45 Million Years Ago. the Oldest Known Horse Was Four-Toed Browser

Total Page:16

File Type:pdf, Size:1020Kb

45 Million Years Ago. the Oldest Known Horse Was Four-Toed Browser H)1acothenum Hyracotherium 55- 45 million years ago. The oldest known horse w as four-toed browser that foraged on nonflbrous foods. Its molars showed the beginning of horse-like ridges be ter SUI ed for grazing Miohippus 33- 29 mya . This two-toed browser was sible for a burst of i side branches in the horse Iy Its descen dants were numerous and distinct. Merychippus 17-11 mya The fi rst grazing horse had stro g, cres • ed teeth that enabled it to eat abraSive grass es. Even w ith primitive three- oed feet, its long legs eqUip ped it for quick escapes and long-distance migrati ons. £quus 5 mya The single survivor of the formerly diverse horse genus, its living species include horses, asse s, and zebras. Domestication of Equus 3,000 years ago dramati cally Impacted the world's ciVilizations by facil­ Ita ting agriculture, migration, ilnd warfare . fQlJU5 • H. Gregory McDonald, Ph.D. Director 0 Sci~ n ce a Pal eo!1lol y University of Col do Museum • Equus Evolves McDonald • Equu~ Evolve~ CHAPTER TWO he mystique of the horse seems universal. It is a survivor, a reli c of the past, a rem inder of a primeva l and very different Earth Today there are eight species of horses, including zebras, donkeys, asses, burros, onagers, kulans, kiangs, and domestic horses, as well as the recently extinct quagga. All eight li ving species belong to the genus Equus, the Lati n word for horse and the source for the term equestrian However, the horses preserved in the foss il record represent as many as 40 Secrets of the MaSlc Valley si x to eight genera, w ith each genus having numerous species. Although scientists once upheld the horse as a model of linear sequence, that model no longer applies Despite the horse's ancient success, by 3.7 million years ago the number of genera fel l to three in North America. Members included a sma ll form known as Nannippus, a larger rel­ ative called Cormohipparion, and Equus. The first two genera repre­ sent lineages with a long history starting si xteen mil lion years ago. Both ultimately became extinct, leaving no descendants. In con­ trast, Equus, a relative latecomer geologically speaking, first appeared only 3.7 mi llion years ago . The genus quickly adapted and diversified, eventually d is­ persing from North America into Asia, Europe, and Africa where its descendants stil l survive. What was it about Equus that made its survival possible when all other types of horses became extinct? Paleontologists look for answers in the anatomy and ecology of Hagerman 's Equus simp/icidens. By examining the fossilized remains of the earliest known species of Equus, science can better explain w hy the horse lineage survived. We refer to the earliest known ARunning species of Equus Ma(hine as the "Hagerman Horse" in refer­ ence to the large sample from the Smithson ian Horse Quarry, located w ithin Hagerman Fossil Beds National Monument and managed by the National Park Service How ever, the scientific history of this species actually goes back to the close of the nine­ teenth century. In 1892, paleontologist Edw ard Drinker Cope first described Equus simp/ici­ dens. Cope found the origi nal specimen, a single tooth, near Mount Bla nco, Crosby County, Texas. Later discoveries of horses from similar age deposits elsewhere in the United States resulted in the description of other species of Equus. 4l Eq!JU5 Evolves Sometimes these other species were not even considered to be Equus. At one time the genus Plesippus was used for what are now Epochs of Equus considered the earliest species of Equus. The primitive anatomy of the skeleton of Pleslppus provided a link betvveen OinohlPPus, the ear li er ancestor, and Equus Such was the case when the Smithsonian visited Presenl Hagerman in 1929. The Smithsonian paleontologist who first worked Horses return to America, the site now known as the Smithsonian Horse Quarry was James W. Gidley, then the lead ing student of fossil horses. When Gidley first described the material from Hagerman, he na med it Pleslppus shoshon­ ensis because of the animal 's primitive skeleta l structure. Later Pleistocene researchers decided that Gidley's species from Hagerman w as the 2mya Horses roam North Amenca sa me as the previously described Equus simplicidens from Texas. Equus buried In Hagerman Since many fossil species of Equus have often been described deposits. based on a sing le tooth, it has been d ifficult to determine if all these d ifferent species are really valid. If one species is based on an upper tooth and another on a low er, then ca n w e really be sure they