(Mammalia, Allotheria) Dentitions Using Mammalian Dietary Proxies
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Enamel Ultrastructure of Multituberculate Mammals: an Investigation of Variability
CO?JTRIBI!TIONS FROM THE MUSEUM OF PALEOK.1-OLOCiY THE UNIVERSITY OF MICHIGAN VOL. 27. NO. 1, p. 1-50 April I, 1985 ENAMEL ULTRASTRUCTURE OF MULTITUBERCULATE MAMMALS: AN INVESTIGATION OF VARIABILITY BY SANDRA J. CARLSON and DAVID W. KRAUSE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRlBUTlONS FROM THE MUSEUM OF PALEON I OLOGY 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, 48109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN Vol . 27, no. 1, p. 1-50, pub1 ished April 1, 1985, Sandra J. Carlson and David W. Krause (Authors) ERRATA Page 11, Figure 4 caption, first line, should read "(1050X)," not "(750X)." ENAMEL ULTRASTRUCTURE OF MULTITUBERCULATE MAMMALS: AN INVESTIGATION OF VARIABILITY BY Sandra J. Carlsonl and David W. Krause' Abstract.-The nature and extent of enamel ultrastructural variation in mammals has not been thoroughly investigated. In this study we attempt to identify and evaluate the sources of variability in enamel ultrastructural patterns at a number of hierarchic levels within the extinct order Multituberculata. -
Multituberculate Mammals from the Wahweap
MULTITUBERCULATE MAMMALS FROM THE WAHWEAP (CAMPANIAN, AQUILAN) AND KAIPAROWITS (CAMPANIAN, JUDITHIAN) FORMATIONS, WITHIN AND NEAR GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, SOUTHERN UTAH Jeffrey G. Eaton Department of Geosciences Weber State University Ogden, UT 84408-2507 phone: (801) 626-6225 fax: (801) 626-7445 e-mail: [email protected] Cover photo by author: Powell Point in “The Blues,” the early Tertiary Claron Formation on the horizon and the Kaiparowits Formation in the foreground. ISBN 1-55791-665-9 Reference to any specific commercial product by trade name, trademark, or manufacturer does not constitute endorsement or recommendation by the Utah Geological Survey MISCELLANEOUS PUBLICATION 02-4 UTAH GEOLOGICAL SURVEY a division of 2002 Utah Department of Natural Resources STATE OF UTAH Michael O. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Robert Morgan, Executive Director UTAH GEOLOGICAL SURVEY Richard G. Allis, Director UGS Board Member Representing Robert Robison (Chairman) ...................................................................................................... Minerals (Industrial) Geoffrey Bedell.............................................................................................................................. Minerals (Metals) Stephen Church .................................................................................................................... Minerals (Oil and Gas) E.H. Deedee O’Brien ....................................................................................................................... -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Vertebrate Paleontology of the Cretaceous/Tertiary Transition of Big Bend National Park, Texas (Lancian, Puercan, Mammalia, Dinosauria, Paleomagnetism)
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1986 Vertebrate Paleontology of the Cretaceous/Tertiary Transition of Big Bend National Park, Texas (Lancian, Puercan, Mammalia, Dinosauria, Paleomagnetism). Barbara R. Standhardt Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Standhardt, Barbara R., "Vertebrate Paleontology of the Cretaceous/Tertiary Transition of Big Bend National Park, Texas (Lancian, Puercan, Mammalia, Dinosauria, Paleomagnetism)." (1986). LSU Historical Dissertations and Theses. 4209. https://digitalcommons.lsu.edu/gradschool_disstheses/4209 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This reproduction was made from a copy of a manuscript sent to us for publication and microfilming. While the most advanced technology has been used to pho tograph and reproduce this manuscript, the quality of the reproduction is heavily dependent upon the quality of the material submitted. Pages in any manuscript may have indistinct print. In all cases the best available copy has been filmed. The following explanation of techniques is provided to help clarify notations which may appear on this reproduction. 1. Manuscripts may not always be complete. When it is not possible to obtain missing pages, a note appears to indicate this. 2. When copyrighted materials are removed from the manuscript, a note ap pears to indicate this. 3. -
Masticatory Musculature of Asian Taeniolabidoid Multituberculate Mammals
