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A.-The Pondaung Fauna
Article VI.-FOSSIL MAMMALS FROM BURMA IN THE AMERICAN MUSEUM OF NATURAL HISTORY BY EDWIN H. COLBERT FIGuRES 1 TO 64 CONTENTS PAGE INTRODUCTION ........................................................ 259 The American Museum Palaeontological Expedition to Burma............ 259 Previous Publications on Fossil Mammals of Burma..................... 259 Studies on the American Museum Burma Collection..................... 261 Acknowledgments ................................................... 262 THIE CONTINENTAL TERTIARY AND QUATERNARY BEDS OF NORTHERN BURMA. 263 General Observations................................................ 263 Mammal-Bearing Beds of Northern Burma............................. 264 The Pondaung Sandstone........................................... 265 The Freshwater Pegu Beds......................................... 267 The Irrawaddy Series.............................................. 267 Correlation of the Mammal Bearing Horizons of Northern Burma ......... 268 Pondaung Fauna.................................................. 268 Pegu Series....................................................... 275 Lower Irrawaddy Fauna............................................ 276 Upper Irrawaddy Fauna............................................ 277 THE FoSSIL MAMMAL FAUNAS OF BURMA ................................ 280 Pondaung Fauna......................................... 280 Mammals from the Pegu Series........................................ 280 Lower Irrawaddy Fauna......................................... 281 Upper Irrawaddy -
Mammal Faunal Change in the Zone of the Paleogene Hyperthermals ETM2 and H2
Clim. Past, 11, 1223–1237, 2015 www.clim-past.net/11/1223/2015/ doi:10.5194/cp-11-1223-2015 © Author(s) 2015. CC Attribution 3.0 License. Mammal faunal change in the zone of the Paleogene hyperthermals ETM2 and H2 A. E. Chew Department of Anatomy, Western University of Health Sciences, 309 E Second St., Pomona, CA 91767, USA Correspondence to: A. E. Chew ([email protected]) Received: 13 March 2015 – Published in Clim. Past Discuss.: 16 April 2015 Revised: 4 August 2015 – Accepted: 19 August 2015 – Published: 24 September 2015 Abstract. “Hyperthermals” are past intervals of geologically vulnerability in response to changes already underway in the rapid global warming that provide the opportunity to study lead-up to the EECO. Faunal response at faunal events B-1 the effects of climate change on existing faunas over thou- and B-2 is also distinctive in that it shows high proportions sands of years. A series of hyperthermals is known from of beta richness, suggestive of increased geographic disper- the early Eocene ( ∼ 56–54 million years ago), including sal related to transient increases in habitat (floral) complexity the Paleocene–Eocene Thermal Maximum (PETM) and two and/or precipitation or seasonality of precipitation. subsequent hyperthermals (Eocene Thermal Maximum 2 – ETM2 – and H2). The later hyperthermals occurred during warming that resulted in the Early Eocene Climatic Opti- mum (EECO), the hottest sustained period of the Cenozoic. 1 Introduction The PETM has been comprehensively studied in marine and terrestrial settings, but the terrestrial biotic effects of ETM2 The late Paleocene and early Eocene (ca. -
Perissodactyla, Mammalia) from the Middle Eocene of Myanmar Un Nouveau Tapiromorphe Basal (Perissodactyla, Mammalia) De L’Eocène Moyen Du Myanmar
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Geobios 39 (2006) 513–519 http://france.elsevier.com/direct/GEOBIO/ Original article A new basal tapiromorph (Perissodactyla, Mammalia) from the middle Eocene of Myanmar Un nouveau tapiromorphe basal (Perissodactyla, Mammalia) de l’Eocène moyen du Myanmar Grégoire Métais a, Aung Naing Soe b, Stéphane Ducrocq c,* a Carnegie Museum of Natural History, Section of Vertebrate Paleontology, 4400 Forbes Avenue, Pittsburgh, PA 15213, USA b Department of Geology, Yangon University, Yangon 11422, Myanmar c Laboratoire de Géobiologie, Biochronologie et Paléontologie Humaine, UMR 