, and its paleoenvironmental context. J Hum Evol 2024; 194:103579. [PMID: 39173445 DOI: 10.1016/j.jhevol.2024.103579] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/19/2024] [Revised: 07/26/2024] [Accepted: 07/27/2024] [Indexed: 08/24/2024]
Abstract
A hominin mandible, KNM-ER 63000, and associated vertebrate remains were recovered in 2011 from Area 40 in East Turkana, Kenya. Tephrostratigraphic and magnetostratigraphic analyses indicate that these fossils date to ∼4.3 Ma. KNM-ER 63000 consists of articulating but worn and weathered mandibular corpora, with a broken right M2 crown and alveoli preserved at other tooth positions. Despite extensive damage, KNM-ER 63000 preserves diagnostic anatomy permitting attribution to Australopithecus anamensis. It can be distinguished from Australopithecus afarensis by its strongly inclined symphyseal axis with a basally convex, 'cut-away' external surface, a lateral corpus that sweeps inferomedially beneath the canine-premolar row, and alignment of the canine alveolus with the postcanine axis. KNM-ER 63000 is distinguished from Ardipithecus ramidus by its thick mandibular corpus and large M2 crown. The functional trait structure and enamel's stable carbon isotopic composition of the Area 40 large-mammal community suggests an environment comparable to Kanapoi and other ∼4.5-4 Ma eastern African sites that would have offered Au. anamensis access to both C3 and C4 food resources. With an age of ∼4.3 Ma, KNM-ER 63000 is the oldest known specimen of Au. anamensis, predating the Kanapoi and Asa Issie samples by at least ∼100 kyr. This specimen extends the known temporal range of Au. anamensis and places it in temporal overlap with fossils of Ar. ramidus from Gona, Ethiopia. The morphology of KNM-ER 63000 indicates that the reconfigured masticatory system differentiating basal hominins from the earliest australopiths existed in the narrow temporal window, if any, separating the two. The very close temporal juxtaposition of these significant morphological and adaptive differences implies that Ar. ramidus was a relative rather than a direct phyletic ancestor of earliest Australopithecus.
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Affiliation(s)
- Jason E Lewis
- Turkana Basin Institute, Department of Anthropology, Stony Brook University, Stony Brook, NY 11794-4364, USA; Chronicle Heritage, 319 E Palm Lane, Phoenix, AZ 85004, USA
| | - Carol V Ward
- Department of Pathology & Anatomical Sciences, University of Missouri, Columbia, MO 65212, USA.
| | - William H Kimbel
- Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85287-4101, USA
| | - Casey L Kidney
- Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112-0112, USA
| | - Frank H Brown
- Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112-0112, USA
| | - Rhonda L Quinn
- School of Earth, Environment & Society, Bowling Green State University, Bowling Green, OH 43403-0085, USA
| | - John Rowan
- Department of Archaeology, University of Cambridge, Cambridge, UK
| | - Ignacio A Lazagabaster
- National Research Center on Human Evolution (CENIEH), Paseo Sierra de Atapuerca 3, Burgos 09002, Spain; Department of Evolution, Ecology and Behaviour, University of Liverpool, Liverpool L69 3BX, UK
| | - William J Sanders
- Museum of Paleontology, University of Michigan, Ann Arbor, MI 48109-1085, USA
| | - Meave G Leakey
- Turkana Basin Institute, Department of Anthropology, Stony Brook University, Stony Brook, NY 11794-4364, USA
| | - Louise N Leakey
- Turkana Basin Institute, Department of Anthropology, Stony Brook University, Stony Brook, NY 11794-4364, USA; Department of Paleontology, National Museums of Kenya, Museum Hill, Nairobi, Kenya
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Reda HG, Frost SR, Simons EA, Quade J, Simpson SW. Description and taxonomic assessment of fossil Cercopithecidae from the Pliocene Galili Formation (Ethiopia). J Hum Evol 2024; 190:103508. [PMID: 38599140 DOI: 10.1016/j.jhevol.2024.103508] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/31/2023] [Revised: 02/06/2024] [Accepted: 02/06/2024] [Indexed: 04/12/2024]
Abstract