Masticatory musculature of Asian taeniolabidoid multituberculate mammals PETR P. GAMBARYAN & ZOFIA KIELAN-JAWOROWSKA* Gambaryan, P.P. & Kielan-Jaworowska, 2. 1995. Masticatory musculature of Asian taeniolabidoid multituberculate mammals. Acta Palaeontologica Polonica 40, 1, 45-108. The backward chewing stroke in multituberculates (unique for mammals) resulted in a more anterior insertion of the masticatory muscles than in any other mammal group, including rodents. Multituberculates differ from tritylodontids in details of the masticatory musculature, but share with them the backward masticatory power stroke and retractory horizontal components of the resultant force of all the masticatory muscles (protractory in Theria). The Taeniolabididae differ from the Eucosmodontidae in having a more powerful masticatory musculature, expressed by the higher zygomatic arch with relatively larger anterior and middle zygomatic ridges and higher coronoid process. It is speculated that the bicuspid, or pointed upper incisors, and semi-procumbent, pointed lower ones, characteristic of non- taeniolabidoid mdtitliberculates were used for picking-up and killing insects or other prey. In relation to the backward power stroke the low position of the condylar process was advantageous for most multituberculates. In extreme cases (Sloanbaataridae and Taeniolabididae), the adaptation for crushing hard seeds, worked against the benefit of the low position of the condylar process and a high condylar process developed. Five new multituberculate autapomorphies are rec- ognized: anterior and intermediate zygomatic ridges: glenoid fossa large, flat and sloping backwards (forwards in rodents), arranged anterolateral and standing out from the braincase; semicircular posterior margin of the dentary with condylar process forming at least a part of it; anterior position of the coronoid process; and anterior position of the masseteric fossa. -
New Specimens of the Multituberculate Mammal Sphenopsalis from China: Implications for Phylogeny and Biology of Taeniolabidoids
New specimens of the multituberculate mammal Sphenopsalis from China: Implications for phylogeny and biology of taeniolabidoids FANG-YUAN MAO, YUAN-QING WANG, and JIN MENG Mao, F.-Y., Wang, Y.-Q., and Meng, J. 2016. New specimens of the multituberculate mammal Sphenopsalis from China: Implications for phylogeny and biology of taeniolabidoids. Acta Palaeontologica Polonica 61 (2): 429–454. Multituberculates are the most diverse and best known group of Mesozoic mammals; they also persisted into the Paleogene and became extinct in the Eocene, possibly outcompeted by rodents that have similar morphological and pre- sumably ecological adaptations. Among the Paleogene multituberculates, those that have the largest body sizes belong to taeniolabidoids, which contain several derived species from North America and Asia and some species with uncertain taxonomic positions. Of the known taeniolabidoids, the poorest known taxon is Sphenopsalis nobilis from Mongolia and Inner Mongolia, China, represented previously by a few isolated teeth. Its relationship with other multituberculates thus has remained unclear. Here we report new specimens of Sphenopsalis nobilis collected from the upper Paleocene of the Erlian Basin, Inner Mongolia, China, during a multi-year field effort beginning in 2000. These new specimens document substantial parts of the dental, partial cranial and postcranial morphologies of Sphenopsalis, including the upper and lower incisors, partial premolars, complete upper and lower molars, a partial rostrum, fragments of the skull roof, middle ear cavity, a partial scapula, and partial limb bones. With the new specimens we are able to present a detailed description of Sphenopsalis, comparisons among relevant taeniolabidoids, and brief phylogenetic analyses based on a dataset consisting of 43 taxa and 102 characters. -
Late Cretaceous Stratigraphy and Vertebrate Faunas of the Markagunt, Paunsaugunt, and Kaiparowits Plateaus, Southern Utah
GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 LATE CRETACEOUS STRATIGRAPHY AND VERTEBRATE FAUNAS OF THE MARKAGUNT, PAUNSAUGUNT, AND KAIPAROWITS PLATEAUS, SOUTHERN UTAH Alan L. Titus, Jeffrey G. Eaton, and Joseph Sertich A Field Guide Prepared For SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA Post-Meeting Field Trip October 30–November 1, 2016 © 2016 Utah Geological Association. All rights reserved. For permission to copy and distribute, see the following page or visit the UGA website at www.utahgeology.org for information. Email inquiries to [email protected]. GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 Editors UGA Board Douglas A. Sprinkel Thomas C. Chidsey, Jr. 2016 President Bill Loughlin [email protected] 435.649.4005 Utah Geological Survey Utah Geological Survey 2016 President-Elect Paul Inkenbrandt [email protected] 801.537.3361 801.391.1977 801.537.3364 2016 Program Chair Andrew Rupke [email protected] 801.537.3366 [email protected] [email protected] 2016 Treasurer Robert Ressetar [email protected] 801.949.3312 2016 Secretary Tom Nicolaysen [email protected] 801.538.5360 Bart J. Kowallis Steven Schamel 2016 Past-President Jason Blake [email protected] 435.658.3423 Brigham Young University GeoX Consulting, Inc. 801.422.2467 801.583-1146 UGA Committees [email protected] [email protected] Education/Scholarship -
Late Cretaceous (65-100 Ma Time-Slice) Time
Late Cretaceous (65-100 Ma time-slice) Time ScaLe R Creator CHRONOS Cen Mesozoic Paleozoic Updated by James G. Ogg (Purdue University) and Gabi Ogg to: GEOLOGIC TIME SCALE 2004 (Gradstein, F.M., Ogg, J.G., Smith, A.G., et al., 2004) and The CONCISE GEOLOGIC TIME SCALE (Ogg, J.G., Ogg, G., and Gradstein, F.M., 2008) Sponsored, in part, by: Precambrian ICS Based, in part, on: CENOZOIC-MESOZOIC BIOCHRONOSTRATIGRAPHY: JAN HARDENBOL, JACQUES THIERRY, MARTIN B. FARLEY, THIERRY JACQUIN, PIERRE-CHARLES DE GRACIANSKY, AND PETER R. VAIL,1998. Mesozoic and Cenozoic Sequence Chronostratigraphic Framework of European Basins in: De Graciansky, P.- C., Hardenbol, J., Jacquin, Th., Vail, P. R., and Farley, M. B., eds.; Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, SEPM Special Publication 60. Standard Geo- Ammonites Sequences Planktonic Foraminifers Smaller Benthic Foraminifers Larger Benthic Foraminifers Calcareous Nannofossils Dinoflagellate Cysts Radiolarians Belemnites Inoceramids Rudists Ostracodes Charophytes Mammals Stage Age Chronostratigraphy magnetic North Atlantic Tethys Age Western Interior, Sequences T-R Major T-R Other Larger Benthic Russian Central Europe / Period Epoch Stage Substage Polarity Boreal Tethyan North America Global Cycles Cycles Zones Zonal Markers Other Foraminifers Boreal Zonal Markers Other Boreal Foraminifers Tethys Zones Zonal Markers Foraminifers Zones Zonal Markers Other Nannofossils Zones Zonal Markers Other Dinocysts Zones Zonal Markers Other Tethyan Dinocysts Zones Zonal Markers NW Europe Balto-Scandia -
Early Paleocene Vertebrates, Stratigraphy, and Biostratigraphy
EarlyPaleocene vertebrates, stratigraphy and biostratigraphy,West Fork of GallegosGanyon, SanJuan Basin, New Mexico bySpencer G. Lucas,Department ofGeology, University of New Mexico, Albuquerque, NM87131 Introduction U.S. Bureauof Land Managementcollected mudstoneand sandstonedetritus locallyde- There are only three well known areasin in this area (Kues and others, 1977). rived from the Nacimiento Formation (Qal, and of Wells, 1982,fig. 101).However, the San |uan Basin where early Paleocene This paper reports the fossil vertebrates Qal, (Puercan)vertebrates occur in the lowermost collectedbv this field partv. establishestheir the Oio Alamo Sandstonedoes form the re- strata of the Nacimiento Formation. These stratigraphicprovenance, ind discussestheir sistanibedrock under the plateauincised by areas,Betonnie Tsosie Wash, Kimbeto Wash, biostratigraphicsignificance. AMNH refers GallegosCanyon and its tributaries, and it and the headlandsof De-na-zinand Alamo to specimensin the Department of Verte- is exposed approximately 1 km (0.5 mi) Washes(Fig. 1), were already known when brate Paleontology,American Museum of northwest of the head of the WestFork (Ree- Sinclairand Granger(1914) published the re- Natural Historv; UNM refers to snecimens side, 1924,p. 30, pl. 1). This relationship to sults of two field seasons (1912-1913) of in the Departmentof Geology,University of the Ojo Alamo Sandstoneand the occurrence stratigraphicand paleontologicstudies of the New Mexico. of Puercanmammals indicate that the Na- strataexposed here are of the lower Paleoceneof the San Juan Basin. However, cimiento Sinclairand Granger(1974, p.315) did men- Stratigraphy -oart of the formation. tion a fourth occurrenceof Puercan verte- More than 37 m (l2I ft) of the Nacimiento The exposedNacimiento Formation con- bratesin the headlandsof the West Fork of Formation are exposedin rugged badlands sists of mudstone (63%), sandstone(33Vo), GallegosCanyon (Fig. -
Enamel Microstructure of the Late Cretaceous Multituberculate Mammal Kogaionon
