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Rowan J, Wood B. Dart and the Taung juvenile: making sense of a century-old record of hominin evolution in Africa. Biol Lett 2024; 20:20240185. [PMID: 39045658 PMCID: PMC11267397 DOI: 10.1098/rsbl.2024.0185] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/10/2024] [Revised: 06/06/2024] [Accepted: 06/17/2024] [Indexed: 07/25/2024] Open
Abstract
The announcement in 1925 by Raymond Dart of the discovery of the Taung juvenile's skull in a quarry in sub-Saharan Africa is deservedly a classic publication in the history of palaeoanthropology. Dart's paper-which designated Taung as the type specimen of the early hominin species Australopithecus africanus-provided the first fossil evidence supporting Charles Darwin's 1871 prediction that Africa was where the human lineage originated. The Taung juvenile's combination of ape and human characteristics eventually led to a paradigm shift in our understanding of human evolution. This contribution focuses on the milieu in which Dart's paper appeared (i.e. what was understood in 1925 about human evolution), the fossil evidence as set out by Dart, his interpretation of how a species represented by a fossilized juvenile's skull fitted within prevailing narratives about human evolution and the significance of the fossil being found in an environment inferred to be very different from that occupied by living apes. We also briefly review subsequent fossil finds that have corroborated the argument Dart made for having discovered evidence of a hitherto unknown close relative of humans, and summarize our current understanding of the earliest stages of human evolution and its environmental context.
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Affiliation(s)
- John Rowan
- Department of Archaeology, University of Cambridge, CambridgeCB2 3DZ, UK
| | - Bernard Wood
- CASHP, Department of Anthropology, George Washington University, Washington, DC20052, USA
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2
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Finestone EM, Plummer TW, Vincent TH, Blumenthal SA, Ditchfield PW, Bishop LC, Oliver JS, Herries AIR, Palfery CV, Lane TP, McGuire E, Reeves JS, Rodés A, Whitfield E, Braun DR, Bartilol SK, Rotich NK, Parkinson JA, Lemorini C, Caricola I, Kinyanjui RN, Potts R. New Oldowan locality Sare-Abururu (ca. 1.7 Ma) provides evidence of diverse hominin behaviors on the Homa Peninsula, Kenya. J Hum Evol 2024; 190:103498. [PMID: 38581918 DOI: 10.1016/j.jhevol.2024.103498] [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: 05/30/2023] [Revised: 01/18/2024] [Accepted: 01/18/2024] [Indexed: 04/08/2024]
Abstract
The Homa Peninsula, in southwestern Kenya, continues to yield insights into Oldowan hominin landscape behaviors. The Late Pliocene locality of Nyayanga (∼3-2.6 Ma) preserves some of the oldest Oldowan tools. At the Early Pleistocene locality of Kanjera South (∼2 Ma) toolmakers procured a diversity of raw materials from over 10 km away and strategically reduced them in a grassland-dominated ecosystem. Here, we report findings from Sare-Abururu, a younger (∼1.7 Ma) Oldowan locality approximately 12 km southeast of Kanjera South and 18 km east of Nyayanga. Sare-Abururu has yielded 1754 artifacts in relatively undisturbed low-energy silts and sands. Stable isotopic analysis of pedogenic carbonates suggests that hominin activities were carried out in a grassland-dominated setting with similar vegetation structure as documented at Kanjera South. The composition of a nearby paleo-conglomerate indicates that high-quality stone raw materials were locally abundant. Toolmakers at Sare-Abururu produced angular fragments from quartz pebbles, representing a considerable contrast to the strategies used to reduce high quality raw materials at Kanjera South. Although lithic reduction at Sare-Abururu was technologically simple, toolmakers proficiently produced cutting edges, made few mistakes and exhibited a mastery of platform management, demonstrating that expedient technical strategies do not necessarily indicate a lack of skill or suitable raw materials. Lithic procurement and reduction patterns on the Homa Peninsula appear to reflect variation in local resource contexts rather than large-scale evolutionary changes in mobility, energy budget, or toolmaker cognition.
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Affiliation(s)
- Emma M Finestone
- Department of Anthropology, Cleveland Museum of Natural History, 1 Wade Oval Dr, Cleveland, OH, 44113, United States; Department of Archaeology, Max Planck Institute for Geoanthropology, Kahlaische Str. 10, 07745, Jena, Germany.
| | - Thomas W Plummer
- Department of Anthropology, Queens College, 314 Powdermaker Hall 65-30 Kissena Boulevard Flushing, Flushing, NY, 11367, United States; The CUNY Graduate Center, 365 5th Ave, New York, NY, 10016, United States; Human Origins Program, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC, 20560, United States
| | - Thomas H Vincent
- Research Centre in Evolutionary Anthropology and Palaeoecology, School of Biological and Environmental Sciences, Liverpool John Moores University, Byrom Street, Liverpool, L3 3AF, United Kingdom
| | - Scott A Blumenthal
- Human Origins Program, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC, 20560, United States; Department of Anthropology, University of Oregon, 1585 East 13th Avenue, Eugene, OR, 97403, United States; Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020 - 2207 Main Mall, Vancouver, BC V6T 1Z4, Canada
| | - Peter W Ditchfield
- School of Archaeology, University of Oxford, 1 S Parks Rd, Oxford, OX1 3TG, United Kingdom
| | - Laura C Bishop
- Research Centre in Evolutionary Anthropology and Palaeoecology, School of Biological and Environmental Sciences, Liverpool John Moores University, Byrom Street, Liverpool, L3 3AF, United Kingdom
| | - James S Oliver
- Anthropology Section, Illinois State Museum, 502 S Spring St, Springfield, IL, 62706, United States
| | - Andy I R Herries
- The Australian Archaeomagnetism Laboratory, Department Archaeology and History, La Trobe University, Melbourne Victoria, 3086, Australia; Paleo-Research Institute, University of Johannesburg, 42 Bunting Rd, Cottesloe, Johannesburg, 2092, South Africa
| | - Christopher Vere Palfery
- The Australian Archaeomagnetism Laboratory, Department Archaeology and History, La Trobe University, Melbourne Victoria, 3086, Australia
| | - Timothy P Lane
- Geography and Environmental Science Research Group, School of Biological and Environmental Sciences, Liverpool John Moores University, Byrom Street, Liverpool, L3 3AF, United Kingdom
| | - Elizabeth McGuire
- Department of Anthropology, University of Oregon, 1585 East 13th Avenue, Eugene, OR, 97403, United States
| | - Jonathan S Reeves
- Technological Origins Research Group, Max Planck Institute for Evolutionary Anthropology, Deutscher Pl. 6, 04103, Leipzig, Germany; Center for the Advanced Study of Human Paleobiology, George Washington University, 800 22nd Street NW, Washington, DC, 20052, United States
| | - Angel Rodés
- Departamento de Xeografía, Universidade de Santiago de Compostela, Praza da Universidade,1, 15703 Santiago de Compostela, Spain; Scottish Universities Environmental Research Centre, University of Glasgow, Rankine Ave, Scottish Enterprise Technology Park, East Kilbride G75 0QF, United Kingdom
| | - Elizabeth Whitfield
- Research Centre in Evolutionary Anthropology and Palaeoecology, School of Biological and Environmental Sciences, Liverpool John Moores University, Byrom Street, Liverpool, L3 3AF, United Kingdom
| | - David R Braun
- Technological Origins Research Group, Max Planck Institute for Evolutionary Anthropology, Deutscher Pl. 6, 04103, Leipzig, Germany; Center for the Advanced Study of Human Paleobiology, George Washington University, 800 22nd Street NW, Washington, DC, 20052, United States
| | - Simion K Bartilol
- Institute of Nuclear Science and Technology, University of Nairobi, P.O. Box 30197, Nairobi, Kenya
| | - Nelson Kiprono Rotich
- Institute of Nuclear Science and Technology, University of Nairobi, P.O. Box 30197, Nairobi, Kenya; Institute of Nuclear Chemistry and Technology, Dorodna 16, 03-195, Warsaw, Poland
| | - Jennifer A Parkinson
- Human Origins Program, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC, 20560, United States; Department of Anthropology, University of San Diego, 5998 Alcala Park Way, San Diego, CA, 92110, United States
| | - Cristina Lemorini
- LTFAPA Laboratory, Department of Science of Antiquities, Sapienza University of Rome, Piazzale Aldo Moro 5, 00185, Rome, Italy
| | - Isabella Caricola
- LTFAPA Laboratory, Department of Science of Antiquities, Sapienza University of Rome, Piazzale Aldo Moro 5, 00185, Rome, Italy; Zinman Institute of Archaeology, Haifa University, 199 Aba Hushi Avenue, Mount Carmel, Haifa, 3498838, Israel
| | - Rahab N Kinyanjui
- Department of Archaeology, Max Planck Institute for Geoanthropology, Kahlaische Str. 10, 07745, Jena, Germany; Human Origins Program, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC, 20560, United States; Department of Earth Sciences, National Museums of Kenya, Kipande Rd, Nairobi, Kenya
| | - Richard Potts
- Human Origins Program, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC, 20560, United States; Department of Earth Sciences, National Museums of Kenya, Kipande Rd, Nairobi, Kenya
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3
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Norwood AL, Wang B, Kingston JD. Linking African herbivore community enamel isotopes and environments: challenges, opportunities, and paleoecological implications. Oecologia 2024; 204:467-489. [PMID: 38517529 DOI: 10.1007/s00442-024-05532-z] [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: 06/17/2023] [Accepted: 02/18/2024] [Indexed: 03/24/2024]
Abstract
Paleoenvironmental reconstructions of fossil sites based on isotopic analyses of enamel typically rely on data from multiple herbivore taxa, with the assumption that this dietary spectrum represents the community's isotopic range and provides insights into local or regional vegetation patterns. However, it remains unclear how representative the sampled taxa are of the broader herbivore community and how well these data correspond to specific ecosystems. Verifying these underlying assumptions is essential to refining the utility of enamel isotopic values for paleoenvironmental reconstructions. This study explores potential links between modern herbivore community carbon isotopic enamel spectra, biome types, and climate in sub-Saharan Africa. This region is one of the most comprehensively isotopically sampled areas globally and is of particular relevance to hominin evolution. Our extensive data compilation reveals that published enamel isotopic data from sub-Saharan Africa typically sample only a small percentage of the taxa documented at most localities and that some biome types (e.g., subtropical savannas) are dramatically overrepresented relative to others (e.g., forests) in these modern data sets. Multiple statistical analyses, including linear models and cluster analyses, revealed weak relationships of associated mammalian herbivore enamel isotopic values, biome type, and climate parameters. These results confound any simple assumptions about how community isotopic profiles map onto specific environments, highlighting the need for more precise strategic approaches in extending isotopic frameworks into the past for paleoecological reconstructions. Developing more refined modern analogs will ultimately allow us to more accurately characterize the isotopic spectra of paleo-communities and link isotopic dietary signatures to specific ecosystems.
