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Diagnosis and Differentiation of the Order Primates
YEARBOOK OF PHYSICAL ANTHROPOLOGY 30:75-105 (1987) Diagnosis and Differentiation of the Order Primates FREDERICK S. SZALAY, ALFRED L. ROSENBERGER, AND MARIAN DAGOSTO Department of Anthropolog* Hunter College, City University of New York, New York, New York 10021 (F.S.S.); University of Illinois, Urbanq Illinois 61801 (A.L. R.1; School of Medicine, Johns Hopkins University/ Baltimore, h4D 21218 (M.B.) KEY WORDS Semiorders Paromomyiformes and Euprimates, Suborders Strepsirhini and Haplorhini, Semisuborder Anthropoidea, Cranioskeletal morphology, Adapidae, Omomyidae, Grades vs. monophyletic (paraphyletic or holophyletic) taxa ABSTRACT We contrast our approach to a phylogenetic diagnosis of the order Primates, and its various supraspecific taxa, with definitional proce- dures. The order, which we divide into the semiorders Paromomyiformes and Euprimates, is clearly diagnosable on the basis of well-corroborated informa- tion from the fossil record. Lists of derived features which we hypothesize to have been fixed in the first representative species of the Primates, Eupri- mates, Strepsirhini, Haplorhini, and Anthropoidea, are presented. Our clas- sification of the order includes both holophyletic and paraphyletic groups, depending on the nature of the available evidence. We discuss in detail the problematic evidence of the basicranium in Paleo- gene primates and present new evidence for the resolution of previously controversial interpretations. We renew and expand our emphasis on postcra- nial analysis of fossil and living primates to show the importance of under- standing their evolutionary morphology and subsequent to this their use for understanding taxon phylogeny. We reject the much advocated %ladograms first, phylogeny next, and scenario third” approach which maintains that biologically founded character analysis, i.e., functional-adaptive analysis and paleontology, is irrelevant to genealogy hypotheses. -
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. -
The Paleontology Synthesis Project and Establishing a Framework for Managing National Park Service Paleontological Resource Archives and Data
Lucas, S.G. and Sullivan, R.M., eds., 2018, Fossil Record 6. New Mexico Museum of Natural History and Science Bulletin 79. 589 THE PALEONTOLOGY SYNTHESIS PROJECT AND ESTABLISHING A FRAMEWORK FOR MANAGING NATIONAL PARK SERVICE PALEONTOLOGICAL RESOURCE ARCHIVES AND DATA VINCENT L. SANTUCCI1, JUSTIN S. TWEET2 and TIMOTHY B. CONNORS3 1National Park Service, Geologic Resources Division, 1849 “C” Street, NW, Washington, D.C. 20240, [email protected]; 2National Park Service, 9149 79th Street S., Cottage Grove, MN 55016, [email protected]; 3National Park Service, Geologic Resources Division, 12795 W. Alameda Parkway, Lakewood, CO 80225, [email protected] Abstract—The National Park Service Paleontology Program maintains an extensive collection of digital and hard copy documents, publications, photographs and other archives associated with the paleontological resources documented in 268 parks. The organization and preservation of the NPS paleontology archives has been the focus of intensive data management activities by a small and dedicated team of NPS staff. The data preservation strategy complemented the NPS servicewide inventories for paleontological resources. The first phase of the data management, referred to as the NPS Paleontology Synthesis Project, compiled servicewide paleontological resource data pertaining to geologic time, taxonomy, museum repositories, holotype fossil specimens, and numerous other topics. In 2015, the second phase of data management was implemented with the creation and organization of a multi-faceted digital data system known as the NPS Paleontology Archives and NPS Paleontology Library. Two components of the NPS Paleontology Archives were designed for the preservation of both park specific and servicewide paleontological resource archives and data. A third component, the NPS Paleontology Library, is a repository for electronic copies of geology and paleontology publications, reports, and other media. -
Pliocene and Early Pleistocene) Faunas from New Mexico
