Astragalar Morphology of Selected Giraffidae
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Browsing and Non-Browsing Extant and Extinct Giraffids Evidence From
Browsing and non-browsing extant and extinct giraffids Evidence from dental microwear textural analysis Gildas Merceron, Marc Colyn, Denis Geraads To cite this version: Gildas Merceron, Marc Colyn, Denis Geraads. Browsing and non-browsing extant and extinct giraffids Evidence from dental microwear textural analysis. Palaeogeography, Palaeoclimatology, Palaeoecol- ogy, Elsevier, 2018, 505, pp.128-139. 10.1016/j.palaeo.2018.05.036. hal-01834854v2 HAL Id: hal-01834854 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01834854v2 Submitted on 6 Sep 2018 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. 1 Browsing and non-browsing extant and extinct giraffids: evidence from dental microwear 2 textural analysis. 3 4 Gildas MERCERON1, Marc COLYN2, Denis GERAADS3 5 6 1 Palevoprim (UMR 7262, CNRS & Université de Poitiers, France) 7 2 ECOBIO (UMR 6553, CNRS & Université de Rennes 1, Station Biologique de Paimpont, 8 France) 9 3 CR2P (UMR 7207, Sorbonne Universités, MNHN, CNRS, UPMC, France) 10 11 1Corresponding author: [email protected] 12 13 Abstract: 14 15 Today, the family Giraffidae is restricted to two genera endemic to the African 16 continent, Okapia and Giraffa, but, with over ten genera and dozens of species, it was far 17 more diverse in the Old World during the late Miocene. -
Original Giraffokeryx Punjabiensis (Artiodactyla, Ruminantia, Giraffidae) from Lower Siwaliks (Chinji Formation) of Dhok Bun
Original Giraffokeryx punjabiensis (Artiodactyla, Ruminantia, Giraffidae) from Lower Siwaliks (Chinji Formation) of Dhok Bun Ameer Khatoon, Pakistan Khizar Samiullah1*, Muhammad Akhtar2, Abdul Ghaffar3, Muhammad Akbar Khan4 Received : 28 January 2011 ; Accepted : 13 September 2011 Abstract Fossil remains of Giraffokeryx punjabiensis (premolar and molar teeth belonging to the upper and lower jaws) have been collected and discussed from Chinji Formation of Dhok Bun Ameer Khatoon (32o 47’ 26.4” N, 72° 55’ 35.7” E). All these (twenty one) specimens are isolated teeth, which provide new data and give valuable information on the biostratigrphy and paleoecology of Giraffokeryx punjabiensis as well as the stratigraphy and paleoclimates of these Miocene rocks of the Chakwal district, Pakistan. Keywords: Giraffokeryx punjabiensis, isolated teeth, Chinji Formation, biostratigraphy Miocene rocks, Chakwal district. Introduction Dhok Bun Ameer Khatoon (DBAK) is poorly known fossil ramii and a number of isolated teeth. Mathew4 studied site of the Siwaliks. Previous pioneer workers 1,2,3,4,5 did the material of this species at the Indian Museum, not visit this site nor mentioned it in their faunal list. Kolkata (Calcutta), and recognized a larger and a During the last decade, this site had got attraction of smaller form. However, Colbert5 suggested there was researchers when few fossils were unearthed during a continuous size gradation of the dental material of the mechanical work for construction of dam for water the species through the Chinji to the Nagri Formation storage purposes. Girafids, bovids, tragulids, suids, and therefore that no such size division exists in the hominids, rhinos, chilothers anthracothers and carnivors material of the genus Giraffokeryx. -
AMERICAN MUSEUM NOVITATES Published by Tnui Amermican MUSZUM W Number 632 Near York Cityratt1ral Historay June 9, 1933
AMERICAN MUSEUM NOVITATES Published by Tnui AmERMICAN MUSZUM W Number 632 Near York CityRATt1RAL HisToRay June 9, 1933 56.9, 735 G: 14.71, 4 A SKULL AND MANDIBLE OF GIRAFFOKERYX PUNJABIENSIS PILGRIM By EDWIN H. COLBERT The genus Giraffokeryx was founded by Dr. G. E. Pilgrim to desig- nate a primitive Miocene giraffe from the lower Siwalik beds of northern India. Doctor Pilgrim, in a series of papers,' described Giraffokeryx on the basis of fragmental and scattered dentitions.. Naturally, Pilgrim's knowledge of the genus was rather incomplete, and he was unable tQ formulate any opinions as to the structure.of the skull or mandible. An almost complete skull, found in the northern Punjab in 1922 by Mr. Barnum Brown of the American Museum, proves to be that of Giraffokeryx, and it exhibits such striking and unusual characters that a separate description of it has seemed necessary. This skull, together with numerous teeth and a lower. jaw, gives us. a very good comprehen- sion of the genus which forms the subject.of this paper. The drawings of the skull were made by John. C. Germann, and the remaining ones were done by Margaret Matthew. MATERIAL DESCRIBED Only the material referred to in this description will here be listed. There' are a great many specimens of Gir'affokeryx in the American'Mu- seum collection, but since 'most of them are'teeth, they will not be considered at this time. A subsequent paper, dealing with the American Museum Siwalik collection in detail, wtyill contain a complete list of the Giraffokeryx material. -