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Affiliation(s)
| | - Bian Wang
- Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China
| | - John D Kingston
- Department of Anthropology, University of Michigan, Ann Arbor, USA
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4
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Foister TIF, Žliobaitė I, Wilson OE, Fortelius M, Tallavaara M. Homo heterogenus: Variability in early Pleistocene Homo environments. Evol Anthropol 2023; 32:373-385. [PMID: 37877200 DOI: 10.1002/evan.22005] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/08/2023] [Revised: 08/29/2023] [Accepted: 09/05/2023] [Indexed: 10/26/2023]
Abstract
To understand the ecological dominance of Homo sapiens, we need to investigate the origins of the plasticity that has enabled our colonization of the planet. We can approach this by exploring the variability of habitats to which different hominin populations have adapted over time. In this article, we draw upon and synthesize the current research on habitats of genus Homo during the early Pleistocene. We examined 121 published environmental reconstructions from 74 early Pleistocene sites or site phases to assess the balance of arguments in the research community. We found that, while grasslands and savannahs were prominent features of Homo habitats in the early Pleistocene, current research does not place early Pleistocene Homo, in any single environmental type, but in a wide variety of environments, ranging from open grasslands to forests. Our analysis also suggests that the first known dispersal of Homo out of Africa was accompanied by niche expansion.
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Affiliation(s)
- Tegan I F Foister
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
| | - Indrė Žliobaitė
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
- Department of Computer Science, University of Helsinki, Helsinki, Finland
- Finnish Museum of Natural History, LUOMUS, Helsinki, Finland
| | - Oscar E Wilson
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
| | - Mikael Fortelius
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
- Finnish Museum of Natural History, LUOMUS, Helsinki, Finland
| | - Miikka Tallavaara
- Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
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5
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Archer W, Presnyakova D, Aldeias V, Colarossi D, Hutten L, Lauer T, Porraz G, Rossouw L, Shaw M. Late Acheulean occupations at Montagu Cave and the pattern of Middle Pleistocene behavioral change in Western Cape, southern Africa. J Hum Evol 2023; 184:103435. [PMID: 37774470 DOI: 10.1016/j.jhevol.2023.103435] [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: 03/01/2023] [Revised: 08/29/2023] [Accepted: 08/30/2023] [Indexed: 10/01/2023]
Abstract
Patterns of so-called modern human behavior are increasingly well documented in an abundance of Middle Stone Age archaeological sites across southern Africa. Contextualized archives directly preceding the southern African Middle Stone Age, however, remain scarce. Current understanding of the terminal Acheulean in southern Africa derives from a small number of localities that are predominantly in the central and northern interior. Many of these localities are surface and deflated contexts, others were excavated prior to the availability of modern field documentation techniques, and yet other relevant assemblages contain low numbers of characteristic artifacts relative to volume of excavated deposit. The site of Montagu Cave, situated in the diverse ecosystem of the Cape Floral Region, South Africa, contains the rare combination of archaeologically rich, laminated and deeply stratified Acheulean layers followed by a younger Middle Stone Age occupation. Yet little is known about the site owing largely to a lack of contextual information associated with the early excavations. Here we present renewed excavation of Levels 21-22 at Montagu Cave, located in the basal Acheulean sequence, including new data on site formation and ecological context, geochronology, and technological variability. We document intensive occupation of the cave by Acheulean tool-producing hominins, likely at the onset of interglacial conditions in MIS 7. New excavations at Montagu Cave suggest that, while Middle Stone Age technologies were practiced by 300 ka in several other regions of Africa, the classic Acheulean persisted later in the Fynbos Biome of the southwestern Cape. We discuss the implications of this regionalized persistence for the biogeography of African later Middle Pleistocene hominin populations, for the ecological drivers of their technological systems, and for the pattern and pace of behavioral change just prior to the proliferation of the southern African later Middle Stone Age.
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Affiliation(s)
- Will Archer
- Max Planck Partner Group, Department of Archaeology and Anthropology, National Museum, Bloemfontein, South Africa; Department of Geology, University of the Free State, Bloemfontein, South Africa.
| | - Darya Presnyakova
- Department of Early Prehistory and Quaternary Ecology, University of Tübingen, Tübingen, Germany; Aix-Marseille Université, CNRS, UMR 7269, Laboratoire Méditerranéen de Préhistoire Europe Afrique (LAMPEA), Aix-en Provence, France
| | - Vera Aldeias
- Interdisciplinary Center for Archaeology and the Evolution of Human Behaviour (ICArEHB), University of Algarve, Faro, Portugal
| | - Debra Colarossi
- Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, Wales, United Kingdom
| | - Louisa Hutten
- Department of Archaeology, University of Cape Town, South Africa
| | - Tobias Lauer
- Department of Geosciences, University of Tübingen, Tübingen, Germany
| | - Guillaume Porraz
- Aix-Marseille Université, CNRS, UMR 7269, Laboratoire Méditerranéen de Préhistoire Europe Afrique (LAMPEA), Aix-en Provence, France
| | - Lloyd Rossouw
- Florisbad Quaternary Research Department, National Museum, Bloemfontein, South Africa
| | - Matthew Shaw
- Centre for Archaeological Science, School of Earth, Atmospheric, and Life Sciences, University of Wollongong, Australia
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6
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MacLatchy LM, Cote SM, Deino AL, Kityo RM, Mugume AAT, Rossie JB, Sanders WJ, Cosman MN, Driese SG, Fox DL, Freeman AJ, Jansma RJW, Jenkins KEH, Kinyanjui RN, Lukens WE, McNulty KP, Novello A, Peppe DJ, Strömberg CAE, Uno KT, Winkler AJ, Kingston JD. The evolution of hominoid locomotor versatility: Evidence from Moroto, a 21 Ma site in Uganda. Science 2023; 380:eabq2835. [PMID: 37053310 DOI: 10.1126/science.abq2835] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 04/15/2023]
Abstract
Living hominoids are distinguished by upright torsos and versatile locomotion. It is hypothesized that these features evolved for feeding on fruit from terminal branches in forests. To investigate the evolutionary context of hominoid adaptive origins, we analyzed multiple paleoenvironmental proxies in conjunction with hominoid fossils from the Moroto II site in Uganda. The data indicate seasonally dry woodlands with the earliest evidence of abundant C4 grasses in Africa based on a confirmed age of 21 million years ago (Ma). We demonstrate that the leaf-eating hominoid Morotopithecus consumed water-stressed vegetation, and postcrania from the site indicate ape-like locomotor adaptations. These findings suggest that the origin of hominoid locomotor versatility is associated with foraging on leaves in heterogeneous, open woodlands rather than forests.
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Affiliation(s)
- Laura M MacLatchy
- Department of Anthropology, University of Michigan, Ann Arbor, MI 48109, USA
- Museum of Paleontology, University of Michigan, Ann Arbor, MI 48109, USA
| | - Susanne M Cote
- Department of Anthropology and Archaeology, University of Calgary, Calgary, Alberta T2N 1N4, Canada
| | - Alan L Deino
- Berkeley Geochronology Center, Berkeley, CA 94709, USA
| | - Robert M Kityo
- Department of Zoology, Entomology and Fisheries Sciences, Makerere University, Kampala, Uganda
| | - Amon A T Mugume
- Department of Zoology, Entomology and Fisheries Sciences, Makerere University, Kampala, Uganda
- Uganda National Museum, Department of Museums and Monuments, Ministry of Tourism, Wildlife and Antiquities, Kampala, Uganda
| | - James B Rossie
- Department of Anthropology, Stony Brook University, Stony Brook, NY 11794, USA
| | - William J Sanders
- Department of Anthropology, University of Michigan, Ann Arbor, MI 48109, USA
- Museum of Paleontology, University of Michigan, Ann Arbor, MI 48109, USA
| | - Miranda N Cosman
- Department of Anthropology, University of Michigan, Ann Arbor, MI 48109, USA
| | - Steven G Driese
- Department of Geosciences, Baylor University, Waco, TX 76798, USA
| | - David L Fox
- Department of Earth & Environmental Sciences, University of Minnesota, Minneapolis, MN 55455, USA
| | - April J Freeman
- Department of Geosciences, Baylor University, Waco, TX 76798, USA
| | - Rutger J W Jansma
- Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85281, USA
| | - Kirsten E H Jenkins
- Department of Social Sciences, Tacoma Community College, Tacoma, WA 98466, USA
| | - Rahab N Kinyanjui
- Earth Sciences Department, National Museums of Kenya, Nairobi, Kenya
- Max Planck Institute for Geoanthropology, Jena D-07743, Germany
- Human Origins Program, National Museum of Natural History, Smithsonian Institution, Washington, DC 20013, USA
| | - William E Lukens
- Department of Geology & Environmental Science, James Madison University, Harrisonburg, VA 22807, USA
| | - Kieran P McNulty
- Department of Anthropology, University of Minnesota, Minneapolis, MN 55455, USA
| | - Alice Novello
- CEREGE, Aix-Marseille Université, CNRS, IRD, Collège de France, INRAE, Aix en Provence, France
- Department of Biology & Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195, USA
| | - Daniel J Peppe
- Department of Geosciences, Baylor University, Waco, TX 76798, USA
| | - Caroline A E Strömberg
- Department of Biology & Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195, USA
| | - Kevin T Uno
- Division of Biology and Paleo Environment, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA
| | - Alisa J Winkler
- Roy M. Huffington Department of Earth Sciences, Southern Methodist University, Dallas, TX 75275, USA
- Section of Anatomy, Department of Surgery, University of Texas Southwestern Medical Center, Dallas, TX 75390, USA
| | - John D Kingston
- Department of Anthropology, University of Michigan, Ann Arbor, MI 48109, USA
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7
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Negash EW, Barr WA. Relative abundance of grazing and browsing herbivores is not a direct reflection of vegetation structure: Implications for hominin paleoenvironmental reconstruction. J Hum Evol 2023; 177:103328. [PMID: 36857987 DOI: 10.1016/j.jhevol.2023.103328] [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: 06/17/2022] [Revised: 01/23/2023] [Accepted: 01/23/2023] [Indexed: 03/03/2023]
Abstract
The diet of fossil herbivores inferred from enamel stable carbon isotopes is often used to make paleoenvironmental reconstructions. While many studies have focused on using environmental indicator taxa to make paleoenvironmental reconstructions, community-based approaches are considered to provide a more complete picture of paleolandscapes. These studies assume that the diet and relative abundance of herbivores are related to the areal extent of different vegetation types on the landscape. Here, we quantitatively test this assumption in 16 modern ecosystems in eastern and southern Africa with a wide range of woody vegetation cover. We conducted a landscape-level spatial analysis of vegetation patterns using a published land cover data set and computed landscape metrics. We compiled data on relative abundance and diet of herbivores inferred from carbon isotope studies for all large herbivores in these ecosystems. We found that despite differences in the total areal extent of different vegetation types, numerous sizable patches of each vegetation type are available in most ecosystems. However, despite variation across the ecosystems examined, grazers are typically the most abundant herbivores even in sites that have a higher proportion of forest and shrub cover. This indicates that the diet and relative abundance of herbivores is not a simple reflection of the total areal extent of vegetation types available on the landscape. The higher proportion of grazers observed in these ecosystems is a result of multiple factors including habitat heterogeneity, differences in biomass turnover rate between grasses and woody vegetation, resource partitioning, and the advantages of group living in open environments. Comparison of diet and relative abundance of herbivores in modern ecosystems to fossil herbivore assemblages shows that very different vegetation regimes can support similar herbivore assemblages. This study has significant implications for paleolandscape reconstructions and cautions against a simplistic wooded vs. grassland paleoenvironmental interpretations based on fossil herbivore assemblages.
