Mammalia, Plesiadapiformes) As Reflected on Selected Parts of the Postcranium
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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. -
Proceedings of the United States National Museum
PALEOCENE PRIMATES OF THE FORT UNION, WITH DIS- CUSSION OF RELATIONSHIPS OF EOCENE PRIMATES. By James Williams Gidley, Assistant Curator, United States National Museum. INTRODUCTION. The first important contribution to the knowledge of Fort Union mammalian life was furnished by Dr. Earl Douglass and was based on a small lot of fragmentary material collected by him in the au- tumn of 1901 from a locality in Sweet Grass County, Montana, about 25 miles northeast of Bigtimber.* The fauna described by Douglass indicated a horizon about equivalent in age to the Torrejon of New Mexico, but the presence of unfamilar forms, suggesting a different faunal phase, was recognized. A few years later (1908 to 1911) this region was much more fully explored for fossil remains by parties of the United States Geological Survey and the United States National Museum. Working under the direction of Dr. T. W. Stanton, Mr. Albert C. Silberling, an ener- getic and successful collector, procured the first specimens in the winter and spring of 1908, continuing operations intermittently through the following years until the early spring of 1911. The present writer visited the field in 1908 and again in 1909, securing a considerable amount of good material. The net result of this com- bined field work is the splendid collection now in the National Museum, consisting of about 1,000 specimens, for the most part upper and lower jaw portions carrying teeth in varying numbers, but including also several characteristic foot and limb bones. Although nearly 10 years have passed since the last of this collec- tion was received, it was not until late in the summer of 1920 that the preparation of the material for study was completed. -
Geology and Vertebrate Paleontology of Western and Southern North America
OF WESTERN AND SOUTHERN NORTH AMERICA OF WESTERN AND SOUTHERN NORTH PALEONTOLOGY GEOLOGY AND VERTEBRATE Geology and Vertebrate Paleontology of Western and Southern North America Edited By Xiaoming Wang and Lawrence G. Barnes Contributions in Honor of David P. Whistler WANG | BARNES 900 Exposition Boulevard Los Angeles, California 90007 Natural History Museum of Los Angeles County Science Series 41 May 28, 2008 Paleocene primates from the Goler Formation of the Mojave Desert in California Donald L. Lofgren,1 James G. Honey,2 Malcolm C. McKenna,2,{,2 Robert L. Zondervan,3 and Erin E. Smith3 ABSTRACT. Recent collecting efforts in the Goler Formation in California’s Mojave Desert have yielded new records of turtles, rays, lizards, crocodilians, and mammals, including the primates Paromomys depressidens Gidley, 1923; Ignacius frugivorus Matthew and Granger, 1921; Plesiadapis cf. P. anceps; and Plesiadapis cf. P. churchilli. The species of Plesiadapis Gervais, 1877, indicate that Member 4b of the Goler Formation is Tiffanian. In correlation with Tiffanian (Ti) lineage zones, Plesiadapis cf. P. anceps indicates that the Laudate Discovery Site and Edentulous Jaw Site are Ti2–Ti3 and Plesiadapis cf. P. churchilli indicates that Primate Gulch is Ti4. The presence of Paromomys Gidley, 1923, at the Laudate Discovery Site suggests that the Goler Formation occurrence is the youngest known for the genus. Fossils from Member 3 and the lower part of Member 4 indicate a possible marine influence as Goler Formation sediments accumulated. On the basis of these specimens and a previously documented occurrence of marine invertebrates in Member 4d, the Goler Basin probably was in close proximity to the ocean throughout much of its existence. -
Plesiadapis ROCK ROCK UNIT COLUMN PERIOD EPOCH AGES MILLIONS of YEARS AGO Common Name: Holocene Oahe .01 Lemur-Like Mammal
