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Human Life Histories in an Evolutionary and Comparative Context;
HUMAN LIFE HISTORIES IN AN EVOLUTIONARY AND COMPARATIVE CONTEXT by Shannen Lorraine Robson A dissertation submitted by the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Anthropology The University of Utah August 2011 Copyright © Shannen Lorraine Robson 2011 All Rights Reserved The University of Utah Graduate School STATEMENT OF DISSERTATION APPROVAL The dissertation of Shannen Lorraine Robson has been approved by the following supervisory committee members: Kristen Hawkes , Chair 04/27/2011 Date Approved Douglas Jones , Member 04/27/2011 Date Approved James O’Connell , Member 04/27/2011 Date Approved Eric Rickart , Member 04/27/2011 Date Approved Ken Smith , Member 04/27/2011 Date Approved and by Elizabeth Cashdan , Chair of the Department of Anthropology and by Charles A. Wight, Dean of The Graduate School. ABSTRACT This dissertation utilizes life history theory to describe traits that are derived in humans through comparisons with other primate species. Modern human life histories are unique in that they are slower, exhibiting distinctly long postmenopausal life spans and later ages at sexual maturity as a result of a reduction in adult mortality since the evolutionary split the last Pan-Homo ancestor. Faster reproduction with shorter than expected interbirth intervals and earlier weaning ages are likely the result of cooperative breeding featuring postmenopausal grandmothers. Life history traits are distinguished from life history related variables (LHRVs) which are used to makes inferences about life history variables in extinct taxa. Body mass LHRV is a strong predictive life history proxy, but brain size and dental development are only weakly associated and inferences using them should be made with caution. -
Bibliography
Bibliography Many books were read and researched in the compilation of Binford, L. R, 1983, Working at Archaeology. Academic Press, The Encyclopedic Dictionary of Archaeology: New York. Binford, L. R, and Binford, S. R (eds.), 1968, New Perspectives in American Museum of Natural History, 1993, The First Humans. Archaeology. Aldine, Chicago. HarperSanFrancisco, San Francisco. Braidwood, R 1.,1960, Archaeologists and What They Do. Franklin American Museum of Natural History, 1993, People of the Stone Watts, New York. Age. HarperSanFrancisco, San Francisco. Branigan, Keith (ed.), 1982, The Atlas ofArchaeology. St. Martin's, American Museum of Natural History, 1994, New World and Pacific New York. Civilizations. HarperSanFrancisco, San Francisco. Bray, w., and Tump, D., 1972, Penguin Dictionary ofArchaeology. American Museum of Natural History, 1994, Old World Civiliza Penguin, New York. tions. HarperSanFrancisco, San Francisco. Brennan, L., 1973, Beginner's Guide to Archaeology. Stackpole Ashmore, w., and Sharer, R. J., 1988, Discovering Our Past: A Brief Books, Harrisburg, PA. Introduction to Archaeology. Mayfield, Mountain View, CA. Broderick, M., and Morton, A. A., 1924, A Concise Dictionary of Atkinson, R J. C., 1985, Field Archaeology, 2d ed. Hyperion, New Egyptian Archaeology. Ares Publishers, Chicago. York. Brothwell, D., 1963, Digging Up Bones: The Excavation, Treatment Bacon, E. (ed.), 1976, The Great Archaeologists. Bobbs-Merrill, and Study ofHuman Skeletal Remains. British Museum, London. New York. Brothwell, D., and Higgs, E. (eds.), 1969, Science in Archaeology, Bahn, P., 1993, Collins Dictionary of Archaeology. ABC-CLIO, 2d ed. Thames and Hudson, London. Santa Barbara, CA. Budge, E. A. Wallis, 1929, The Rosetta Stone. Dover, New York. Bahn, P. -
Cave Radon Exposure, Dose, Dynamics and Mitigation