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Affiliation(s)
- Enquye W Negash
- Center for the Advanced Study of Human Paleobiology, George Washington University, 800 22nd Street, Northwest, Washington D.C. 20052, USA.
| | - W Andrew Barr
- Center for the Advanced Study of Human Paleobiology, George Washington University, 800 22nd Street, Northwest, Washington D.C. 20052, USA
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8
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Townsend C, Ferraro JV, Habecker H, Flinn MV. Human cooperation and evolutionary transitions in individuality. Philos Trans R Soc Lond B Biol Sci 2023; 378:20210414. [PMID: 36688393 PMCID: PMC9869453 DOI: 10.1098/rstb.2021.0414] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/24/2023] Open
Abstract
A major evolutionary transition in individuality involves the formation of a cooperative group and the transformation of that group into an evolutionary entity. Human cooperation shares principles with those of multicellular organisms that have undergone transitions in individuality: division of labour, communication, and fitness interdependence. After the split from the last common ancestor of hominoids, early hominins adapted to an increasingly terrestrial niche for several million years. We posit that new challenges in this niche set in motion a positive feedback loop in selection pressure for cooperation that ratcheted coevolutionary changes in sociality, communication, brains, cognition, kin relations and technology, eventually resulting in egalitarian societies with suppressed competition and rapid cumulative culture. The increasing pace of information innovation and transmission became a key aspect of the evolutionary niche that enabled humans to become formidable cooperators with explosive population growth, the ability to cooperate and compete in groups of millions, and emergent social norms, e.g. private property. Despite considerable fitness interdependence, the rise of private property, in concert with population explosion and socioeconomic inequality, subverts potential transition of human groups into evolutionary entities due to resurgence of latent competition and conflict. This article is part of the theme issue 'Human socio-cultural evolution in light of evolutionary transitions'.
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Affiliation(s)
- Cathryn Townsend
- Department of Anthropology, Baylor University, Waco, TX 76798-7334, USA
| | - Joseph V. Ferraro
- Department of Anthropology, Baylor University, Waco, TX 76798-7334, USA
| | - Heather Habecker
- Department of Psychology and Neuroscience, Baylor University, Waco, TX 76798-7334, USA
| | - Mark V. Flinn
- Department of Anthropology, Baylor University, Waco, TX 76798-7334, USA
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9
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Plio-Pleistocene environmental variability in Africa and its implications for mammalian evolution. Proc Natl Acad Sci U S A 2022; 119:e2107393119. [PMID: 35412903 PMCID: PMC9169865 DOI: 10.1073/pnas.2107393119] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022] Open
Abstract
We have developed an Africa-wide synthesis of paleoenvironmental variability over the Plio-Pleistocene. We show that there is strong evidence for orbital forcing of variability during this time that is superimposed on a longer trend of increasing environmental variability, supporting a combination of both low- and high-latitude drivers of variability. We combine these results with robust estimates of mammalian speciation and extinction rates and find that variability is not significantly correlated with these rates. These findings do not currently support a link between environmental variability and turnover and thus fail to corroborate predictions derived from the variability selection hypothesis. Understanding the climatic drivers of environmental variability (EV) during the Plio-Pleistocene and EV’s influence on mammalian macroevolution are two outstanding foci of research in African paleoclimatology and evolutionary biology. The potential effects of EV are especially relevant for testing the variability selection hypothesis, which predicts a positive relationship between EV and speciation and extinction rates in fossil mammals. Addressing these questions is stymied, however, by 1) a lack of multiple comparable EV records of sufficient temporal resolution and duration, and 2) the incompleteness of the mammalian fossil record. Here, we first compile a composite history of Pan-African EV spanning the Plio-Pleistocene, which allows us to explore which climatic variables influenced EV. We find that EV exhibits 1) a long-term trend of increasing variability since ∼3.7 Ma, coincident with rising variability in global ice volume and sea surface temperatures around Africa, and 2) a 400-ky frequency correlated with seasonal insolation variability. We then estimate speciation and extinction rates for fossil mammals from eastern Africa using a method that accounts for sampling variation. We find no statistically significant relationship between EV and estimated speciation or extinction rates across multiple spatial scales. These findings are inconsistent with the variability selection hypothesis as applied to macroevolutionary processes.
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10
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A chimpanzee enamel-diet δ 13C enrichment factor and a refined enamel sampling strategy: Implications for dietary reconstructions. J Hum Evol 2021; 159:103062. [PMID: 34536662 DOI: 10.1016/j.jhevol.2021.103062] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/08/2020] [Revised: 08/01/2021] [Accepted: 08/01/2021] [Indexed: 11/24/2022]
Abstract
Reconstructing diets from stable carbon isotopic signals in enamel bioapatite requires the application of a δ13C enamel-diet enrichment factor, or the isotopic offset between diet and enamel, which has not been empirically determined for any primate. In this study, an enamel-diet enrichment factor (ε∗enamel-diet) of 11.8 ± 0.3‰ is calculated for chimpanzees (Pan troglodytes) at Ngogo in Kibale National Park, Uganda, based on a comprehensive isotopic assessment of previously analyzed dietary plant data and new isotopic analyses of enamel apatite. Different enamel sampling methods are evaluated to determine the potential influence of weaning on isotopic enamel values and dietary interpretations. The new chimpanzee enrichment factor and a sampling strategy that excludes teeth that formed before weaning completion are applied to all known chimpanzee δ13Cenamel data, either previously published or newly derived in this study, resulting in a dietary range of almost 6‰ across all chimpanzees sampled. This new chimpanzee enamel-diet enrichment factor is then used to reassess dietary reconstructions of 12 fossil hominin species whose isotopic enamel signatures have been determined. Results reveal hominin diets that are isotopically more positive than previously reconstructed, highlighting the widespread contribution of 13C-enriched C4/crassulacean acid metabolism (CAM) resources in fossil hominin diets and emphasizing the broad use of these resources during human evolution. These findings stress the importance of ascertaining and employing an appropriate enrichment factor for dietary reconstructions of specific taxa as well as standardizing the sampling protocol for tooth enamel in isotopic paleodietary reconstructions.
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11
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Hunt KD, Dunevant SE, Yohler RM, Carlson KJ. Femoral Bicondylar Angles among Dry-Habitat Chimpanzees ( Pan troglodytes schweinfurthii) Resemble Those of Humans: Implications for Knee Function, Australopith Sexual Dimorphism, and the Evolution of Bipedalism. JOURNAL OF ANTHROPOLOGICAL RESEARCH 2021. [DOI: 10.1086/715398] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
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12
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Faith JT, Du A, Behrensmeyer AK, Davies B, Patterson DB, Rowan J, Wood B. Rethinking the ecological drivers of hominin evolution. Trends Ecol Evol 2021; 36:797-807. [PMID: 34059368 DOI: 10.1016/j.tree.2021.04.011] [Citation(s) in RCA: 17] [Impact Index Per Article: 5.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/10/2021] [Revised: 04/21/2021] [Accepted: 04/26/2021] [Indexed: 11/19/2022]
Abstract
A central goal of paleoanthropology is understanding the role of ecological change in hominin evolution. Over the past several decades researchers have expanded the hominin fossil record and assembled detailed late Cenozoic paleoclimatic, paleoenvironmental, and paleoecological archives. However, effective use of these data is precluded by the limitations of pattern-matching strategies for inferring causal relationships between ecological and evolutionary change. We examine several obstacles that have hindered progress, and highlight recent research that is addressing them by (i) confronting an incomplete fossil record, (ii) contending with datasets spanning varied spatiotemporal scales, and (iii) using theoretical frameworks to build stronger inferences. Expanding on this work promises to transform challenges into opportunities and set the stage for a new phase of paleoanthropological research.
