Root Caries on a Paranthropus Robustus Third Molar from Drimolen
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Recent Origin of Low Trabecular Bone Density in Modern Humans
Recent origin of low trabecular bone density in modern humans Habiba Chirchira,b,1, Tracy L. Kivellc,d, Christopher B. Ruffe, Jean-Jacques Hublind, Kristian J. Carlsonf,g, Bernhard Zipfelf, and Brian G. Richmonda,b,h,1 aCenter for the Advanced Study of Hominid Paleobiology, Department of Anthropology, The George Washington University, Washington, DC 20052; bHuman Origins Program, Department of Anthropology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560; cAnimal Postcranial Evolution Laboratory, School of Anthropology and Conservation, University of Kent, Canterbury, Kent, CT2 7NR, United Kingdom; dDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, D-04103 Leipzig, Germany; eCenter for Functional Anatomy and Evolution, Johns Hopkins University School of Medicine, Baltimore, MD 21205; fEvolutionary Studies Institute, The University of the Witwatersrand, Braamfontein 2000 Johannesburg, South Africa; gDepartment of Anthropology, Indiana University, Bloomington, IN 47405; and hDivision of Anthropology, American Museum of Natural History, New York, NY 10024 Edited by Erik Trinkaus, Washington University, St. Louis, MO, and approved November 26, 2014 (received for review June 23, 2014) Humans are unique, compared with our closest living relatives humans relative to earlier hominins generally has been attributed (chimpanzees) and early fossil hominins, in having an enlarged to a decrease in daily physical activity via technological and body size and lower limb joint surfaces in combination with a rel- cultural innovations (6, 10, 13–15, 19–22). atively gracile skeleton (i.e., lower bone mass for our body size). There also is evidence that increased activity level and me- Some analyses have observed that in at least a few anatomical chanical loading increases trabecular bone mineral density within regions modern humans today appear to have relatively low tra- limb bones (ref. -
Paranthropus Boisei: Fifty Years of Evidence and Analysis Bernard A
Marshall University Marshall Digital Scholar Biological Sciences Faculty Research Biological Sciences Fall 11-28-2007 Paranthropus boisei: Fifty Years of Evidence and Analysis Bernard A. Wood George Washington University Paul J. Constantino Biological Sciences, [email protected] Follow this and additional works at: http://mds.marshall.edu/bio_sciences_faculty Part of the Biological and Physical Anthropology Commons Recommended Citation Wood B and Constantino P. Paranthropus boisei: Fifty years of evidence and analysis. Yearbook of Physical Anthropology 50:106-132. This Article is brought to you for free and open access by the Biological Sciences at Marshall Digital Scholar. It has been accepted for inclusion in Biological Sciences Faculty Research by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected], [email protected]. YEARBOOK OF PHYSICAL ANTHROPOLOGY 50:106–132 (2007) Paranthropus boisei: Fifty Years of Evidence and Analysis Bernard Wood* and Paul Constantino Center for the Advanced Study of Hominid Paleobiology, George Washington University, Washington, DC 20052 KEY WORDS Paranthropus; boisei; aethiopicus; human evolution; Africa ABSTRACT Paranthropus boisei is a hominin taxon ers can trace the evolution of metric and nonmetric var- with a distinctive cranial and dental morphology. Its iables across hundreds of thousands of years. This pa- hypodigm has been recovered from sites with good per is a detailed1 review of half a century’s worth of fos- stratigraphic and chronological control, and for some sil evidence and analysis of P. boi se i and traces how morphological regions, such as the mandible and the both its evolutionary history and our understanding of mandibular dentition, the samples are not only rela- its evolutionary history have evolved during the past tively well dated, but they are, by paleontological 50 years. -
Title: Drimolen Crania Indicate Contemporaneity of Australopithecus, Paranthropus and Early Homo Erectus in S