Chris L. Waring, Stuart I. Hankin, Stephen B. Solomon, Stephen Long, Andrew Yule, Robert Blackley, Sylvester Werczynski, and Andrew C. Baker. Cave radon exposure, dose, dynamics and mitigation. Journal of Cave and Karst Studies, v. 83, no. 1, p. 1-19. DOI:10.4311/2019ES0124 CAVE RADON EXPOSURE, DOSE, DYNAMICS AND MITIGATION Chris L. Waring1, C, Stuart I. Hankin1, Stephen B. Solomon2, Stephen Long2, Andrew Yule2, Robert Blackley1, Sylvester Werczynski1, and Andrew C. Baker3 Abstract Many caves around the world have very high concentrations of naturally occurring 222Rn that may vary dramatically with seasonal and diurnal patterns. For most caves with a variable seasonal or diurnal pattern, 222Rn concentration is driven by bi-directional convective ventilation, which responds to external temperature contrast with cave temperature. Cavers and cave workers exposed to high 222Rn have an increased risk of contracting lung cancer. The International Commission on Radiological Protection (ICRP) has re-evaluated its estimates of lung cancer risk from inhalation of radon progeny (ICRP 115) and for cave workers the risk may now (ICRP 137) be 4–6 times higher than previously recognized. Cave Guides working underground in caves with annual average 222Rn activity 1,000 Bq m3 and default ICRP assumptions (2,000 workplace hours per year, equilibrium factor F 0.4, dose conversion factor DCF 14 µSv 3 1 1 d13 (kBq h m ) could now receive a dose of 20 mSv y . Using multiple gas tracers ( C CO2, Rn and N2O), linked weather, source gas flux chambers, and convective air flow measurements a previous study unequivocally identified the external soil above Chifley Cave as the source of cave222 Rn. -
CV Karkanas 2018.Pdf
PANAGIOTIS (TAKIS) KARKANAS CURRICULUM VITAE May 2018 Malcolm H. Wiener Laboratory for Archaeological Science American School of Classical Studies 54 Soudias, 10676 Athens, Greece Tel.: (30) 2130002400x224 Fax: (30) 2107294047 E-mail: [email protected] Personal Web Pages: https://www.researchgate.net/profile/Panagiotis_Karkanas https://ascsa.academia.edu/PanagiotisKarkanas EDUCATIONAL BACKGROUND 1994: Ph.D. in Geology (Specialty: mineralogy, petrology, geochemistry), Department of Geology, University of Athens. 1990: Postgraduate Seminar (300 hours) in Geology of sedimentary basin and energy resources. EU funded Research Seminar for Geologists, Department of Geology, University of Athens. 1986: B.Sc. in Geology, Department of Geology, University of Athens. AREAS OF INTEREST Geoarchaeology: site formation processes (stratigraphy, micromorphology, post-depositional chemical alterations) palaeoenvironmental reconstructions, paleoclimate, methods and techniques (dating, petrography, mineralogy, sedimentary analysis, provenance analysis). PROFESSIONAL APPOINTMENTS 2014-: Director, Malcolm H. Wiener Laboratory of Archaeological Science, American School of Classical Studies at Athens, Greece. 1994-2014: Senior Geologist, Ephoreia of Palaeoanthropology-Speleology (EPS), Ministry of Culture, Greece. 2004-2013: Adjunct Lecturer, Department of Geography, Harokopio University of Athens. OTHER PROFESSIONAL AND LABORATORY EXPERIENCE 1995-2003 (approx. one month per year): Visiting research scientist, Kimmel Center for Archaeological Sciences, -
The Carnivore Remains from the Sima De Los Huesos Middle Pleistocene Site
N. Garcia & The carnivore remains from the Sima de J. L. Arsuaga los Huesos Middle Pleistocene site Departamento de Paleontologia, (Sierra de Atapuerca, Spain) Facultad de Ciencias Geologicas, U.A. de Paleoantropologia & Instituto de View metadata, citation and similar papersRemain ats ocore.ac.ukf carnivores from the Sima de los Huesos sitebrought representin to you gby a t COREleast Geologia Economica, Universidad 158 adult individuals of a primitive (i.e., not very speleoid) form of Ursus Complutense de Madrid, Ciudad provided by Servicio de Coordinación de Bibliotecas de la... deningeri Von Reichenau 1906, have been recovered through the 1995 field Universitaria, 28040 Madrid, Spain season. These new finds extend our knowledge of this group in the Sierra de Atapuerca Middle Pleistocene. Material previously classified as Cuoninae T. Torres indet. is now assigned to Canis lupus and a third metatarsal assigned in 1987 to Departamento de Ingenieria Geoldgica, Panthera cf. gombaszoegensis, is in our opinion only attributable to Panthera sp. The Escuela Tecnica Superior de Ingenieros family Mustelidae is added to the faunal list and includes Maites sp. and a de Minas, Universidad Politecnica smaller species. The presence of Panthera leo cf. fossilis, Lynxpardina spelaea and de Madrid, Rios Rosas 21, Fells silvestris, is confirmed. The presence of a not very speloid Ursus deningeri, 28003 Madrid, Spain together with the rest of the carnivore assemblage, points to a not very late Middle Pleistocene age, i.e., oxygen isotope stage 7 or older. Relative frequencies of skeletal elements for the bear and fox samples are without major biases. The age structure of the bear sample, based on dental wear stages, does not follow the typical hibernation mortality profile and resembles a cata strophic profile. -