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Affiliation(s)
- J Tyler Faith
- Natural History Museum of Utah, University of Utah, Salt Lake City, UT 84108, USA; Department of Anthropology, University of Utah, Salt Lake City, UT 84112, USA.
| | - Andrew Du
- Department of Anthropology and Geography, Colorado State University, Fort Collins, CO 80523, USA
| | - Anna K Behrensmeyer
- Department of Paleobiology, National Museum of Natural History, Washington, DC 20013, USA
| | - Benjamin Davies
- Department of Anthropology, University of Utah, Salt Lake City, UT 84112, USA
| | - David B Patterson
- Department of Biology, University of North Georgia, Dahlonega, GA 30597, USA
| | - John Rowan
- Department of Anthropology, University at Albany, Albany, NY 12222, USA
| | - Bernard Wood
- Center for the Advanced Study of Human Paleobiology, The George Washington University, Washington, DC 20052, USA
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13
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Intrataxonomic trends in herbivore enamel δ 13C are decoupled from ecosystem woody cover. Nat Ecol Evol 2021; 5:995-1002. [PMID: 33941906 DOI: 10.1038/s41559-021-01455-7] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/23/2020] [Accepted: 03/25/2021] [Indexed: 11/08/2022]
Abstract
Analysis of enamel stable carbon isotopes (δ13Cenamel) of fossil herbivores is an important tool for making inferences about Plio-Pleistocene vegetation structure in Africa and the environmental context of hominin evolution. Many palaeoecological studies implicitly or explicitly assume that individual variation in C3-C4 plant consumption among fossil herbivores directly reflects the abundance of C3 (trees, shrubs) or C4 (low-altitude tropical grasses) vegetation. However, a strong link between δ13Cenamel of herbivores and ecosystem vegetation structure has not been rigorously established. Here we combine δ13Cenamel data from a large dataset (n = 1,643) with multidecadal Landsat estimates of C3 woody cover across 30 African ecosystems to show that there is little relationship between intrataxonomic variation in δ13Cenamel and vegetation structure. This is especially true when removing forested ecosystems (>80% woody cover)-which numerous lines of evidence suggest are rare in the Plio-Pleistocene fossil record of eastern Africa-from our analyses. Our findings stand in contrast with the common assumption that variation in herbivore δ13Cenamel values reflects changes in the relative abundance of C3-C4 vegetation. We conclude that analyses using herbivore δ13Cenamel data to shed light on the environmental context of hominin evolution should look to explicitly community-level approaches for making vegetation inferences.
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14
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Braun DR, Faith JT, Douglass MJ, Davies B, Power MJ, Aldeias V, Conard NJ, Cutts R, DeSantis LRG, Dupont LM, Esteban I, Kandel AW, Levin NE, Luyt J, Parkington J, Pickering R, Quick L, Sealy J, Stynder D. Ecosystem engineering in the Quaternary of the West Coast of South Africa. Evol Anthropol 2021; 30:50-62. [PMID: 33604991 DOI: 10.1002/evan.21886] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/01/2019] [Revised: 06/30/2020] [Accepted: 12/22/2020] [Indexed: 11/09/2022]
Abstract
Despite advances in our understanding of the geographic and temporal scope of the Paleolithic record, we know remarkably little about the evolutionary and ecological consequences of changes in human behavior. Recent inquiries suggest that human evolution reflects a long history of interconnections between the behavior of humans and their surrounding ecosystems (e.g., niche construction). Developing expectations to identify such phenomena is remarkably difficult because it requires understanding the multi-generational impacts of changes in behavior. These long-term dynamics require insights into the emergent phenomena that alter selective pressures over longer time periods which are not possible to observe, and are also not intuitive based on observations derived from ethnographic time scales. Generative models show promise for probing these potentially unexpected consequences of human-environment interaction. Changes in the uses of landscapes may have long term implications for the environments that hominins occupied. We explore other potential proxies of behavior and examine how modeling may provide expectations for a variety of phenomena.
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Affiliation(s)
- David R Braun
- The George Washington University, Center for the Advanced Study of Human Paleobiology, Washington, District of Columbia, USA.,Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany
| | - John Tyler Faith
- Natural History Museum of Utah, University of Utah, Salt Lake City, Utah, USA.,Department of Anthropology, University of Utah, Salt Lake City, Utah, USA
| | - Matthew J Douglass
- College of Agricultural Sciences and Natural Resources, University of Nebraska-Lincoln, Lincoln, Nebraska, USA.,Agricultural Research Division, University of Nebraska-Lincoln, Lincoln, Nebraska, USA
| | - Benjamin Davies
- Natural History Museum of Utah, University of Utah, Salt Lake City, Utah, USA
| | - Mitchel J Power
- Natural History Museum of Utah, University of Utah, Salt Lake City, Utah, USA.,Department of Geography, Natural History Museum of Utah, University of Utah, Salt Lake City, Utah, USA
| | - Vera Aldeias
- Interdisciplinary Center for Archaeology and Evolution of Human Behaviour (ICArEHB), Universidade do Algarve, Faro, Portugal
| | - Nicholas J Conard
- Department of Early Prehistory and Quaternary Ecology, University of Tübingen, Schloss Hohentübingen, Tübingen, Germany
| | - Russell Cutts
- Emory University-Oxford College, History and Social Sciences (Anthropology), Oxford, Georgia, USA
| | - Larisa R G DeSantis
- Department of Biological Sciences, Vanderbilt University, Nashville, Tennessee, USA
| | - Lydie M Dupont
- MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
| | - Irene Esteban
- Evolutionary Studies Institute, University of Witwatersrand, Johannesburg, South Africa
| | - Andrew W Kandel
- The Role of Culture in Early Expansions of Humans, Heidelberg Academy of Sciences and Humanities, Tübingen, Germany
| | - Naomi E Levin
- Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan, USA
| | - Julie Luyt
- Department of Archaeology, University of Cape Town, Cape Town, South Africa
| | - John Parkington
- Department of Archaeology, University of Cape Town, Cape Town, South Africa
| | - Robyn Pickering
- Department of Geological Science, University of Cape Town, Cape Town, Western Cape, South Africa.,Human Evolution Research Institute, University of Cape Town, Cape Town, Western Cape, South Africa
| | - Lynne Quick
- African Centre for Coastal Palaeoscience, Nelson Mandela University, Port Elizabeth, South Africa
| | - Judith Sealy
- Department of Archaeology, University of Cape Town, Cape Town, South Africa
| | - Deano Stynder
- Department of Archaeology, University of Cape Town, Cape Town, South Africa
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15
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van der Merwe PDW, Cotterill FPD, Kandziora M, Watters BR, Nagy B, Genade T, Flügel TJ, Svendsen DS, Bellstedt DU. Genomic fingerprints of palaeogeographic history: The tempo and mode of rift tectonics across tropical Africa has shaped the diversification of the killifish genus Nothobranchius (Teleostei: Cyprinodontiformes). Mol Phylogenet Evol 2020; 158:106988. [PMID: 33059071 DOI: 10.1016/j.ympev.2020.106988] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/28/2020] [Revised: 09/16/2020] [Accepted: 10/07/2020] [Indexed: 01/04/2023]
Abstract
This paper reports a phylogeny of the African killifishes (Genus Nothobranchius, Order Cyprinodontiformes) informed by five genetic markers (three nuclear, two mitochondrial) of 80 taxa (seven undescribed and 73 of the 92 recognized species). These short-lived annual fishes occupy seasonally wet habitats in central and eastern Africa, and their distribution coincides largely with the East African Rift System (EARS). The fossil dates of sister clades used to constrain a chronometric tree of all sampled Nothobranchius recovered the origin of the genus at ~13.27 Mya. It was followed by the radiations of six principal clades through the Neogene. An ancestral area estimation tested competing biogeographical hypotheses to constrain the ancestral origin of the genus to the Nilo-Sudan Ecoregion, which seeded a mid-Miocene dispersal event into the Coastal ecoregion, followed closely (~10 Mya) by dispersals southward across the Mozambique coastal plain into the Limpopo Ecoregion. Extending westwards across the Tanzanian plateau, a pulse of radiations through the Pliocene were associated with dispersals and fragmentation of wetlands across the Kalahari and Uganda Ecoregions. We interpret this congruence of drainage rearrangements with dispersals and cladogenic events of Nothobranchius to reflect congruent responses to recurrent uplift and rifting. The coevolution of these freshwater fishes and wetlands is attributed to ultimate control by tectonics, as the EARS extended southwards during the Neogene. Geobiological consilience of the combined evidence supports a tectonic hypothesis for the evolution of Nothobranchius.
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Affiliation(s)
| | | | - Martha Kandziora
- Department of Botany, Faculty of Science, Charles University, Prague, Czech Republic
| | - Brian R Watters
- 6141 Parkwood Drive, Nanaimo, British Columbia V9T6A2, Canada
| | - Béla Nagy
- 30, Rue du Mont Ussy, 77300 Fontainebleau, France
| | - Tyrone Genade
- Biomedical Sciences, East Tennessee State University, USA
| | - Tyrel J Flügel
- Department of Geography and Environmental Studies, Stellenbosch University, South Africa
| | - David S Svendsen
- Department of Geography and Environmental Studies, Stellenbosch University, South Africa
| | - Dirk U Bellstedt
- Department of Biochemistry, Stellenbosch University, South Africa.
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16
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Diets of mammalian fossil fauna from Kanapoi, northwestern Kenya. J Hum Evol 2020; 140:102338. [DOI: 10.1016/j.jhevol.2017.05.005] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/02/2016] [Revised: 04/27/2017] [Accepted: 05/04/2017] [Indexed: 11/19/2022]
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17
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Revisiting the pedogenic carbonate isotopes and paleoenvironmental interpretation of Kanapoi. J Hum Evol 2020; 140:102549. [DOI: 10.1016/j.jhevol.2018.11.005] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/14/2016] [Revised: 09/15/2018] [Accepted: 11/06/2018] [Indexed: 11/18/2022]
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18
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Swedell L, Plummer T. Social evolution in Plio-Pleistocene hominins: Insights from hamadryas baboons and paleoecology. J Hum Evol 2019; 137:102667. [PMID: 31629289 DOI: 10.1016/j.jhevol.2019.102667] [Citation(s) in RCA: 19] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/31/2019] [Revised: 08/21/2019] [Accepted: 08/23/2019] [Indexed: 11/16/2022]
Abstract
Reconstructions of hominin evolution have long benefited from comparisons with nonhuman primates, especially baboons and chimpanzees. The hamadryas baboon (Papio hamadryas) is arguably one of the best such models, as it exhibits both the male kin bonding and the cross-sex pair bonding thought to have been important in hominin evolution. Here we link processes of behavioral evolution in hamadryas baboons with those in a Plio-Pleistocene hominin, provisionally identified as Homo erectus (sensu lato) - a pivotal species in that its larger body and brain size and wider ranging patterns increased female costs of reproduction, increasing the importance of sociality. The combination of these higher costs of reproduction and shifts in diet and food acquisition have previously been argued to have been alleviated either via strengthening of male-female bonds (involving male provisioning and the evolution of monogamy) or via the assistance of older, post-reproductive females (leading to post-reproductive longevity in females, i.e., the grandmother hypothesis). We suggest that both arrangements could have been present in Plio-Pleistocene hominins if they lived in multilevel societies. Here we expand on our earlier scenario with two sets of recent data in support of it, (1) archaeological data from the 2 million year old Oldowan site of Kanjera South, Kenya and other sites that are suggestive of tool dependent foraging on nutrient dense resources (animal carcasses and plant underground storage organs), cooperation, and food sharing; and (2) a pattern of genetic variation in hamadryas baboons that suggests the operation of kin selection among both males and females at multiple levels of society. Taken together, these two sets of data strengthen our model and support the idea of a complex society linked by male-male, male-female, and female-female bonds at multiple levels of social organization in Plio-Pleistocene hominins.
