100 Years of Primate Paleontology
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The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
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. -
A New Mammalian Fauna from the Earliest Eocene (Ilerdian) of the Corbie`Res (Southern France): Palaeobiogeographical Implications
Swiss J Geosci (2012) 105:417–434 DOI 10.1007/s00015-012-0113-5 A new mammalian fauna from the earliest Eocene (Ilerdian) of the Corbie`res (Southern France): palaeobiogeographical implications Bernard Marandat • Sylvain Adnet • Laurent Marivaux • Alain Martinez • Monique Vianey-Liaud • Rodolphe Tabuce Received: 27 April 2012 / Accepted: 19 September 2012 / Published online: 4 November 2012 Ó Swiss Geological Society 2012 Abstract A new mammal fauna from the earliest Eocene Keywords Ypresian Á Europe Á Mammals Á of Le Clot (Corbie`res, Southern France) is described. Some Multituberculates Á Palaeoclimate Á Palaeobiogeography taxa identified there, such as Corbarimys hottingeri and Paschatherium plaziati, allow a correlation with the pre- viously described Corbie`res fauna of Fordones. Moreover, 1 Introduction the presence at Le Clot of Lessnessina praecipuus, which is defined in Palette (Provence, Southern France) allows The beginning of the Eocene is characterized by two major correlating both localities. All three of these localities are phenomena: the warming event known as the Paleocene referred to the MP7 reference level, even if a direct cor- Eocene thermal maximum (PETM) (Stott et al. 1996), relation with the type locality of MP7 (Dormaal, Belgium) which likely triggered the second one: the mammalian is not ascertained. A Southern Europe biochronological dispersal event (MDE) (Beard and Dawson 1999; Hooker sequence is proposed for the beginning of the Eocene: 2000). This MDE is a critical event in the history of Silveirinha, Fordones/Palette/Le Clot, Rians/Fournes. The mammals as it corresponds to both the origin and dispersal diagnosis of a new species of a neoplagiaulacid multitu- of several modern mammalian orders (Perissodactyla, berculate (?Ectypodus riansensis nov. -
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. -
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. -
Evidence for a Convergent Slowdown in Primate Molecular Rates and Its Implications for the Timing of Early Primate Evolution
Evidence for a convergent slowdown in primate molecular rates and its implications for the timing of early primate evolution Michael E. Steipera,b,c,d,1 and Erik R. Seifferte aDepartment of Anthropology, Hunter College of the City University of New York (CUNY), New York, NY 10065; Programs in bAnthropology and cBiology, The Graduate Center, CUNY, New York, NY 10016; dNew York Consortium in Evolutionary Primatology, New York, NY; and eDepartment of Anatomical Sciences, Stony Brook University, Stony Brook, NY 11794-8081 Edited by Richard G. Klein, Stanford University, Stanford, CA, and approved February 28, 2012 (received for review November 29, 2011) A long-standing problem in primate evolution is the discord divergences—that molecular rates were exceptionally rapid in between paleontological and molecular clock estimates for the the earliest primates, and that these rates have convergently time of crown primate origins: the earliest crown primate fossils slowed over the course of primate evolution. Indeed, a conver- are ∼56 million y (Ma) old, whereas molecular estimates for the gent rate slowdown has been suggested as an explanation for the haplorhine-strepsirrhine split are often deep in the Late Creta- large differences between the molecular and fossil evidence for ceous. One explanation for this phenomenon is that crown pri- the timing of placental mammalian evolution generally (18, 19). mates existed in the Cretaceous but that their fossil remains However, this hypothesis has not been directly tested within have not yet been found. Here we provide strong evidence that a particular mammalian group. this discordance is better-explained by a convergent molecular Here we test this “convergent rate slowdown” hypothesis in rate slowdown in early primate evolution. -
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. -
Early Eocene Primates from Gujarat, India
ARTICLE IN PRESS Journal of Human Evolution xxx (2009) 1–39 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Early Eocene Primates from Gujarat, India Kenneth D. Rose a,*, Rajendra S. Rana b, Ashok Sahni c, Kishor Kumar d, Pieter Missiaen e, Lachham Singh b, Thierry Smith f a Johns Hopkins University School of Medicine, Baltimore, Maryland 21205, USA b H.N.B. Garhwal University, Srinagar 246175, Uttarakhand, India c Panjab University, Chandigarh 160014, India d Wadia Institute of Himalayan Geology, Dehradun 248001, Uttarakhand, India e University of Ghent, B-9000 Ghent, Belgium f Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium article info abstract Article history: The oldest euprimates known from India come from the Early Eocene Cambay Formation at Vastan Mine Received 24 June 2008 in Gujarat. An Ypresian (early Cuisian) age of w53 Ma (based on foraminifera) indicates that these Accepted 8 January 2009 primates were roughly contemporary with, or perhaps predated, the India-Asia collision. Here we present new euprimate fossils from Vastan Mine, including teeth, jaws, and referred postcrania of the Keywords: adapoids Marcgodinotius indicus and Asiadapis cambayensis. They are placed in the new subfamily Eocene Asiadapinae (family Notharctidae), which is most similar to primitive European Cercamoniinae such as India Donrussellia and Protoadapis. Asiadapines were small primates in the size range of extant smaller Notharctidae Adapoidea bushbabies. Despite their generally very plesiomorphic morphology, asiadapines also share a few derived Omomyidae dental traits with sivaladapids, suggesting a possible relationship to these endemic Asian adapoids. In Eosimiidae addition to the adapoids, a new species of the omomyid Vastanomys is described. -
