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New Fossils of Oldest American Primate 16 November 2011
New fossils of oldest American primate 16 November 2011 (PhysOrg.com) -- Johns Hopkins researchers have Prior excavations in the same region revealed identified the first ankle and toe bone fossils from fossils of early relatives of horses, carnivores and the earliest North American true primate, which rodents, as well as Teilhardina. The researchers they say suggests that our earliest forerunners screened through hundreds of pounds of may have dwelled or moved primarily in trees, like sedimentary rock, reducing it to fine-grained modern day lemurs and similar mammals. concentrate, which was transported back to the lab for examination under the microscope. Some early Previous excavations have yielded pieces of the primate teeth specimens are known to be many jaw and teeth of Teilhardina, primates that first times smaller than a grain of rice and only appear appeared just after the beginning of the Eocene as specks to the human eye. Under the Epoch about 55.5 million years ago. In a report on microscope, the researchers discovered not only their analysis of the fossils, published in the teeth and jawbones from Teilhardina as before, but October issue of the American Journal of Physical also three fossilized toe bones and three ankle Anthropology, the Johns Hopkins team said they bones, which Rose says are the first found in North identified the latest bones when they went America. The bones were relatively free of attached prospecting for evidence of the earliest Eocene sediment and appeared smooth and dark - due to mammals in the badlands of the Bighorn Basin, the type of minerals accumulated during Wyoming, an area rich in fossils. -
Paralouatta Varonai. a New Quaternary Platyrrhine from Cuba
Manuel River0 Paralouatta varonai. a new Quaternary Faruldad de Biologia, 1 ~niversidadde platyrrhine from Cuba IA Habana, Ln Habana, Cuba Paralouatta varonai, new gen. and sp., from the Quaternary of Cuba, is diag- Oscar Arredondo nosed on the basis ofa skull lacking only portions of the face and the anterior dentition. Among extant platyrrhines, the new monkey shares important derived resemblances with Alouatta, including: (1) form of hafting of the neurocranium and face, (2) depth of malar corpus, and (3) marked lateral flaring of the maxillary root of the zygomatic process. It differs from Alouatta Received 27 June 1990 in mostly primitive ways, including: (1) presence of downwardly-directed Revision received 1 October 1990 foramen magnum, (2) less vertical orientation ofnuchal plane, and (3) curw and accepted I November 1990 of Spee opening less sharply upward. A conspicuous autapomorphy of P. vnronai is the extremely large size of the orbits, paralleled among living ~~vul~,rds;Platyrrhini, Atelidae. piatyrrhines only in Aotw. ~w&xuztln onrona:, Quaternary, Cuba, Fossil primates. journal oj Human .!hlution ( 1991) 21, l-1 1 introduction It is increasingly apparent that the Greater Antilles possessed a diverse array of platyrrhine primates during geologically recent times. To date, primate remains have been recovered from cave sites on three of these islands-Jamaica, Hispaniola and Cuba (Ameghino, 19 10; Miller, 1916, 1929; Williams & Koopman, 1952; Rimoli, 1977; MacPhee & Woods, 1982; Ford & Morgan, 1986,1988; Ford, 1990; MacPhee & Fleagle, in press). Some of this material has yet to be formally described and the number of good species represented in existing collections is unclear. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. -
Closest Relatives of Primates Earliest True Primates Share