Estrategias De Subsistencia De Los Primeros Grupos Humanos Que Poblaron Europa
ESTRATEGIAS DE SUBSISTENCIA DE LOS PRIMEROS GRUPOS HUMANOS QUE POBLARON EUROPA ESTRATEGIAS DE SUBSISTENCIA DE LOS PRIMEROS GRUPOS HUMANOS QUE POBLARON EUROPA: EVIDENCIAS CONSERVADAS EN BARRANCO LEÓN Y FUENTE NUEVA-3 (ORCE) M. PATROCINIO ESPIGARES* RESUMEN Varios yacimientos del Pleistoceno inferior de España, Francia e Italia preservan las evidencias de presencia humana más antiguas de Europa. En este contexto, son particularmente interesantes dos localidades ubicadas en las inmediaciones de la villa de Orce (Cuenca de Baza, Granada), Barranco León (BL) y Fuente Nueva-3 (FN-3), datadas en torno a 1,4 Ma. En estos yacimientos se han identificado evidencias de procesado de cadáveres de grandes mamíferos, realizado con herra- mientas líticas de factura Olduvayense. A estos hallazgos hay que sumarle la presencia de un diente de leche atribuido a Homo sp. en Barranco León. En este trabajo se describen en detalle las marcas de origen antrópico localizadas en estos yacimientos, se analizan los patrones de procesado de los cadáveres, y se discute sobre las estrategias de subsistencia de las primeras comunidades humanas que habitaron Europa. Palabras clave: Marcas de corte, Estrategias de subsistencia, Pleistoceno Inferior, Homo sp. ABSTRACT Several Early Pleistocene sites from Spain, France and Italy preserve ancient evidence of human presence. In this context are particularly interesting two localities placed near the town of Orce (Baza Basin, Granada), Barranco León (BL) and Fuente Nueva-3 (FN-3), dated to ~1.4 Ma. At these sites, evidence of processing of large mammal carcasses produced with Oldowan tools have been recovered. These findings are accompanied by the presence of a deciduous tooth, attributed to Homo sp., in Barranco León. -
Isotopic Analysis of the Ecology of Herbivores and Carnivores from the Middle Pleistocene Deposits of the Sierra De Atapuerca, Northern Spain N
Isotopic analysis of the ecology of herbivores and carnivores from the Middle Pleistocene deposits of the Sierra De Atapuerca, northern Spain N. Garcia Gar~ia~,~,",R.S. FeranecC.*, J.L. ~rsua~a~,~,J.M. BermGdez de Castrod, E. Carbonelle 'Deportomento de Poleontologio, Focultod de Ciencior Geoldgicor, Univerridod Complutense de Modrid, Ciudod Univerritorio, 28040 Modrid, Spoin Centlo Mkt0 (UCM-ISUII) de Evolucidn y Comportomiento Humonor, CfSinerio Delgodo 4, Pob. 14, 29029 Modrid, Spoin 'New York Stote Museum. 3140 Culturol Education Center. Albonv. NY 12230. USA *centre Nocionol de Invertigoci6n robre 10 Evoluci6n Humono -?M, Avda de ia Pog 28, 09004 Burger, Spoin eInstitut Cotold de Poleoecologio Humono i Evoluci6 Sociol (IPHES), C/ Erconodor, r/n 43003 Torrogono, Spoin ABSTRACT Carbon and oxygen isotope values reveal resource partitioning among the large mammal fauna from three contemporaneous Middle Pleistocene hominid-bearing localities within the Sierra de Atapuerca (northern Spain). Carbon isotope values sampled from the tooth enamel of fauna present during Ata- ouerca Faunal Unit 6 show that a C?-dominated ecosvstem surrounded the area where fossils were preserved during this time. For the herbivores, Fallow deer isotope values are significantly different from Red deer and horses and show that this species did not forage in open environments at this locality. Red Keywords: deer and horses show similar feedine strateeies with less neeative carbon values imolvine use of more C-l3 Diet Ecology Enamel that this species is herbivorous. Special metabolic mechanisms involved in hibernation in U deningeri Mammal might also have influenced its isotope values. The carbon isotope values of remaining carnivores were 0-18 similar and suggest that each was typically a generalist carnivore, eating a wide variety of prey items. -
Rodentia, Mammalia) in Europe'
