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![November, 1907.] 56 882 Bulletin American Museum of Natural History](https://docslib.b-cdn.net/cover/9349/november-1907-56-882-bulletin-american-museum-of-natural-history-169349.webp)
November, 1907.] 56 882 Bulletin American Museum of Natural History
56.9,725E( 1182:7) Article XXXV.- REVISION OF THE MIOCENE AND PLIO- CENE EQUII)DE OF NORTH AMERICA. BY JAMES WILLIAMs GIDLEY. With an introductory Note by Henry Fairfield Osborn. INTRODUCTORY NOTE. The American Museum collection of Horses -from the Eocene to the Pleistocene inielusive - now numbers several thousand specimens, includ- ing nearly fifty types and about as many casts of types. It is desired gradually, as opportunity permits, to make this type collection absolutely complete either through originals or casts. The first step towards a thorough understanding of the Equidse is a systematic revision of all the generic and specific names which have been proposed, and of the characters of the valid genera and species, starting with an exact study and comparison of the type specimens. As planned this is being done by co6peration of the writer, of Mr. Walter Granger of the American Museum staff, and especially of Mr. J. W. Gidley, formerly of this Museum, now of the United States National Museum, and the author of the present paper, who has made a specialty of the horse from the Oligo- cene to the' Pleistocene inclusive. The list of these revisions, as completed or in progress, is as follows: Pleistocene. Tooth Characters and Revision of the North American Species of the Genus Equus. By J. W. Gidley. Bull. Am. Mus. Nat. Hist., Vol. XIV, 1901, pp. 91-141, pll. xvii-xxi, and 27 text figures. Miocene and Pliocene. Proper Generic Names of Miocene Horses. By J. W. Gidley. Bull. Amer. Mus. Nat. Hist., Vol. XX, 1904, pp. -
Catalogue Palaeontology Vertebrates (Updated July 2020)
Hermann L. Strack Livres Anciens - Antiquarian Bookdealer - Antiquariaat Histoire Naturelle - Sciences - Médecine - Voyages Sciences - Natural History - Medicine - Travel Wetenschappen - Natuurlijke Historie - Medisch - Reizen Porzh Hervé - 22780 Loguivy Plougras - Bretagne - France Tel.: +33-(0)679439230 - email: [email protected] site: www.strackbooks.nl Dear friends and customers, I am pleased to present my new catalogue. Most of my book stock contains many rare and seldom offered items. I hope you will find something of interest in this catalogue, otherwise I am in the position to search any book you find difficult to obtain. Please send me your want list. I am always interested in buying books, journals or even whole libraries on all fields of science (zoology, botany, geology, medicine, archaeology, physics etc.). Please offer me your duplicates. Terms of sale and delivery: We accept orders by mail, telephone or e-mail. All items are offered subject to prior sale. Please do not forget to mention the unique item number when ordering books. Prices are in Euro. Postage, handling and bank costs are charged extra. Books are sent by surface mail (unless we are instructed otherwise) upon receipt of payment. Confirmed orders are reserved for 30 days. If payment is not received within that period, we are in liberty to sell those items to other customers. Return policy: Books may be returned within 14 days, provided we are notified in advance and that the books are well packed and still in good condition. Catalogue Palaeontology Vertebrates (Updated July 2020) Archaeology AE11189 ROSSI, M.S. DE, 1867. € 80,00 Rapporto sugli studi e sulle scoperte paleoetnologiche nel bacino della campagna romana del Cav. -
Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals Willow H
