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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. -
Unit-V Evolution of Horse
UNIT-V EVOLUTION OF HORSE Horses (Equus) are odd-toed hooped mammals belong- ing to the order Perissodactyla. Horse evolution is a straight line evolution and is a suitable example for orthogenesis. It started from Eocene period. The entire evolutionary sequence of horse history is recorded in North America. " Place of Origin The place of origin of horse is North America. From here, horses migrated to Europe and Asia. By the end of Pleis- tocene period, horses became extinct in the motherland (N. America). The horses now living in N. America are the de- scendants of migrants from other continents. Time of Origin The horse evolution started some 58 million years ago, m the beginning of Eocene period of Coenozoic era. The modem horse Equus originated in Pleistocene period about 2 million years ago. Evolutionary Trends The fossils of horses that lived in different periods, show that the body parts exhibited progressive changes towards a particular direction. These directional changes are called evo- lutionary trends. The evolutionary trends of horse evolution are summarized below: 1. Increase in size. 2. Increase in the length of limbs. 3. Increase in the length of the neck. 4. Increase in the length of preorbital region (face). 5. Increase in the length and size of III digit. 6. Increase in the size and complexity of brain. 7. Molarization of premolars. Olfactory bulb Hyracotherium Mesohippus Equus Fig.: Evolution of brain in horse. 8. Development of high crowns in premolars and molars. 9. Change of plantigrade gait to unguligrade gait. 10. Formation of diastema. 11. Disappearance of lateral digits. -
Skeleton of the Oligocene (30 Million-Year-Old) Horse, Mesohippus, Is a Featured Exhibit at the New North Dakota Cowboy Hall of Fame in Medora
Skeleton of the Oligocene (30 million-year-old) horse, Mesohippus, is a featured exhibit at the new North Dakota Cowboy Hall of Fame in Medora By John W. Hoganson Developers of the recently opened North Dakota Cowboy Hall of Fame contacted me about having a fossil exhibit in the new Hall in Medora. Of course, what would be more appropriate than an exhibit interpreting the evolution of the horse? Most people are under the false impression that horses did not inhabit North America until they were introduced by the Spaniards during the early days of conquest. But horses are indigenous to North America. Fossil remains of the earliest horse, referred to as Hyracotherium (or sometimes Eohippus), have been recovered from early Eocene (about 50 million years old) rocks in North America. In fact, they were some of the most abundant mammals that lived during that time. The fossil record of horses in North Dakota extends back to the Oligocene, about 30 million years ago, when the diminutive horse, Mesohippus roamed western North Dakota. Mesohippus was tiny, about the size of a sheep. The adults were only about 20 inches tall at the shoulder. They also had three toes on each foot compared to the modern horse Equus that has one. Mesohippus was also probably more of a browsing herbivore compared to the modern grazing horse. We have found many Mesohippus fossils in North Dakota but no complete skeletons. Consequently, the Mesohippus skeleton on exhibit at the Cowboy Hall of Fame is an exact cast replica. We have also found the remains of 50,000-year-old horses in North Dakota indicating that horses lived here during the last Ice Age. -
Scale-Dependence of Cope's Rule in Body Size Evolution of Paleozoic
Scale-dependence of Cope’s rule in body size evolution of Paleozoic brachiopods Philip M. Novack-Gottshall* and Michael A. Lanier Department of Geosciences, University of West Georgia, Carrollton, GA 30118-3100 Edited by Steven M. Stanley, University of Hawaii at Manoa, Honolulu, HI, and approved January 22, 2008 (received for review October 10, 2007) The average body size of brachiopods from a single habitat type volume) for 369 adult genera [see supporting information (SI) increased gradually by more than two orders of magnitude during Appendix, Tables 1 and 2] from deep-subtidal, soft-substrate their initial Cambrian–Devonian radiation. This increase occurred habitats demonstrates that brachiopod body size increased sub- nearly in parallel across all major brachiopod clades (classes and stantially and gradually during the Early and Mid-Paleozoic (Fig. orders) and