North Dakota Stratigraphy Plesiadapis ROCK ROCK UNIT COLUMN PERIOD EPOCH AGES MILLIONS OF YEARS AGO Common Name: Holocene Oahe .01 Lemur-like mammal Coleharbor Pleistocene QUATERNARY Classification: 1.8 Pliocene Unnamed 5 Miocene Class: Mammalia 25 Arikaree Order: Primates Family: Plesiadapidae Brule Oligocene 38 South Heart Chadron Jaw of the lemur-like mammal, Plesiadapis. Bullion Creek Chalky Buttes Camels Butte Formation, Billings County. Width 24 mm. Science Museum of Eocene Golden 55 Valley Bear Den Minnesota Collection. Sentinel Butte TERTIARY Description: Plesiadapis was a lemur-like mammal the size of a modern-day beaver, about 2 ½ feet long. They had long tails, agile limbs with Bullion Paleocene Creek claws rather than nails, and eyes placed on the sides of their heads. Unlike modern primates, the head of Plesiadapis had a long snout Slope with rodentlike jaws and teeth and long, gnawing incisors Cannonball separated by a gap from its molars. It was well-adapted for climbing in trees with its long, clawed fingers and toes. Ludlow 65 Plesiadapis inhabited the vast forests that covered western North Hell Creek Dakota when the climate was subtropical, similar to south Florida today. Fox Hills ACEOUS Pierre CRET 84 Niobrara Carlile Carbonate Calcareous Shale Claystone/Shale Siltstone Sandstone Sand & Gravel Mudstone Lignite Glacial Drift Plesiadapis. Painting courtesy of Simon and Schuster Publishing Company. Locations where fossils have been found ND State Fossil Collection Prehistoric Life of ND Map North Dakota Geological Survey Home Page. -
Recherches De Mammiferes Paleogenes Dans Les Departements De L'aisne Et De La Marne Pendant La Deuxieme Moitie Du Vingtieme Siecle
RECHERCHES DE MAMMIFERES PALEOGENES DANS LES DEPARTEMENTS DE L'AISNE ET DE LA MARNE PENDANT LA DEUXIEME MOITIE DU VINGTIEME SIECLE par Pierre LOUIS * SOMMAIRE Page Résumé, Abstract , ' , , , ' , , , , , ' , , , , , , , , , , , ' , , ' , , ' , , ' , , , , , , , , , , ' , , ' , , , ' , , ' , , , ' , , ' , , , , 84 Historique des découvertes jusqu'à la fin de la première moitié du XXème siècle, , , ' , , , ' , , , , , , , 84 Gisements à mammifères exploités depuis 1950 , , , , , , , , , , , , , , , , , , , , , , , , ' , , , , , , , , , , , , , , , , 88 Thanétien ,',',',""',""""',"""',',,",","',",",,""',,",,',,', 88 Les gisements , , , , ' , , ' , , , , , , , , , , , , , ' , , , ' , , ' , , , , , ' , , , ' , , ' , , , ' , , ' , , , ' , , ' , , ' , , 88 Environnement du Pays rémois au Thanétien supérieur, , , , , , , , , , , , , , ' , , ' , , , ' , , ' , , , , 90 Yprésien "',""",",""",",,",,',,",",,',,",,',,',,",",',',,',,', 91 Les gisements du début de l'Yprésien ,,""""""""',',"",',,',',',,',", 91 Environnement de Reims et d'Epernay au début de l'Yprésien, , , " , ' , ' , , , " , , , , , , , , , 95 Les gisements de l'Yprésien supérieur, , , , , , , ' , , ' , , ' , , , , , , , , , ' , , ' , , ' , , , ' , , , , , , ' , 96 Environnement de l'Est du Bassin Parisien à l'Yprésien , , , , , , , , , , , , , , , , , , , , , , , ' , , , , 99 Lutétien "","',",,',,",",,',,",,',',',,',,',',',",,',,",,',,",",,', 99 Bartonien , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , ' , , , , , , , , , , , , , , ' , , , , , , , , , , , -
Sectional Geometry in a Simulated Fine Branch Niche
JOURNAL OF MORPHOLOGY 276:759–765 (2015) Mouse Hallucal Metatarsal Cross-Sectional Geometry in a Simulated Fine Branch Niche Craig D. Byron,1* Anthony Herrel,2,3 Elin Pauwels,4 Amelie De Muynck,4 and Biren A. Patel5,6 1Department of Biology, Mercer University, Macon, Georgia 2Departement d’Ecologie et de Gestion de la Biodiversite, CNRS/MNHN, Paris, France 3Department of Vertebrate Evolutionary Morphology, Ghent University, Gent, Belgium 4Department of Physics and Astronomy, Ghent University, UGCT, Ghent, Belgium 5Department of Cell and Neurobiology, Keck School of Medicine, University of Southern California, Los Angeles, California 6Human and Evolutionary Biology Section, Department of Biological Sciences, University of Southern California, Los Angeles, California ABSTRACT Mice raised in experimental habitats con- arboreal substrates (Le Gros Clark, 1959; Cart- taining an artificial network of narrow “arboreal” sup- mill, 1972; Szalay and Drawhorn, 1980; Sussman, ports frequently use hallucal grasps during locomotion. 