A Study of the Pulp Cavities and Roots of the Lower Premolars and Molars of Prosimii, Ceboidea and Cercopithecoidea1
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SMC 136 Gazin 1958 1 1-112.Pdf
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 136, NUMBER 1 Cftarlesi 3B, anb JKarp "^aux OTalcott 3^es(earcf) Jf unb A REVIEW OF THE MIDDLE AND UPPER EOCENE PRIMATES OF NORTH AMERICA (With 14 Plates) By C. LEWIS GAZIN Curator, Division of Vertebrate Paleontology United States National Museum Smithsonian Institution (Publication 4340) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JULY 7, 1958 THE LORD BALTIMORE PRESS, INC. BALTIMORE, MD., U. S. A. CONTENTS Page Introduction i Acknowledgments 2 History of investigation 4 Geographic and geologic occurrence 14 Environment I7 Revision of certain lower Eocene primates and description of three new upper Wasatchian genera 24 Classification of middle and upper Eocene forms 30 Systematic revision of middle and upper Eocene primates 31 Notharctidae 31 Comparison of the skulls of Notharctus and Smilodectcs z:^ Omomyidae 47 Anaptomorphidae 7Z Apatemyidae 86 Summary of relationships of North American fossil primates 91 Discussion of platyrrhine relationships 98 References 100 Explanation of plates 108 ILLUSTRATIONS Plates (All plates follow page 112) 1. Notharctus and Smilodectes from the Bridger middle Eocene. 2. Notharctus and Smilodectes from the Bridger middle Eocene. 3. Notharctus and Smilodectcs from the Bridger middle Eocene. 4. Notharctus and Hemiacodon from the Bridger middle Eocene. 5. Notharctus and Smilodectcs from the Bridger middle Eocene. 6. Omomys from the middle and lower Eocene. 7. Omomys from the middle and lower Eocene. 8. Hemiacodon from the Bridger middle Eocene. 9. Washakius from the Bridger middle Eocene. 10. Anaptomorphus and Uintanius from the Bridger middle Eocene. 11. Trogolemur, Uintasorex, and Apatcmys from the Bridger middle Eocene. 12. Apatemys from the Bridger middle Eocene. -
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. -
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. -
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. -
The Genus Cantius and the Phylogenetic Importance of North American Primates Dakota R
The Genus Cantius and the Phylogenetic Importance of North American Primates Dakota R. Pavell1, James E. Loudon1, Robert L. Anemone2 1Department of Anthropology, East Carolina University 2Department of Anthropology, University of North Carolina at Greensboro Introduction Results Discussion During the Eocene Epoch (54 to 33 million years ago), the world experienced a Avizo-generated 3D images of Cantius teeth revealed the 1. Project Status: period of global warming with temperatures ranging from 9 to 23 degrees following distinctive traits: • This project began in July of 2020. Celsius higher than today. The rise in average temperatures created an • Currently ongoing environment suitable for nonhuman primates to inhabit North America. One of • Well developed, mesially positioned paraconids on lower 2. Currently: These data further support the hypothesis that the most common groups of primates during the Eocene Epoch were the molars. Cantius was the first Notharctine primate to evolve. After Notharctine primates. The Notharctine primates had five primary genera: • Conical shaped molars Cantius, there appear to be two major lineage splits within Cantius, Pelycodus, Copelemur, Smilodectes, and Notharctus. • Comparatively short and wide upper molars the Notharctine primates: • Unfused mandibular symphysis • Split 1: Pelycodus and Copelemur (Wasatchian North Purpose American Land Mammal Age – Early Eocene). This project focuses on the dental morphology of Cantius in order to i.) better • Split 2: Smilodectes and Notharctus (Bridgerian North understand its evolutionary relationships to the other Notharctine primates and American Land Mammal Age – Middle/Late Eocene). ii.) its relationship to extant primates. Cantius exhibits a distinct anterior dental The dental morphology of Cantius morphology that can be observed in extinct and extant strepsirrhine primates, suggests this genus is ancestral including modern-day Malagasy lemurs. -