is consistent with Cope’s rule: the tendency for size to 1), from a Cambrian mean of 0.04 ml (Ϫ1.40 log10 ml Ϯ 0.27 SE, increase over geological time. The increase is not observed within n ϭ 18 genera) to a Devonian mean of 1.55 ml (0.19 log10 ml Ϯ small, constituent clades (represented here by families), which 0.06, n ϭ 150). The magnitude of size increase between periods underwent random, unbiased size changes. This scale-dependence is statistically significant. We evaluated within-phylum dynamics is caused by the preferential origination of new families possessing by using maximum-likelihood comparisons among three evolu- initially larger body sizes. However, this increased family body size tionary models: directional (driven, biased, general random does not confer advantages in terms of greater geological duration walk) change (DRW), unbiased (passive) random walk (URW), or genus richness over families possessing smaller body sizes. -
Paleobiology of Archaeohippus (Mammalia; Equidae), a Three-Toed Horse from the Oligocene-Miocene of North America
PALEOBIOLOGY OF ARCHAEOHIPPUS (MAMMALIA; EQUIDAE), A THREE-TOED HORSE FROM THE OLIGOCENE-MIOCENE OF NORTH AMERICA JAY ALFRED O’SULLIVAN A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2002 Copyright 2002 by Jay Alfred O’Sullivan This study is dedicated to my wife, Kym. She provided all of the love, strength, patience, and encouragement I needed to get this started and to see it through to completion. She also provided me with the incentive to make this investment of time and energy in the pursuit of my dream to become a scientist and teacher. That incentive comes with a variety of names - Sylvan, Joanna, Quinn. This effort is dedicated to them also. Additionally, I would like to recognize the people who planted the first seeds of a dream that has come to fruition - my parents, Joseph and Joan. Support (emotional, and financial!) came to my rescue also from my other parents—Dot O’Sullivan, Jim Jaffe and Leslie Sewell, Bill and Lois Grigsby, and Jerry Sewell. To all of these people, this work is dedicated, with love. ACKNOWLEDGMENTS I thank Dr. Bruce J. MacFadden for suggesting that I take a look at an interesting little fossil horse, for always having fresh ideas when mine were dry, and for keeping me moving ever forward. I thank also Drs. S. David Webb and Riehard C. Hulbert Jr. for completing the Triple Threat of Florida Museum vertebrate paleontology. In each his own way, these three men are an inspiration for their professionalism and their scholarly devotion to Florida paleontology. -
Florida Fossil Horse Newsletter
Florida Fossil horse Newsletter Volume 10, Number 1, 1st Half 2001 What's Inside? Fossil Horses On the Road: Archaeohippus and Parahippus Check Out the Bluegrass State Meet Our Artists Volunteers Help the Museum While Enhancing Their Own Education Thunderbeasts, Sexual Selection and Extinction Skeleton "Under Construction" Homeschooling Groups Request More Family Days at Thomas Farm Book Review - The Fossil Vertebrates of Florida Introducing A New Logo For Pony Express's 10th Anniversary Fossil Horses On the Road: Archaeohippus and Parahippus Check Out the Bluegrass State Lexington, Kentucky welcomed Miocene horses at a special event at the Lexington Children's Museum, March 3, 2001. Loaned by the Florida Museum of Natural History, many fossils of the two small prehistoric horses from Thomas Farm are being displayed at the Children's Museum through March and April. Touchable casts of the skulls and feet are also charming the kids, who think the "little horses" are just awesome. At the all-day fossil event, a large display was set up with a case for some of the more fragile horse Seth Woodring, 3, of Winchester, made himself a plaster "fossil" with some help from his mother, fossils. Three Beth, and 5-year-old sister, Rayne. David Stephenson photo (reprinted with permission from tables held fossil Herald Leader) bones and casts, with modern horse bones for comparison. Experts Dr. Teri Lear and Dr. Lenn Harrison, with the Department of Veterinary Science at the University of Kentucky, presented Archaeohippus and Parahippus to the public. Teri has participated in several digs at Thomas Farm, and talked with visitors about the Miocene digs and fossils. -
The Dinosaurs of North America