1991; Schmitt and Lemelin, 2002; Bloch et al., Therefore, mice in these experiments can be used to 2007; Sargis et al., 2007). There are also examples model a rudimentary form of arboreal locomotion in an of rodent (Orkin and Pontzer, 2011), carnivoran animal without other morphological specializations for using a fine branch niche. This model would prove use- (Fabre et al., 2013), marsupial (Lemelin and ful to better understand the origins of arboreal behav- Schmitt, 2007; Shapiro et al., 2014), and nonmam- iors in mammals like primates. In this study, we malian vertebrates including frogs, lizards, and examined if locomotion on these substrates influences birds (Herrel et al., 2013; Sustaita et al., 2013) the mid-diaphyseal cross-sectional geometry of mouse that are effective in this niche without primate- metatarsals. -
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. -
Late Paleocene) of the Eastern Crazy Mountain Basin, Montana
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 26, NO. 9, p. 157-196 December 3 1, 1983 MAMMALIAN FAUNA FROM DOUGLASS QUARRY, EARLIEST TIFFANIAN (LATE PALEOCENE) OF THE EASTERN CRAZY MOUNTAIN BASIN, MONTANA BY DAVID W. KRAUSE AND PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director Gerald R. Smith, Editor This series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan, 48 109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. MAMMALIAN FAUNA FROM DOUGLASS QUARRY, EARLIEST TIFFANIAN (LATE PALEOCENE) OF THE EASTERN CRAZY MOUNTAIN BASIN, MONTANA BY David W. ~rause'and Philip D. ~in~erich' Abstract.-Douglass Quarry is the fourth major locality to yield fossil mammals in the eastern Crazy Mountain Basin of south-central Montana. It is stratigraphically intermediate between Gidley and Silberling quarries below, which are late Torrejonian (middle Paleocene) in age, and Scarritt Quarry above, which is early Tiffanian (late Paleocene) in age. The stratigraphic position of Douglass Quarry and the presence of primitive species of Plesiadapis, Nannodectes, Phenacodus, and Ectocion (genera first appearing at the Torrejonian-Tiffanian boundary) combine to indicate an earliest Tiffanian age. -
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. -
Cynocephalid Dermopterans from the Palaeogene of South Asia (Thailand, Myanmar and Pakistan): Systematic, Evolutionary and Palaeobiogeographic Implications
CynocephalidBlackwell Publishing Ltd dermopterans from the Palaeogene of South Asia (Thailand, Myanmar and Pakistan): systematic, evolutionary and palaeobiogeographic implications LAURENT MARIVAUX, LOÏC BOCAT, YAOWALAK CHAIMANEE, JEAN-JACQUES JAEGER, BERNARD MARANDAT, PALADEJ SRISUK, PAUL TAFFOREAU, CHOTIMA YAMEE & JEAN-LOUP WELCOMME Accepted: 5 April 2006 Marivaux, L., Bocat, L., Chaimanee, Y., Jaeger, J.-J., Marandat, B., Srisuk, P., Tafforeau, P., doi:10.1111/j.1463-6409.2006.00235.x Yamee, C. & Welcomme, J.-L. (2006). Cynocephalid dermopterans from the Palaeogene of South Asia (Thailand, Myanmar and Pakistan): systematic, evolutionary and palaeobiogeographic implications. — Zoologica Scripta, 35, 395–420. Cynocephalid dermopterans (flying lemurs) are represented by only two living genera (Cynocephalus and Galeopterus), which inhabit tropical rainforests of South-East Asia. Despite their very poor diversity and their limited distribution, dermopterans play a critical role in higher- level eutherian phylogeny inasmuch as they represent together with Scandentia (tree-shrew) the sister group of the Primates clade (Plesiadapiformes + Euprimates). However, unlike primates, for which the fossil record extends back to the early Palaeogene on all Holarctic continents and in Africa, the evolutionary history of the order Dermoptera sensu stricto (Cynocephalidae) has so far remained undocumented, with the exception of a badly preserved fragment of mandi- ble from the late Eocene of Thailand (Dermotherium major). In this paper, we described newly discovered fossil dermopterans (essentially dental remains) from different regions of South Asia (Thailand, Myanmar, and Pakistan) ranging from the late middle Eocene to the late Oligocene. We performed microtomographic examinations at the European Synchrotron Radiation Facility (ESRF, Grenoble, France) to analyse different morphological aspects of the fossilized jaws. -
