14. Rooneyia, Postorbital Closure, and the Beginnings of the Age of Anthropoidea
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
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
LIS T OF ILL US TRA TIONS. IX Pa«e. Apices of ovipositors : o, Polysphincta texaiui Cresson ; &, Eymenoepi- meois iciltii (Cresson); Mandible; c, H. tmltii (Cresson) 389 Apex of ovipositor of Theronia fulvesceiis Cresson 389 Apices of ovipositors: a, Itoplectis canqMisitor Say; b, Apechthis pictir cornis (Cresson) 389 Apex of abdomen of female of Coleocentrus occidentalis 390 Areolet of Lahena grallatoi- (Say) 390 Areolets: a, Tromatohia rufovariata (Cresson) ; b, Itoplectis conquisitor (Say) ; c, Epiurus alboricta (Cresson) 390 Sessile first tergite of Perithous pleuralis (Cresson) 390 Petioatel first tergite of Xorides yukonensis (Rohwer) 390 Mandible of Poemenva americana (Cresson) 391 Female of Labena confusa Rohwer 412 Female of Rhyssella nitida (Cresson) 424 Propodeum of Zonde* picea*u« (Rohwer) 434 Front view of head of Xoi'ides albopictus (Cresson) 437 Propodeum and basal abdominal segments of Xorides albopictus (Cresson) 437 Apical abdomen segments of Xorides albopictus (Cresson) 437 Female of Xorides rileyi (Ashmead) 440 Front view of head of Deuteroxorides caryae (Harrington) 446 Propodeum and basal abdominal segments of Deuteroxorides caryae (Harrington) 446 Apical abdominal segments of Z)c«feroa:ori<Ze« caryae (Harrington) 446 Female of Deuteroxorides caryae (Harrington) 447 Female of Odontomerus canadensis Provancher 459 Female of Phytodietus annulatus (Provancher) 467 Femaie of Phydotietus annulatus (Provancher) 467 Diagram showing relation of dike to vein, Hecla Mine. A, Dike; B, Crushed material with quartz and ore; C, Galena; D, Quartzite wall rock ; width of section 15 feet 481 Showing relation to dikes (A) to vein (B) on No. 1 level of Marsh Mine_ 484 Showing relation of dike (A) to vein (B) on 2,000-foot level of Standard- Mammoth Mine 492 Showing relation of dike (A) to vein (B) on 1,200-foot level of Standard- Mammoth Mine 492 Coleocentrus occidentalis. -
Fossil Lemur from Northern Madagascar (Palaeopropithecidae/Primate Evolution/Postcranium) WILLIAM L
Proc. Natl. Acad. Sci. USA Vol. 88, pp. 9082-9086, October 1991 Evolution Phylogenetic and functional affinities of Babakotia (Primates), a fossil lemur from northern Madagascar (Palaeopropithecidae/primate evolution/postcranium) WILLIAM L. JUNGERSt, LAURIE R. GODFREYt, ELWYN L. SIMONS§, PRITHUJIT S. CHATRATH§, AND BERTHE RAKOTOSAMIMANANA$ tDepartment of Anatomical Sciences, State University of New York, Stony Brook, NY 117948081; tDepartment of Anthropology, University of Massachusetts, Amherst, MA 01003; §Department of Biological Anatomy and Anthropology and Primate Center, Duke University, Durham, NC 27705; and IService de Paldontologie, Universit6 d'Antananarivo, Antananarivo, Madagascar Contributed by Elwyn L. Simons, July 2, 1991 ABSTRACT Recent paleontological expeditions to the An- Craniodental Anatomy and Tooth Shape karana range of northern Madagascar have recovered the partial remains offour individuals ofa newly recognized extinct With an estimated body mass ofjust over 15 kg, Babakotia lemur, Babakoda radofia. Craniodental and postcranial ma- is a medium-sized indroid somewhat larger than the largest terial serve to identify Babakota as a member of the palae- living indrid (Indri) but similar in size to several of the opropithecids (also including the extinct genera Palaeopropith- smallest extinct lemurs, Mesopropithecus and Pachylemur ecus, Archaeoindris, and Mesopropithecus). Living indrids (4). A detailed description of the maxillary dentition of form the sister group to this fossil lade. The postcranial Babakotia exists -
For Early Anthropoids