Closest relatives of Primates Earliest true primates share: • Archonta • Inner ear morphology – Scandentia (tree shrews) • Postorbital bar, orbital convergence – Dermoptera (flying lemurs) • Large brain case with large orbits – Chiroptera (bats) • Modifications of the elbow • Plesiadapiformes • Elongation of the heel, opposable thumb – Paleocene radiation of unusual critters and nails (instead of claws) – Replaced by rodents – Put in and out of Primate order Eocene Oligocene • Lots of fossils from N America and Europe; little • Continents mostly in present positions from Africa or Asia; • S America and Australia separate from • Prosimians anatomically and likely behaviorally Antarctica • Adapoids and Omomyoids, ecologically diverse; • Best site is Fayum, Egypt 28-32 my very similar early so likely monophyly Lemurs, Lorises • Adapoids like higher primates with large size, • , early anthropoid primates diurnality, frugivory and folivory (feet like lemurs) • Propliopithecus and Aegyptopithecus • Omomyoids more similar to galagos but • Dental apes but New World monkey bodies increase in size and folivorous late • Late Oligocene settling of S. America by • Where are prosimians lately? anthropoid primates Relationships based on fossils and Monkey Evolution molecular evidence • Hominoid and cercopithecoid apomorphies • New World Monkeys (Platyrrhini) show up in Oligocene, primitive versions by Miocene and at 20 and 18 my thereafter look very much like modern forms • Gibbons and Siamangs at 17 my • Old World Monkeys (Catarrhini) show up in Miocene (after apes); Victoriapithecus and then • Orang utans at 12 my split between colobines and cercopithecines; lots of evolutionary change late and lots of • Gorillas at 9 my convergences make systematics challenging • Pan troglodytes and Pan paniscus at 6 my • Also absence of fossils from many lineages • Very successful lately; out competing most apes • Putting chimp vs. -
A Unique Middle Miocene European Hominoid and the Origins of the Great Ape and Human Clade Salvador Moya` -Sola` A,1, David M
A unique Middle Miocene European hominoid and the origins of the great ape and human clade Salvador Moya` -Sola` a,1, David M. Albab,c, Sergio Alme´ cijac, Isaac Casanovas-Vilarc, Meike Ko¨ hlera, Soledad De Esteban-Trivignoc, Josep M. Roblesc,d, Jordi Galindoc, and Josep Fortunyc aInstitucio´Catalana de Recerca i Estudis Avanc¸ats at Institut Catala`de Paleontologia (ICP) and Unitat d’Antropologia Biolo`gica (Dipartimento de Biologia Animal, Biologia Vegetal, i Ecologia), Universitat Auto`noma de Barcelona, Edifici ICP, Campus de Bellaterra s/n, 08193 Cerdanyola del Valle`s, Barcelona, Spain; bDipartimento di Scienze della Terra, Universita`degli Studi di Firenze, Via G. La Pira 4, 50121 Florence, Italy; cInstitut Catala`de Paleontologia, Universitat Auto`noma de Barcelona, Edifici ICP, Campus de Bellaterra s/n, 08193 Cerdanyola del Valle`s, Barcelona, Spain; and dFOSSILIA Serveis Paleontolo`gics i Geolo`gics, S.L. c/ Jaume I nu´m 87, 1er 5a, 08470 Sant Celoni, Barcelona, Spain Edited by David Pilbeam, Harvard University, Cambridge, MA, and approved March 4, 2009 (received for review November 20, 2008) The great ape and human clade (Primates: Hominidae) currently sediments by the diggers and bulldozers. After 6 years of includes orangutans, gorillas, chimpanzees, bonobos, and humans. fieldwork, 150 fossiliferous localities have been sampled from the When, where, and from which taxon hominids evolved are among 300-m-thick local stratigraphic series of ACM, which spans an the most exciting questions yet to be resolved. Within the Afro- interval of 1 million years (Ϸ12.5–11.3 Ma, Late Aragonian, pithecidae, the Kenyapithecinae (Kenyapithecini ؉ Equatorini) Middle Miocene). -
Apparent Competition Structures Ecological Assemblages
letters to nature 20. Leakey, R. E. & Leakey, M. G. A new Miocene hominoid from Kenya. Nature 342, 143–146 (1986). 21. Leakey, M. G., Leakey, R. E., Richtsmeier, J. T., Simons, E. L. & Walker, A. C. Similarities in Aegyptopithecus and Afropithecus facial morphology. Folia Primatol. 56, 65–85 (1991). 22. Delson, E. & Andrews, P.in Phylogeny of the Primates: A Multidisciplinary Approach (eds Luckett, W. P. & Szalay, F. S.) 405–446 (Plenum, New York, 1975). 