Oldest Known Euarchontan Tarsals and Affinities of Paleocene Purgatorius to Primates
Oldest known euarchontan tarsals and affinities of Paleocene Purgatorius to Primates Stephen G. B. Chestera,b,c,1, Jonathan I. Blochd, Doug M. Boyere, and William A. Clemensf aDepartment of Anthropology and Archaeology, Brooklyn College, City University of New York, Brooklyn, NY 11210; bNew York Consortium in Evolutionary Primatology, New York, NY 10024; cDepartment of Anthropology, Yale University, New Haven, CT 06520; dFlorida Museum of Natural History, University of Florida, Gainesville, FL 32611; eDepartment of Evolutionary Anthropology, Duke University, Durham, NC 27708; and fUniversity of California Museum of Paleontology, Berkeley, CA 94720 Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved December 24, 2014 (received for review November 12, 2014) Earliest Paleocene Purgatorius often is regarded as the geologi- directly outside Placentalia with the contemporary condylarths cally oldest primate, but it has been known only from fossilized (archaic ungulates) Protungulatum and Oxyprimus (10–12). How- dentitions since it was first described half a century ago. The den- ever, the addition of new tarsal data for Purgatorius and increased tition of Purgatorius is more primitive than those of all known taxon sampling, including a colugo and four plesiadapiforms, using living and fossil primates, leading some researchers to suggest this same matrix, results in a strict consensus tree that supports that it lies near the ancestry of all other primates; however, others a monophyletic Euarchonta with Sundatheria (treeshrews and have questioned its affinities to primates or even to placental colugos) as the sister group to a fairly unresolved Primates clade mammals. Here we report the first (to our knowledge) nondental that includes Purgatorius (Fig. -
A Note on the Origin of Rodents
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by American Museum of Natural History Scientific... PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2037 JULY 7, I96I A Note on the Origin of Rodents BY MALCOLM C. MCKENNA Knowledge of Paleocene rodents is still restricted to a single species, Paramys atavus, from a single locality, the Eagle Coal Mine at Bear Creek, Montana. The age of this deposit is late Paleocene. Incisors of P. atavus were first described by Simpson (1928, p. 14), but were referred by him to the Multituberculata. Jepsen (1937) recognized the true affinities of the incisors and described a newly found lower molar. No additional material has been reported since 1937. The purpose of the present paper is to place on record the morphology of a recently identified upper cheek tooth of Paramys atavus and to discuss briefly its significance. I am in- debted to Drs. Albert E. Wood and Mary Dawson for helpful comments. Mr. Chester Tarka prepared the figure. ORDER RODENTIA FAMILY PARAMYIDAE GENUS PARAMYS LEIDY, 1871 Paramys atavusJepsen, 1937 MATERIAL: A.M.N.H. No. 22195 (fig. 1), a left P 4, M 1, or M 2, figured by Simpson (1929, p. 10, fig. 2). LOCALITY: Eagle Coal Mine, Bear Creek, Carbon County, Montana. FORMATION: Polecat Bench formation (Fort Union of the United States Geological Survey and others). AGE: Tiffanian (= approximately late, but not latest, Paleocene). DESCRIPTION: Small, tritubercular, rodent upper cheek tooth with 2 AMERICAN MUSEUM NOVITATES NO.