The Mount Galili Formation in the Afar region, Ethiopia, samples a critical time in hominin evolution, 4.4 to 3.8 Ma, documenting the last appearance of Ardipithecus and the origin of Australopithecus. This period is also important in the evolution of cercopithecids, especially the origin of Theropithecus in general and Theropithecus oswaldi lineage in particular. Galili has provided a total of 655 cercopithecid specimens that include crania, mandibles, isolated teeth and postcrania. All the fossils were recovered from the Lasdanan (5.3-4.43 Ma), Dhidinley (4.43-3.9 Ma) and Shabeley Laag (∼3.92-3.8 Ma) Members. Here, we described and analyzed 362 fossils employing both qualitative and quantitative methods. Descriptions of the material were supplemented with dental metrics and cranial shape analysis using three-dimensional geometric morphometrics. Results indicate the presence of at least six cercopithecid taxa: Theropithecus oswaldi serengetensis (n = 28), Theropithecus sp. (n = 2), three non-Theropithecus papionin groups (n = 134) and one colobine-size group (n = 58). The T. o. serengetensis represents the earliest form of the lineage, documented from ∼3.9 Ma Galili sediments. The three Galili papionins include a smaller taxon, a medium-sized taxon comparable to Pliopapio alemui and a large papionin overlapping in size with Soromandrillus, Gorgopithecus and Dinopithecus. The majority of Galili colobines have closest affinities to Kuseracolobus aramisi and some overlap with other taxa. Papionins dominate the Galili cercopithecid collection, although colobines are still fairly common (approximately 25% of the sample). Thus, Galili sample is like Kanapoi (4.2-4.1 Ma) and Gona (5.2-3.9 Ma) localities but distinct from Aramis, suggesting paleoecological similarity to the former sites. On the other hand, Theropithecus is less abundant at Galili than geologically younger Hadar (3.4-3.2 Ma) and Woranso-Mille (3.8-3.6 Ma) sites. Whether this difference is due to sampling, time or landscape variation requires further investigation.
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Affiliation(s)
- Hailay G Reda
- Department of Anthropology, University of Oregon, Eugene, OR, 97403-1218, USA.
| | - Stephen R Frost
- Department of Anthropology, University of Oregon, Eugene, OR, 97403-1218, USA
| | - Evan A Simons
- Department of Behavioral Neuroscience, Oregon Health and Science University, 3181 SW Sam Jackson Park Rd, L470, Portland, OR, 97239, USA
| | - Jay Quade
- Department of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, AZ, 85721, USA
| | - Scott W Simpson
- Department of Anatomy, Case Western Reserve University, Cleveland, OH, 44106-4930, USA; Laboratory of Physical Anthropology, Cleveland Museum of Natural History, Cleveland, OH, 44106, USA
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Getahun DA, Delson E, Seyoum CM. A review of Theropithecus oswaldi with the proposal of a new subspecies. J Hum Evol 2023; 180:103373. [PMID: 37269782 DOI: 10.1016/j.jhevol.2023.103373] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/14/2022] [Revised: 04/02/2023] [Accepted: 04/03/2023] [Indexed: 06/05/2023]
Abstract
Theropithecus oswaldi darti, as currently understood, is the oldest Theropithecus taxon in the fossil record and the earliest subspecies in the Theropithecusoswaldi lineage. Theropithecus oswaldi darti is typified at the site of Makapansgat in South Africa, and a similar form (T. o. cf. darti) is usually recognized at Hadar, Dikika, some Middle Awash localities, and Woranso-Mille in Ethiopia. This taxon is also tentatively believed to occur in Kenya at Kanam and Koobi Fora and in Member C of the Shungura Formation in Ethiopia. While there is a general consensus that the East African 'darti' specimens are sufficiently similar to each other, there has always been a question of whether they are too distinct from the South African type material of T. o. darti to belong to the same subspecies. Here we conduct a morphological comparison of the different samples previously assigned to T. o. darti and T. o. cf. darti. The results of our analyses overwhelmingly support the hypothesis that the East African samples are distinct from the South African ones, and they are likely distinct in geological age as well. Therefore, we propose a new subspecies designation for the material previously termed T. o. cf. darti from East Africa: Theropithecus (Theropithecus) oswaldi ecki subsp. nov. We also formally recognize Theropithecus (Theropithecus) oswaldi serengetensis (Dietrich, 1942) for specimens from Laetoli, Woranso-Mille, and perhaps Galili.