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Affiliation(s)
- Larissa Swedell
- Dept of Anthropology, Queens College, City University of New York, Flushing, NY 11367-1597, USA; New York Consortium in Evolutionary Primatology, New York, NY, USA; Anthropology Program, CUNY Graduate Center, 365 Fifth Avenue, New York, NY 10016, USA; Biology and Psychology Programs, CUNY Graduate Center, 365 Fifth Avenue, New York, NY 10016, USA; Dept of Archaeology, University of Cape Town, Rondebosch 7701, Cape Town, South Africa.
| | - Thomas Plummer
- Dept of Anthropology, Queens College, City University of New York, Flushing, NY 11367-1597, USA; New York Consortium in Evolutionary Primatology, New York, NY, USA; Anthropology Program, CUNY Graduate Center, 365 Fifth Avenue, New York, NY 10016, USA.
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19
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Abstract
Present-day African ecosystems serve as referential models for conceptualizing the environmental context of early hominin evolution, but the degree to which modern ecosystems are representative of those in the past is unclear. A growing body of evidence from eastern Africa's rich and well-dated late Cenozoic fossil record documents communities of large-bodied mammalian herbivores with ecological structures differing dramatically from those of the present day, implying that modern communities may not be suitable analogs for the ancient ecosystems of hominin evolution. To determine when and why the ecological structure of eastern Africa's herbivore faunas came to resemble those of the present, here we analyze functional trait changes in a comprehensive dataset of 305 modern and fossil herbivore communities spanning the last ∼7 Myr. We show that nearly all communities prior to ∼700 ka were functionally non-analog, largely due to a greater richness of non-ruminants and megaherbivores (species >1,000 kg). The emergence of functionally modern communities precedes that of taxonomically modern communities by 100,000s of years, and can be attributed to the combined influence of Plio-Pleistocene C4 grassland expansion and pulses of aridity after ∼1 Ma. Given the disproportionate ecological impacts of large-bodied herbivores on factors such as vegetation structure, hydrology, and fire regimes, it follows that the vast majority of early hominin evolution transpired in the context of ecosystems that functioned unlike any today. Identifying how past ecosystems differed compositionally and functionally from those today is key to conceptualizing ancient African environments and testing ecological hypotheses of hominin evolution.
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20
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Rausch L, Stoica M. AN EARLY PLEISTOCENE ANOMALOHALINE WATER OSTRACOD FAUNA FROM LAKE DEPOSITS OF THE HOMO ERECTUS-BEARING KOCABAŞ LOCALITY (SW TURKEY). ACTA ACUST UNITED AC 2019. [DOI: 10.35463/j.apr.2019.02.04] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
Abstract
The early Pleistocene travertines from the Denizli Basin in SW Anatolia, from which the only known Homo erectus finding from Turkey was recovered, are unconformably overlain by a 20 m thick succession of alkaline lake deposits that bear a rich ostracod fauna. The ostracod assemblage consists of a mixture of freshwater and mesohaline tolerant taxa. The following sixteen species have been identified: Candona neglecta, C. ex. gr. candida, Cypria sp., Darwinulina stevensovi, Lineocypris sp., Prinocypris zenkeri, Cyrpideis torosa, C. sp., Tyrrhencythere pontica, T. ex. gr. bailovi, T. sp. 1, T. sp. 2, Amnicythere pediformis, A. mutlituberculata, Loxoconchissa (Loxocaspia) aff. reticulata, L. (L.) aff. reticulata var. rugosa. The conditions inside the lake were interpreted from the encountered assemblage, suggesting a restricted anomalohaline shallow water environment with a salinity no greater than lower mesohaline. The age of the studied succession was previously constrained by cosmogenic nuclide concentration, palaeomagnetic measurements and large mammal biostratigraphy which suggest deposition occurred between ~ 1.6 and 1.1 Ma.
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21
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Joordens JC, Feibel CS, Vonhof HB, Schulp AS, Kroon D. Relevance of the eastern African coastal forest for early hominin biogeography. J Hum Evol 2019; 131:176-202. [DOI: 10.1016/j.jhevol.2019.03.012] [Citation(s) in RCA: 16] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/15/2018] [Revised: 03/10/2019] [Accepted: 03/13/2019] [Indexed: 12/25/2022]
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22
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Quinn RL. Isotopic equifinality and rethinking the diet of
Australopithecus anamensis. AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 2019; 169:403-421. [DOI: 10.1002/ajpa.23846] [Citation(s) in RCA: 11] [Impact Index Per Article: 2.2] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/16/2018] [Revised: 03/08/2019] [Accepted: 04/16/2019] [Indexed: 01/06/2023]
Affiliation(s)
- Rhonda L. Quinn
- Department of Sociology, Anthropology and Social WorkSeton Hall University South Orange New Jersey
- Department of Earth and Planetary SciencesRutgers University Piscataway New Jersey
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23
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Roach NT, Du A, Hatala KG, Ostrofsky KR, Reeves JS, Braun DR, Harris JW, Behrensmeyer AK, Richmond BG. Pleistocene animal communities of a 1.5 million-year-old lake margin grassland and their relationship to Homo erectus paleoecology. J Hum Evol 2018; 122:70-83. [DOI: 10.1016/j.jhevol.2018.04.014] [Citation(s) in RCA: 12] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/01/2016] [Revised: 04/03/2018] [Accepted: 04/24/2018] [Indexed: 12/01/2022]
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24
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Du A, Alemseged Z. Diversity analysis of Plio-Pleistocene large mammal communities in the Omo-Turkana Basin, eastern Africa. J Hum Evol 2018; 124:25-39. [PMID: 30153945 DOI: 10.1016/j.jhevol.2018.07.004] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/05/2017] [Revised: 07/13/2018] [Accepted: 07/16/2018] [Indexed: 11/19/2022]
Abstract
Knowing how the diversity of large mammal communities changes across space and time provides an important ecological framework for studying hominin evolution. However, diversity studies that apply methods currently used by neoecologists are rare in paleoanthropology and are also challenging due to diversity's unusual statistical properties. Here, we apply up-to-date analytical methods for understanding how species- and genus-level large mammalian diversity in the Omo-Turkana Basin changed through time and across space at multiple spatiotemporal scales (within each formation:102-3 km2 and 104-5 years; and within the basin as a whole: 103 km2 and 105 years). We found that, on average, Koobi Fora's large mammal community was more diverse than Nachukui's, which in turn was more diverse than Shungura's. Diversity was stable through time within each of these formations (alpha diversity), as was diversity in the basin as a whole (gamma diversity). Compositional dissimilarity between these three formations (beta diversity) was relatively low through time, with a 0.6 average proportion of shared species, suggesting dispersal acted to homogenize the region. Though alpha and gamma diversity were fairly stable through time, we do observe several notable peaks: during the KBS Member in Koobi Fora (30% increase), the Lokalalei Member in Nachukui (120% increase), and at 1.7 Ma in the entire basin (100% increase). We conclude by (1) demonstrating that habitat heterogeneity was an important factor influencing alpha diversity within each of the three formations, and (2) hypothesizing that diversity stability may have been driven by equilibrial dynamics in which overall diversity was constrained by resource availability, implying biotic interactions were an important factor in structuring the communities that included hominins as members. Our findings demonstrate the need to quantify how large mammal diversity changes across time and space in order to further our understanding of hominin ecology and evolution.
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Affiliation(s)
- Andrew Du
- Department of Organismal Biology and Anatomy, The University of Chicago, 1027 E 57th St, Chicago, IL 60637, USA.
| | - Zeresenay Alemseged
- Department of Organismal Biology and Anatomy, The University of Chicago, 1027 E 57th St, Chicago, IL 60637, USA
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Tuomisto H, Tuomisto M, Tuomisto JT. How scientists perceive the evolutionary origin of human traits: Results of a survey study. Ecol Evol 2018; 8:3518-3533. [PMID: 29607043 PMCID: PMC5869357 DOI: 10.1002/ece3.3887] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/24/2017] [Revised: 12/31/2017] [Accepted: 01/02/2018] [Indexed: 11/08/2022] Open
Abstract
Various hypotheses have been proposed for why the traits distinguishing humans from other primates originally evolved, and any given trait may have been explained both as an adaptation to different environments and as a result of demands from social organization or sexual selection. To find out how popular the different explanations are among scientists, we carried out an online survey among authors of recent scientific papers in journals covering relevant fields of science (paleoanthropology, paleontology, ecology, evolution, human biology). Some of the hypotheses were clearly more popular among the 1,266 respondents than others, but none was universally accepted or rejected. Even the most popular of the hypotheses were assessed "very likely" by <50% of the respondents, but many traits had 1-3 hypotheses that were found at least moderately likely by >70% of the respondents. An ordination of the hypotheses identified two strong gradients. Along one gradient, the hypotheses were sorted by their popularity, measured by the average credibility score given by the respondents. The second gradient separated all hypotheses postulating adaptation to swimming or diving into their own group. The average credibility scores given for different subgroups of the hypotheses were not related to respondent's age or number of publications authored. However, (paleo)anthropologists were more critical of all hypotheses, and much more critical of the water-related ones, than were respondents representing other fields of expertise. Although most respondents did not find the water-related hypotheses likely, only a small minority found them unscientific. The most popular hypotheses were based on inherent drivers; that is, they assumed the evolution of a trait to have been triggered by the prior emergence of another human-specific behavioral or morphological trait, but opinions differed as to which of the traits came first.
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26
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Correlates and catalysts of hominin evolution in Africa. Theory Biosci 2017; 136:123-140. [PMID: 28597395 DOI: 10.1007/s12064-017-0250-5] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/30/2016] [Accepted: 05/28/2017] [Indexed: 10/19/2022]
Abstract
Hominin evolution in the African Pliocene and Pleistocene was accompanied and mediated by changes in the abiotic and biotic spheres. It has been hypothesized that such environmental changes were catalysts of hominin morphological evolution and speciations. Whereas there is little doubt that ecological changes were relevant to shaping the trajectories of mammalian evolution, testing specific hypotheses with data from the fossil record has yielded ambiguous results regarding environmental disruption as a primary catalyst. Proposed mechanisms for abiotic and biotic causes of evolution are not always consistent with the timing and trends exhibited by the African fossil record of hominins and other mammals. Analyses of fossil and genetic data suggest that much of hominin evolution, and by extension mammalian evolution, was autocatalytic, driven by feedback loops within a species or lineage, irrespective of changes in the external environment.