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 7-2017 Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals Willow H. Nguy University of Nebraska-Lincoln, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Nguy, Willow H., "Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals" (2017). Dissertations & Theses in Earth and Atmospheric Sciences. 91. http://digitalcommons.unl.edu/geoscidiss/91 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. MIDDLE MIOCENE PALEOENVIRONMENTAL RECONSTRUCTION OF THE CENTRAL GREAT PLAINS FROM STABLE CARBON ISOTOPES IN LARGE MAMMALS by Willow H. Nguy A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Ross Secord Lincoln, Nebraska July, 2017 MIDDLE MIOCENE PALEOENVIRONMENTAL RECONSTRUCTION OF THE CENTRAL GREAT PLAINS FROM STABLE CARBON ISOTOPES IN LARGE MAMMALS Willow H. Nguy, M.S. University of Nebraska, 2017 Advisor: Ross Secord Middle Miocene (18-12 Mya) mammalian faunas of the North American Great Plains contained a much higher diversity of apparent browsers than any modern biome. -
Morton County, Kansas Michael Anthony Calvello Fort Hays State University
Fort Hays State University FHSU Scholars Repository Master's Theses Graduate School Summer 2011 Mammalian Fauna From The ulF lerton Gravel Pit (Ogallala Group, Late Miocene), Morton County, Kansas Michael Anthony Calvello Fort Hays State University Follow this and additional works at: https://scholars.fhsu.edu/theses Part of the Geology Commons Recommended Citation Calvello, Michael Anthony, "Mammalian Fauna From The ulF lerton Gravel Pit (Ogallala Group, Late Miocene), Morton County, Kansas" (2011). Master's Theses. 135. https://scholars.fhsu.edu/theses/135 This Thesis is brought to you for free and open access by the Graduate School at FHSU Scholars Repository. It has been accepted for inclusion in Master's Theses by an authorized administrator of FHSU Scholars Repository. - MAMMALIAN FAUNA FROM THE FULLERTON GRAVEL PIT (OGALLALA GROUP, LATE MIOCENE), MORTON COUNTY, KANSAS being A Thesis Presented to the Graduate Faculty of the Fort Hays State University in Partial Fulfillment of the Requirements for the Degree of Master of Science by Michael Anthony Calvello B.A., State University of New York at Geneseo Date Z !J ~4r u I( Approved----c-~------------- Chair, Graduate Council Graduate Committee Approval The Graduate Committee of Michael A. Calvello hereby approves his thesis as meeting partial fulfillment of the requirement for the Degree of Master of Science. Approved: )<--+-- ----+-G~IJCommittee Meilnber Approved: ~J, iii,,~ Committee Member 11 ABSTRACT The Fullerton Gravel Pit, Morton County, Kansas is one of many sites in western Kansas at which the Ogallala Group crops out. The Ogallala Group was deposited primarily by streams flowing from the Rocky Mountains. Evidence of water transport is observable at the Fullerton Gravel Pit through the presence of allochthonous clasts, cross-bedding, pebble alignment, and fossil breakage and subsequent rounding. -
Man, His Origin and Destiny by Joseph Fielding Smith
Man, His Origin and Destiny by Joseph Fielding Smith FOREWORD Conflicting attitudes expressed concerning science and religion have confused many people. Especially has this been true in the class room where hypotheses have been set forth erroneously as facts and where deductions made from those theories have been regarded as established truth. Many of the followers of Darwin, for instance, carried his views to the extreme of materialistic atheism, declaring not only that creation occurred without the aid of any Intelligent Creator, but that as a matter of fact, no such Being even exists. Both science and religion have suffered as a result. The greatest damage, however, has been among students who have lost their faith in God through accepting these man-made theories as facts. But time changes things. Whereas for years atheistic deductions were made from scientific research, now true scientists, armed with what they term "the new knowledge," are revising their "hasty first conclusions" as Sir James Jeans expressed it, and have discovered "evidence of a designing or controlling power that has something in common with our individual minds." The present day attitude of top scientists was expressed recently by Dr. Joseph W. Barker, president and chairman of the Research Corporation of America, and formerly dean of the engineering school at Columbia University, in an address at Ripon University. He explained there that scientists of the nineteenth century were misled by certain of their observations, and as a result came to conclusions which were definitely atheistic. "But now," said Dr. Barker, "even the most pragmatic materialist, in the face of present day scientific knowledge, is led to the inevitable conclusion that the heavens declare the glory of God and the firmament showeth his handiwork." Dr. -