Evolutionary History of Lorisiform Primates
Evolution: Reviewed Article Folia Primatol 1998;69(suppl 1):250–285 oooooooooooooooooooooooooooooooo Evolutionary History of Lorisiform Primates D. Tab Rasmussen, Kimberley A. Nekaris Department of Anthropology, Washington University, St. Louis, Mo., USA Key Words Lorisidae · Strepsirhini · Plesiopithecus · Mioeuoticus · Progalago · Galago · Vertebrate paleontology · Phylogeny · Primate adaptation Abstract We integrate information from the fossil record, morphology, behavior and mo- lecular studies to provide a current overview of lorisoid evolution. Several Eocene prosimians of the northern continents, including both omomyids and adapoids, have been suggested as possible lorisoid ancestors, but these cannot be substantiated as true strepsirhines. A small-bodied primate, Anchomomys, of the middle Eocene of Europe may be the best candidate among putative adapoids for status as a true strepsirhine. Recent finds of Eocene primates in Africa have revealed new prosimian taxa that are also viable contenders for strepsirhine status. Plesiopithecus teras is a Nycticebus- sized, nocturnal prosimian from the late Eocene, Fayum, Egypt, that shares cranial specializations with lorisoids, but it also retains primitive features (e.g. four premo- lars) and has unique specializations of the anterior teeth excluding it from direct lorisi- form ancestry. Another unnamed Fayum primate resembles modern cheirogaleids in dental structure and body size. Two genera from Oman, Omanodon and Shizarodon, also reveal a mix of similarities to both cheirogaleids and anchomomyin adapoids. Resolving the phylogenetic position of these Africa primates of the early Tertiary will surely require more and better fossils. By the early to middle Miocene, lorisoids were well established in East Africa, and the debate about whether these represent lorisines or galagines is reviewed. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN Vol. 24, No. 15, p. 163-170 (3 text-figs.) September 5, 1975 A NEW GENUS OF ADAPIDAE (MAMMALIA, PRIMATES) FROM THE LATE EOCENE OF SOUTHERN FRANCE, AND ITS SIGNIFICANCE FOR THE ORIGIN OF HIGHER PRIMATES BY PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Gerald R. Smith, Director Robert V. Kesling, Editor Nancy E. Friedland, Editor for this number The 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, 481 04. VOLS. 11-XXIV. Parts of volumes may be obtained if available. Price lists available upon inquiry. printed in Ann Arbor, Michigan by Litho Crafters, Inc. A NEW GENUS OF ADAPIDAE (MAMMALIA, PRIMATES) FROM THE LATE EOCENE OF SOUTHERN FRANCE, AND ITS SIGNIFICANCE FOR THE ORIGIN OF HIGHER PRIMATES BY Philip D. Gingerich Abstract.- A primate mandible from the late Eocene Phosphorites du Quercy of south- ern France, originally described by Stehlin (1 91 2) as Protoadapis brachyrhynchus, is here placed in the new genus Cercamonius. Comparison with other Eocene primates indicates that the genus represents a new subfamily, Cercamoninae, of the lemuriform family Adapidae. -
A Revision of the Eocene Primates of the Genus Notharctus
56.9.81N(1181: 7) Article XXXIV.- A REVISION OF THE EOCENE PRIMATES OF THE GENUS NOTHARCTUS. BY WALTER GRANGER AND WILLIAM K. GREGORY. PLATES CIII-CVII. In 1902 Professor Osborn1 referred to the genus Notharctm Leidy a number of Middle Eocene primates which had been placed in distinct genera by Marsh and by Cope; he traced the successive stages in the evolution of the dentition from the very primitive Pelycodus frugivorwz of the Wasatch, with tritubercular upper molars, to the very advanced No- tharctus (Telmatolestes) crassus of the Bridger; he defined the genera Pely- codus and Notharctus as follows: Pelycodus. Notharctus. Jaw elongate. Mandibular symphy- Jaw