EVOLUTIONARY ANTHROPOLOGY 24:41–42 (2015) NEWS Westward Ho! for Early Anthropoids etween March 17 and 19, The likely have been an ideal time for dis- quarries, discussed the chronological School for Advanced Research persals from Asia to Africa because of dates of the stratigraphic section, the Bin Santa Fe, New Mexico, the geographical positions of Middle adaptations of the many species, and hosted a short but intense, seminar/ Eastern tectonic blocks and the likeli- the ongoing debates about the phylo- workshop on “The Colonization of hood of high water volume flowing genetic relationships of different Africa by Early Anthropoid Primates.” southwest from large Asian rivers taxa. The seminar, organized by Chris toward Africa in conjunction with pre- Chris Beard (Kansas) reviewed the Beard (Kansas), involved two full and vailing westward currents. evidence of anthropoid evolution in intense days of presentations and dis- Gregoire Metais (Museum National Africa and Asia, then addressed the cussions, followed by a field trip to d’Histoire Naturelle, France) discussed importance of over-water dispersal Paleocene and Eocene localities in the “Potential Role of Turkey as a Bio- in primate evolution. He argued that northern New Mexico’s San Juan geographic Crossroads for Eurasian the phenomenon that is often called Basin. and African Mammals During the “sweepstakes dispersal” is not ran- Africa has been a major center for Paleogene.” Modern Turkey has an dom (and thus should perhaps be the evolution of anthropoid primates intricate geological history. Recent referred to as a special case of filter over at least the last 35 million years. paleontological work by Metais and dispersal). -
Late Middle Eocene Primate from Myanmar and the Initial Anthropoid Colonization of Africa
Late Middle Eocene primate from Myanmar and the initial anthropoid colonization of Africa Abstract Reconstructing the origin and early evolutionary history of anthropoid primates (monkeys, apes, and humans) is a current focus of paleoprimatology. Although earlier hypotheses frequently supported an African origin for anthropoids, recent discoveries of older and phylogenetically more basal fossils in China and Myanmar indicate that the group originated in Asia. Given the Oligocene-Recent history of African anthropoids, the colonization of Africa by early anthropoids hailing from Asia was a decisive event in primate evolution. However, the fossil record has so far failed to constrain the nature and timing of this pivotal event. Here we describe a fossil primate from the late middle Eocene Pondaung Formation of Myanmar, Afrasia djijidae gen. et sp. nov., that is remarkably similar to, yet dentally more primitive than, the roughly contemporaneous North African anthropoid Afrotarsius. Phylogenetic analysis suggests that Afrasia and Afrotarsius are sister taxa within a basal anthropoid clade designated as the infraorder Eosimiiformes. Current knowledge of eosimiiform relationships and their distribution through space and time suggests that members of this clade dispersed from Asia to Africa sometime during the middle Eocene, shortly before their first appearance in the African fossil record. Crown anthropoids and their nearest fossil relatives do not appear to be specially related to Afrotarsius, suggesting one or more additional episodes of dispersal from Asia to Africa. Hystricognathous rodents, anthracotheres, and possibly other Asian mammal groups seem to have colonized Africa at roughly the same time or shortly after anthropoids gained their first toehold there . -
New Paleocene Skeletons and the Relationship of Plesiadapiforms to Crown-Clade Primates
New Paleocene skeletons and the relationship of plesiadapiforms to crown-clade primates Jonathan I. Bloch*†, Mary T. Silcox‡, Doug M. Boyer§, and Eric J. Sargis¶ʈ *Florida Museum of Natural History, University of Florida, P. O. Box 117800, Gainesville, FL 32611; ‡Department of Anthropology, University of Winnipeg, 515 Portage Avenue, Winnipeg, MB, Canada, R3B 2E9; §Department of Anatomical Science, Stony Brook University, Stony Brook, NY 11794-8081; ¶Department of Anthropology, Yale University, P. O. Box 208277, New Haven, CT 06520; and ʈDivision of Vertebrate Zoology, Peabody Museum of Natural History, Yale University, New Haven, CT 06520 Communicated by Alan Walker, Pennsylvania State University, University Park, PA, November 30, 2006 (received for review December 6, 2005) Plesiadapiforms are central to