are dis­ tinct, or do the differences merely reflect the d ifferences betvveen Pliocene : upper and low er teeth? There are many fac tors that contribute to the 5 mya . variations we see in fossi ls They may reflect the age of an individual or Three -toed horse types be indicative of the differences betvveen males and females. What spread south across the makes the Smithsonian Horse Quarry sample so important is that it rep­ Panamanian Isthmus. resents a large sample of a single species; it includes males, females, and individuals of all different ages. This site provides a paleontologist w ith the opportunity to examine the range of variation present in a Miocene species. Such a site is a rare occurrence in a 17 mya, fossil record that often consists of bits and Zebraltke Equus first An epoch of diversIficatIOn, pieces rather than whole skulls or ske letons. appeared 3.7 million Merychlppus , a grazer, The sc ience of paleontology is constant ly vee rs ago dunng tile appears among brolNSing reexam ining the available fossil evidence, pro­ Pliocene, Left: Grevy's horses. Apelike humans for­ zebra stallions battle age near wooded Tuscany posing hypotheses regarding the ecology or for dominance relationships of extinct an ima ls based on tha t Previous: excavating tile evidence, and then testing each hypothesis as Horse Qwrry new evidence becomes ava ilable. A hypothe­ Oligocene sis on the ecology of an extinct species Will be weak when only isolat­ 33 mya. ed bones and teeth are avai lable. When a large sample of individuals Early apes, primitive such as tha t of the Hagerman Horse from the Smithson ian Quarry mastodons, shallow-jawed Miohlj:)pUS horses becomes available, an earlier hypothes is may be strengthened, or as is often the case, revised. Such a large sample provides an opportunity to Eocene gain a wea lth of information that might not be otherwise possible to SSmya, glean from the fossil record. Stud ies of the skeleton of the Hagerman Hyracotherium, or '"Dawn Horse from this sample, and compa rison with its modern livi ng rela­ H~· the first equid. tives, suggest that it is actually more zebralike than horse like. More speci fically, its sku ll , teeth, and skeleton are most similar to the living Paleocene Grevy's zebra, w hich inhabits arid regions in the northern part of Africa. 65 mya . Extinction of dinosaurs 42 Secrets of the Magic Valley Some horse experts consider Grevy's zebra the most primitive of the living members of the horse fami ly, so some of the features shared with the Hagerman Horse may reflect the generally more primitive skeletal structure of Grevy's zebra One of the features they have in common is a long skul l with a ~trange Beait1 ExcJUSNe to North America, QreoCionts combined characteris­ tiCS of camels, deer, and pigs. Their most extraordinary and specialized member, Pronomotherium, appeared In the late Miocene exhibiting the kind of bizarre changes often found in the family. Its exaggerated probosCIS masked d skull similar to great apes. About the size of a Wild boar, it lived In large herds and shared grassy plains with early. horses prominent occipital region, the back of the skull wnere the neck musc les attach. Also, the folds of eniJmel on the lower molar teeth are similar. like modern zebras, the Hagerman Horse has a small hoof in proportion to its body size. Whi le the horse was larger than its anc ient ancestors, it was not an especially large animal. Slightly smaller than today's zebras, it stood about 4.3 feet (13 hands) at the shoulder Some of its descendants are larger, but not all. The living donkey is smaller than the Hagerman Horse. Like al l modern members of the family Equidae, Hagerman's Equus simp/ieidens was one-toed with reduced side toes. The middle toe supported all the anima l's w eight. This adaptation to running had already occurred earlier, so Equus w as not the only one-toed horse. It merely continued the trend, with the remnant splints of the side toes completely hidden beneath the skin. The main bones for support in the ha nd and feet (metacarpal and metatarsal ) continued to become elongated, increasing the overal l length. Longer legs meant a longer stride and more ground covered . "In the horse," paleontologist W B. Scott said, "everything has been sacrificed to speed, making the animal a "'cursorial machine'" Perhaps one of the most telling features of the skeleton in this early ancestor of modern horses is the upper leg bone, or humerus One of the very distinct characteristics of living horses is their ability to stand, even sleep, upright for long periods of time. This is possible because of a specialized system of muscles, ligaments, and deep fasc ia (a connective tissue) known as the stay-apparatus.