6046 CNRS, Faculté des Sciences de Poitiers, 40, avenue du recteur-Pineau, 86022 Poitiers cedex, France Received 29 September 2004; accepted 10 May 2005 Available online 20 March 2006 Abstract A new genus and species of tapiromorph, Skopaiolophus burmese nov. gen., nov. sp., is described from the middle Eocene Pondaung For- mation in central Myanmar. This small form displays a striking selenolophodont morphology associated with a mixture of primitive “condylar- thran” dental characters and derived tapiromorph features. Skopaiolophus is here tentatively referred to a group of Asian tapiromorphs unknown so far. The occurrence of such a form in Pondaung suggests that primitive tapiromorphs might have persisted in southeast Asia until the late middle Eocene while they became extinct elsewhere in both Eurasia and North America. © 2006 Elsevier SAS. All rights reserved. Résumé Un nouveau genre et une nouvelle espèce de tapiromorphe, Skopaiolophus burmese nov. gen. nov. sp., sont décrits dans la Formation de Pondaung d’âge fini-éocène moyen, au Myanmar. -
Proceedings of the United States National Museum
NOTES ON THE OSTEOLOGY AND RELATIONSHIP OF THE FOSSIL BIRDS OF THE GENERA HESPERORNIS HAR- GERIA BAPTORNIS AND DIATRYMA. By Frederic A. Lucas, Acting Curator, Section of Vertebrate Fossils. Our knowledge of the few Cretaceous birds that have been discov- ered in North America is very imperfect in spite of Professor Marsh's memoir on the Odontonithes; their origin and man}^ points of their structure are still unknown and their relationship uncertain. By the kindness of Professor Williston, I am able to add a little to our knowl- edge of the structure of ITe><per<yrniH grdcUlH and Bdj^tornis advenus^ while the acquisition of a specimen of IL'sperornis regalis, by the United States National Museum, enables me to add a few details con- cerning that species. ' CRANIUM OF HESPERORNIS GRACILIS. The example of Ilesperornis gracilh belongs to the Universit}'' of Kansas, and comprises a large portion of the skeleton, including the skull. Unfortunately the neck was doubled backward, so that the skull lay against the pelvis, while portions of dorsal and sternal ribs had become crushed into and intimately associated with the cranium, so that it was impossible to make or.t the shape of the palatal bones, provided even they were present. This was particularly unfortunate, as information as to the character of the palate of the toothed birds is greatly to be desired. Theoretically, the arrangement of the bones of the palate should be somewhat reptilian, or, if the struthious ])irds are survivals, the palate of such a bird as Hesperornis should present some droma^ognathous characters. -
Othniel Charles Marsh
NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA BIOGRAPHICAL MEMOIRS VOLUME XX-FIRST MEMOIR BIOGRAPHICAL hlEhlOIR OE OTHNIEL CHARLES MARSH BY CHARLES SCHUCHEKT PRESENTED TO THE -4C.4DEhlY AT THE ASSU.\L JIEETIPU'G, 1938 OTHNIEL CHARLES MARSH BY CHARLES SCHUCIIERT Othniel Charles Marsh, for ,twelve years president of the National r\caderny of Sciences, was born to Caleb Marsh and Mary Gaines Peabody on October 29, 1831, in Lockport, New York, and died in New Haven, Connecticut, on March 18, 1899. One of the three founders of the science of vertebrate paleon- tology in America, his career furnishes an outstanding exatnple of the indomitable spirit that drives men on to a determined goal. His motto might well have been. "\l.That 1 have, I hold." He asked no quarter, and gave none. :It home around a camp fire or in an army tent, formal as a presiding officer or in society, at times austere and autocratic, at others a raconteur of note, he left a lasting impression on his chosen 111-anch of science. Summarizing his work statistically, it may be said that he- tween 1861 and 1899 he published about 300 papers, reports, and books. Of new genera he described 225, and of new species, 496; of new families 64, of su1)orders 8, of orders 19, and of subclasses I. Of his work on vertebrate fossils in general, Osbom says that he "carried out the most intensive field esl)loration known to science ant1 pul~lishetl a large num1)er of 1)reliminary papcrs, which fairly revol~~tionizedour knowledge." ANCESTRY AKD TIZ:\INISG John hlarsh of Salem, the first of his name recorded as emigrating from England to America, is believctl to have reached In the preparation of this memorial, the writer has been aided greatly by the excellent skctches of Professor Marsh writtcn by George Bird Grinnell, Charles E. -