Chapter 12 Mammalian Biochronology of Blancan and Irvingtonian (Pliocene and Early Pleistocene) Faunas from New Mexico GARY S. MORGAN1 AND SPENCER G. LUCAS2 ABSTRACT Signi®cant mammalian faunas of Pliocene (Blancan) and early Pleistocene (early and medial Irvingtonian) age are known from the Rio Grande and Gila River valleys of New Mexico. Fossiliferous exposures of the Santa Fe Group in the Rio Grande Valley, extending from the EspanÄola basin in northern New Mexico to the Mesilla basin in southernmost New Mexico, have produced 21 Blancan and 6 Irvingtonian vertebrate assemblages; three Blancan faunas occur in the Gila River Valley in the Mangas and Duncan basins in southwestern New Mexico. More than half of these faunas contain ®ve or more species of mammals, and many have associated radioisotopic dates and/or magnetostratigraphy, allowing for correlation with the North American land-mammal biochronology. Two diverse early Blancan (4.5±3.6 Ma) faunas are known from New Mexico, the Truth or Consequences Local Fauna (LF) from the Palomas basin and the Buckhorn LF from the Mangas basin. The former contains ®ve species of mammals indicative of the early Blancan: Borophagus cf. B. hilli, Notolagus lepusculus, Neo- toma quadriplicata, Jacobsomys sp., and Odocoileus brachyodontus. Associated magnetostra- tigraphic data suggest correlation with either the Nunivak or Cochiti Subchrons of the Gilbert Chron (4.6±4.2 Ma), which is in accord with the early Blancan age indicated by the mam- malian biochronology. The Truth or Consequences LF is similar in age to the Verde LF from Arizona, and slightly older than the Rexroad 3 and Fox Canyon faunas from Kansas. -
Resolving the Relationships of Paleocene Placental Mammals
Biol. Rev. (2015), pp. 000–000. 1 doi: 10.1111/brv.12242 Resolving the relationships of Paleocene placental mammals Thomas J. D. Halliday1,2,∗, Paul Upchurch1 and Anjali Goswami1,2 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, U.K. 2Department of Genetics, Evolution and Environment, University College London, Gower Street, London WC1E 6BT, U.K. ABSTRACT The ‘Age of Mammals’ began in the Paleocene epoch, the 10 million year interval immediately following the Cretaceous–Palaeogene mass extinction. The apparently rapid shift in mammalian ecomorphs from small, largely insectivorous forms to many small-to-large-bodied, diverse taxa has driven a hypothesis that the end-Cretaceous heralded an adaptive radiation in placental mammal evolution. However, the affinities of most Paleocene mammals have remained unresolved, despite significant advances in understanding the relationships of the extant orders, hindering efforts to reconstruct robustly the origin and early evolution of placental mammals. Here we present the largest cladistic analysis of Paleocene placentals to date, from a data matrix including 177 taxa (130 of which are Palaeogene) and 680 morphological characters. We improve the resolution of the relationships of several enigmatic Paleocene clades, including families of ‘condylarths’. Protungulatum is resolved as a stem eutherian, meaning that no crown-placental mammal unambiguously pre-dates the Cretaceous–Palaeogene boundary. Our results support an Atlantogenata–Boreoeutheria split at the root of crown Placentalia, the presence of phenacodontids as closest relatives of Perissodactyla, the validity of Euungulata, and the placement of Arctocyonidae close to Carnivora. Periptychidae and Pantodonta are resolved as sister taxa, Leptictida and Cimolestidae are found to be stem eutherians, and Hyopsodontidae is highly polyphyletic. -
Report of the Workshop on Geologic Applications of Remote Sensing To
General Disclaimer One or more of the Following Statements may affect this Document This document has been reproduced from the best copy furnished by the organizational source. It is being released in the interest of making available as much information as possible. This document may contain data, which exceeds the sheet parameters. It was furnished in this condition by the organizational source and is the best copy available. This document may contain tone-on-tone or color graphs, charts and/or pictures, which have been reproduced in black and white. This document is paginated as submitted by the original source. Portions of this document are not fully legible due to the historical nature of some of the material. However, it is the best reproduction available from the original submission. Produced by the NASA Center for Aerospace Information (CASI) lu i^`i/ E86-10002 (F86- 10012 NASA-CP-176211) P£POPT OF THE 99 WOPKSHOP ON GEOLOGIC APPLICATIONS nF P.FM.nTD. SENSING ^0 THE STUDY OF SEDIMEN T APY 3ASINS 09 ,let Propulsion Lab.) 81 p HC A'1 5/MF A01 4 v JPL PUBLICATION 85-44 0 Report of the Workshop on Geologic Applications of Remot. S'ensing to the Study of Sedimentary Basins Lakewood, Colorado January 10-11, 1985 Edited by Harold Lang YI August 1. 1985 Sponsored by the Jet Propulsion Laboratory California Institute of Technology Pasadena, California under the auspices of the Earth Science and Applications Division National Aeronautics and Space Administration This publication was prepared by the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administrator. -
Pliocene Climates: Scenario for Global Warming