Recommended publications
  • Carnivora from the Late Miocene Love Bone Bed of Florida
    Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 413-434 413 CARNIVORA FROM THE LATE MIOCENE LOVE BONE BED OF FLORIDA Jon A. Baskin1 Eleven genera and twelve species of Carnivora are known from the late Miocene Love Bone Bed Local Fauna, Alachua County, Florida. Taxa from there described in detail for the first time include the canid cf. Urocyon sp., the hemicyonine ursid cf. Plithocyon sp., and the mustelids Leptarctus webbi n. sp., Hoplictis sp., and ?Sthenictis near ?S. lacota. Postcrania of the nimravid Barbourofelis indicate that it had a subdigitigrade posture and most likely stalked and ambushed its prey in dense cover. The postcranial morphology of Nimravides (Felidae) is most similar to the jaguar, Panthera onca. The carnivorans strongly support a latest Clarendonian age assignment for the Love Bone Bed. Although the Love Bone Bed local fauna does show some evidence of endemism at the species level, it demonstrates that by the late Clarendonian, Florida had become part of the Clarendonian chronofauna of the midcontinent, in contrast to the higher endemism present in the early Miocene and in the later Miocene and Pliocene of Florida. Key Words: Carnivora; Miocene; Clarendonian; Florida; Love Bone Bed; Leptarctus webbi n. sp. INTRODUCTION can Museum of Natural History, New York; F:AM, Frick The Love Bone Bed Local Fauna, Alachua County, fossil mammal collection, part of the AMNH; UF, Florida Florida, has produced the largest and most diverse late Museum of Natural History, University of Florida. Miocene vertebrate fauna known from eastern North All measurements are in millimeters. The follow- America, including 43 species of mammals (Webb et al.
    [Show full text]
  • 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.
    [Show full text]
  • Genomics and the Evolutionary History of Equids Pablo Librado, Ludovic Orlando
    Genomics and the Evolutionary History of Equids Pablo Librado, Ludovic Orlando To cite this version: Pablo Librado, Ludovic Orlando. Genomics and the Evolutionary History of Equids. Annual Review of Animal Biosciences, Annual Reviews, 2021, 9 (1), 10.1146/annurev-animal-061220-023118. hal- 03030307 HAL Id: hal-03030307 https://hal.archives-ouvertes.fr/hal-03030307 Submitted on 30 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Annu. Rev. Anim. Biosci. 2021. 9:X–X https://doi.org/10.1146/annurev-animal-061220-023118 Copyright © 2021 by Annual Reviews. All rights reserved Librado Orlando www.annualreviews.org Equid Genomics and Evolution Genomics and the Evolutionary History of Equids Pablo Librado and Ludovic Orlando Laboratoire d’Anthropobiologie Moléculaire et d’Imagerie de Synthèse, CNRS UMR 5288, Université Paul Sabatier, Toulouse 31000, France; email: [email protected] Keywords equid, horse, evolution, donkey, ancient DNA, population genomics Abstract The equid family contains only one single extant genus, Equus, including seven living species grouped into horses on the one hand and zebras and asses on the other. In contrast, the equine fossil record shows that an extraordinarily richer diversity existed in the past and provides multiple examples of a highly dynamic evolution punctuated by several waves of explosive radiations and extinctions, cross-continental migrations, and local adaptations.