FEOM THE SIXTEENTH ANNUAL KEPOKT OF THE U. S, GEOLOGICAL SURVEY THE DINOSAURS OF NORTH AMERICA OTHNIEL CHARLES MARSH TALE UNIVERSITY WASHINGTON 1896 ^33/^, I/BRAKt 4 ,\ . THE DINOSAURS OF NORTH AMERICA. BY OTHNIEL CHARLES MARSH. 133 CONTENTS. Pajje. Introduction 143 Part I. —Triassic dinosaurs 146 Theropoda 146 Anchisaurida? 147 Anchisaurus 147 The skull 148 The fore limbs 149 The hind limbs 149 Anchisaurus solus 149 Amniosaurus rTT 150 Eestoration of Anchisaurus 150 Dinosaurian footprints 151 Distribution of Triassic dinosaurs 152 Part II. —Jurassic dinosaurs 152 Theropoda : 153 Hallopus 153 Fore and hind limbs 154 Coelurus _ 155 The vertebra:- 155 The hind limbs 156 Ceratosaurus 156 The skull 157 The brain 159 The lower iaws 159 The vertebra: 159 The scapular arch 160 The pelvic arch 160 The metatarsals 162 Eestoration of Ceratosaurus 163 Allosaurus 163 European Theropoda 163 Sauropoda 164 Atlantosaurus beds 164 Families of Sauropoda 165 Atlantosauridie 166 Atlantosaurus 166 Apatosaurus 166 The sacral cavity 166 The vertebra- 167 Brontosaurus 168 The scapular arch 168 The cervical vertebra.- 169 The dorsal vertebree 169 The sacrum 170 The caudal vertebra- 171 The pelric arch 172 The fore limbs 173 The hind limbs 173 135 136 CONTENTS. Part II. —Jurassic dinosaurs—Continued. Page. Sauropoda—Continued. Atlantosaurida? —Continued. Restoration of Brontosaurus 173 Barnsaurus 174 Diplodoeida? 175 Diplodocus 175 The skull 175 The brain 178 The lower jaws 178 The teeth 179 The vertebra; 180 The sternal bones 180 The pelvic girdle 180 Size and habits 180 Morosaurida? 181 Morosaurus 181 The skull 181 The vertebra? 181 The fore limbs 182 The pelvis 182 The hind limbs 183 Pleuroccelida? : 183 Pleurocoelus 183 The skull 183 The vertebras 183 Distribution of the Sauropoda 185 Comparison with European forms 185 Predentata ». -
Bruce J. Macfadden*
MacFadden, B.J., 2006, Early Pliocene (latest Hemphillian) horses from the Yepómera Local 33 Fauna, Chihuahua, Mexico, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Advances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic Interchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 33–43. EARLY PLIOCENE (LATEST HEMPHILLIAN) HORSES FROM THE YEPÓMERA LOCAL FAUNA, CHIHUAHUA, MEXICO Bruce J. MacFadden* ABSTRACT The latest Hemphillian (Hh4) is characterized by a distinctive equid assemblage, four spe- cies of which are widespread in North America. One of the largest collections of Hh4 equids is from Yepómera, located in Chihuahua, Mexico. Although Yepómera is actually a series of sub-localities, the equids are morphologically similar from each of these and therefore can be considered as a local faunal assemblage of four sympatric species. The distinctive dental patterns, size of the cheek teeth, and (in most cases) metapodial dimensions, make these horses readily distinguishable in the field. Yepómera equids include the monodactyl Astrohippus stockii and Dinohippus mexicanus, and tridactyl Neohipparion eurystyle and Nannippus aztecus. Yepómera is the type locality for the species A. stockii and D. mexica- nus, both described by Lance in 1950. Neohipparion eurystyle and the genus Neohipparion and A. stockii and the genus Astrohippus become extinct at the end of Hh4. Nannippus aztecus is a sister taxon of later Nannippus and D. mexicanus is the sister taxon of Equus, the equid genera that survived in North America during the Plio-Pleistocene. With hypsodonty indices between 2.6 and 3.7, all of the Yepómera horse species have high-crowned teeth, traditionally interpreted as a grazing adaptation. -
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. -
Evolution of the Horse M
Volume 2 | Issue 2 Article 10 1940 Evolution of the Horse M. R. Benson Iowa State College Follow this and additional works at: https://lib.dr.iastate.edu/iowastate_veterinarian Part of the Evolution Commons, and the Large or Food Animal and Equine Medicine Commons Recommended Citation Benson, M. R. (1940) "Evolution of the Horse," Iowa State University Veterinarian: Vol. 2 : Iss. 2 , Article 10. Available at: https://lib.dr.iastate.edu/iowastate_veterinarian/vol2/iss2/10 This Article is brought to you for free and open access by the Journals at Iowa State University Digital Repository. It has been accepted for inclusion in Iowa State University Veterinarian by an authorized editor of Iowa State University Digital Repository. For more information, please contact [email protected]. Evolution of the Horse M. R. BENSON Class of 1940 HE phylogeny of the horse family digits (c) on both fore and rear feet. The T is perhaps the most complete record animal was more adapted