Submitted Manuscript: Confidential Title: Drimolen crania indicate contemporaneity of Australopithecus, Paranthropus and early Homo erectus in S. Africa Authors: Andy I.R. Herries1,2*†, Jesse M. Martin1†, A.B. Leece1†, Justin W. Adams3,2†, Giovanni Boschian4,2†, Renaud Joannes-Boyau5,2, Tara R. Edwards1, Tom Mallett1, Jason Massey3,6, Ashleigh Murszewski1, Simon Neuebauer7, Robyn Pickering8.9, David Strait10,2, Brian J. Armstrong2, Stephanie Baker2, Matthew V. Caruana2, Tim Denham11, John Hellstrom12, Jacopo Moggi-Cecchi13, Simon Mokobane2, Paul Penzo-Kajewski1, Douglass S. Rovinsky3, Gary T. Schwartz14, Rhiannon C. Stammers1, Coen Wilson1, Jon Woodhead12, Colin Menter13 Affiliations: 1. Palaeoscience Labs, Dept. Archaeology and History, La Trobe University, Bundoora, 3086, VIC, Australia. 2. Palaeo-Research Institute, University of Johannesburg, Gauteng Province, South Africa. 3. Department of Anatomy and Developmental Biology, Biomedicine Discovery Institute, Monash University, VIC, Australia. 4. Department of Biology, University of Pisa, Italy 5. Geoarchaeology and Archaeometry Research Group (GARG), Southern Cross University, Military Rd, Lismore, 2480, NSW, Australia 6. Department of Integrative Biology and Physiology, University of Minnesota Medical School, USA 7. Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Germany. 8. Department of Geological Sciences, University of Cape Town, Western Cape, South Africa 9. Human Evolution Research Institute, University of Cape Town, Western Cape, South Africa 10. Department of Anthropology, Washington University in St. Louis, St. Louis, USA 11. Geoarchaeology Research Group, School of Archaeology and Anthropology, Australian National University, Canberra, ACT, Australia 12. Earth Sciences, University of Melbourne, Australia 13. Department of Biology, University of Florence, Italy 14. Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, U.S.A. -
Informative Potential of Multiscale Observations in Archaeological Biominerals Down to the Nanoscale Ina Reiche, Aurélien Gourrier
Informative potential of multiscale observations in archaeological biominerals down to the nanoscale Ina Reiche, Aurélien Gourrier To cite this version: Ina Reiche, Aurélien Gourrier. Informative potential of multiscale observations in archaeologi- cal biominerals down to the nanoscale. Philippe Dillmann; Irène Nenner; Ludovic Bellot-Gurlet. Nanoscience and Cultural Heritage, Atlantis Press, 2016, 978-94-6239-197-0. 10.2991/978-94-6239- 198-7_4. hal-01380156 HAL Id: hal-01380156 https://hal.archives-ouvertes.fr/hal-01380156 Submitted on 12 Oct 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NonCommercial - ShareAlike| 4.0 International License Chapter 4 Informative potential of multiscale observations in archaeological biominerals down to the nanoscale. Ina Reiche1,2*, Aurélien Gourrier3,4** 1 Sorbonne Universités, Université Paris 06, Laboratoire d’Archéologie Moléculaire et Structurale, UMR 8220 CNRS, 75005 Paris, France. 2 Rathgen Forschungslabor, Staatliche Museen zu Berlin Stiftung Preußischer Kulturbesitz, 14059 Berlin, Allemagne 3 Univ. Grenoble Alpes, LIPHY, F-38000 Grenoble, France 4 CNRS, LIPHY, F-38000 Grenoble, France * [email protected] ** [email protected] Abstract Humans have intentionally used biological materials such as bone, ivory and shells since prehistoric times due to their particular physical and chemical properties. -
Paranthropus Through the Looking Glass COMMENTARY Bernard A
COMMENTARY Paranthropus through the looking glass COMMENTARY Bernard A. Wooda,1 and David B. Pattersona,b Most research and public interest in human origins upper jaw fragment from Malema in Malawi is the focuses on taxa that are likely to be our ancestors. southernmost evidence. However, most of what we There must have been genetic continuity between know about P. boisei comes from fossils from Koobi modern humans and the common ancestor we share Fora on the eastern shore of Lake Turkana (4) and from with chimpanzees and bonobos, and we want to know sites in the Nachukui Formation on the western side of what each link in this chain looked like and how it be- the lake (Fig. 1A). haved. However, the clear evidence for taxic diversity The cranial and dental morphology of P.boisei is so in the human (aka hominin) clade means that we also distinctive its remains are relatively easy to identify (5). have close relatives who are not our ancestors (1). Two Unique features include its flat, wide, and deep face, papers in PNAS focus on the behavior and paleoenvi- flexed cranial base, large and thick lower jaw, and ronmental context of Paranthropus boisei, a distinctive small incisors and canines combined with massive and long-extinct nonancestral relative that lived along- chewing teeth. The surface area available for process- side our early Homo ancestors in eastern Africa between ing food is extended both forward—by having premo- just less than 3 Ma and just over 1 Ma. Both papers use lar teeth that look like molars—and backward—by the stable isotopes to track diet during a largely unknown, unusually large third molar tooth crowns, all of which but likely crucial, period in our evolutionary history. -
Australopiths Wading? Homo Diving?