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. -
Fossil Birds in the Marsh Collection of Yale University 7
TRANSACTIONS OF THE CONNECTICUT ACADEMY OF ARTS AND SCIENCES VOLUME 19, PAGES 1-llO FEBRUARY, 1915 CONTRIBUTIONS FROM THE MARSH PUBLICATION FUND, PEABODY MUSEUM, YALE UNIVERSITY Fossil Birds in the Marsh Collection of Yale University BY R. W. SHUFELDT YALE UNIVERSITY PRESS NEW HAVEN, CONN. 1915 COMPOSED AND PRINTED AT THE WAVERLY PRESS BY THE WILLIAMS & WILKINS CoMPANY BALTIMORE, Mo., U.S. A. TABLE OF CONTENTS Page INTRODUCTION............ ..............................•........., ...... , 5 CRETACEOUS BIRDS..................................................... 8 EoCENE BIRDs...... ....................•....•.......................... 28 OLIGOCENE BIRDS.. • . • . 54 MIOCENE BIRDS.. • . 60 PLEISTOCENE BIRDS... .. .... ................................ ......... 64 BIRDS OF UNCERTAIN GEOLOGICAL PoSITION ........... ......., ...... ... , . 70 FRAGMENTARY MATERIAL.... ......................•.....•............ , . 73 SUMMARY.......• ................................••..••.••..•.••..•...•. 74 FOSSIL BIRDS IN THE MARSH COLLEC TION OF YALE UNIVERSITY BY R. w. SHUFELDT. INTRODUCTION. On the twelfth of March, 1914, Professor Charles Schuchert, Curator of the Geological Department of the Peabody Museum, Yale University, sent me for revision nearly all the fossil birds (types) that had, in former years, been described, and in some few instances figured,by Professor 0. C. Marsh. These did not include the species of the genera Ichthyornis and Hesperornis, and one or two others, as they were then receiving the attention of Professor R. S. Lull of the above institution. The material upon which Marsh based his Grus proavus could not, after long and careful search, be located, and up to the present writing I have never seen it. Five of the types described by that distinguished palreontologist were in the collection of the Academy of Natural Sciences of Phila delphia, and for the loan of these I am under great obligations to Doctor Witmer Stone of that institution who, with unbounded kind ness, sent them to me for study in the present connection. -
New Early Eocene Basal Tapiromorph from Southern China and Its Phylogenetic Implications
New Early Eocene Basal tapiromorph from Southern China and Its Phylogenetic Implications Bin Bai1,2*, Yuanqing Wang1*, Jin Meng2,1, Qian Li1, Xun Jin1 1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China, 2 Division of Paleontology, American Museum of Natural History, New York, New York, United States of America Abstract A new Early Eocene tapiromorph, Meridiolophus expansus gen. et sp. nov., from the Sanshui Basin, Guangdong Province, China, is described and discussed. It is the first reported Eocene mammal from the basin. The new taxon, represented by a left fragmentary mandible, is characterized by an expanded anterior symphyseal region, a long diastema between c1 and p1, a rather short diastema between p1 and p2, smaller premolars relative to molars, an incipient metaconid appressed to the protoconid on p3, a prominent entoconid on p4, molar metaconid not twinned, cristid obliqua extending mesially and slightly lingually from the hypoconid, inclined metalophid and hypolophid, and small hypoconulid on the lower preultimate molars. Meridiolophus is morphologically intermediate between basal Homogalax-like taxa and derived tapiromorphs (such as Heptodon). Phylogenetic analysis indicates Equidae is more closely related to Tapiromorpha than to Palaeotheriidae, although the latter is only represented by a single species Pachynolophus eulaliensis. ‘Isectolophidae’, with exception of Meridiolophus and Karagalax, has the closest affinity with Chalicotherioidea. Furthermore, the majority rule consensus tree shows that Meridiolophus is closer to Karagalax than to any other ‘isectolophid’, and both genera represent stem taxa to crown group Ceratomorpha. Citation: Bai B, Wang Y, Meng J, Li Q, Jin X (2014) New Early Eocene Basal tapiromorph from Southern China and Its Phylogenetic Implications. -