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Affiliation(s)
- Dagmawit Abebe Getahun
- PhD Program in Anthropology, City University of New York Graduate Center, 365 Fifth Avenue, New York, NY 10016, USA; Department of Anthropology, Lehman College, City University of New York, 250 Bedford Park Boulevard West, Bronx, NY 10468, USA; New York Consortium in Evolutionary Primatology and NYCEP Morphometrics Group, New York, NY 10016, USA.
| | - Eric Delson
- PhD Program in Anthropology, City University of New York Graduate Center, 365 Fifth Avenue, New York, NY 10016, USA; Department of Anthropology, Lehman College, City University of New York, 250 Bedford Park Boulevard West, Bronx, NY 10468, USA; New York Consortium in Evolutionary Primatology and NYCEP Morphometrics Group, New York, NY 10016, USA; Division of Paleontology, American Museum of Natural History, 200 Central Park West, New York, NY 10024, USA; PhD Program in Earth and Environmental Sciences, City University of New York Graduate Center, 365 Fifth Avenue, New York, NY 10016, USA; Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona, Edifici ICTA-ICP, Campus de la UAB, c/ Columnes, s/n, 08193 Cerdanyola del Vallès, Barcelona, Spain.
| | - Chalachew Mesfin Seyoum
- Department of Basic Medical Sciences, The University of Arizona, College of Medicine, 475 N 5th St., Phoenix, AZ 85004, USA; Department of Pathology and Anatomical Sciences, University of Missouri, Columbia, MO 65211, USA
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Villaseñor A, Uno KT, Kinyanjui RN, Behrensmeyer AK, Bobe R, Advokaat EL, Bamford M, Carvalho SC, Hammond AS, Palcu DV, Sier MJ, Ward CV, Braun DR. Pliocene hominins from East Turkana were associated with mesic environments in a semiarid basin. J Hum Evol 2023; 180:103385. [PMID: 37229946 DOI: 10.1016/j.jhevol.2023.103385] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/03/2022] [Revised: 04/15/2023] [Accepted: 04/19/2023] [Indexed: 05/27/2023]
Abstract
During the middle Pliocene (∼3.8-3.2 Ma), both Australopithecus afarensis and Kenyanthropus platyops are known from the Turkana Basin, but between 3.60 and 3.44 Ma, most hominin fossils are found on the west side of Lake Turkana. Here, we describe a new hominin locality (ET03-166/168, Area 129) from the east side of the lake, in the Lokochot Member of the Koobi Fora Formation (3.60-3.44 Ma). To reconstruct the paleoecology of the locality and its surroundings, we combine information from sedimentology, the relative abundance of associated mammalian fauna, phytoliths, and stable isotopes from plant wax biomarkers, pedogenic carbonates, and fossil tooth enamel. The combined evidence provides a detailed view of the local paleoenvironment occupied by these Pliocene hominins, where a biodiverse community of primates, including hominins, and other mammals inhabited humid, grassy woodlands in a fluvial floodplain setting. Between <3.596 and 3.44 Ma, increases in woody vegetation were, at times, associated with increases in arid-adapted grasses. This suggests that Pliocene vegetation included woody species that were resilient to periods of prolonged aridity, resembling vegetation structure in the Turkana Basin today, where arid-adapted woody plants are a significant component of the ecosystem. Pedogenic carbonates indicate more woody vegetation than other vegetation proxies, possibly due to differences in temporospatial scale and ecological biases in preservation that should be accounted for in future studies. These new hominin fossils and associated multiproxy paleoenvironmental indicators from a single locale through time suggest that early hominin species occupied a wide range of habitats, possibly including wetlands within semiarid landscapes. Local-scale paleoecological evidence from East Turkana supports regional evidence that middle Pliocene eastern Africa may have experienced large-scale, climate-driven periods of aridity. This information extends our understanding of hominin environments beyond the limits of simple wooded, grassy, or mosaic environmental descriptions.