Symposium: Water and Human Evolution, April 30th 1999, University Gent, Flanders, Belgium Proceedings Australopiths wading? Homo diving? http://allserv.rug.ac.be/~mvaneech/Symposium.html http://www.flash.net/~hydra9/marcaat.html Marc Verhaegen & Stephen Munro – 23 July 1999 Abstract Asian pongids (orangutans) and African hominids (gorillas, chimpanzees and humans) split 14-10 million years ago, possibly in the Middle East, or elsewhere in Eurasia, where the great ape fossils of 12-8 million years ago display pongid and/or hominid features. In any case, it is likely that the ancestors of the African apes, australopithecines and humans, lived on the Arabian-African continent 8-6 million years ago, when they split into gorillas and humans-chimpanzees. They could have frequently waded bipedally, like mangrove proboscis monkeys, in the mangrove forests between Eurasia and Africa, and partly fed on hard-shelled fruits and oysters like mangrove capuchin monkeys: thick enamel plus stone tool use is typically seen in capuchins, hominids and sea otters. The australopithecines might have entered the African inland along rivers and lakes. Their dentition suggests they ate mostly fruits, hard grass-like plants, and aquatic herbaceous vegetation (AHV). The fossil data indicates that the early australopithecines of 4-3 million years ago lived in waterside forests or woodlands; and their larger, robust relatives of 2-1 million years ago in generally more open milieus near marshes and reedbeds, where they could have waded bipedally. Some anthropologists believe the present-day African apes evolved from australopithecine-like ancestors, which would imply that knuckle-walking gorillas and chimpanzees evolved in parallel from wading- climbing ‘aquarborealists’. -
Evidence of Termite Foraging by Swartkrans Early Hominids
Evidence of termite foraging by Swartkrans early hominids Lucinda R. Backwell*† and Francesco d’Errico‡§ *Palaeo-Anthropology Unit for Research and Exploration, Department of Palaeontology, Palaeo-Anthropology Research Group, and †Department of Anatomical Sciences, University of the Witwatersrand, Private Bag 3, Wits, 2050, Johannesburg, South Africa; and ‡Institut de Pre´histoire et de Ge´ologie du Quaternaire, Unite´Mixte de Recherche 5808 du Centre National de la Recherche Scientifique, Baˆtiment 18, Avenue des Faculte´s, 33405 Talence, France Communicated by Erik Trinkaus, Washington University, St. Louis, MO, November 20, 2000 (received for review September 14, 2000) Previous studies have suggested that modified bones from the body surface activated silicone paste for molds, and Araldite M Lower Paleolithic sites of Swartkrans and Sterkfontein in South resin and HY 956 Hardener for casts) was used to replicate the Africa represent the oldest known bone tools and that they were 68 Swartkrans (SKX) and 1 Sterkfontein (SE) purported bone used by Australopithecus robustus to dig up tubers. Macroscopic tools, and optical and scanning electron microscopy was used to and microscopic analysis of the wear patterns on the purported identify their surface modifications. Microscopic images of the bone tools, pseudo bone tools produced naturally by known transparent resin replicas were digitized at 40ϫ magnification on taphonomic processes, and experimentally used bone tools con- a sample of 18 fossils from Swartkrans. The orientation and firm the anthropic origin of the modifications. However, our dimension of all visible striations were recorded by using MI- analysis suggests that these tools were used to dig into termite CROWARE image analysis software (14). -
The First Bone Tools from Kromdraai and Stone Tools from Drimolen, And