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27
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Robinson JR, Rowan J, Campisano CJ, Wynn JG, Reed KE. Late Pliocene environmental change during the transition from Australopithecus to Homo. Nat Ecol Evol 2017; 1:159. [DOI: 10.1038/s41559-017-0159] [Citation(s) in RCA: 29] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/06/2016] [Accepted: 04/07/2017] [Indexed: 11/09/2022]
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28
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Robinson JR. Thinking locally: Environmental reconstruction of Middle and Later Stone Age archaeological sites in Ethiopia, Kenya, and Zambia based on ungulate stable isotopes. J Hum Evol 2017; 106:19-37. [DOI: 10.1016/j.jhevol.2017.01.013] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/19/2015] [Revised: 01/25/2017] [Accepted: 01/26/2017] [Indexed: 11/26/2022]
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Climatic variability, plasticity, and dispersal: A case study from Lake Tana, Ethiopia. J Hum Evol 2016; 87:32-47. [PMID: 26472274 DOI: 10.1016/j.jhevol.2015.07.007] [Citation(s) in RCA: 22] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/14/2014] [Revised: 03/06/2015] [Accepted: 07/12/2015] [Indexed: 12/23/2022]
Abstract
The numerous dispersal events that have occurred during the prehistory of hominin lineages are the subject of longstanding and increasingly active debate in evolutionary anthropology. As well as research into the dating and geographic extent of such dispersals, there is an increasing focus on the factors that may have been responsible for dispersal. The growing body of detailed regional palaeoclimatic data is invaluable in demonstrating the often close relationship between changes in prehistoric environments and the movements of hominin populations. The scenarios constructed from such data are often overly simplistic, however, concentrating on the dynamics of cyclical contraction and expansion during severe and ameliorated conditions respectively. This contribution proposes a two-stage hypothesis of hominin dispersal in which populations (1) accumulate high levels of climatic tolerance during highly variable climatic phases, and (2) express such heightened tolerance via dispersal in subsequent low-variability phases. Likely dispersal phases are thus proposed to occur during stable climatic phases that immediately follow phases of high climatic variability. Employing high resolution palaeoclimatic data from Lake Tana, Ethiopia, the hypothesis is examined in relation to the early dispersal of Homo sapiens out of East Africa and into the Levant. A dispersal phase is identified in the Lake Tana record between c. 112,550 and c. 96,975 years ago, a date bracket that accords well with the dating evidence for H. sapiens occupation at the sites of Qafzeh and Skhul. Results are discussed in relation to the complex pattern of H. sapiens dispersal out of East Africa, with particular attention paid to the implications of recent genetic chronologies for the origin of non-African modern humans.
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Curran SC, Haile-Selassie Y. Paleoecological reconstruction of hominin-bearing middle Pliocene localities at Woranso-Mille, Ethiopia. J Hum Evol 2016; 96:97-112. [DOI: 10.1016/j.jhevol.2016.04.002] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/21/2014] [Revised: 04/14/2016] [Accepted: 04/16/2016] [Indexed: 10/21/2022]
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Magill CR, Ashley GM, Domínguez-Rodrigo M, Freeman KH. Dietary options and behavior suggested by plant biomarker evidence in an early human habitat. Proc Natl Acad Sci U S A 2016; 113:2874-9. [PMID: 26903646 PMCID: PMC4801266 DOI: 10.1073/pnas.1507055113] [Citation(s) in RCA: 23] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
The availability of plants and freshwater shapes the diets and social behavior of chimpanzees, our closest living relative. However, limited evidence about the spatial relationships shared between ancestral human (hominin) remains, edible resources, refuge, and freshwater leaves the influence of local resources on our species' evolution open to debate. Exceptionally well-preserved organic geochemical fossils--biomarkers--preserved in a soil horizon resolve different plant communities at meter scales across a contiguous 25,000 m(2) archaeological land surface at Olduvai Gorge from about 2 Ma. Biomarkers reveal hominins had access to aquatic plants and protective woods in a patchwork landscape, which included a spring-fed wetland near a woodland that both were surrounded by open grassland. Numerous cut-marked animal bones are located within the wooded area, and within meters of wetland vegetation delineated by biomarkers for ferns and sedges. Taken together, plant biomarkers, clustered bone debris, and hominin remains define a clear spatial pattern that places animal butchery amid the refuge of an isolated forest patch and near freshwater with diverse edible resources.
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Affiliation(s)
| | - Gail M Ashley
- Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854
| | | | - Katherine H Freeman
- Department of Geosciences, The Pennsylvania State University, University Park, PA 16802
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Reed D, Barr WA, Mcpherron SP, Bobe R, Geraads D, Wynn JG, Alemseged Z. Digital data collection in paleoanthropology. Evol Anthropol 2015; 24:238-49. [PMID: 26662947 DOI: 10.1002/evan.21466] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/11/2015] [Indexed: 11/10/2022]
Abstract
Understanding patterns of human evolution across space and time requires synthesizing data collected by independent research teams, and this effort is part of a larger trend to develop cyber infrastructure and e-science initiatives. At present, paleoanthropology cannot easily answer basic questions about the total number of fossils and artifacts that have been discovered, or exactly how those items were collected. In this paper, we examine the methodological challenges to data integration, with the hope that mitigating the technical obstacles will further promote data sharing. At a minimum, data integration efforts must document what data exist and how the data were collected (discovery), after which we can begin standardizing data collection practices with the aim of achieving combined analyses (synthesis). This paper outlines a digital data collection system for paleoanthropology. We review the relevant data management principles for a general audience and supplement this with technical details drawn from over 15 years of paleontological and archeological field experience in Africa and Europe. The system outlined here emphasizes free open-source software (FOSS) solutions that work on multiple computer platforms; it builds on recent advances in open-source geospatial software and mobile computing.
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Schoeninger MJ, Most CA, Moore JJ, Somerville AD. Environmental variables across Pan troglodytes study sites correspond with the carbon, but not the nitrogen, stable isotope ratios of chimpanzee hair. Am J Primatol 2015; 78:1055-69. [PMID: 26513527 DOI: 10.1002/ajp.22496] [Citation(s) in RCA: 26] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/26/2015] [Revised: 10/08/2015] [Accepted: 10/18/2015] [Indexed: 01/04/2023]
Abstract
Diet influences the stable isotope ratios of carbon and nitrogen (δ(13) C and δ(15) N values) in animal tissue; but here we explore the influences of particular aspects of the local environment on those values in chimpanzees (Pan troglodytes). In this article we present new δ(13) C and δ(15) N values in Gombe chimpanzees using hairs collected from night nests in 1989. Then, we explore the influence of environmental factors by comparing our Gombe data to those from eight additional Pan study sites with previously published stable isotope data. We compare chimpanzee δ(13) Chair and δ(15) Nhar values to specific characteristics of local site ecology (biome and ecoregion) and to local Mean Annual Precipitation (MAP) to test hypotheses based on known effects of these variables on the δ(13) C and δ(15) N values in plant tissues. The comparison shows that hair from chimpanzees living in savanna sites with lower MAP have higher δ(13) Chair values than do chimpanzees living in woodland and forested sites with higher MAP. These results demonstrate the potential of using δ(13) C values in primate tissue to indicate aspects of their local ecology in cases where the ecology is uncertain, such as samples collected early in the last century and in fossil hominins. In contrast to expectations, however, chimpanzee δ(15) Nhair values from some savanna sites with lower MAP are lower, not higher, than those living in more forested areas with higher MAP. It is likely that diet selectivity by chimpanzees affects δ(15) Nhair values to a greater extent than does the influence of precipitation on plants. Am. J. Primatol. 78:1055-1069, 2016. © 2015 Wiley Periodicals, Inc.
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Affiliation(s)
| | - Corinna A Most
- Department of Anthropology, University of California, San Diego, La Jolla, California
| | - Jim J Moore
- Department of Anthropology, University of California, San Diego, La Jolla, California
| | - Andrew D Somerville
- Department of Anthropology, University of California, San Diego, La Jolla, California
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Potts R, Faith JT. Alternating high and low climate variability: The context of natural selection and speciation in Plio-Pleistocene hominin evolution. J Hum Evol 2015; 87:5-20. [DOI: 10.1016/j.jhevol.2015.06.014] [Citation(s) in RCA: 116] [Impact Index Per Article: 12.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/12/2014] [Revised: 06/15/2015] [Accepted: 06/26/2015] [Indexed: 01/01/2023]
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Negash EW, Alemseged Z, Wynn JG, Bedaso ZK. Paleodietary reconstruction using stable isotopes and abundance analysis of bovids from the Shungura Formation of South Omo, Ethiopia. J Hum Evol 2015; 88:127-136. [PMID: 26341031 DOI: 10.1016/j.jhevol.2015.07.009] [Citation(s) in RCA: 16] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/03/2015] [Revised: 07/10/2015] [Accepted: 07/15/2015] [Indexed: 11/25/2022]
Abstract
Preservation of the stable carbon isotopic composition of fossil tooth enamel enables us to estimate the relative proportion of C3 versus C4 vegetation in an animal's diet, which, combined with analysis of faunal abundance, may provide complementary methods of paleoenvironmental reconstruction. To this end, we analyzed stable carbon isotopic composition (δ(13)C values) of tooth enamel from four bovid tribes (Tragelaphini, Aepycerotini, Reduncini, and Alcelaphini) derived from six members of the Shungura Formation (Members B, C, D, F, G, and L; ages from ca. 2.90-1.05 Ma (millions of years ago) in the Lower Omo Valley of southwestern Ethiopia. The bovids show a wide range of δ(13)C values within taxa and stratigraphic members, as well as temporal changes in the feeding strategies of taxa analyzed throughout the middle to late Pliocene and early Pleistocene. Such variation suggests that the use of actualistic approaches for paleoenvironmental reconstruction may not always be warranted. Alcelaphini was the only taxon analyzed that retained a consistent dietary preference throughout the sequence, with entirely C4-dominated diets. Reduncini had a mixed C3/C4 to C4-dominated diet prior to 2.4 Ma, after which this taxon shifted to a largely C4-dominated diet. Aepycerotini generally showed a mixed C3/C4 diet, with a period of increased C4 diet from 2.5 to 2.3 Ma. Tragelaphini showed a range of mixed C3/C4 diets, with a median value that was briefly nearer the C4 end member from 2.9 to 2.4 Ma but was otherwise towards the C3 end member. These isotopic results, combined with relative abundance data for these bovids, imply that the environment of the Lower Omo Valley consisted of a mosaic of closed woodlands, with riverine forests and open grasslands. However, our data also signify that the overall environment gradually became more open, and that C4 grasses became more dominant. Finally, these results help document the range and extent of environments and potential diets that were available to the four hominin species encountered in the Shungura sequence.
