Frontal Fusion: Collapse of Another Anthropoid Synapomorphy
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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. -
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. -
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. -
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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
Mammalia, Plesiadapiformes) As Reflected on Selected Parts of the Postcranium
SHAPE MEETS FUNCTION: STRUCTURAL MODELS IN PRIMATOLOGY Edited by Emiliano Bruner Proceedings of the 20th Congress of the International Primatological Society Torino, Italy, 22-28 August 2004 MORPHOLOGY AND MORPHOMETRICS JASs Journal of Anthropological Sciences Vol. 82 (2004), pp. 103-118 Locomotor adaptations of Plesiadapis tricuspidens and Plesiadapis n. sp. (Mammalia, Plesiadapiformes) as reflected on selected parts of the postcranium Dionisios Youlatos1, Marc Godinot2 1) Aristotle University of Thessaloniki, School of Biology, Department of Zoology, GR-54124 Thessaloniki, Greece. email [email protected] 2) Ecole Pratique des Hautes Etudes, UMR 5143, Case Courrier 38, Museum National d’Histoire Naturelle, Institut de Paleontologie, 8 rue Buffon, F-75005 Paris, France Summary – Plesiadapis is one of the best-known Plesiadapiformes, a group of Archontan mammals from the Late Paleocene-Early Eocene of Europe and North America that are at the core of debates con- cerning primate origins. So far, the reconstruction of its locomotor behavior has varied from terrestrial bounding to semi-arboreal scansoriality and squirrel-like arboreal walking, bounding and claw climbing. In order to elucidate substrate preferences and positional behavior of this extinct archontan, the present study investigates quantitatively selected postcranial characters of the ulna, radius, femur, and ungual pha- langes of P. tricuspidens and P. n .sp. from three sites (Cernay-les-Reims, Berru, Le Quesnoy) in the Paris Basin, France. These species of Plesiadapis was compared to squirrels of different locomotor habits in terms of selected functional indices that were further explored through a Principal Components Analysis (PCA), and a Discriminant Functions Analysis (DFA). The indices treated the relative olecranon height, form of ulnar shaft, shape and depth of radial head, shape of femoral distal end, shape of femoral trochlea, and dis- tal wedging of ungual phalanx, and placed Plesiadapis well within arboreal quadrupedal, clambering, and claw climbing squirrels. -
Abstracts Volume
SVPCA 58, Cambridge 2010, Preface Welcome to the 58th Symposium of Vertebrate Palaeontology and Comparative Anatomy, hosted by the University Museum of Zoology, Cambridge. We very much hope you find the meeting rewarding, and that you have time to enjoy the other attractions of the university, colleges, and city centre. The meeting logo was designed by Julia Molnar1 and depicts the finback whale (Balaenoptera physalus) on display above the Museum of Zoology. Enjoy your time in Cambridge! 1JuliaMolnar,RoyalVeterinaryCollege,jmolnar-at-rvc.ac.uk 1 SPPC/SVPCA 2010 Programme Overview Tuesday 14th September: SPPC Session 1, Chair: Matt Lowe 15.30-15.50 Christian Baars Infacol – if it’s good enough for babies, it’s good enough for ammonites. 15.50-15.10 Nigel R Larkin The joy of steel: How to master your awkward fossil in the field. 16.10-16.30 Frank Osbaeck Mechanical and chemical preparation methods used on the lower Eocene cementstone concretions from the Mo-Clay of northern Denmark 19.00 onwards EVENING RECEPTION, ZOOLOGY MUSEUM Wednesday 15th September 9.10-9.20 Welcome, notices for the day Session 1, Chair: Paul Barret 9.20-9.40 Eric Buffetaut et al. The Early Cretaceous vertebrate assemblage from the Napai Formation of Guangxi, southern China: a comparison with Thai assemblages 9.40-10.00 Michael J Benton et al. Recovery and expansion of marine vertebrate faunas in the Triassic of South China 10.00-10.20 Susan E Evans and Magdalend Borsuk-Bialynicka The Early Triassic faunal assemblage of Czatkowice, Poland 10.20-10.40 Sweetman, Steven C The first records of amphibians, lizards and maniraptoran dinosaurs from the Lower Cretaceous Hastings Group of south-east England 10.40-11.10 COFFEE BREAK Session 2, Chair: Jenny Clack 11.10-11.30 Tim Smithson and Stan Wood Eliminating Romer’s Gap: new tetrapods from the basal Carboniferous of the Scottish Borders 2 11.30-11.50 Per E Ahlberg et al. -
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. -
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. -
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. -
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.