Quaternary International 495 (2018) 87–101 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint The first bone tools from Kromdraai and stone tools from Drimolen, and the place of bone tools in the South African Earlier Stone Age T ∗ Rhiannon C. Stammersa, Matthew V. Caruanab,c, Andy I.R. Herriesa,c, a Palaeoscience Labs, Department of Archaeology and History, La Trobe University, Melbourne Campus, Bundoora, 3086, VIC, Australia b Archaeology Department, School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, Private Bag 3, WITS, 2050, South Africa c Centre for Anthropological Research, University of Johannesburg, Auckland Park, 2006, Johannesburg, South Africa ARTICLE INFO ABSTRACT Keywords: An apparently unique part of the Earlier Stone Age record of Africa are a series of bone tools dated to between Paranthropus robustus ∼2 and ∼1 Ma from the sites of Olduvai in East Africa, and Swartkrans, Drimolen and Sterkfontein in South Early Stone Age Africa. The South and East African bone tools are quite different, with the South African tools having a number of Karst distinct characters formed through utilisation, whereas the East African tools are flaked tools that in some cases Bone tools mirror stone tool production. The South African bone tools currently consists of 108 specimens from the three Acheulian sites above. They have been interpreted as being used for digging into homogenous grained soil to access high Oldowan Palaeocave quality food resources, or as a multi-purpose tools. It has generally been assumed that they were made by Stone tools Paranthropus robustus, as this species is most often associated with bone tool bearing deposits, especially when high numbers occur. -
Isotopic Evidence for the Timing of the Dietary Shift Toward C4 Foods in Eastern African Paranthropus Jonathan G
Isotopic evidence for the timing of the dietary shift toward C4 foods in eastern African Paranthropus Jonathan G. Wynna,1, Zeresenay Alemsegedb, René Bobec,d, Frederick E. Grinee, Enquye W. Negashf, and Matt Sponheimerg aDivision of Earth Sciences, National Science Foundation, Alexandria, VA 22314; bDepartment of Organismal Biology and Anatomy, The University of Chicago, Chicago, IL 60637; cSchool of Anthropology, University of Oxford, Oxford OX2 6PE, United Kingdom; dGorongosa National Park, Sofala, Mozambique; eDepartment of Anthropology, Stony Brook University, Stony Brook, NY 11794; fCenter for the Advanced Study of Human Paleobiology, George Washington University, Washington, DC 20052; and gDepartment of Anthropology, University of Colorado Boulder, Boulder, CO 80302 Edited by Thure E. Cerling, University of Utah, Salt Lake City, UT, and approved July 28, 2020 (received for review April 2, 2020) New approaches to the study of early hominin diets have refreshed the early evolution of the genus. Was the diet of either P. boisei or interest in how and when our diets diverged from those of other P. robustus similar to that of the earliest members of the genus, or did African apes. A trend toward significant consumption of C4 foods in thedietsofbothdivergefromanearliertypeofdiet? hominins after this divergence has emerged as a landmark event in Key to addressing the pattern and timing of dietary shift(s) in human evolution, with direct evidence provided by stable carbon Paranthropus is an appreciation of the morphology and dietary isotope studies. In this study, we report on detailed carbon isotopic habits of the earliest member of the genus, Paranthropus evidence from the hominin fossil record of the Shungura and Usno aethiopicus, and how those differ from what is observed in later Formations, Lower Omo Valley, Ethiopia, which elucidates the pat- representatives of the genus. -
Male Philopatry and Female Dispersal Amongst Two Species of Early Hominins from the Sterkfontein Valley
Page 1 of 2 News and Views Male philopatry and female dispersal amongst two species of early hominins from the Sterkfontein valley An article by Sandi Copeland and colleagues,1 which appeared in Nature on 02 June 2011, strongly Author: Nikolaas J. van der Merwe1 suggests that amongst two species of early hominins that were present in the Sterkfontein Valley, the male individuals were much less likely to disperse from their natal group than the female Affiliation: individuals. The two species were Australopithecus africanus from Sterkfontein and Paranthropus 1Department of Archaeology, robustus from nearby Swartkrans. The ranges on the landscape of the male and female fossil University of Cape Town, Cape Town, South Africa specimens were determined by measuring the strontium isotope ratios in their tooth enamel and comparing the results with those from the geological substrate of the Sterkfontein Valley. Most of Email: the male specimens had lived in the area from birth (thus male philopatry), whilst a