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Affiliation(s)
- Enquye W Negash
- Department of Anthropology, The George Washington University, Washington, DC 20052, USA
| | - Zeresenay Alemseged
- Department of Anthropology, The California Academy of Sciences, 55 Music Concourse Dr., San Francisco, CA 94118, USA.
| | - Jonathan G Wynn
- School of Geosciences, University of South Florida, 4202 E Fowler Ave. NES107, Tampa, FL 33620, USA
| | - Zelalem K Bedaso
- Department of Geology, University of Dayton, 300 College Park, Dayton, OH 45469-2364, USA
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Abstract
Humans are unique in many respects including being furless, striding bipeds that excel at walking and running long distances in hot conditions. This review summarizes what we do and do not know about the evolution of these characteristics, and how they are related. Although many details remain poorly known, the first hominins (species more closely related to humans than to chimpanzees) apparently diverged from the chimpanzee lineage because of selection for bipedal walking, probably because it improved their ability to forage efficiently. However, because bipedal hominins are necessarily slow runners, early hominins in open habitats likely benefited from improved abilities to dump heat in order to forage safely during times of peak heat when predators were unable to hunt them. Endurance running capabilities evolved later, probably as adaptations for scavenging and then hunting. If so, then there would have been strong selection for heat-loss mechanisms, especially sweating, to persistence hunt, in which hunters combine endurance running and tracking to drive their prey into hyperthermia. As modern humans dispersed into a wide range of habitats over the last few hundred thousand years, recent selection has helped populations cope better with a broader range of locomotor and thermoregulatory challenges, but all humans remain essentially adapted for long distance locomotion rather than speed, and to dump rather than retain heat.
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Affiliation(s)
- Daniel E Lieberman
- Department of Human Evolutionary Biology, Harvard University, 11 Divinity Avenue, Cambridge, MA 02138, USA
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37
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Marean CW, Anderson RJ, Bar-Matthews M, Braun K, Cawthra HC, Cowling RM, Engelbrecht F, Esler KJ, Fisher E, Franklin J, Hill K, Janssen M, Potts AJ, Zahn R. A new research strategy for integrating studies of paleoclimate, paleoenvironment, and paleoanthropology. Evol Anthropol 2015; 24:62-72. [DOI: 10.1002/evan.21443] [Citation(s) in RCA: 45] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/12/2023]
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Stable isotope paleoecology of Late Pleistocene Middle Stone Age humans from the Lake Victoria basin, Kenya. J Hum Evol 2015; 82:1-14. [PMID: 25805041 DOI: 10.1016/j.jhevol.2014.10.005] [Citation(s) in RCA: 48] [Impact Index Per Article: 5.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/16/2013] [Revised: 06/12/2014] [Accepted: 10/10/2014] [Indexed: 11/21/2022]
Abstract
Paleoanthropologists have long argued that environmental pressures played a key role in human evolution. However, our understanding of how these pressures mediated the behavioral and biological diversity of early modern humans and their migration patterns within and out of Africa is limited by a lack of archaeological evidence associated with detailed paleoenvironmental data. Here, we present the first stable isotopic data from paleosols and fauna associated with Middle Stone Age (MSA) sites in East Africa. Late Pleistocene (∼100-45 ka, thousands of years ago) sediments on Rusinga and Mfangano Islands in eastern Lake Victoria (Kenya) preserve a taxonomically diverse, non-analog faunal community associated with MSA artifacts. We analyzed the stable carbon and oxygen isotope composition of paleosol carbonate and organic matter and fossil mammalian tooth enamel, including the first analyses for several extinct bovids such as Rusingoryx atopocranion, Damaliscus hypsodon, and an unnamed impala species. Both paleosol carbonate and organic matter data suggest that local habitats associated with human activities were primarily riverine woodland ecosystems. However, mammalian tooth enamel data indicate that most large-bodied mammals consumed a predominantly C4 diet, suggesting an extensive C4 grassland surrounding these riverine woodlands in the region at the time. These data are consistent with other lines of paleoenvironmental evidence that imply a substantially reduced Lake Victoria at this time, and demonstrate that C4 grasslands were significantly expanded into equatorial Africa compared with their present distribution, which could have facilitated dispersal of human populations and other biotic communities. Our results indicate that early populations of Homo sapiens from the Lake Victoria region exploited locally wooded and well-watered habitats within a larger grassland ecosystem.
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Environments and trypanosomiasis risks for early herders in the later Holocene of the Lake Victoria basin, Kenya. Proc Natl Acad Sci U S A 2015; 112:3674-9. [PMID: 25775535 DOI: 10.1073/pnas.1423953112] [Citation(s) in RCA: 53] [Impact Index Per Article: 5.9] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
Specialized pastoralism developed ∼3 kya among Pastoral Neolithic Elmenteitan herders in eastern Africa. During this time, a mosaic of hunters and herders using diverse economic strategies flourished in southern Kenya. It has been argued that the risk for trypanosomiasis (sleeping sickness), carried by tsetse flies in bushy environments, had a significant influence on pastoral diversification and migration out of eastern Africa toward southern Africa ∼2 kya. Elmenteitan levels at Gogo Falls (ca. 1.9-1.6 kya) preserve a unique faunal record, including wild mammalian herbivores, domestic cattle and caprines, fish, and birds. It has been suggested that a bushy/woodland habitat that harbored tsetse fly constrained production of domestic herds and resulted in subsistence diversification. Stable isotope analysis of herbivore tooth enamel (n = 86) from this site reveals, instead, extensive C4 grazing by both domesticates and the majority of wild herbivores. Integrated with other ecological proxies (pollen and leaf wax biomarkers), these data imply an abundance of C4 grasses in the Lake Victoria basin at this time, and thus little risk for tsetse-related barriers to specialized pastoralism. These data provide empirical evidence for the existence of a grassy corridor through which small groups of herders could have passed to reach southern Africa.
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40
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Reynolds SC, Wilkinson DM, Marston CG, O'Regan HJ. The ‘mosaic habitat’ concept in human evolution: past and present. ACTA ACUST UNITED AC 2015. [DOI: 10.1080/0035919x.2015.1007490] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/23/2022]
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41
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Maslin MA, Shultz S, Trauth MH. A synthesis of the theories and concepts of early human evolution. Philos Trans R Soc Lond B Biol Sci 2015; 370:20140064. [PMID: 25602068 PMCID: PMC4305165 DOI: 10.1098/rstb.2014.0064] [Citation(s) in RCA: 37] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/12/2022] Open
Abstract
Current evidence suggests that many of the major events in hominin evolution occurred in East Africa. Hence, over the past two decades, there has been intensive work undertaken to understand African palaeoclimate and tectonics in order to put together a coherent picture of how the environment of Africa has varied over the past 10 Myr. A new consensus is emerging that suggests the unusual geology and climate of East Africa created a complex, environmentally very variable setting. This new understanding of East African climate has led to the pulsed climate variability hypothesis that suggests the long-term drying trend in East Africa was punctuated by episodes of short alternating periods of extreme humidity and aridity which may have driven hominin speciation, encephalization and dispersals out of Africa. This hypothesis is unique as it provides a conceptual framework within which other evolutionary theories can be examined: first, at macro-scale comparing phylogenetic gradualism and punctuated equilibrium; second, at a more focused level of human evolution comparing allopatric speciation, aridity hypothesis, turnover pulse hypothesis, variability selection hypothesis, Red Queen hypothesis and sympatric speciation based on sexual selection. It is proposed that each one of these mechanisms may have been acting on hominins during these short periods of climate variability, which then produce a range of different traits that led to the emergence of new species. In the case of Homo erectus (sensu lato), it is not just brain size that changes but life history (shortened inter-birth intervals, delayed development), body size and dimorphism, shoulder morphology to allow thrown projectiles, adaptation to long-distance running, ecological flexibility and social behaviour. The future of evolutionary research should be to create evidence-based meta-narratives, which encompass multiple mechanisms that select for different traits leading ultimately to speciation.
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Affiliation(s)
- Mark A Maslin
- Department of Geography, University College London, Pearson Building, Gower Street, London, UK
| | - Susanne Shultz
- Faculty of Life Sciences, University of Manchester, Manchester, UK
| | - Martin H Trauth
- University of Potsdam, Institute of Earth and Environmental Science, Karl-Liebknecht-Street 24-25, Potsdam 14476, Germany
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Taylor PJ, Maree S, Cotterill FPD, Missoup AD, Nicolas V, Denys C. Molecular and morphological evidence for a Pleistocene radiation of laminate-toothed rats (Otomys: Rodentia) across a volcanic archipelago in equatorial Africa. Biol J Linn Soc Lond 2014. [DOI: 10.1111/bij.12317] [Citation(s) in RCA: 19] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/02/2023]
Affiliation(s)
- Peter J. Taylor
- SARChI Chair on Biodiversity & Change, School of Mathematical & Natural Sciences; University of Venda; Private Bag X5050 Thohoyandou 0950 South Africa
- School of Life Sciences; University of KwaZulu Natal; Durban South Africa
- Core Team Member, Centre for Invasion Biology, Department of Botany & Zoology; Stellenbosch University; Private Bag X1 Matieland 7602 South Africa
| | - Sarita Maree
- Mammal Research Institute, Department of Zoology and Entomology; University of Pretoria; Private Bag X20 Pretoria 0028 South Africa
- Molecular Ecology and Evolution Program, Department of Genetics; University of Pretoria; Private Bag X20 Pretoria 0028 South Africa
| | - Fenton P. D. Cotterill
- Africa Earth Observatory Network, Geoecodynamics Research Hub, Department of Botany and Zoology; University of Stellenbosch; Private Bag X1 Matieland 7602 Stellenbosch South Africa
| | - Alain Didier Missoup
- Muséum National d'Histoire naturelle, Départment Systématique et Evolution; UMR 7205 CNRS; OSEB, 45 rue Buffon Paris France
- Department of Animal Biology and Physiology; University of Yaoundé I; Yaoundé Cameroon
- Département de Biologie des Organismes Animaux; Université de Douala; Douala Cameroon
| | - Violaine Nicolas
- Muséum National d'Histoire naturelle, Départment Systématique et Evolution; UMR 7205 CNRS; OSEB, 45 rue Buffon Paris France
| | - Christiane Denys
- Muséum National d'Histoire naturelle, Départment Systématique et Evolution; UMR 7205 CNRS; OSEB, 45 rue Buffon Paris France
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43
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Antón SC, Potts R, Aiello LC. Evolution of earlyHomo: An integrated biological perspective. Science 2014; 345:1236828. [DOI: 10.1126/science.1236828] [Citation(s) in RCA: 339] [Impact Index Per Article: 33.9] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Integration of evidence over the past decade has revised understandings about the major adaptations underlying the origin and early evolution of the genusHomo. Many features associated withHomo sapiens, including our large linear bodies, elongated hind limbs, large energy-expensive brains, reduced sexual dimorphism, increased carnivory, and unique life history traits, were once thought to have evolved near the origin of the genus in response to heightened aridity and open habitats in Africa. However, recent analyses of fossil, archaeological, and environmental data indicate that such traits did not arise as a single package. Instead, some arose substantially earlier and some later than previously thought. From ~2.5 to 1.5 million years ago, three lineages of earlyHomoevolved in a context of habitat instability and fragmentation on seasonal, intergenerational, and evolutionary time scales. These contexts gave a selective advantage to traits, such as dietary flexibility and larger body size, that facilitated survival in shifting environments.