stout. Symphysis typically co- sis uncoossified. Superior molars trian- ossified. Superior molars quadrate with gular with rudimentary hypocone; no pronounced hypocone; a mesostyle. mesostyle. In 1903 and 1904 the American Museum expeditions to the Bridger Basin, in charge of W. Granger, discovered much additional material of Notharctus, including a large number of jaws and teeth, a nearly perfect skull and two incomplete skeletons. The dentition, skull and skeletons will shortly be described from the morphological and phylogenetic view- point in the 'Studies on the Evolution of the Primates' by W. K. Gregory; the jaws and teeth of the Bridger Notharctinae are studied with reference to their generic and specific characters in the present paper. In 1905 and subsequent years the American Museum expeditions to the Lower Eocene formations of Wyoming and New Mexico, in charge of W. Granger, secured large collections of primate jaws and teeth from ascending horizons; this material was described in 1915 by Dr. -
Evidence for a Grooming Claw in a North American Adapiform Primate: Implications for Anthropoid Origins
City University of New York (CUNY) CUNY Academic Works Publications and Research Brooklyn College 2012 Evidence for a Grooming Claw in a North American Adapiform Primate: Implications for Anthropoid Origins Stephanie Maiolino Stony Brook University Doug M. Boyer CUNY Brooklyn College Jonathan I. Bloch University of Florida Christopher C. Gilbert CUNY Hunter College Joseph Groenke Stony Brook University How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/bc_pubs/76 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Evidence for a Grooming Claw in a North American Adapiform Primate: Implications for Anthropoid Origins Stephanie Maiolino1*, Doug M. Boyer2*, Jonathan I. Bloch3, Christopher C. Gilbert4, Joseph Groenke5 1 Stony Brook University, Stony Brook, New York, United States of America, 2 Brooklyn College, City University of New York, Brooklyn, New York, United States of America, 3 Florida Museum of Natural History, University of Florida, Gainesville, Florida, United States of America, 4 Hunter College, City University of New York, New York, New York, United States of America, 5 Stony Brook University, Stony Brook, New York, United States of America Abstract Among fossil primates, the Eocene adapiforms have been suggested as the closest relatives of living anthropoids (monkeys, apes, and humans). Central to this argument is the form of the second pedal digit. Extant strepsirrhines and tarsiers possess a grooming claw on this digit, while most anthropoids have a nail. While controversial, the possible presence of a nail in certain European adapiforms has been considered evidence for anthropoid affinities. -
Geology* Paleontology, and Correlation of Eocene Volcaniclastic Rocks, Southeast Absaroka Range, Hot Springs County, Wyoming
Geology* Paleontology, and Correlation of Eocene Volcaniclastic Rocks, Southeast Absaroka Range, Hot Springs County, Wyoming GEOLOGICAL SURVEY PROFESSIONAL PAPER 1201-A Geology, Paleontology, and Correlation of Eocene Volcaniclastic Rocks, Southeast Absaroka Range, Hot Springs County, Wyoming By T. M. BOWN GEOLOGY OF THE ABSAROKA RANGE, NORTHWEST WYOMING GEOLOGICAL SURVEY PROFESSIONAL PAPER 1201-A Relations of Eocene volcaniclastic rocks and Eocene fossils date the sedimentary and structural evolution of the southeast Absaroka Range, clarify correlations with adjacent areas, and aid in timing large-scale events of gravity faulting UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Bown, Thomas M. Geology, paleontology, and correlation of Eocene volcaniclastic rocks, southeast Absaroka Range, Hot Springs County, Wyoming. (Geological Survey Professional Paper 1201-A) Bibliography: p.71 Supt.ofDocs.no.: II9.I6:1201-A 1. Geology, Stratigraphic Eocene. 2. Volcanic ash, tuff, etc. Wyoming Hot Springs Co. 3. Mammals, Fossil. 4. Stratigraphic correlation Wyoming Hot Springs Co. 5. Geology Wyoming Hot Springs Co. 1. Title. II. Series: United States. Geological Survey. Professional Paper 1201-A. QE692.2.B68 55I.7'84'0978743 80-607125 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract ------------------------------------------------- -