substantial nikolaas.vandermerwe@uct. number of the female specimens had come from somewhere else. ac.za Postal address: All the cave sites that have yielded hominin fossils in the Cradle of Humankind occur in the Department of Archaeology, Malmani dolomite formation. These sites include Sterkfontein, Swartkrans, Kromdraai, University of Cape Town, Makapansgat and Drimolen. The Malmani dolomite is a relatively narrow formation on the Private Bag, Rondebosch 7701, South Africa landscape, running from south-west to north-east for more than 60 km, but with a width of only 7 km – 9 km. From the cave sites of Sterkfontein and Swartkrans, the formation extends about How to cite this article: 2 km – 3 km to the south-east and 5 km – 6 km to the north-west. -
Sterkfontein (South Africa) Work, the Descent of Man
mankind, as Charles Darwin had predicted in his 1871 Sterkfontein (South Africa) work, The Descent of Man. Hence, from both an historical and an heuristic point of view, the Sterkfontein discoveries gave rise to No 915 major advances, factually and conceptually, in the understanding of the time, place, and mode of evolution of the human family. This seminal role continued to the present with the excavation and analysis of more specimens, representing not only the skull, endocranial casts, and teeth, but also the bones of the vertebral column, the shoulder girdle and upper Identification limb, and the pelvic girdle and lower limb. The Sterkfontein assemblage of fossils has made it Nomination The Fossil Hominid Sites of possible for palaeoanthropologists to study not merely Sterkfontein, Swartkrans, Kromdraai individual and isolated specimens, but populations of and Environs early hominids, from the points of view of their demography, variability, growth and development, Location Gauteng, North West Province functioning and behaviour, ecology, taphonomy, and palaeopathology. State Party Republic of South Africa The cave sites of the Sterkfontein Valley represent the Date 16 June 1998 combined works of nature and of man, in that they contain an exceptional record of early stages of hominid evolution, of mammalian evolution, and of Justification by State Party hominid cultural evolution. They include in the deposits from 2.0 million years onwards in situ The Sterkfontein Valley landscape comprises a archaeological remains which are of outstanding number of fossil-bearing cave deposits which are universal value from especially the anthropological considered to be of outstanding universal value, point of view. -
Terrestrial Laser Scanning and Photogrammetry Techniques for Documenting Fossil‐Bearing Palaeokarst with an Example from the Drimolen Palaeocave System, South Africa
Revised: 15 February 2017 Accepted: 11 July 2017 DOI: 10.1002/arp.1580 RESEARCH ARTICLE Terrestrial laser scanning and photogrammetry techniques for documenting fossil‐bearing palaeokarst with an example from the Drimolen Palaeocave System, South Africa Brian J. Armstrong1 | Alex F. Blackwood1 | Paul Penzo‐Kajewski1 | Colin G. Menter2 | Andy I.R. Herries1,2 1 Palaeoscience Laboratories, Department of Archaeology and History, La Trobe University, Abstract Melbourne Campus, Bundoora, 3086, Victoria, This paper presents the results of a recent three‐dimensional (3D) survey at the Drimolen Australia Makondo palaeontological deposits in the Hominid Sites of South Africa UNESCO World 2 Centre for Anthropological Research, Heritage site. The Drimolen Makondo is a palaeokarstic feature that consists of a heavily eroded University of Johannesburg, Johannesburg, 2.6‐2.0 Ma fossil‐bearing palaeocave remnant. With photogrammetry and a laser scan survey, Gauteng Province, South Africa two 3D site models were created, georectified, and imported into geographical information sys- Correspondence Brian J. Armstrong, Palaeoscience tem software. This paper outlines both of these survey techniques and provides an assessment Laboratories, Department of Archaeology and of the relevant merits of each method and their applicability for detailed recording and archival History, La Trobe University, Melbourne documentation of palaeokarstic palaeontological and archaeological sites. Given the complex Campus, Bundoora, 3086, VIC, Australia. Email: [email protected];