for speed. of organic evolution that modern science Many representatives of this group have has discovered. This article is an at been discovered, ranging from 18 inches tempt to show briefly the outstanding to 24 inches, or 6 hands in height. This steps in the development of the modern animal is usually considered as a tran horse. sitional type between the earlier forest Most investigators agree that the horse dwelling animal and the later plains tribe originated during the Eocene epoch. inhabiting creature. Luxuriant forests grew in the warm, The Miocene era was a time of great humid climate which characterized this topographical change during which our era in North America. -
Recent Polydactyle Horses ; by 0
I 338 Scientific Intelligence. figures in this paper from the same beds several other apparently aquatic plants, a palm, and three conifers. Two of these latter, Brenclopsis Iioheneggeri and Geinitzia cretacea are indicative of an even earlier period. L. F. W. 0. Hec/icrches sur la Vegetation 'du niveau Aquitanien de Manosque; par le Marquis G. DE SAPORTA. Memoires de la Soc. Geol. do France, tome ii; I, Nympheinees, Fasc. i, Mem. No. 9, APPENDIX. pp. 22, pi. iii-vi; II, Palmiers, Fasc. 2, Mem. No. 9, pp. 23-34, pi. ix-xi.—The first of these papers treats of some important re cent discoveries of Nympheaceous plants in the beds of Manosque, Cerestc, and Bois rt'Asson, chiefly by local collectors, the princi ART. XLIII.—Recent Polydactyle Horses ; by 0. 0. MARSH. pal of whom are M. Nalin and Mile. Rostan. The flora of these deposits as previously published by the author is reviewed and IN this Journal for June, 1879, the writer made a brief the new species described and fully illustrated. These include five species of Nymphsea, one of Aneectomeria, and one of Nelumbium. summary of the facts then known to him in regard to existing Associated with these was found a Ceratophyllum (C. aquitani- horses with extra digits, especially in relation to the extinct cum), and the view is expressed that this anomalous genus is species he had discovered in the Rocky Mountains, and also really related to the Nymphajaceae. This view had already been gave figures of typical examples of existing and fossil forms.* suggested by Brongniart based on the similarity of the seeds, but Since then, he has collected much material bearing on the most authors put this genus in an apetalous order by itself, though question, particularly of extinct horses, and an illustrated Baillon places it in the Piperacese. -
Evolution of Horse
UNIT 11 EVOLUTION OF HORSE Structure____________________________________________________ 11.1 Introduction 11.3 Role of Climate in the Evolution of Horse Expected Learning Outcomes 11.4 Activity 11.2 Evolution of Horse 11.5 Summary Systematic Palaeontology 11.6 Terminal Questions Place and Time of Origin 11.7 References Major Evolutionary Transitions 11.8 Further/Suggested Readings Phylogeny of Horse 11.9 Answers 11.1 INTRODUCTION Vertebrates are a diverse group of organisms ranging from lampreys to human beings. The group includes animals with backbone, such as fishes, amphibians, reptiles, birds and mammals. The dinosaurs that have caught public attention by making their appearance in several films and books too are vertebrates. Vertebrates have a long geological history on the planet Earth beginning more than 500 million years (Myr) ago, starting from the Cambrian to the present. They first appeared in the fossil record during the Cambrian period of the Palaeozoic era. Fishes, amphibians and reptiles were the most dominant groups of vertebrates in the Palaeozoic and Mesozoic eras. In the Mesozoic era, dinosaurs- a group of reptiles, and mammals made their appearance. Dinosaurs had a wide geographic distribution, being reported from all continents and were the largest animals to roam the Earth during the Mesozoic era. The mammals began to diversify only after the demise of dinosaurs at the close of the Mesozoic era at around 66 Myr ago. In the Cenozoic era, mammals rapidly occupied every niche and corner of the globe and therefore, the Cenozoic era is also known as the “Age of Mammals”. Introduction to Palaeontology Block……………………………………………………………………………………………….….............….…........ 3 Mammals of the Cenozoic era belong to three groups: placentals (that give birth to young ones), marsupials (in which an offspring after birth continues to develop within the pouch of the mother) and monotremes (egg laying mammals).