Timing the Extant Avian Radiation: the Rise of Modern Birds, and The
1 Timing the extant avian radiation: The rise of modern birds, and the importance of modeling molecular rate variation Daniel J. Field1, Jacob S. Berv2, Allison Y. Hsiang3, Robert Lanfear4, Michael J. Landis5, Alex Dornburg6 1 Department of Earth Sciences, University of Cambridge, Cambridge, Cambridgeshire, United Kingdom 2Department of Ecology & Evolutionary Biology, Cornell University, Ithaca, New York, USA 3Department of Bioinformatics and Genetics, Swedish Museum of Natural History, Stockholm, Sweden 4Ecology and Evolution, Research School of Biology, Australian National University, Canberra, Australia 5Department of Ecology & Evolutionary Biology, Yale University, New Haven, Connecticut, USA 6 North Carolina Museum of Natural Sciences, Raleigh, North Carolina, USA Corresponding author: Daniel J. Field1 Email address: [email protected] PeerJ Preprints | https://doi.org/10.7287/peerj.preprints.27521v1 | CC BY 4.0 Open Access | rec: 6 Feb 2019, publ: 6 Feb 2019 2 ABSTRACT Unravelling the phylogenetic relationships among the major groups of living birds has been described as the greatest outstanding problem in dinosaur systematics. Recent work has identified portions of the avian tree of life that are particularly challenging to reconstruct, perhaps as a result of rapid cladogenesis early in crown bird evolutionary history (specifically, the interval immediately following the end-Cretaceous mass extinction). At face value this hypothesis enjoys support from the crown bird fossil record, which documents the first appearances of most major crown bird lineages in the early Cenozoic—in line with a model of rapid post-extinction niche filling among surviving avian lineages. However, molecular-clock analyses have yielded strikingly variable estimates for the age of crown birds, and conflicting inferences on the impact of the end-Cretaceous mass extinction on the extant bird radiation. -
A New Specimen of the Early Cretaceous Bird Hongshanornis Longicresta: Insights Into the Aerodynamics and Diet of a Basal Ornithuromorph
A new specimen of the Early Cretaceous bird Hongshanornis longicresta: insights into the aerodynamics and diet of a basal ornithuromorph Luis M. Chiappe1, Zhao Bo2, Jingmai K. O’Connor3, Gao Chunling2, Wang Xuri2,4, Michael Habib5, Jesus Marugan-Lobon6, Meng Qingjin7 and Cheng Xiaodong2 1 Dinosaur Institute, Natural History Museum of Los Angeles County, Los Angeles, CA, USA 2 Dalian Natural History Museum, District Dalian, PR China 3 Institute of Vertebrate Paleontology and Paleoanthroplogy, Beijing, PR China 4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing, PR China 5 University of Southern California, Health Sciences Campus, Los Angeles, CA, USA 6 Unidad de Paleontolog´ıa, Dpto. Biolog´ıa, Universidad Autonoma´ de Madrid, Cantoblanco, Spain 7 Beijing Natural History Museum, Beijing, PR China ABSTRACT The discovery of Hongshanornis longicresta, a small ornithuromorph bird with un- usually long hindlimb proportions, was followed by the discovery of two closely related species, Longicrusavis houi and Parahongshanornis chaoyangensis. Together forming the Hongshanornithidae, these species reveal important information about the early diversity and morphological specialization of ornithuromorphs, the clade that contains all living birds. Here we report on a new specimen (DNHM D2945/6) referable to Hongshanornis longicresta that contributes significant information to bet- ter understand the morphology, trophic ecology, and aerodynamics of this species, as well as the taxonomy of the Hongshanornithidae. Most notable are the well- preserved wings and feathered tail of DNHM D2945/6, which afford an accurate reconstruction of aerodynamic parameters indicating that as early as 125 million Submitted 30 August 2013 years ago, basal ornithuromorphs had evolved aerodynamic surfaces comparable in Accepted 11 December 2013 Published 2 January 2014 size and design to those of many modern birds, and flight modes alike to those of some small living birds. -