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Affiliation(s)
- Amelia Villaseñor
- Department of Anthropology, The University of Arkansas, 330 Old Main, Fayetteville, AR, 72701, USA.
| | - Kevin T Uno
- Lamont-Doherty Earth Observatory of Columbia University, Division of Biology and Paleo Environment, Palisades, NY, 10964, USA
| | - Rahab N Kinyanjui
- Department of Earth Sciences, National Museums of Kenya, Nairobi, 40658-00100, Kenya; Department of Archaeology, Max Planck Institute of Geoanthropology, 07745, Jena, Germany; Human Origins Program, National Museum of Natural History, Smithsonian Institution, MRC 121, Washington, DC, 20013, USA
| | - Anna K Behrensmeyer
- Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, Washington, DC, 20013, USA
| | - René Bobe
- Primate Models for Behavioural Evolution Lab, Institute of Human Sciences, University of Oxford, 64 Banbury Road, Oxford, OX2 6PN, UK; Gorongosa National Park, Sofala, Mozambique
| | - Eldert L Advokaat
- Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
| | - Marion Bamford
- Evolutionary Studies Institute and School of Geosciences, University of the Witwatersrand, P Bag 3, WITS, 2050, South Africa
| | - Susana C Carvalho
- Primate Models for Behavioural Evolution Lab, Institute of Human Sciences, University of Oxford, 64 Banbury Road, Oxford, OX2 6PN, UK; Gorongosa National Park, Sofala, Mozambique; Interdisciplinary Center for Archaeology and Evolution of Human Behaviour (ICArEHB), Universidade do Algarve, 8005-139, Faro, Portugal
| | - Ashley S Hammond
- Division of Anthropology, American Museum of Natural History (AMNH), New York, NY, 10024, USA; New York Consortium in Evolutionary Primatology at AMNH, New York, NY, 10024, USA
| | - Dan V Palcu
- Oceanographic Institute of the University of São Paulo, Brazil; Paleomagnetic Laboratory 'Fort Hoofddijk', Utrecht University, Budapestlaan 17, 3584 CD, Utrecht, the Netherlands
| | - Mark J Sier
- Centro Nacional de Investigación Sobre la Evolución Humana (CENIEH), Paseo Sierra de Atapuerca 3, 09002, Burgos, Spain; Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK; Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
| | - Carol V Ward
- Department of Pathology and Anatomical Sciences, University of Missouri, Columbia, MO, USA
| | - David R Braun
- Center for the Advanced Study of Human Paleobiology, Anthropology Department, George Washington University, Washington, DC, USA
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Frost SR, Jablonski NG, Haile-Selassie Y. The earliest most complete skeleton of Theropithecus. J Hum Evol 2023; 180:103370. [PMID: 37167814 DOI: 10.1016/j.jhevol.2023.103370] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/05/2022] [Revised: 03/30/2023] [Accepted: 03/30/2023] [Indexed: 05/13/2023]
Abstract
The middle Pliocene site of Woranso-Mille in the Afar Region of Ethiopia has yielded numerous significant early hominin fossils representing multiple, coexisting taxa. Here we report on another significant discovery, the oldest partial skeleton of the papionin, Theropithecus. The specimen was recovered from the Aralee Issie collection area over multiple field seasons from 2004 through 2019. The specimen was unearthed in situ from the fluvial facies of the Mesgid Dora Tuff dated to 3.66-3.57 Ma. The partial skeleton, ARI-VP-1/26, is that of a subadult male lacking a skull. In the absence of unambiguously associated craniodental remains, the male status of the specimen was established from the dimensions of the long bones in comparison to those of other Theropithecus from Woranso-Mille. ARI-VP-1/26 is noteworthy because it preserves partial hand and foot skeletons, including a complete set of metacarpals from the left side. The theropith status of ARI-VP-1/26 was established based on the detailed anatomy of the postcranial skeleton, especially the proximal and distal humerus, proximal radius, and proximal femur. The morphology of the postcranium of ARI-VP-1/26 is consistent with that of recognized Theropithecus from Woranso-Mille and, specifically, with specimens recognized as Theropithecus oswaldi cf. darti from other sites. The ratio of the lengths of the first metacarpal to metacarpals 2-5 in ARI-VP-1/26 is intermediate between that seen in extant Papio and Theropithecus. In Theropithecus gelada and Theropithecus brumpti, the pairing of pollical and indical metacarpals of near equal length contributes to the species' high opposability index and is associated with a 'manual grazing' feeding habit. Cercopithecids constitute 43% of the identified vertebrates at Aralee Issie, and T. oswaldi cf. darti is the most common mammalian species. The monkeys of Aralee Issie lived in an open shrubland habitat, but the specific reasons for their high prevalence at the site are unclear.