23. Strasser, E. & Delson, E. Cladistic analysis of cercopithecid relationships. J. Hum. Evol. 16, 81–99 (1987). Acknowledgements. Excavations at Maboko were conducted with permission of the Office of the President, Republic of Kenya and in collaboration with the National Museums of Kenya. We thank the field crew (especially B. Onyango, V. Oluoch and S. Gitau) and M. G. Leakey for assistance, and E. Delson, M. Kohler, S. Moya-Sola and D. Pilbeam for comments and advice. This work was supported by NSF, L. S. B. Leakey Foundation, National Geographic Society, Wenner Gren Foundation for Anthropological Research, Fulbright, and Boise Fund. Correspondence and requests for materials should be addressed to B.R.B. (e-mail: bbenefi[email protected]). Apparent competition structures ecological assemblages M. B. Bonsall & M. P. Hassell Department of Biology and the NERC Centre for Population Biology, Imperial College at Silwood Park, Ascot, Berkshire SL5 7PY, UK ......................................................................................................................... Competition is a major force in structuring ecological com- munities1. It acts directly2 or indirectly, in which case it may be mediated by shared natural enemies and is known as ‘apparent 3–6 Figure 3 Bivariate plot of log10-transformed mean brain and body weight data for competition’ . -
8. Primate Evolution
8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America. -
Fossil Primates
AccessScience from McGraw-Hill Education Page 1 of 16 www.accessscience.com Fossil primates Contributed by: Eric Delson Publication year: 2014 Extinct members of the order of mammals to which humans belong. All current classifications divide the living primates into two major groups (suborders): the Strepsirhini or “lower” primates (lemurs, lorises, and bushbabies) and the Haplorhini or “higher” primates [tarsiers and anthropoids (New and Old World monkeys, greater and lesser apes, and humans)]. Some fossil groups (omomyiforms and adapiforms) can be placed with or near these two extant groupings; however, there is contention whether the Plesiadapiformes represent the earliest relatives of primates and are best placed within the order (as here) or outside it. See also: FOSSIL; MAMMALIA; PHYLOGENY; PHYSICAL ANTHROPOLOGY; PRIMATES. Vast evidence suggests that the order Primates is a monophyletic group, that is, the primates have a common genetic origin. Although several peculiarities of the primate bauplan (body plan) appear to be inherited from an inferred common ancestor, it seems that the order as a whole is characterized by showing a variety of parallel adaptations in different groups to a predominantly arboreal lifestyle, including anatomical and behavioral complexes related to improved grasping and manipulative capacities, a variety of locomotor styles, and enlargement of the higher centers of the brain. Among the extant primates, the lower primates more closely resemble forms that evolved relatively early in the history of the order, whereas the higher primates represent a group that evolved more recently (Fig. 1). A classification of the primates, as accepted here, appears above. Early primates The earliest primates are placed in their own semiorder, Plesiadapiformes (as contrasted with the semiorder Euprimates for all living forms), because they have no direct evolutionary links with, and bear few adaptive resemblances to, any group of living primates. -
Knowledge of the Evolution of African Paleogene Mammals
Knowledge of the évolution of African Paleogene mammals Contribution of the Bir El Ater locality (Eocène, Algeria) Rodolphe Tabuce Brigitte Coiffait Philippe-Emmanuel Coiffait Mohamed Mahboubi Jean-Jacques Jaeger 1 1 Introduction: The Early African Paleogene mammals The African fossil record of therians begins with the Early Cretaceous ofthe Middle Atlas (Morocco) (Sigogneau-Russell, 1991); however, the modem mammalian orders appear only during the early Tertiary in North Africa (figure 1A). The Paleocene and Ypresian localities from the Ouarzazate Basin (Morocco) hâve yielded mammalian faunas with possible creodonts, « insectivores » (paleoryctids, todralestids and adapisoriculids) (Gheerbrant, 1992, 1994, 1995), the oldest représentative ofeupri- mates (Sigé et al, 1990) and archaic ungulates (Sudre et al, 1993). Recently, the discovery of Phosphatherium (Proboscidea) in J\) .... Ypresian Early to Mlddla Mlddlalo Lata C> mlcldla BOCena eocena Ialaeocene eocena "III N'Tagourt2 ElKohol GllbZagdou GourLazib Chambl lnTaliclel M'Bodlone Bir el Ater DoralTalha Qaar (Moroc:co) (Algerla) (Algerla) (Algerla) (Tunlala) and (Sanagal) (Algarla) ·Evaporlt e1Sagha lamagullell Unit· (Fayum, (Mali) (LIbye) Egypt) Matatharla Kassarinolherium tunisiansa Creodonta Koholis gen. el sp. Aprarodon stlasansa indet Hyaanodon Carnlvora Glibzagdouis I8balbslsensis Condylarthra Condyfarthra Condylarthra Inda!. Inda!. Artlodaetyla cl.Bolhrio- ganys sp. Proboscldell KhSmsBcornJS Numidotherium Moerilharium Moenlherium Moarilherium 8srytherium 8srythenum buJbosus -