Department of the Interior U.S. Geological Survey Pliocene Climates: Scenario for Global Warming Abstracts from USGS Workshop, Denver, Colorado, October 23 - 25,1989 Edited by Linda B. Gosnell and Richard Z. Poore U.S. Geological Survey, Reston, VA 22092 Open-File Report 90-64 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Introduction: USGS Workshop on Pliocene Climates The US. Geological Survey (USGS) held a work tate quantitative estimates of environmental informa shop on Pliocene climates in Denver, Colorado on tion and the development of regional and global pat October 23-25,1989. The workshop brought together terns of climate data. members of the USGS who are working on a long- Better understanding of Pliocene climates, their ev term project to understand and map Pliocene cli olution, and rates and causes of change will provide mates and environments of the Northern Hemi important dues to future earth systems changes and sphere with interested collaborators from the USSR, impacts that will occur as a result of a greenhouse- The Geological Survey of Canada, the National Cen effect global warming. A major goal of the USGS Pli ter for Atmospheric Research, and the Institute for ocene Project is to produce a synoptic map or "snap Arctic and Alpine Research, University of Colorado. shot" of climate parameters during a time in the Plio Paleoclimate researchers from the USSR attended the cene representing conditions that are significantly workshop as part of an exchange and cooperative warmer than modern climates. The Pliocene "Scenar study of Pliocene climates that is organized under the io for Global Warming" will provide a means for test auspices of Working Group VIII of the US-USSR Bi ing and validating results of general circulation mod lateral Agreement on Protection of the Environment els (GCMs) which attempt to model global warming. -
Tarsioid Primate from the Early Tertiary of the Mongolian People's Republic
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. 22 1977 No.2 DEMBERELYIN DASHZEVEG & MALCOLM C. McKENNA TARSIOID PRIMATE FROM THE EARLY TERTIARY OF THE MONGOLIAN PEOPLE'S REPUBLIC Abstract. - A tiny tarsioid primate occurs in early Eocene sediments of the Naran Bulak Formation, southern Gobi Desert, Mongolian People's Republic. The new primate, Altanius orlovi, new genus and species, is an anaptomorphine omomyid and t,herefore belongs to a primarily American group of primates. Altanius is appar ently not a direct ancestor of the Asian genus Tarsius. American rather than Euro pean zoogeographic affinities are indicated, and this in turn supports the view that for a time in the earliest Eocene the climate of the Bering Route was sufficiently warm to support a primate smaller than Microcebus. INTRODUCTION The discovery of a new genus and species of tiny fossil primate, Altanius orlovi, from the upper part of the early Tertiary Naran Bulak Formation of the southwestern Mongolian People's Republic extends the known geologic range of the order Primates in Asia back to the very be ginning of the Eocene and establishes that anaptomorphine tarsioid pri mates were living in that part of the world a little more than fifty million years ago. Previously, the oldest known Asian animals referred by various authors to the Primates were Pondaungia Pilgrim, 1927, Hoanghonius Zdansky, 1930, Amphipithecus Colbert, 1937, Lushius Chow, 1961, and Lantianius Chow, 1964, described on the basis of a handfull of specimens from late Eocene deposits in China and Burma about ten million years or more younger than the youngest part of the Naran Bulak Formation. -
Curriculum Vitae Christopher J
C. J. Bell Curriculum Vitae Christopher J. Bell 10 January, 2012 Professor The University of Texas at Austin Department of Geological Sciences 1 University Station C1100 Austin, TX 78712-0254 (512) 471-7301 [email protected] Date and Place of Birth: 12 March, 1966; Marietta, Georgia, U.S.A. Education University of California, Berkeley, California. Department of Integrative Biology. Ph.D., 1997. Northern Arizona University, Flagstaff, Arizona. Quaternary Studies Program. M.S., 1990. The College of William and Mary in Virginia, Williamsburg, Virginia. Department of Geology. B.S., 1988. Professional Appointments - Current Sep., 2010 – present: Professor, Department of Geological Sciences, The University of Texas at Austin. April, 2007 – present: Research Associate, Department of Terrestrial Vertebrates, Western Australian Museum, Perth, Western Australia. Professional Appointments - Historical Sep., 2003 – Sept. 2010 : Associate Professor, Department of Geological Sciences, The University of Texas at Austin. September, 1997 - August, 2003: Assistant Professor, Department of Geological Sciences, The University of Texas at Austin. January, 1997 - May, 1997: Graduate Student Instructor, ‘Natural History of the Vertebrates,’ Department of Integrative Biology, U.C. Berkeley. August - December, 1996: Curatorial Assistant, Museum of Vertebrate Zoology, U.C. Berkeley. June - August, 1996: Graduate Student Curatorial Assistant, Museum of Paleontology, U.C. Berkeley. August - December, 1995: Graduate Student Instructor, ‘Morphology of the Vertebrate Skeleton,’ Department of Integrative Biology, U.C. Berkeley. June - August, 1995: Move Coordinator, Museum of Paleontology, U.C. Berkeley. January - May, 1995: Graduate Student Instructor, ‘The Age of Mammals,’ Department of Integrative Biology, U.C. Berkeley. 1 C. J. Bell August - December, 1994: Research Assistant to A. D. Barnosky, Porcupine Cave Project, Museum of Paleontology, U. -