Resumen EI yacimiento de Trinchera Oolina es uno de los mas importantes de la Sierra de Atapuerca par su contenido en restos humanos, Homo antecessor en el nivel de Trinchera Dolina 6. Ade mas de esto la enorme riqueza en restos arqueol6gicos y paleontol6gicos hace de Trinchera Dolina un yacimiento unico, de referencia obligada para el Pleistoceno y Paleolitico de Euro pa. Bioestratigraficamente, el yacimiento de Trinchera Oolina (TO) puede dividirse en tres grandes unidades: la que comprende los niveles TD3 a T06; la de los niveles T07 a TOS infe rior y I. de TO 8 superior. T011. Palabras clave: Mamiferos, Pleistoceno. Abstract Gran Dolina is one of the Pleistocene sites located at the Sierra de Atapuerca (Spain). The Gran Dolina deposits belong to different chronological periods of the Early and Middle Pleistocene. The uppermost levels of Gran Dolina (TDII, TDIO and TD8b) contain Middle Pleistocene (post-Cromerian) macro- and micromammal assemblages. The excavation works have overpassed level TDII and have not concluded yet at TDIO: TDII is poor in macromammal remains (carnivores and herbivores) but rich in rodents. The macromammals fossil material from TDtt is very scarce and this enables (for the macromammals) definite conclusions about the chronology and type of community of these levels. The lowermost levels of Gran Dolina (TD3/4, TD5, TD6 and TD8a) contain a different mammal assemblage with typical late Early Pleistocene-Cromerian species. This radical substitution of taxa is placed at TD8 layer probably due to a stratigraphic gap in this level. The level TD6 of the Gran Dolina site contains the earliest fossil human remains of Europe, Homo antecessor, and it has also a rich and diverse micromammal assemblage. -
Pleistocene Cave Hyenas in the Iberian Peninsula: New Insights from Los Aprendices Cave (Moncayo, Zaragoza)
Palaeontologia Electronica palaeo-electronica.org Pleistocene cave hyenas in the Iberian Peninsula: New insights from Los Aprendices cave (Moncayo, Zaragoza) Víctor Sauqué, Raquel Rabal-Garcés, Joan Madurell-Malaperia, Mario Gisbert, Samuel Zamora, Trinidad de Torres, José Eugenio Ortiz, and Gloria Cuenca-Bescós ABSTRACT A new Pleistocene paleontological site, Los Aprendices, located in the northwest- ern part of the Iberian Peninsula in the area of the Moncayo (Zaragoza) is presented. The layer with fossil remains has been dated by amino acid racemization to 143.8 ± 38.9 ka (earliest Late Pleistocene or latest Middle Pleistocene). Five mammal species have been identified in the assemblage: Crocuta spelaea (Goldfuss, 1823) Capra pyre- naica (Schinz, 1838), Lagomorpha indet, Arvicolidae indet and Galemys pyrenaicus (Geoffroy, 1811). The remains of C. spelaea represent a mostly complete skeleton in anatomical semi-connection. The hyena specimen represents the most complete skel- eton ever recovered in Iberia and one of the most complete remains in Europe. It has been compared anatomically and biometrically with both European cave hyenas and extant spotted hyenas. In addition, a taphonomic study has been carried out in order to understand the origin and preservation of these exceptional remains. The results sug- gest rapid burial with few scavenging modifications putatively produced by a medium sized carnivore. A review of the Pleistocene Iberian record of Crocuta spp. has been carried out, enabling us to establish one of the earliest records of C. spelaea in the recently discovered Los Aprendices cave, and also showing that the most extensive geographical distribution of this species occurred during the Late Pleistocene (MIS4- 2). -
Homo Erectus: a Bigger, Faster, Smarter, Longer Lasting Hominin Lineage
Homo erectus: A Bigger, Faster, Smarter, Longer Lasting Hominin Lineage Charles J. Vella, PhD August, 2019 Acknowledgements Many drawings by Kathryn Cruz-Uribe in Human Career, by R. Klein Many graphics from multiple journal articles (i.e. Nature, Science, PNAS) Ray Troll • Hominin evolution from 3.0 to 1.5 Ma. (Species) • Currently known species temporal ranges for Pa, Paranthropus aethiopicus; Pb, P. boisei; Pr, P. robustus; A afr, Australopithecus africanus; Ag, A. garhi; As, A. sediba; H sp., early Homo >2.1 million years ago (Ma); 1470 group and 1813 group representing a new interpretation of the traditionally recognized H. habilis and H. rudolfensis; and He, H. erectus. He (D) indicates H. erectus from Dmanisi. • (Behavior) Icons indicate from the bottom the • first appearance of stone tools (the Oldowan technology) at ~2.6 