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Affiliation(s)
- Stephen R Frost
- Department of Anthropology, University of Oregon, Eugene, OR 97403-1218, USA.
| | - Nina G Jablonski
- Department of Anthropology, The Pennsylvania State University, 409 Carpenter Building, University Park, PA 16802, USA
| | - Yohannes Haile-Selassie
- Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85281, USA
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Pallas L, Daver G, Merceron G, Boisserie JR. The anatomy of the hindlimb of Theropithecus brumpti (Cercopithecidae, Papionini): Morphofunctional implications. J Hum Evol 2023; 178:103333. [PMID: 36965446 DOI: 10.1016/j.jhevol.2023.103333] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/25/2021] [Revised: 01/27/2023] [Accepted: 01/29/2023] [Indexed: 03/27/2023]
Abstract
Theropithecus brumpti is a primate known from numerous craniodental specimens in the Plio-Pleistocene Shungura Formation (Lower Omo Valley, Ethiopia), but the anatomy of its hindlimb is documented only by a few associated and mostly incomplete postcranial specimens. The adaptations of T. brumpti are still debated, with its substrate preferences and its use of squatting postures recently discussed based on anatomical differences when compared with its extant representative, Theropithecus gelada. Here, we describe an associated femur and tibia (L 869-1 and L 869-2) of a presumed T. brumpti male and a partial foot (L 865-1r and L 865-1t) of a male T. brumpti, dated to ca. 2.6 Ma and ca. 2.32 Ma respectively. Based on univariate and bivariate morphometric analyses, we provide new data on the morphological correlates of substrate preferences and postural behaviors of this fossil species. Our results are in agreement with previous analyses and present T. brumpti as a predominantly terrestrial primate. We demonstrate the presence of osteological correlates associated with the use of squatting behaviors in T. brumpti but also point to significant anatomical differences between this paleontological species and T. gelada. These differences blur the functional value of characters previously identified as diagnostic of T. gelada and its postural behavior. We further document the postcranial distinctiveness of the Theropithecus clade in relation to the Papio clade. This study thus provides new insights into the postcranial anatomy and paleoecology of an abundant fossil primate from the Plio-Pleistocene of eastern Africa.
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Affiliation(s)
- Laurent Pallas
- Laboratoire de Paléontologie, Evolution, Paléoécosystèmes et Paléoprimatologie (PALEVOPRIM), UMR CNRS 7262, Université de Poitiers, Poitiers Cedex 86022, France.
| | - Guillaume Daver
- Laboratoire de Paléontologie, Evolution, Paléoécosystèmes et Paléoprimatologie (PALEVOPRIM), UMR CNRS 7262, Université de Poitiers, Poitiers Cedex 86022, France
| | - Gildas Merceron
- Laboratoire de Paléontologie, Evolution, Paléoécosystèmes et Paléoprimatologie (PALEVOPRIM), UMR CNRS 7262, Université de Poitiers, Poitiers Cedex 86022, France
| | - Jean-Renaud Boisserie
- Laboratoire de Paléontologie, Evolution, Paléoécosystèmes et Paléoprimatologie (PALEVOPRIM), UMR CNRS 7262, Université de Poitiers, Poitiers Cedex 86022, France; Centre Français des Études Éthiopiennes, CNRS & Ministère de l'Europe et des affaires étrangères, PO BOX 5554, Addis Ababa, Ethiopia
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Arenson JL, Harrison T, Sargis EJ, Taboada HG, Gilbert CC. A new species of fossil guenon (Cercopithecini, Cercopithecidae) from the Early Pleistocene Lower Ngaloba Beds, Laetoli, Tanzania. J Hum Evol 2022; 163:103136. [PMID: 35033736 DOI: 10.1016/j.jhevol.2021.103136] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/10/2021] [Revised: 12/06/2021] [Accepted: 12/06/2021] [Indexed: 11/30/2022]
Abstract
The living guenons (Cercopithecini, Cercopithecidae) are speciose and widely distributed across sub-Saharan Africa but are poorly represented in the fossil record. In addition, the craniodental and skeletal similarity of the guenons has hampered the identification of fragmentary material, likely obscuring the taxonomic diversity represented in the fossil record. Here, we describe a new fossil guenon specimen (LAET 75-3703) from the Lower Ngaloba Beds, Laetoli in Tanzania, dated to ∼1.7-1.2 Ma and preserving the lower face and mandible. Comparison to 278 extant guenon specimens, representing all six extant genera, identified several informative traits for distinguishing between the morphologically similar Chlorocebus and Cercopithecus, and these support the attribution of LAET 75-3703 to Chlorocebus. A discriminant function analysis of seven craniodental indices on a subsample of Chlorocebus and Cercopithecus was robust with an overall correct classification rate of 80.4%, and it classified LAET 75-3703 as a member of Chlorocebus with a posterior probability of 92.7%. LAET 75-3703 shares with Chlorocebus the presence of small 'thumbprint' depressions on the maxilla; a tall, narrow, and diamond-shaped nasal aperture; a relatively longer and shallower face; relatively buccolingually broader molars; and a shallow mandible that decreases in depth posteriorly. In addition, LAET 75-3703 is distinguished from all extant guenons, including other species of Chlorocebus, in having a very small P3 relative to M1 area. As such, LAET 75-3703 is assigned to a new species, Chlorocebus ngedere sp. nov. This specimen represents the first cercopithecin from Laetoli, as well as the oldest fossil cercopithecin confidently attributed to a modern genus.