The Evolution of the Platyrrhine Talus: a Comparative Analysis of the Phenetic Affinities of the Miocene Platyrrhines with Their Modern Relatives
Journal of Human Evolution 111 (2017) 179e201 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol The evolution of the platyrrhine talus: A comparative analysis of the phenetic affinities of the Miocene platyrrhines with their modern relatives * Thomas A. Püschel a, , Justin T. Gladman b, c,Rene Bobe d, e, William I. Sellers a a School of Earth and Environmental Sciences, University of Manchester, M13 9PL, United Kingdom b Department of Anthropology, The Graduate Center, CUNY, New York, NY, USA c NYCEP, New York Consortium in Evolutionary Primatology, New York, NY, USA d Departamento de Antropología, Universidad de Chile, Santiago, Chile e Institute of Cognitive and Evolutionary Anthropology, School of Anthropology, University of Oxford, United Kingdom article info abstract Article history: Platyrrhines are a diverse group of primates that presently occupy a broad range of tropical-equatorial Received 8 August 2016 environments in the Americas. However, most of the fossil platyrrhine species of the early Miocene Accepted 26 July 2017 have been found at middle and high latitudes. Although the fossil record of New World monkeys has Available online 29 August 2017 improved considerably over the past several years, it is still difficult to trace the origin of major modern clades. One of the most commonly preserved anatomical structures of early platyrrhines is the talus. Keywords: This work provides an analysis of the phenetic affinities of extant platyrrhine tali and their Miocene New World monkeys counterparts through geometric morphometrics and a series of phylogenetic comparative analyses. Talar morphology fi Geometric morphometrics Geometric morphometrics was used to quantify talar shape af nities, while locomotor mode per- Locomotor mode percentages centages (LMPs) were used to test if talar shape is associated with locomotion. -
Primates, Adapiformes) Skull from the Uintan (Middle Eocene) of San Diego County, California
AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 98:447-470 (1995 New Notharctine (Primates, Adapiformes) Skull From the Uintan (Middle Eocene) of San Diego County, California GREGG F. GUNNELL Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 481 09-1079 KEY WORDS Californian primates, Cranial morphology, Haplorhine-strepsirhine dichotomy ABSTRACT A new genus and species of notharctine primate, Hespero- lemur actius, is described from Uintan (middle Eocene) aged rocks of San Diego County, California. Hesperolemur differs from all previously described adapiforms in having the anterior third of the ectotympanic anulus fused to the internal lateral wall of the auditory bulla. In this feature Hesperolemur superficially resembles extant cheirogaleids. Hesperolemur also differs from previously known adapiforms in lacking bony canals that transmit the inter- nal carotid artery through the tympanic cavity. Hesperolemur, like the later occurring North American cercamoniine Mahgarita steuensi, appears to have lacked a stapedial artery. Evidence from newly discovered skulls ofNotharctus and Smilodectes, along with Hesperolemur, Mahgarita, and Adapis, indicates that the tympanic arterial circulatory pattern of these adapiforms is charac- terized by stapedial arteries that are smaller than promontory arteries, a feature shared with extant tarsiers and anthropoids and one of the character- istics often used to support the existence of a haplorhine-strepsirhine dichot- omy among extant primates. The existence of such a dichotomy among Eocene primates is not supported by any compelling evidence. Hesperolemur is the latest occurring notharctine primate known from North America and is the only notharctine represented among a relatively diverse primate fauna from southern California. The coastal lowlands of southern California presumably served as a refuge area for primates during the middle and later Eocene as climates deteriorated in the continental interior. -
Evidence for an Asian Origin of Stem Anthropoids
Evidence for an Asian origin of stem anthropoids Richard F. Kay1 Department of Evolutionary Anthropology, Duke University, Durham, NC 27708-03083 n PNAS, Chaimanee et al. (1) report Genetic, embryological, and anatomical We are not there yet. Recent comprehen- a previously undescribed species of evidence demonstrates that the sister sive phylogenetic analyses stemming from I primate, Afrasia, from the late Middle group of Anthropoidea is the south Asian virtually the same datasets yield somewhat Eocene of Burma. They identify tarsier, with the two forming the crown different cladograms that reflect sensitivity Afrasia as the sister taxon to the African group Haplorhini (6–8). The other clade of to which taxa are included in the analysis genus Afrotarsius but slightly more primitive extant primates is the lemurs and lorises, and which sets of analytical assumptions are than it and allied with stem Anthropoidea called Strepsirrhini. Eocene Holarctic selected. Pertinent to the biogeographic of south Asia. Anthropoidea is the taxo- Omomyoidea are generally considered as conclusions of Chaimanee et al. (1), Seiffert nomic group that today includes New and stem haplorhines, although the precise et al. (11) conclude that Afrotarsius cha- Old World monkeys, apes, and humans. If relationship of omomyoids to tarsiers and trathi [a younger species than the one that upheld, the biogeographic significance of anthropoids is uncertain (8). Tarsius often Chaimanee et al. (1) describe] is an African these results is profound: If Afrasia and is considered to be a relictual omomyoid tarsioid. If Seiffert et al. (11) are correct, Afrotarsius are as closely related as Chai- in south Asia. -
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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.