studies of the origin and evolution preserved cranium of a paromomyid (10) seemed to independently of primates and other euarchontan mammals (tree shrews and support a plesiadapiform–dermopteran link, leading to the wide- flying lemurs). We report results from a comprehensive cladistic spread acceptance of this phylogenetic hypothesis. The evidence analysis using cranial, postcranial, and dental evidence including supporting this interpretation has been questioned (7, 9, 13, 15, 16, data from recently discovered Paleocene plesiadapiform skeletons 19, 20), but no previous study has evaluated the plesiadapiform– (Ignacius clarkforkensis sp. nov.; Dryomomys szalayi, gen. et sp. dermopteran link by using cranial, postcranial, and dental evidence, -
From the Gulf Coastal Plain
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 355-361 355 EKGMOWECHASHALA (MAMMALIA, ?PRIMATES) FROM THE GULF COASTAL PLAIN L. Barry Albright III1 A single, small, water-worn tooth from the “middle” Arikareean Toledo Bend Local Fauna of the Gulf Coastal Plain closely resembles the lower fourth premolar of the questionable primate Ekgmowechashala. The only known species of the genus, Ekgmowechashala philotau Macdonald (1963), was originally recovered from the early Arikareean Sharps Formation of South Dakota, but is also known from similar aged strata of the John Day Formation, Oregon. Although the Toledo Bend specimen differs somewhat in morphology from the p4 of E. philotau, a new species is not named in this report because of such limited material and because the specimen is incomplete. Unfortunately, the specimen does not provide information that helps clarify current arguments regarding the affinities of Ekgmowechashala with primates or plagiomenids. It does, however, provide (1) a temporal range extension for the genus to the early late Arikareean, or about four million years younger than previously known, and (2) a geographic extension east and considerably south of its prior distribution. If Ekgmowechashala is ultimately deter- mined to belong to the Primates, then the Toledo Bend species would become the last known North American representative of the order. Key Words: Ekgmowechashala; Primates; Plagiomenidae; Texas Gulf Coastal Plain; Arikareean INTRODUCTION brate paleontology collections of the Louisiana State Uni- In 1990, while screen-washing matrix from the “middle” versity Museum of Geoscience (LSUMG V). Arikareean Toledo Bend site in the Fleming Formation of easternmost Texas (Albright 1994, 1996, 1998a, 1998b, BACKGROUND 1999), a small, unusual, water-worn tooth was recov- Ekgmowechashala philotau is a small “enigmatic late ered that differed considerably from the site’s more com- Oligocene mammal” (McKenna, 1990:226) heretofore mon and readily identifiable rodent teeth. -
For Peer Review
View metadata, citation and similar papers at core.ac.uk brought to you by CORE Page 1 of 57 Journal of Morphology provided by Archivio della Ricerca - Università di Pisa 1 2 3 Title: The locomotion of Babakotia radofilai inferred from epiphyseal and diaphyseal 4 5 6 morphology of the humerus and femur. 7 8 9 Damiano Marchi1,2*, Christopher B. Ruff3, Alessio Capobianco, 1,4, Katherine L. Rafferty5, 10 11 Michael B. Habib6, Biren A. Patel2,6 12 13 14 1 15 Department of Biology, University of Pisa, Pisa, Italy, 56126 16 17 2 18 Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South 19 20 Africa, WITS 2050 For Peer Review 21 22 23 3 Center for Functional Anatomy and Evolution, Johns Hopkins University School of 24 25 26 Medicine, Baltimore, MD 21111 27 28 4 29 Scuola Normale Superiore, Pisa, Italy, 56126 30 31 5 32 Department of Orthodontics, School of Dentistry, University of Washington, Seattle, WA 33 34 35 98195 36 37 6 38 Department of Cell and Neurobiology, Keck School of Medicine, University of Southern 39 40 California, Los Angeles, CA 90033 41 42 43 Text pages: 28; Bibliography pages: 9; Figures: 6; Tables: 6 Appendices: 1 44 45 46 Running title: Babakotia radofilai postcranial suspensory adaptations 47 48 49 *Corresponding author: 50 51 52 Damiano Marchi 53 54 55 56 Address: Dipartimento di Biologia, Università di Pisa, Via Derna, 1 - ZIP 56126, Pisa - Italy 57 58 59 Ph: +39 050 2211350; Fax: +39 050 2211475 60 1 John Wiley & Sons Journal of Morphology Page 2 of 57 1 2 3 Email: [email protected] -