    [Show full text]
  • Supplement 1999-11.Pdf
    Ìàòåðèàëû VI Ìåæäóíàðîäíîãî ñèìïîçèóìà, Êèåâ-Àñêàíèÿ Íîâà, 1999 ã. 7 UDC 591 POSSIBLE USE OF PRZEWALSKI HORSE IN RESTORATION AND MANAGEMENT OF AN ECOSYSTEM OF UKRAINIAN STEPPE – A POTENTIAL PROGRAM UNDER LARGE HERBIVORE INITIATIVE WWF EUROPE Akimov I.1, Kozak I.2, Perzanowski K.3 1Institute of Zoology, National Academy of Sciences of Ukraine 2Institute of the Ecology of the Carpathians, National Academy of Sciences of Ukraine 3International Centre of Ecology, Polish Academy of Sciences Âîçìîæíîå èñïîëüçîâàíèå ëîøàäè Ïðæåâàëüñêîãî â âîññòàíîâëåíèè è â óïðàâëåíèè ýêîñèñòåìîé óê- ðàèíñêèõ ñòåïåé êàê ïîòåíöèàëüíàÿ ïðîãðàììà â èíèöèàòèâå WWE Åâðîïà “êðóïíûå òðàâîÿäíûå”. Àêèìîâ È., Êîçàê È., Ïåðæàíîâñêèé Ê. –  ñâÿçè ñ êëþ÷åâîé ðîëüþ âèäîâ êðóïíûõ òðàâîÿäíûõ æèâîòíûõ â ãàðìîíèçàöèè ýêîñèñòåì ïðåäëàãàåòñÿ øèðå èñïîëüçîâàòü åäèíñòâåííûé âèä äèêîé ëîøàäè — ëîøàäü Ïðæåâàëüñêîãî – â ïðîãðàìíîé èíèöèàòèâå Âñåìèðíîãî ôîíäà äèêîé ïðèðîäû â Åâðîïå (LHF WWF). Êîíöåïöèÿ èñïîëüçîâàíèÿ ýòîãî âèäà êàê èíñòðóìåíòà âîññòàíîâëåíèÿ è óïðàâëåíèÿ â ñòåïíûõ ýêîñèñòåìàõ â Óêðàèíå õîðîøî ñîîòâåòñòâóåò îñíîâíîé íàïðàâëåííîñòè LHJ WWF: à) ñîõðàíåíèè ëàíäøàôòîâ è ýêîñèñòåì êàê ìåñò îáèòàíèÿ êðóïíûõ òðàâîÿäíûõ á) ñî- õðàíåíèå âñåõ êðóïíûõ òðàâîÿäíûõ â âèäå æèçíåñïðîñîáíûõ è øèðîêîðàñïðîñòðàíåííûõ ïîïóëÿ- öèé â) ðàñïðîñòðàíåíèå çíàíèé î êðóïíûõ òðàâîÿäíûõ ñ öåëüþ óñèëåíèÿ áëàãîïðèÿòíîãî îòíîøå- íèÿ ê íèì ñî ñòîðîíû íàñåëåíèÿ. Íàìå÷åíû òåððèòîðèè ïîòåíöèàëüíî ïðèãîäíûå äëÿ èíòðîäóê- öèè ýòîãî âèäà. The large part of Eurasia is undergoing now considerable economic and land use changes, which brings a threat to some endangered populations or even species, but on the other hand creates new opportunities for ecological restoration of former wilderness areas. Large herbivores are key species for numerous ecosystems being the link between producers (vegetation), and secondary consumers (predators), including people.
    [Show full text]
  • 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.