Ancestral Facial Morphology of Old World Higher Primates (Anthropoidea/Catarrhini/Miocene/Cranium/Anatomy) BRENDA R
Proc. Natl. Acad. Sci. USA Vol. 88, pp. 5267-5271, June 1991 Evolution Ancestral facial morphology of Old World higher primates (Anthropoidea/Catarrhini/Miocene/cranium/anatomy) BRENDA R. BENEFIT* AND MONTE L. MCCROSSINt *Department of Anthropology, Southern Illinois University, Carbondale, IL 62901; and tDepartment of Anthropology, University of California, Berkeley, CA 94720 Communicated by F. Clark Howell, March 11, 1991 ABSTRACT Fossil remains of the cercopithecoid Victoia- (1, 5, 6). Contrasting craniofacial configurations of cercopithe- pithecus recently recovered from middle Miocene deposits of cines and great apes are, in consequence, held to be indepen- Maboko Island (Kenya) provide evidence ofthe cranial anatomy dently derived with regard to the ancestral catarrhine condition of Old World monkeys prior to the evolutionary divergence of (1, 5, 6). This reconstruction has formed the basis of influential the extant subfamilies Colobinae and Cercopithecinae. Victoria- cladistic assessments ofthe phylogenetic relationships between pithecus shares a suite ofcraniofacial features with the Oligocene extant and extinct catarrhines (1, 2). catarrhine Aegyptopithecus and early Miocene hominoid Afro- Reconstructions of the ancestral catarrhine morphotype pithecus. AU three genera manifest supraorbital costae, anteri- are based on commonalities of subordinate morphotypes for orly convergent temporal lines, the absence of a postglabellar Cercopithecoidea and Hominoidea (1, 5, 6). Broadly distrib- fossa, a moderate to long snout, great facial -
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27 2 Novel p53-mediated human- Endocrine-Related J W Nyce 27:2 R51–R65 specific ‘kill switch’ tumor Cancer suppression mechanism REVIEW A lex naturalis delineates components of a human-specific, adrenal androgen-dependent, p53-mediated ‘kill switch’ tumor suppression mechanism Jonathan Wesley Nyce ACGT Biotechnology, Collegeville, Pennsylvania, USA Correspondence should be addressed to J W Nyce: [email protected] Abstract We have recently described in this journal our detection of an anthropoid primate- Key Words specific, adrenal androgen-dependent, p53-mediated, ‘kill switch’ tumor suppression f p53 mechanism that reached its fullest expression only in humans, as a result of human- f TP53 specific exposure to polycyclic aromatic hydrocarbons caused by the harnessing of fire – f DHEA but which has components reaching all the way back to the origin of the primate lineage. f cancer prevention We proposed that species-specific mechanisms of tumor suppression are a generalized f vitamin C requirement for vertebrate species to increase in body size or lifespan beyond those of species basal to their lineage or to exploit environmental niches which increase exposure to carcinogenic substances. Using empirical dynamic modeling, we have also reported our detection of a relationship between body size, lifespan, and species-specific mechanism of tumor suppression (and here add carcinogen exposure), such that a change in any one of these variables requires an equilibrating change in one or more of the others in order to maintain lifetime cancer risk at a value of about 4%, as observed in virtually all larger, longer-lived species under natural conditions. Here we show how this relationship, which we refer to as the lex naturalis of vertebrate speciation, elucidates the evolutionary steps underlying an adrenal androgen-dependent, human-specific ‘kill switch’ tumor suppression mechanism; and further, how it prescribes a solution to ‘normalize’ lifetime cancer risk in our species from its current aberrant 40% to the 4% that characterized primitive humans.