ZOOLOGY Exploring the Biodiversity of Colorado and Theworld
CHAPTER 4 — ZOOLOGY Exploring the Biodiversity of Colorado and the World CHAPTER 4 ZOOLOGY Exploring the Biodiversity of Colorado and the World Jeffrey T. Stephenson, Before the Museum Paula E. Cushing, The first collections of specimens that make up what is now the Denver John R. Demboski, and Museum of Nature & Science were actually established well before the Frank-T. Krell founding of the institution in 1900, the selection of a board of trustees, or the construction of a building to house and exhibit the specimens. Edwin Carter (1830–1900) (Fig. 4.1) collected Colorado birds and mammals from the 1860s through the 1890s. Born in New York in 1830, Carter arrived in Colorado in 1859 hoping to make it rich in the goldfields, but he soon became interested in the region’s natural history. He learned hide tanning and, as his prospects for hitting the mother lode faded, he earned his living selling buckskin clothing that he handcrafted. Carter supplemented these earnings by mar- keting foodstuffs and other provisions to the growing population of successful and (mostly) unsuccessful prospectors flooding the region. His interest in nature turned to concern as he observed dwindling numbers of mammals and birds, owing largely to habitat destruction and overhunting. Period photographs of the area’s mining district show a landscape largely denuded of vegetation. By the 1870s, Carter noted that many animal species were becoming scarce. The state’s forests were being devastated, ranches and farms were replacing open prairie, and some species, including the last native bison in Colorado, were on the verge of extirpation or extinction. -
Convergent Evolution of Olfactory and Thermoregulatory Capacities in Small Amphibious Mammals
Convergent evolution of olfactory and thermoregulatory capacities in small amphibious mammals Quentin Martineza,1, Julien Clavelb,c, Jacob A. Esselstynd,e, Anang S. Achmadif, Camille Grohég,h, Nelly Piroti,j, and Pierre-Henri Fabrea,k aInstitut des Sciences de l’Évolution de Montpellier (ISEM), CNRS, Institut de recherche pour le développement (IRD), Université de Montpellier (UM), UMR 5554, 34095 Montpellier, France; bDepartment of Life Sciences, The Natural History Museum, SW7 5DB London, United Kingdom; cUniv. Lyon Laboratoire d’Ecologie des Hydrosystèmes Naturels et Anthropisés, UMR CNRS 5023, Université Claude Bernard Lyon 1, École Nationale des Travaux Publics de l’État (ENTPE), F‐69622 Villeurbanne, Cedex, France; dMuseum of Natural Science, Louisiana State University, Baton Rouge, LA 70803; eDepartment of Biological Sciences, Louisiana State University, Baton Rouge, LA 70803; fMuseum Zoologicum Bogoriense, Research Center for Biology, Indonesian Institute of Sciences (LIPI), 16911 Cibinong, Indonesia; gDivision of Paleontology, American Museum of Natural History, New York, NY 10024; hLaboratoire Paléontologie Évolution Paléoécosystèmes Paléoprimatologie (PALEVOPRIM, UMR 7262, CNRS-Institut écologie et environnement [INEE]), Université de Poitiers, 86073 Poitiers, Cedex 9, France; iInstitut de Recherche en Cancérologie de Montpellier (IRCM), INSERM, U1194 UM, Institut du Cancer de Montpellier (ICM), F-34298 Montpellier, Cedex 5, France; jRéseau d’Histologie Expérimentale de Montpellier, UMS3426 CNRS-US009 INSERM-UM, 34298 Montpellier, France; and kMammal Section, Department of Life Sciences, The Natural History Museum, SW7 5DB London, United Kingdom Edited by David B. Wake, University of California, Berkeley, CA, and approved February 28, 2020 (received for review October 11, 2019) Olfaction and thermoregulation are key functions for mammals. The partitioning has been documented in histological, airflow dynamic, former is critical to feeding, mating, and predator avoidance behaviors, and performance test studies (9–13). -
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.