The Flaxville Gravel and ·Its Relation to Other Terrace Gravels of the Northern Great Plains
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary . -UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Professional Paper 108-J THE FLAXVILLE GRAVEL AND ·ITS RELATION TO OTHER TERRACE GRAVELS OF THE NORTHERN GREAT PLAINS BY ARTHUR J. COLLIER AND W. T. THOM, JR. Published January 26,1918 Shorter contributions to general geology, 1917 ( Paates 179-184 ) WASHINGTON GOVERNMENT PRINTING OFFICE 1918 i, '!· CONTENTS. Page. Introduction ............... ~ ... ~ ........... , ........... .......... ~ ......................... ~ .... -.----- 179 Flaxville gravel ......................................................................· .. ............ ·.... 179 Late Pliocene or early Pleistocene gravel. ..................................... ..... .. .................• - 182 Late Pleistocene and Recent erosion and deposition ........................ ..... ............ ~ ............ 182 Oligocene beds in Cypress Hilla .................... .' ................. ........................ .......... 183 Summary ....•......................... ················· · ·· · ·········.···············"···················· 183 ILLUSTRA 'fl ONS. Page. PLATE LXII. Map of northeastern Montana and adjacent parts of Canada, showing the distribution of erosion levels and gravel horizons................................................................ 180 J,XIII. A, Surface of the Flaxville plateau, northeastern Montana; B, Outcrop of cemented Flaxville gravel in escarpment ·of plateau northwest of Opheim, Mont.; C; Escarpment of the Flaxville plateau, northeastern -
Early Eocene Fossils Suggest That the Mammalian Order Perissodactyla Originated in India
ARTICLE Received 7 Jul 2014 | Accepted 15 Oct 2014 | Published 20 Nov 2014 DOI: 10.1038/ncomms6570 Early Eocene fossils suggest that the mammalian order Perissodactyla originated in India Kenneth D. Rose1, Luke T. Holbrook2, Rajendra S. Rana3, Kishor Kumar4, Katrina E. Jones1, Heather E. Ahrens1, Pieter Missiaen5, Ashok Sahni6 & Thierry Smith7 Cambaytheres (Cambaytherium, Nakusia and Kalitherium) are recently discovered early Eocene placental mammals from the Indo–Pakistan region. They have been assigned to either Perissodactyla (the clade including horses, tapirs and rhinos, which is a member of the superorder Laurasiatheria) or Anthracobunidae, an obscure family that has been variously considered artiodactyls or perissodactyls, but most recently placed at the base of Proboscidea or of Tethytheria (Proboscidea þ Sirenia, superorder Afrotheria). Here we report new dental, cranial and postcranial fossils of Cambaytherium, from the Cambay Shale Formation, Gujarat, India (B54.5 Myr). These fossils demonstrate that cambaytheres occupy a pivotal position as the sister taxon of Perissodactyla, thereby providing insight on the phylogenetic and biogeographic origin of Perissodactyla. The presence of the sister group of perissodactyls in western India near or before the time of collision suggests that Perissodactyla may have originated on the Indian Plate during its final drift toward Asia. 1 Center for Functional Anatomy & Evolution, Johns Hopkins University School of Medicine, 1830 E. Monument Street, Baltimore, Maryland 21205, USA. 2 Department of Biological Sciences, Rowan University, Glassboro, New Jersey 08028, USA. 3 Department of Geology, H.N.B. Garhwal University, Srinagar 246175, Uttarakhand, India. 4 Wadia Institute of Himalayan Geology, Dehradun 248001, Uttarakhand, India. 5 Research Unit Palaeontology, Ghent University, Krijgslaan 281-S8, B-9000 Ghent, Belgium. -
The Lost World of Fossil Lake