Ma, • the dispersal of Homo to Eurasia at ~1.85 Ma, • and the appearance of the Acheulean technology at ~1.76 Ma. • The number of contemporaneous hominin taxa during this period reflects different Susan C. Antón, Richard Potts, Leslie C. Aiello, 2014 strategies of adaptation to habitat variability. Origins of Homo: Summary of shifts in Homo Early Homo appears in the record by 2.3 Ma. By 2.0 Ma at least two facial morphs of early Homo (1813 group and 1470 group) representing two different adaptations are present. And possibly 3 others as well (Ledi-Geraru, Uraha-501, KNM-ER 62000) The 1813 group survives until at least 1.44 Ma. Early Homo erectus represents a third more derived morph and one that is of slightly larger brain and body size but somewhat smaller tooth size. -
Large Mammal Biochronology Framework in Europe at Jaramillo: the Epivillafranchian As a Formal Biochron
Quaternary International 389 (2015) 84e89 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Large mammal biochronology framework in Europe at Jaramillo: The Epivillafranchian as a formal biochron Luca Bellucci a, Raffaele Sardella a, Lorenzo Rook b, * a Dipartimento di Scienze della Terra, “Sapienza e Universita di Roma”, P.le A. Moro 5, 00185, Roma, Italy b Dipartimento di Scienze della Terra, Universita di Firenze, via G. La Pira 4, 50121, Firenze, Italy article info abstract Article history: European large mammal assemblages in the 1.2e0.9 Ma timespan included Villafranchian taxa together Available online 3 December 2014 with newcomers, mostly from Asia, persisting in the Middle Pleistocene. A number of biochronological schemes have been suggested to define these “transitional” faunas. The term Epivillafranchian, originally Keywords: proposed by Bourdier in 1961 and reconsidered as a biochron by Kahlke in the 1990s, is at present widely Biochronology introduced in the literature. This contribution, after selecting the most representative European large Jaramillo mammal assemblages within this chronological interval, provides a new definition proposal for the Epivillafranchian Epivillafranchian as a biochron included within the Praemegaceros verticornis FO/Bison menneri FO, and Late Villafranchian Crocuta crocuta Galerian FO. Europe © 2014 Elsevier Ltd and INQUA. All rights reserved. 1. Historical background communities of this time span primarily include survivors from the latest Villafranchian, as well as more evolved taxa characteristic of The Villafranchian Mammal Age corresponds, in the Interna- the beginning Middle Pleistocene (Kahlke, 2007; Rook and tional Stratigraphic Scale, to a timespan from Late Pliocene to most Martinez Navarro, 2010). -
Phylogenetic and Phylogeographic Analysis of Iberian Lynx Populations
Journal of Heredity 2004:95(1):19–28 ª 2004 The American Genetic Association DOI: 10.1093/jhered/esh006 Phylogenetic and Phylogeographic Analysis of Iberian Lynx Populations W. E. JOHNSON,J.A.GODOY,F.PALOMARES,M.DELIBES,M.FERNANDES,E.REVILLA, AND S. J. O’BRIEN From the Laboratory of Genomic Diversity, National Cancer Institute-FCRDC, Frederick, MD 21702-1201 (Johnson and O’Brien), Department of Applied Biology, Estacio´ n Biolo´ gica de Don˜ana, CSIC, Avda. Marı´a Luisa s/n, 41013, Sevilla, Spain (Godoy, Palomares, Delibes, and Revilla), and Instituto da Conservac¸a˜o da Natureza, Rua Filipe Folque, 46, 28, 1050-114 Lisboa, Portugal (Fernandes). E. Revilla is currently at the Department of Ecological Modeling, UFZ-Center for Environmental Research, PF 2, D-04301 Leipzig, Germany. The research was supported by DGICYT and DGES (projects PB90-1018, PB94-0480, and PB97-1163), Consejerı´a de Medio Ambiente de la Junta de Andalucı´a, Instituto Nacional para la Conservacion de la Naturaleza, and US-Spain Joint Commission for Scientific and Technological Cooperation. We thank A. E. Pires, A. Piriz, S. Cevario, V. David, M. Menotti-Raymond, E. Eizirik, J. Martenson, J. H. Kim, A. Garfinkel, J. Page, C. Ferris, and E. Carney for advice and support in the laboratory and J. Calzada, J. M. Fedriani, P. Ferreras, and J. C. Rivilla for assistance in the capture of lynx. Museo Nacional de Ciencias Naturales, Don˜ana Biological Station scientific collection, Don˜ana National Park, and Instituto da Conservac¸a˜o da Natureza of Portugal provided samples of museum specimens.