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Affiliation(s)
- Julia L Arenson
- PhD Program in Anthropology, The Graduate Center of the City University of New York, 365 Fifth Avenue, New York, NY, 10016, USA; New York Consortium in Evolutionary Primatology (NYCEP), New York, NY, 10016, USA.
| | - Terry Harrison
- New York Consortium in Evolutionary Primatology (NYCEP), New York, NY, 10016, USA; Center for the Study of Human Origins, Department of Anthropology, New York University, 25 Waverly Place, New York, NY, 10003, USA
| | - Eric J Sargis
- Department of Anthropology, Yale University, 10 Sachem Street, New Haven, CT, 06511, USA; Divisions of Vertebrate Paleontology and Vertebrate Zoology, Yale Peabody Museum of Natural History, 170 Whitney Avenue, New Haven, CT, 06511, USA; Yale Institute for Biospheric Studies, P.O. Box 208118, New Haven, CT, 06520, USA
| | - Hannah G Taboada
- Center for the Study of Human Origins, Department of Anthropology, New York University, 25 Waverly Place, New York, NY, 10003, USA
| | - Christopher C Gilbert
- PhD Program in Anthropology, The Graduate Center of the City University of New York, 365 Fifth Avenue, New York, NY, 10016, USA; New York Consortium in Evolutionary Primatology (NYCEP), New York, NY, 10016, USA; Department of Anthropology, Hunter College, CUNY, 695 Park Avenue, New York, NY, 10065, USA; Division of Paleontology, American Museum of Natural History, Central Park West, New York, NY, 10024, USA
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8
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Dumouchel L, Bobe R, Wynn JG, Barr WA. The environments of Australopithecus anamensis at Allia Bay, Kenya: A multiproxy analysis of early Pliocene Bovidae. J Hum Evol 2021; 151:102928. [PMID: 33453510 DOI: 10.1016/j.jhevol.2020.102928] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/25/2020] [Revised: 12/01/2020] [Accepted: 12/01/2020] [Indexed: 11/18/2022]
Abstract
Australopithecus anamensis, among the earliest fully bipedal hominin species, lived in eastern Africa around 4 Ma. Much of what is currently known about the paleoecology of A. anamensis comes from the type locality, Kanapoi, Kenya. Here, we extend knowledge of the range of environments occupied by A. anamensis by presenting the first multiproxy paleoecological analysis focusing on Bovidae excavated from another important locality where A. anamensis was recovered, locality 261-1 (ca. 3.97 Ma) at Allia Bay, East Turkana, Kenya. Paleoenvironments are reconstructed using astragalar ecomorphology, mesowear, hypsodonty index, and oxygen and carbon isotopes from dental enamel. We compare our results to those obtained from Kanapoi. Our results show that the bovid community composition is similar between the two fossil assemblages. Allia Bay and Kanapoi bovid astragalar ecomorphology spans the spectrum of modern morphologies indicative of grassland, woodland, and even forest-adapted forms. Dietary reconstructions based on stable isotopes, mesowear, and hypsodonty reveal that these bovids' diet encompassed the full C3 to C4 dietary spectrum and overlap in the two data sets. Our results allow us to confidently extend our reconstructions of the paleoenvironments of A. anamensis at Kanapoi to Allia Bay, where this pivotal hominin species is associated with heterogeneous settings including habitats with varying degrees of tree cover, including grasslands, bushlands, and woodlands.