Snapshots from Deep Time THE LOST WORLD of FOSSIL LAKE lance grande With photography by Lance Grande and John Weinstein The University of Chicago Press | Chicago and London Ray-Finned Fishes ( Superclass Actinopterygii) The vast majority of fossils that have been mined from the FBM over the last century and a half have been fossil ray-finned fishes, or actinopterygians. Literally millions of complete fossil ray-finned fish skeletons have been excavated from the FBM, the majority of which have been recovered in the last 30 years because of a post- 1970s boom in the number of commercial fossil operations. Almost all vertebrate fossils in the FBM are actinopterygian fishes, with perhaps 1 out of 2,500 being a stingray and 1 out of every 5,000 to 10,000 being a tetrapod. Some actinopterygian groups are still poorly understood be- cause of their great diversity. One such group is the spiny-rayed suborder Percoidei with over 3,200 living species (including perch, bass, sunfishes, and thousands of other species with pointed spines in their fins). Until the living percoid species are better known, ac- curate classification of the FBM percoids (†Mioplosus, †Priscacara, †Hypsiprisca, and undescribed percoid genera) will be unsatisfac- tory. 107 Length measurements given here for actinopterygians were made from the tip of the snout to the very end of the tail fin (= total length). The FBM actinop- terygian fishes presented below are as follows: Paddlefishes (Order Acipenseriformes, Family Polyodontidae) Paddlefishes are relatively rare in the FBM, represented by the species †Cros- sopholis magnicaudatus (fig. 48). †Crossopholis has a very long snout region, or “paddle.” Living paddlefishes are sometimes called “spoonbills,” “spoonies,” or even “spoonbill catfish.” The last of those common names is misleading because paddlefishes are not closely related to catfishes and are instead close relatives of sturgeons. -
Article XXXVIII. -NOTE on SOME WORM (?) BUR- ROWS in ROCKS of the CHEMUNG GROUP of NEW YORK
Article XXXVIII. -NOTE ON SOME WORM (?) BUR- ROWS IN ROCKS OF THE CHEMUNG GROUP OF NEW YORK. By R. P. WHITFIELD. Arenicolites chemungensis, sp. nov. PLATE XIV, FIGS. I AND 2. While working up the fossils of the Potsdam sandstone for the Wisconsin Report, in I876 and I877, there came into my hands a number of specimens representing the so-called Scolithus, which I described as Arenicolites woodi in Volume IV of Prof. T. C. Chamberlain's Report of I882. One block of that series showed the original surface of the mud-covered sandstone with the burrows of the worm (?) which made the perforations, together with the little hillocks surrounding the outlet of the burrows, just as the animal built them up by its castings during life; proving pretty conclusively that it must have been a marine worm-like animal which caused the perforations. Among the geological specimens of the Chemung Group in the Museum, from near Bath, Steuben Co., New York, I find an example so nearly resembling that figured in the Wis- consin Report above referred to, that there can be no ques- tion as to the similarity of its origin. On this Chemung specimen the hillocks are somewhat larger and the funnels more distinct, being generally 5 or 6 mm. in diameter, and the walls surrounding them about 2 mm. thick, while some of the hillocks are much larger and higher and appear to have collapsed from the semifluidity of the sand, closing up the top of the burrow so as to show a mere slit in its place. -
The Evolution of Occlusal Enamel Complexity in Middle
THE EVOLUTION OF OCCLUSAL ENAMEL COMPLEXITY IN MIDDLE MIOCENE TO RECENT EQUIDS (MAMMALIA: PERISSODACTYLA) OF NORTH AMERICA by NICHOLAS ANTHONY FAMOSO A THESIS Presented to the Department of Geological Sciences and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Master of Science June 2013 THESIS APPROVAL PAGE Student: Nicholas Anthony Famoso Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America This thesis has been accepted and approved in partial fulfillment of the requirements for the Master of Science degree in the Department of Geological Sciences by: Dr. Edward Davis Chair Dr. Qusheng Jin Member Dr. Stephen Frost Outside Member and Kimberly Andrews Espy Vice President for Research & Innovation/Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded June 2013 ii © 2013 Nicholas Anthony Famoso iii THESIS ABSTRACT Nicholas