    [Show full text]
  • Tulane Studies Tn Geology and Paleontology Pliocene
    TULANE STUDIES TN GEOLOGY AND PALEONTOLOGY Volu me 22, Number 2 Sepl<'mber 20. l!J8~) PLIOCENE THREE-TOED HORSES FROM LOUISIANA. WITH COMMENTS ON THE CITRONELLE FORMATION EAHL M. MANNING MUSP.UM OF'GEOSCIF:NCE. LOUISJJ\NA STATE UNIVF:RSlTY. JJATO.\I ROI.JG/<. LOL'/S//\;\':1 and llRUCE J. MACFADDlrn DEJ>ARTM/<:NTOF NATUH/\LSCIENCES. F'LORJD/\ MUSf:UM Of<'NJ\TUIV\/, lllSTOUY UNIVERSITY OF FLOH!IJJ\. GJ\/NESVlU.E. Fl.OH/DA CONTENTS Page T. ABSTRACT 3.5 II INTRODUCTION :l5 Ill. ACKNOWLEDGMENTS :rn TV . ABBREVIATIONS :l7 V. SYSTEMATIC PALEONTOLOGY ;37 VI. AGE OF THE TUNICA HILLS HIPPARIONINES 38 VIL STRATIGRAPHIC PROVENIENCE 38 Vlll. PLIOCENE TERRESTRIAL VERTEBRATES OF THE GULF AND ATLANTIC COASTAL PLAIN .JO IX. COMMENTS ON THE CITRONELLE FORMATION .JI X. AGE OF THE CITRONELLE 42 XL TH E CITRONELLE FORMATION IN nm TUNICA HILLS .t:1 XII. LITERATURE CITED l.J January of 1985, the senior author was L ABSTRACT shown a large collection of late Pleistocene Teeth and metacarpals of early Pliocene (Rancholabrean land-mammal agel ver­ (latest Hemphillian land-mammal age) tebrate fossils from the Tunica Hills of three-toed (hipparionine) horses are de­ Louisiana (Fig. I) by Dr. A. Bradley scribed from the Tunica Hills of West McPherson of Centenary College, Feliciana Parish in east-central Louisiana. Shreveport. McPherson and Mr. Bill Lee An upper molar perta ins to Nannippus of Balon Rouge had collected fossils from minor, known from the Hcmphillian of that area since about 1981. Among the Central and North America, and two teeth standard assemblage of Rancholabrean and two distal metacarpals pertain to a re­ taxa (e.g.
    [Show full text]
  • Sankey, J.T. 2002. Vertebrate Paleontology And
    SANKEY - GLENNS FERRY AND BRUNEAU FORMATIONS. IDAHO Table 2. Stratigraphic level and geologic unit of fossils discussed in this paper. See Systematic Paleontology section (this paper) for referenced specimens and their corresponding IMNH locality. GF, upper Glenns Ferry Formation (normal polarity, upper Olduvai subchron); B, lower Bruneau Formation (lowest Bruneau Formation, normal polarity, uppermost Olduvai subchron; remaining Bruneau Formation, reversed polarity; Fig. 5). IMNH 158 and 159 (collected by the John Tyson family) have imprecise locations, and a wide range of elevations are shown for these two localities. xxxx x x ¥f XX x X XXX a mw Eiychocheilus arcifems Mcheilus --Gila milleri ~u~yes&us -sp. cf. & tierinurn cf. WQsp. &ma SP- d. && sp. cf. *lopolus sp. Colubridae-indeterminate cf. Qm sp. d. sp. d. & sp. sp. cf. M.kptc-stomus param"lodon Taxidea taxus htimiun pid~nrn sp. d. C. &xg&gs Q& sp. cf. c. priscolatrans Felis lacustrjs EAk SP. -v Jhnlwu SP. fdbQmy3Q.1 patus sbdaka- lYlkmV3- I3Ywmu .SP. d-LsEia Leporidae-indeterminate sp. cf. E. sirn~licidm I3aY!ws- cf. Qglntocamelus Sp. '3. QE%!Qps sp. cf. J-Iemiauche0Ul sp. QdQQihsSP. saYs SP. d-- AND WHEREAS.. Honoring John A. White T.3S. Fo Snake River (5 km) Figure 3. Tyson Ranch. Topographic map with locations of the three measured sections (Sinker Butte 7.5' U.S.G.S. Quadrangle). Photograph of TRl (view to Sinker Butte) with arrow pointing to the phreatic tuff near the Glenns Ferry-Bruneau Formational contact. SANKEY - GLENNS FERRY AND BRUNEAU FORMATIONS, IDAHO Figure 4. Three Mile East. Topographic map with locations of measured section (Silver City 4 NE and Sinker Butte 7.5' U.S.G.S.