Late Paleocene) Mammals from Cochrane 2, Southwestern Alberta, Canada
New earliest Tiffanian (late Paleocene) mammals from Cochrane 2, southwestern Alberta, Canada CRAIG S.SCOTT, RICHARD C.FOX, and GORDON P.YOUZWYSHYN Scott, C.S., Fox, R.C., and Youzwyshyn, G.P. 2002. New earliest Tiffanian (late Paleocene) mammals from Cochrane 2, southwestern Alberta, Canada. Acta Palaeontologica Polonica 47 (4): 691–704. New mammalian fossils at Cochrane 2, Paskapoo Formation, Alberta, Canada, document five new species and two new combinations: Ptilodus gnomus sp.nov.and Baiotomeus russelli sp.nov.(Multituberculata), Thryptacodon orthogonius comb.nov.and Litomylus grandaletes sp.nov.(“Condylarthra”), Pararyctes rutherfordi sp.nov., Bessoecetor septentrionalis comb.nov.,and Paleotomus junior sp.nov.(Eutheria incertae sedis).These new taxa supplement a taxo − nomically diverse Cochrane 2 local fauna, representing one of the most species rich Paleocene mammalian localities in the world.An earliest Tiffanian age is estimated for the locality based on the presence of the index taxa Plesiadapis praecursor, Nannodectes intermedius, and Ectocion collinus.The Cochrane 2 local fauna fails to demonstrate a decrease in species number relative to those of late Torrejonian localities from the United States, as would be predicted by current paleoclimate scenarios; the rarity of earliest Tiffanian localities in North America suggests sampling error as a partial ex− planation for the apparent incongruity. Key words: Multituberculata, “Condylarthra”, Eutheria, Paleocene, Paskapoo Formation, Canada. Craig S. Scott [[email protected]] and Richard C. Fox [[email protected]], Laboratory for Vertebrate Paleon− tology, Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada T6G 2E9; Gordon P. Youzwyshyn [[email protected]], Grant MacEwan Community College, Edmonton, Canada, T5J 4S2. -
(Arborimus Longicaudus), Sonoma Tree Vole (A. Pomo), and White-Footed Vole (A
United States Department of Agriculture Annotated Bibliography of the Red Tree Vole (Arborimus longicaudus), Sonoma Tree Vole (A. pomo), and White-Footed Vole (A. albipes) Forest Pacific Northwest General Technical Report August Service Research Station PNW-GTR-909 2016 In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all pro- grams). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimi- nation Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/com- plaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. -
Polyphyly, Paraphyly, Provinciality, and the Promise Of
Palaeontologia Electronica http://palaeo-electronica.org Polyphyly, paraphyly, provinciality, and the promise of intercontinental correlation: Charles Repenning’s contributions to the study of arvicoline rodent evolution and biochronology Christopher J. Bell and Christopher N. Jass “The science of systematics has long been affected by profound philosophical preconceptions, which have been all the more influential for being usually covert, even subconscious.” George Gaylord Simpson, 1953 ABSTRACT We review the history of Charles A. Repenning’s contributions to the study of arvi- coline rodents, with emphasis on his philosophical approach to the study of fossils, their taxonomic affinities, biostratigraphic distribution, and biochronologic significance. Rep viewed these issues in an explicitly evolutionary context under which gradational and anagenetic change was accepted as the dominant mode of evolution. He recog- nized a polyphyletic origin of five independent arvicoline lineages, and viewed para- phyletic higher taxa within those lineages as some of the best evidence of evolution. That perspective, combined with his view that the rock record preserved an adequate material history of population-level evolution in arvicolines, led him to adopt taxonomic practices that can be confusing and cumbersome to non-specialists. He used fossils of arvicolines as tools to develop an intercontinental correlation scheme extending across North America, northern Asia, and Europe. A core component of his correlation scheme was the hypothesis of a bi-directionally balanced history of dispersal events across the Arctic Ocean borderland that introduced comparable arvicoline taxa into Europe and North America from source areas in Asia. Within North America, his bio- chronology was structured around a concept of immigrant taxa, although definitive establishment of immigrant status often was an elusive goal.