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Wren CD, Xue JZ, Costopoulos A, Burke A. The role of spatial foresight in models of hominin dispersal. J Hum Evol 2014; 69:70-8. [PMID: 24613470 DOI: 10.1016/j.jhevol.2014.02.004] [Citation(s) in RCA: 21] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/01/2013] [Revised: 02/07/2014] [Accepted: 02/07/2014] [Indexed: 11/20/2022]
Abstract
Increasingly sophisticated hominin cognition is assumed to play an important role in major dispersal events but it is unclear what that role is. We present an agent-based model showing that there is a close relationship between level of foresight, environmental heterogeneity, and population dispersibility. We explore the dynamics between these three factors and discuss how they may affect the capacity of a hominin population to disperse. Generally, we find that high levels of environmental heterogeneity select for increased foresight and that high levels of foresight tend to reduce dispersibility. This suggests that cognitively complex hominins in heterogeneous environments have low dispersibility relative to cognitively less complex organisms in more homogeneous environments. The model predicts that the environments leading up to major episodes of dispersal, such as the initial hominin dispersal into Eurasia, were likely relatively low in spatial heterogeneity and that the dispersing hominins had relatively low foresight.
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Affiliation(s)
- Colin D Wren
- Department of Anthropology, McGill University, 855 Sherbrooke St. West., Montreal, QC H3A 2T7, Canada.
| | - Julian Z Xue
- Department of Biology, McGill University, Montreal, Canada
| | - Andre Costopoulos
- Department of Anthropology, McGill University, 855 Sherbrooke St. West., Montreal, QC H3A 2T7, Canada
| | - Ariane Burke
- Département d'anthropologie, Université de Montréal, Montréal, Canada
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45
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Domínguez-Rodrigo M. Is the “Savanna Hypothesis” a Dead Concept for Explaining the Emergence of the Earliest Hominins? CURRENT ANTHROPOLOGY 2014. [DOI: 10.1086/674530] [Citation(s) in RCA: 75] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
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46
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Crevecoeur I, Skinner MM, Bailey SE, Gunz P, Bortoluzzi S, Brooks AS, Burlet C, Cornelissen E, De Clerck N, Maureille B, Semal P, Vanbrabant Y, Wood B. First early hominin from central Africa (Ishango, Democratic Republic of Congo). PLoS One 2014; 9:e84652. [PMID: 24427292 PMCID: PMC3888414 DOI: 10.1371/journal.pone.0084652] [Citation(s) in RCA: 17] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/06/2013] [Accepted: 11/17/2013] [Indexed: 11/19/2022] Open
Abstract
Despite uncontested evidence for fossils belonging to the early hominin genus Australopithecus in East Africa from at least 4.2 million years ago (Ma), and from Chad by 3.5 Ma, thus far there has been no convincing evidence of Australopithecus, Paranthropus or early Homo from the western (Albertine) branch of the Rift Valley. Here we report the discovery of an isolated upper molar (#Ish25) from the Western Rift Valley site of Ishango in Central Africa in a derived context, overlying beds dated to between ca. 2.6 to 2.0 Ma. We used µCT imaging to compare its external and internal macro-morphology to upper molars of australopiths, and fossil and recent Homo. We show that the size and shape of the enamel-dentine junction (EDJ) surface discriminate between Plio-Pleistocene and post-Lower Pleistocene hominins, and that the Ishango molar clusters with australopiths and early Homo from East and southern Africa. A reassessment of the archaeological context of the specimen is consistent with the morphological evidence and suggest that early hominins were occupying this region by at least 2 Ma.
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Affiliation(s)
- Isabelle Crevecoeur
- Unité Mixte de Recherche 5199, de la Préhistoire à l’Actuel: Culture, Environnement et Anthropologie (UMR 5199 - PACEA), Centre National de la Recherche Scientifique (CNRS), Université de Bordeaux, Talence, France
- * E-mail:
| | - Matthew M. Skinner
- Department of Anthropology, University College London, London, United Kingdom
- Max Planck Institute for Evolutionary Anthropology, Department of Human Evolution, Leipzig, Germany
| | - Shara E. Bailey
- Center for the Study of Human Origins, Department of Anthropology, New York University, New York, New York, United States of America
- Max Planck Institute for Evolutionary Anthropology, Department of Human Evolution, Leipzig, Germany
| | - Philipp Gunz
- Max Planck Institute for Evolutionary Anthropology, Department of Human Evolution, Leipzig, Germany
| | - Silvia Bortoluzzi
- Laboratori di Antropologia, Dipartimento di Biologia Evoluzionistica “Leo Pardi”, Università di Firenze, Florence, Italy
| | - Alison S. Brooks
- Center for the Advanced Study of Hominid Paleobiology, Department of Anthropology, The George Washington University, Washington DC, United States of America
| | - Christian Burlet
- Geological Survey of Belgium, Royal Belgian Institute for Natural Sciences, Brussels, Belgium
| | - Els Cornelissen
- Section of Prehistory and Archaeology, Royal Museum for Central Africa, Tervuren, Belgium
| | - Nora De Clerck
- Microtomography CT Research Group, University of Antwerp, Wilrijk, Belgium
| | - Bruno Maureille
- Unité Mixte de Recherche 5199, de la Préhistoire à l’Actuel: Culture, Environnement et Anthropologie (UMR 5199 - PACEA), Centre National de la Recherche Scientifique (CNRS), Université de Bordeaux, Talence, France
| | - Patrick Semal
- Anthropology and Prehistory, Royal Belgian Institute for Natural Sciences, Brussels, Belgium
| | - Yves Vanbrabant
- Geological Survey of Belgium, Royal Belgian Institute for Natural Sciences, Brussels, Belgium
| | - Bernard Wood
- Center for the Advanced Study of Hominid Paleobiology, Department of Anthropology, The George Washington University, Washington DC, United States of America
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Zanolli C. Additional evidence for morpho-dimensional tooth crown variation in a New Indonesian H. erectus sample from the Sangiran Dome (Central Java). PLoS One 2013; 8:e67233. [PMID: 23843996 PMCID: PMC3700995 DOI: 10.1371/journal.pone.0067233] [Citation(s) in RCA: 40] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/15/2013] [Accepted: 05/15/2013] [Indexed: 11/19/2022] Open
Abstract
This contribution reports fifteen human fossil dental remains found during the last two decades in the Sangiran Dome area, in Central Java, Indonesia. Among this sample, only one of the specimens had already been briefly described, with the other fourteen remaining unreported. Seven of the fifteen isolated teeth were found in a secured stratigraphic context in the late Lower-early Middle Pleistocene Kabuh Formation. The remaining elements were surface finds which, based on coincidental sources of information, were inferred as coming from the Kabuh Formation. Mainly constituted of permanent molars, but also including one upper incisor and one upper premolar, this dental sample brings additional evidence for a marked degree of size variation and time-related structural reduction in Javanese H. erectus. This is notably expressed by a significant decrease of the mesiodistal diameter, frequently associated to the reduction or even loss of the lower molar distal cusp (hypoconulid) and to a more square occlusal outline. In addition to the hypoconulid reduction or loss, this new sample also exhibits a low frequency of the occlusal Y-groove pattern, with a dominance of the X and, to a lesser extent, of the+patterns. This combination is rare in the Lower and early Middle Pleistocene paleoanthropological record, including in the early Javanese dental assemblage from the Sangiran Dome. On the other hand, similar dental features are found in Chinese H. erectus and in H. heidelbergensis. As a whole, this new record confirms the complex nature of the intermittent exchanges that occurred between continental and insular Southeast Asia through the Pleistocene.
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Affiliation(s)
- Clément Zanolli
- Multidisciplinary Laboratory, International Centre for Theoretical Physics, Trieste, Italy.
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Abstract
The role of savannas during the course of early human evolution has been debated for nearly a century, in part because of difficulties in characterizing local ecosystems from fossil and sediment records. Here, we present high-resolution lipid biomarker and isotopic signatures for organic matter preserved in lake sediments at Olduvai Gorge during a key juncture in human evolution about 2.0 Ma--the emergence and dispersal of Homo erectus (sensu lato). Using published data for modern plants and soils, we construct a framework for ecological interpretations of stable carbon-isotope compositions (expressed as δ(13)C values) of lipid biomarkers from ancient plants. Within this framework, δ(13)C values for sedimentary leaf lipids and total organic carbon from Olduvai Gorge indicate recurrent ecosystem variations, where open C(4) grasslands abruptly transitioned to closed C(3) forests within several hundreds to thousands of years. Carbon-isotopic signatures correlate most strongly with Earth's orbital geometry (precession), and tropical sea-surface temperatures are significant secondary predictors in partial regression analyses. The scale and pace of repeated ecosystem variations at Olduvai Gorge contrast with long-held views of directional or stepwise aridification and grassland expansion in eastern Africa during the early Pleistocene and provide a local perspective on environmental hypotheses of human evolution.
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Potts R. Environmental and Behavioral Evidence Pertaining to the Evolution of Early Homo. CURRENT ANTHROPOLOGY 2012. [DOI: 10.1086/667704] [Citation(s) in RCA: 67] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
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