    [Show full text]
  • Horse Tooth Enamel Ultrastructure: a Review of Evolutionary, Morphological, and Dentistry Approaches
    e-ISSN 1734-9168 Folia Biologica (Kraków), vol. 69 (2021), No2 http://www.isez.pan.krakow.pl/en/folia-biologica.html https://doi.org/10.3409/fb_69-2.09 Horse Tooth Enamel Ultrastructure: A Review of Evolutionary, Morphological, and Dentistry Approaches Vitalii DEMESHKANT , Przemys³aw CWYNAR and Kateryna SLIVINSKA Accepted June 15, 2021 Published online July 13, 2021 Issue online July 13, 2021 Review article DEMESHKANT V., CWYNAR P., SLIVINSKA K. 2021. Horse tooth enamel ultrastructure: a review of evolutionary, morphological, and dentistry approaches. Folia Biologica (Kraków) 69: 67-79. This review searches for and analyzes existing knowledge on horse tooth anatomy in terms of evolutionary and morphological changes, feeding habits, breeding practices, and welfare. More than 150 articles from relevant databases were analyzed, taking into account the issues of our experimental research on the ultrastructure of Equidae tooth enamel. After our analysis, the knowledge on this subject accumulated up in the past, almost 50 years has been logically arranged into three basic directions: evolutionary-palaeontological, morpho-functional, and dentistic, which is also demonstrated by the latest trends in the study of enamel morphology and in the practice of equine dentistry. The obtained data show that in recent years we have observed a rapid increase in publications and a thematic expansion of the scope of research. It is caused by the need to deepen knowledge in theory and in the practice of feeding species in nature and in captivity as well as the possibility of using new technical resources to improve the excellence of such research. It is a summary of the knowledge of a certain stage of equine tooth enamel studies for this period of time, which serves as the basis for our experimental research (the materials are prepared for publication) and at the same time, defines research perspectives for the next stage of development.
    [Show full text]
  • Hipparion” Cf
    ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 30:15-24, Wien 2006 Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene by Miranda A rmour -Chelu 1}, Raymond L. Bernor 1} & Hans-Walter Mittmann * 2) A rmour -C helu , M., Bernor , R.L. & M ittmann , H.-W., 2006. Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene. — Beitr. Palaont., 30:15-24, Wien. Abstract cranialen Elemente die Hooijer zu diesem Taxon gestellt hat, auf die er sich bezogen hat oder die in irgendeiner We review here the problematic history of the nomen Beziehung dazu stehen, haben wir wiedergefunden. Selbst “Hipparion”cf. ethiopicum and Hooijer’s efforts to bring zusätzliche Fundstücke aus zeitgleichen Horizonten haben some taxonomic sense to the later Pliocene - Pleistocene wir miteinbezogen, in der Absicht, die Gültigkeit von Eu­ hipparion record. We review his reasoning, and the shifts rygnathohippus cf.“ethiopicum" und seines Verwandten in taxonomic allocation made by him and other equid Eurygnathohippus cornelianus und weiterer Formen, von researchers during the 1970’s. We have relocated many denen Hooijer geglaubt hat, dass sie in einem evolutionären of the postcranial specimens attributed by Hooijer to Zusammenhang mit „ Hipparion“ cf. ethiopicum stehen, “Hipparion” cf. ethiopicum, as well as other specimens zu testen. Wir machen statistische und vergleichende which he referred to, or related to this species. We have Analysen um dieses Hypodigma zu klären. also considered additional specimens from contempo­ raneous horizons, in order to reevaluate the efficacy of Eurygnathohippus cf “ethiopicum” and its apparent rela­ 1.