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Affiliation(s)
- Laurence Dumouchel
- Department of Anthropology, Wichita State University, 1845 Fairmount Street, Wichita, KS 67260, USA.
| | - René Bobe
- Primate Models for Behavioural Evolution Lab, Institute of Cognitive & Evolutionary Anthropology, School of Anthropology, University of Oxford, 64 Banbury Rd, Park Town, Oxford, OX2 6PN, UK; Paleo-Primate Project Gorongosa, Gorongosa National Park, Sofala, Mozambique; Interdisciplinary Center for Archaeology and Evolution of Human Behaviour (ICArEHB), Universidade Do Algarve, Campus de Penha, Faro, 8005-139, Portugal
| | - Jonathan G Wynn
- Division of Earth Sciences, National Science Foundation, 2415 Eisenhower Avenue, Alexandria, VA 22314, USA
| | - W Andrew Barr
- Center for the Advanced Study of Human Paleobiology, The George Washington University, 800 22(nd)Street Northwest, Suite 6000, Washington, DC 20052, USA
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Elton S, Dunn J. Baboon biogeography, divergence, and evolution: Morphological and paleoecological perspectives. J Hum Evol 2020; 145:102799. [DOI: 10.1016/j.jhevol.2020.102799] [Citation(s) in RCA: 9] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/11/2019] [Revised: 04/01/2020] [Accepted: 04/01/2020] [Indexed: 11/30/2022]
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Frost SR, Simpson SW, Levin NE, Quade J, Rogers MJ, Semaw S. Fossil Cercopithecidae from the Early Pliocene Sagantole Formation at Gona, Ethiopia. J Hum Evol 2020; 144:102789. [PMID: 32485477 DOI: 10.1016/j.jhevol.2020.102789] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/12/2019] [Revised: 03/18/2020] [Accepted: 03/18/2020] [Indexed: 10/24/2022]
Abstract
The Early Pliocene Sagantole Fm. in the Gona Project area, Afar State, Ethiopia, is noted for discoveries of the early hominin Ardipithecus ramidus. A large series of fossil cercopithecid primates dated to between 4.8 and 4.3 Ma has also been collected from these sediments. In this paper, we use qualitative analysis and standard dental and postcranial measures to systematically describe the craniodental remains and tentatively allocate postcrania to taxa where we are able to. We then use these data to compare these specimens to fossil assemblages from contemporary sites, interpret their paleobiology, and discuss implications for the paleoecology of the Gona Sagantole Fm. We recognize three cercopithecid species in the Gona Sagantole Fm. Pliopapio alemui makes up approximately two-thirds of the identifiable specimens; nearly all of the rest are allocated to Kuseracolobus aramisi, and a single molar indicates the presence of a second, somewhat larger but morphologically distinct papionin. Among the Early Pliocene cercopithecids from Gona are also a number of postcranial elements. None of the postcranial remains are directly associated with any of the cranial material. Nonetheless, some of the distal humeri and proximal femora can be tentatively allocated to either Pl. alemui or K. aramisi based on a combination of size, as the latter is approximately 50% larger than the former, and morphology. If these assignments are correct, they suggest K. aramisi was primarily arboreal and similar to most extant colobines, whereas Pl. alemui was more mixed in its substrate use, being more terrestrially adapted than K. aramisi, but less so than extant Papio or Theropithecus. Thus, we interpret the predominance of Pl. alemui over K. aramisi is consistent with a somewhat more open environment at Gona than at Aramis.
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Affiliation(s)
- Stephen R Frost
- Department of Anthropology, University of Oregon, Eugene, OR, 97403-1218, USA.
| | - Scott W Simpson
- Department of Anatomy, Case Western Reserve University-School of Medicine, 10900 Euclid Avenue, Cleveland, OH, 44106, USA; Laboratory of Physical Anthropology, Cleveland Museum of Natural History, Cleveland, OH, 44106, USA
| | - Naomi E Levin
- Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI, 48109, USA
| | - Jay Quade
- Department of Geosciences, University of Arizona, Tucson, AZ, 85721, USA
| | - Michael J Rogers
- Department of Anthropology, Southern Connecticut State University, 501 Crescent Street, New Haven, CT, 06515-1355, USA
| | - Sileshi Semaw
- Centro Nacional de Investigación Sobre La Evolución Humana, Paseo de Atapuerca 3, 09002, Burgos, Spain; Stone Age Institute & CRAFT Research Center, Gosport, IN, 47408, USA
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