University of Michigan University Library
OVERVIEW OF MAMMALIAN BIOSTRATIGRAPHY IN THE PALEOCENE-EOCENE FORT UNION AND WILLWOOD FORMATIONS OF THE BIGHORN AND CLARKS FORK BASINS PHILIPD. GINGERICH~and WILLIAMC. CLYDE^ 1Department of Geological Sciences and Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48109-1079 2Department of Earth Sciences, University of New Hampshire, Durham, New Hampshire 03824-3589 Abstract. -Some 2200 fossil vertebrate localities are known from the Paleocene Fort Union Formation and from the Paleocene and lower Eocene Willwood Formation of the Bighorn and Clarks Fork basins in northwestern Wyoming. Many localities yield faunas adequate to enable reference to one of the twenty distinct land-mammal zones representing the Puercan, Torrejonian, Tiffanian, Clarkforkian, and Wasatchian land-mammal ages spanning Paleo- cene and early Eocene time here. These are grouped biostratigraphically and plotted on a map of the two basins combined. Range charts of mammalian genera are compared for (1) the Polecat Bench-Sand Coulee area in the Clarks Fork and northern Bighorn basins, (2) the Foster Gulch-McCullough Peaks area in the northern Bighorn Basin, (3) the central Bighorn Basin, and (4) the southern Bighorn Basin. These show that mammalian biostratigraphy is similar in all four areas, with parts of the stratigraphic record being better developed in some areas than in others. The Paleocene and earliest Eocene are best known from the Clarks Fork Basin and from the northern Bighorn Basin, whereas middle and late early Eocene faunas are principally known from the west side of the northern and central parts of the Bighorn Basin. East-west asymmetry in the distribution of mammalian faunas reflects overthrusting from the west as strata and their contained fossil faunas accumulated and were buried. -
The Oldest Known Bird Archaeopteryx Lithographica Lived During the Tithonian Stage of the Jurassic Some 150 Ma (Megannum = Million Years) Ago
T y r b e r g , T .: Cretaceous© Ornithologische Birds Gesellschaft Bayern, download unter www.biologiezentrum.at 249 Verh. orn. Ges. Bayern 24, 1986: 249—275 Cretaceous Birds - a short review of the first half of avian history By Tommy Tyrberg 1. Introduction The oldest known bird Archaeopteryx lithographica lived during the Tithonian stage of the Jurassic some 150 Ma (Megannum = million years) ago. The Cretaceous period which lasted from ca 144 Ma to 65 Ma therefore constitutes approximately one half of known avian history (table 1). During these 80 Ma birds evolved from the primitive Archaeopteryx — in many ways intermediate between birds and reptiles - to essentially modern forms which in some cases are recognizable as members of extant avian orders. Unfortunately this process is very poorly documented by fossils. Fossil birds as a general rule are not common. The lifestyle of birds and their fragile, often pneumatized, bones are not conducive to successful fossilization, and even when preserved avian bones are probably often overlooked or misidentified. Col- lectors investigating Mesozoic Continental deposits are likely to have their “search image” centered on either dinosaurs or mammals. It is symptomatic that of the five known specimens of Archaeopteryx two were originally misidentified, one as a ptero- saur and the other as a small dinosaur Compsognathus. Even when a fossil has been collected and identified as avian, problems are far from over. Avian skeletal elements are frequently badly preserved and rather undiagnostic, moreover birds (usually) lack teeth. This is a serious handicap since teeth are durable and frequently yield a remarkable amount of information about the lifestyle and taxo- nomic position of the former owners.