ALPHA TAXONOMY of EOCENE PRIMATES from the GREAT DIVIDE BASIN, WYOMING by Dakota R. Pavell July 2021 Director of Thesis: James E
ALPHA TAXONOMY OF EOCENE PRIMATES FROM THE GREAT DIVIDE BASIN, WYOMING By Dakota R. Pavell July 2021 Director of Thesis: James E. Loudon Major Department: Anthropology The identification of the alpha taxonomy of an extinct species is the first step towards understanding its evolutionary history. The alpha taxonomy refers to the initial classification of the specimen based on the analysis of the observable morphological traits. Many paleoprimatologists, paleobiologists, and paleoanthropologists in the past have conducted these morphological examinations via visible observations or with the use of a microscope. As technology advances, new methods have been introduced that have changed the process of these morphological examinations. I examined eleven specimens that have been previously identified as primate teeth from the Eocene Epoch (~55-41 mya) using a micro computed tomography (CT) scanner located at the Shared Materials and Instrumentation Facility at Duke University. The projections of the specimens taken from the micro CT scanner were imported into Avizo, a three- dimensional visualization software, to generate digital reconstructions. The digital reconstructions were used for further morphological analyses to aid in the identification of the taxonomic classifications of the study specimens. Ten of the specimens were classified into the genus Cantius, the stem genus for a group of lemur-like primates known as the Nothartcine primates. One of the specimens was classified into the genus Copelemur, another Notharctine primate genus. The study specimens were classified through the combination of observable dental morphology and molar measurements. Given the similarities between the study specimens and modern Malagasy lemurs, a brief comparison of dental morphology is also provided. -
Download a High Resolution
DENVER MUSEUM OF NATURE & SCIENCE ANNALS NUMBER 1, SEPTEMBER 1, 2009 Land Mammal Faunas of North America Rise and Fall During the Early Eocene Climatic Optimum Michael O. Woodburne, Gregg F. Gunnell, and Richard K. Stucky WWW.DMNS.ORG/MAIN/EN/GENERAL/SCIENCE/PUBLICATIONS The Denver Museum of Nature & Science Annals is an Frank Krell, PhD, Editor-in-Chief open-access, peer-reviewed scientific journal publishing original papers in the fields of anthropology, geology, EDITORIAL BOARD: paleontology, botany, zoology, space and planetary Kenneth Carpenter, PhD (subject editor, Paleontology and sciences, and health sciences. Papers are either authored Geology) by DMNS staff, associates, or volunteers, deal with DMNS Bridget Coughlin, PhD (subject editor, Health Sciences) specimens or holdings, or have a regional focus on the John Demboski, PhD (subject editor, Vertebrate Zoology) Rocky Mountains/Great Plains ecoregions. David Grinspoon, PhD (subject editor, Space Sciences) Frank Krell, PhD (subject editor, Invertebrate Zoology) The journal is available online at www.dmns.org/main/en/ Steve Nash, PhD (subject editor, Anthropology and General/Science/Publications free of charge. Paper copies Archaeology) are exchanged via the DMNS Library exchange program ([email protected]) or are available for purchase EDITORIAL AND PRODUCTION: from our print-on-demand publisher Lulu (www.lulu.com). Betsy R. Armstrong: project manager, production editor DMNS owns the copyright of the works published in the Ann W. Douden: design and production Annals, which are published under the Creative Commons Faith Marcovecchio: proofreader Attribution Non-Commercial license. For commercial use of published material contact Kris Haglund, Alfred M. Bailey Library & Archives ([email protected]).