Anthony Famoso Master of Science Department of Geological Sciences June 2013 Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America Four groups of equids, “Anchitheriinae,” Merychippine-grade Equinae, Hipparionini, and Equini, coexisted in the middle Miocene, and only the Equini remains after 16 million years of evolution and extinction. Each group is distinct in its occlusal enamel pattern. These patterns have been compared qualitatively but rarely quantitatively. The processes controlling the evolution of these occlusal patterns have not been thoroughly investigated with respect to phylogeny, tooth position, and climate through geologic time. I investigated two methods of quantitative analysis, Occlusal Enamel Index for shape and fractal dimensionality for complexity. -
Mammalian Faunal Change During the Early Eocene Climatic
MAMMALIAN FAUNAL CHANGE DURING THE EARLY EOCENE CLIMATIC OPTIMUM (WASATCHIAN AND BRIDGERIAN) AT RAVEN RIDGE IN THE NORTHEASTERN UINTA BASIN, COLORADO AND UTAH by ALEXANDER R. DUTCHAK B.Sc., University of Alberta, 2002 M.Sc., University of Alberta, 2005 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Geological Sciences 2010 This thesis entitled: Mammalian faunal change during the Early Eocene Climatic Optimum (Wasatchian and Bridgerian) at Raven Ridge in the northeastern Uinta Basin, Colorado and Utah written by Alexander R. Dutchak has been approved for the Department of Geological Sciences ______________________________ Jaelyn J. Eberle (Supervisor) ______________________________ John Humphrey ______________________________ Mary Kraus ______________________________ Tom Marchitto ______________________________ Richard Stucky Date: ________________________ The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. ABSTRACT Dutchak, Alexander R. (Ph.D., Geological Sciences, Department of Geological Sciences) Mammalian faunal change during the Early Eocene Climatic Optimum (Wasatchian and Bridgerian) at Raven Ridge in the northeastern Uinta Basin, Colorado and Utah Thesis directed by Assistant Professor Jaelyn J. Eberle This project investigated patterns of mammalian faunal change at Raven Ridge, which straddles the Colorado-Utah border on the northeastern edge of the Uinta Basin and consists of intertonguing units of the fluvial Colton and lacustrine Green River Formations. Fossil vertebrate localities comprising >9,000 fossil mammal specimens from 62 genera in 34 families were identified and described. -
Six Genera Are Represented: Parahippus, Hypohippus, Merychippu, Hipparion, Protohippus, and Pliohippus
1918] Matthew, Contributions to the Snake Creek Fauna 211 Teleoceras sp. The best specimen is No. 13874, a lower jaw from the Snake Creek beds, 23 miles south of Agate, Neb. It is smaller than T. medicornutus, with decidedly smaller tusk; pi present, although very small. The teeth are well worn, the molars large and hypsodont, premolars reduced, symphysis short, lower tusk upward curving; these characters place it in Teleoceras but it is much smaller and more primitive than T. fossiger. A number of teeth, and skull and skeleton parts are referable to this genus and probably to the same species. One shows the characteristic nasal with its rudi- mentary horn; various foot bones also show the generic characters, but all of them indicate a smaller and less specialized species than T. fossiger. Equidw Six genera are represented: Parahippus, Hypohippus, Merychippu, Hipparion, Protohippus, and Pliohippus. The first two are scarce; the third occurs in overwhelming abundance in most of the pockets; the fourth is almost as abundant in certain pockets; the last two are also common in certain pockets. Thus far, no skulls or skeletons have been obtained except one of Pliohippus found by H. J. Cook, but numerous upper or lower jaws and vast numbers of separate teeth. Parahippus There is evidence of but one species, which is not separable from P. cognatus Leidy. The permanent upper and lower teeth show a medium- sized, moderately progressive species with a little cement in the valleys and slopes of the cusps, but not enough to fill them until the teeth are nearly worn down.