    [Show full text]
  • Spring 2010 Newsletter
    National Association of Geoscience Teachers Pacific Northwest Section Spring 2010 President Ralph Dawes, Earth Sciences Dept. This Issue Includes: Wenatchee Valley College 2010 PNW Section Annual Meeting, Twin Falls, ID 1300 Fifth Street , Wenatchee, WA 98801 PNW Section Election Ballot [email protected] Ron Kahle Travel Grants for K-12 teachers- apply Vice President Ron Metzger From the President Southwestern Oregon Community College As I hand over the Pacific Northwest section presidency to 1988 Newmark Avenue, Coos Bay, OR 97420 [email protected] Ron Metzger, there are three things I want to leave you with. Secretary/Treasurer Robert Christman-Department of Geology First, this is the century of earth science, not just for Western Washington University knowledge, but for our future on planet earth. Together, we Bellingham, WA 98225 humans are measurably changing the earth and altering the [email protected] course of earth history. The decisions we make and the Newsletter Editor Cassandra Strickland, Physical Sciences, S-1 actions we take during this century will determine how many Columbia Basin College people will be able to live on planet earth in the future, and how they live. To shape this Pasco, WA 99301 future, we will have to solve problems such as limits on energy and material resources; [email protected] reduced biodiversity and its effect on survival of remaining species ; climate change; and State Councilors increased human exposure to earthquakes, eruptions, floods, storms, wildfires, AK Cathy Connor, Univ. of Alaska Southeast, Juneau landslides, and more. Solving these problems will require the special methods of [email protected] gaining and refining knowledge that we have as earth scientists.
    [Show full text]
  • The First Occurrence of Eurygnathohippus Van Hoepen, 1930 (Mammalia, Perissodactyla, Equidae) Outside Africa and Its Biogeograph
    TO L O N O G E I L C A A P I ' T A A T L E I I A Bollettino della Società Paleontologica Italiana, 58 (2), 2019, 171-179. Modena C N O A S S. P. I. The frst occurrence of Eurygnathohippus Van Hoepen, 1930 (Mammalia, Perissodactyla, Equidae) outside Africa and its biogeographic signifcance Advait Mahesh Jukar, Boyang Sun, Avinash C. Nanda & Raymond L. Bernor A.M. Jukar, Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington DC 20013, USA; [email protected] B. Sun, Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China; University of Chinese Academy of Sciences, Beijing 100039, China; College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059, USA; [email protected] A.C. Nanda, Wadia Institute of Himalayan Geology, Dehra Dun 248001, India; [email protected] R.L. Bernor, College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059, USA; [email protected] KEY WORDS - South Asia, Pliocene, Biogeography, Dispersal, Siwalik, Hipparionine horses. ABSTRACT - The Pliocene fossil record of hipparionine horses in the Indian Subcontinent is poorly known. Historically, only one species, “Hippotherium” antelopinum Falconer & Cautley, 1849, was described from the Upper Siwaliks. Here, we present the frst evidence of Eurygnathohippus Van Hoepen, 1930, a lineage hitherto only known from Africa, in the Upper Siwaliks during the late Pliocene. Morphologically, the South Asian Eurygnathohippus is most similar to Eurygnathohippus hasumense (Eisenmann, 1983) from Afar, Ethiopia, a species with a similar temporal range.
    [Show full text]
  • Late Hemphillian Colubrid Snakes (Serpentes, Colubridae) from the Gray Fossil Site of Northeastern Tennessee Author(S): Steven E
    Late Hemphillian Colubrid Snakes (Serpentes, Colubridae) from the Gray Fossil Site of Northeastern Tennessee Author(s): Steven E. Jasinski and David A. Moscato Source: Journal of Herpetology, 51(2):245-257. Published By: The Society for the Study of Amphibians and Reptiles DOI: http://dx.doi.org/10.1670/16-020 URL: http://www.bioone.org/doi/full/10.1670/16-020 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. Journal of Herpetology, Vol. 51, No. 2, 245–257, 2017 Copyright 2017 Society for the Study of Amphibians and Reptiles Late Hemphillian Colubrid Snakes (Serpentes, Colubridae) from the Gray Fossil Site of Northeastern Tennessee 1,2,3,4 3 STEVEN E.
    [Show full text]