- a Vol. 46, No. 3, p. 437440, Warszawa 2001 Enamel microstructure of the Late Cretaceous multituberculate mammal Kogaionon GISLE FOSSE, COSTIN ~DULESCU,and PETRE-MIHAI SAM SON^ Cretaceous multituberculate mammals of Europe are poorly known, as a rule represented by isolated teeth. The only exception is the Late Cretaceous (Maastrichtian) monotypic genus Kogaionon Riidulescu & Samson, 1996 from Romania, represented by a single skull, without dentaries, assigned to Kogaionidae Rhdulescu & Samson, 1996, Another kogaionid genus is Hainina Vianey-Liaud, 1979, represented by several isolated teeth from the Paleocene of Belgium and Spain, and from the Maastrichtian of Romania. The skull of Kogaionon is roughly rectangular in palatal view, resembling superficially that of Paleocene Taeniolabis (except for having a strongly elongated snout), but the upper dentition differentiates the Kogaionidae from all other multituberculates. In this paper we studied the enamel microstructure of Kogaionon and demonstrate that it is of giganto- prismatic type. In recent decades, mammalian systematists have recognized the utility of characteristics of enamel microstructure in phylogenetic interpretation, particularly among multituberculates (e.g., Carlson & Krause 1985; Fosse et al. 1985; Krause & Carlson 1986,1987; Simmons 1993; see also papers in Koenigswald & Sander 1997, and a summary by Kielan-Jaworowska & Hurum 2001). Sloan & Van Valen (1965) divided advanced Multituberculata (subsequently re- ferred to by McKenna 1975 as Cimolodonta) into two suborders Taeniolabidoidea and Ptilo- dontoidea. This division is now not valid. Kielan-Jaworowska & Hurum (2001, but see McKenna & Bell 1997 for an alternative classification) divided the order Multituberculata into a paraphyletic suborder 'Plagiaulacida' and a suborder of derived multituberculates Cimolo- donta McKenna, 1975. -
Mammals Across the K/Pg Boundary in Northeastern
Mammals across the K/Pg boundary in northeastern Montana, U.S.A.: dental morphology and body-size patterns reveal extinction selectivity and immigrant-fueled ecospace filling Author(s): Gregory P. Wilson Source: Paleobiology, 39(3):429-469. 2013. Published By: The Paleontological Society DOI: http://dx.doi.org/10.1666/12041 URL: http://www.bioone.org/doi/full/10.1666/12041 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/ terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Paleobiology, 39(3), 2013, pp. 429–469 DOI: 10.1666/12041 Mammals across the K/Pg boundary in northeastern Montana, U.S.A.: dental morphology and body-size patterns reveal extinction selectivity and immigrant-fueled ecospace filling Gregory P. Wilson Abstract.—The Cretaceous/Tertiary (K/Pg) mass extinction has long been viewed as a pivotal event in mammalian evolutionary history, in which the extinction of non-avian dinosaurs allowed mammals to rapidly expand from small-bodied, generalized insectivores to a wide array of body sizes and ecological specializations. -
The Taphonomy, Paleoecology, and Depositional Environment Of
W&M ScholarWorks Undergraduate Honors Theses Theses, Dissertations, & Master Projects 5-2011 The Taphonomy, Paleoecology, and Depositional Environment of Vertebrate Microfossil Bonebeds from the Late Cretaceous Hell Creek Formation in Garfield County, Montana Sean Michael Moran College of William and Mary Follow this and additional works at: https://scholarworks.wm.edu/honorstheses Part of the Geology Commons Recommended Citation Moran, Sean Michael, "The Taphonomy, Paleoecology, and Depositional Environment of Vertebrate Microfossil Bonebeds from the Late Cretaceous Hell Creek Formation in Garfield County, Montana" (2011). Undergraduate Honors Theses. Paper 419. https://scholarworks.wm.edu/honorstheses/419 This Honors Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Undergraduate Honors Theses by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. The Taphonomy, Paleoecology, and Depositional Environment of Vertebrate Microfossil Bonebeds from the Late Cretaceous Hell Creek Formation in Garfield County, Montana A thesis submitted in partial fulfillment of the requirement for the degree of Bachelors of Science in Geology from The College of William and Mary by Sean Michael Moran Accepted for (Honors, High Honors) Rowan Lockwood, Director Matthew Carrano Christopher Bailey John Swaddle Williamsburg, VA April 15, 2011 Table of Contents List of Figures and Tables 3 Abstract 4 Introduction 5 Vertebrate Microfossil Bonebed Formation 7 Vertebrate Microfossil Bonebed Paleoecology 8 Geologic Setting 9 Hell Creek Vertebrate Fauna 12 Methods 16 HC10.01 20 HC10.02 21 HC10.03 23 HC10.04 24 HC10.05 25 Percent Diversity and Percent Abundance 26 Rarefaction 32 Amount of Wear 39 Differences in Maximum Dimension 41 Size vs.