Sivatherium (Artiodactyla, Ruminantia, Giraffidae) from the Upper Siwaliks, Pakistan
Khan et al. The Journal of Animal & Plant Sciences, 21(2): 2011, Page: J.202 Anim.-206Plant Sci. 21(2):2011 ISSN: 1018-7081 SIVATHERIUM (ARTIODACTYLA, RUMINANTIA, GIRAFFIDAE) FROM THE UPPER SIWALIKS, PAKISTAN A. A. Khan, M. A. Khan*, M. Iqbal**, M. Akhtar*** and M. Sarwar*** Institute of Pure & Applied Biology, Zoology Division, Bahauddin Zakariya University, Multan 60800, Pakistan *Zoology Department, GC University, Faisalabad, **Zoology Department, Government College Science, Wahdat Road, Lahore ***Zoology Department, Quaid-e-Azam Campus, Punjab University, Lahore Correspondence author e-mail: <[email protected]>; ABSTRACT A complete lower molar series of giraffid remains from the Pleistocene locality of the village Sardhok (Gujrat, Punjab, Pakistan) has been identified as belonging to Sivatherium sp. The comparison of the material was made with several Siwalik representatives of the giraffids. The giraffid Sivatherium is a gigantic giraffid found in the early Pleistocene sediments of the Upper Siwaliks. The village Sardhok locality has yielded one of the best collections of Giraffidae from the early Pleistocene of the Siwaliks. The locality belongs to the Pinjor Formation of the Upper Siwaliks (2.6-0.6 Ma). Key words: Giraffids, Sivatherium, Upper Siwaliks, Pleistocene, Pinjor Formation. INTRODUCTION The material described here comes from the outcrops of the village Sardhok, Gujrat district, Punjab, The fossil Chinese record shown by Bohlin Pakistan. In the Potwar Plateau, the Upper Siwalik is well (1927) and that of Asia shown by Colbert (1935) exposed in the Pabbi hills situated in the east of the River indicates that the giraffids had their origin in the Jhelum. The village Sardhok is situated in these low Holarctic Region. -
Discovery of a Bramatherium (Giraffid) Horn-Core From
Geol. Bull. Punjab Univ. Vol. 40-41, 2005-6, pp 21-25 21 DISCOVERY OF A BRAMATHERIUM (GIRAFFID) HORN CORE FROM THE DHOK PATHAN FORMATION (MIDDLE SIWALIKS) OF HASNOT, POTWAR PLATEAU, PAKISTAN MUHAMMAD AKBAR KHAN, MUHAMMAD AKHTAR Department of Zoology, Quid-e-Azam Campus, University of the Punjab, Lahore (54590), Pakistan Email: [email protected] AND MUHAMMAD ANWAR QURESHI Institute of Geology, University of Azad Jammu & Kashmir, Muzaffrabad, Pakistan Abstract: The recent collection from Hasnot has brought about the discovery of a horn core belongs to a gigantic Upper Tertiary giraffe. The giraffids are abundant in the Upper Tertiary rocks of the Siwaliks and mostly diverse in the Tertiary rocks of Hasnot and Dhok Pathan. The studied specimen is found from the locality H 7 situated at 4 kilo meters west of the Hasnot village. INTRODUCTION giraffids (Bohlin, 1926) and has already been noted in Middle Miocene ones (Gentry et al., 1999). The Hasnot The Late Miocene to early Pleistocene deposited in the village (Lat. 32° 49′ N: Long. 73° 18′ E) is situated at elongated foreland basin of the Himalayas are well known about 70 km west of the Jhelum city in the Potwar Plateau and have been studied intensively for many years of the northern Pakistan (Fig. 1). The village is (Biswas, 1994; Behrensmeyer et al., 1997). Although surrounded by extensive Neogene freshwater sedimentary Tertiary Vertebrate remains have been known from the rocks. The region of the Hasnot exposes the most Siwaliks for more than a century however there had been complete sequence of the Siwalik Group and yields a mostly foreigners who collected the remains (Falconer diversified assemblage of the Middle Siwalik Formation. -
Comparisons of Schansitherium Tafeli with Samotherium Boissieri (Giraffidae, Mammalia) from the Late Miocene of Gansu Province, China
RESEARCH ARTICLE Comparisons of Schansitherium tafeli with Samotherium boissieri (Giraffidae, Mammalia) from the Late Miocene of Gansu Province, China 1,2,3 4 5 4,6 Sukuan HouID *, Michael Cydylo , Melinda Danowitz , Nikos SolouniasID 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 CAS Center for Excellence in Life and Paleoenvironment, Beijing, China, 3 College of Earth and Planetary a1111111111 Sciences, University of Chinese Academy of Sciences, Beijing, China, 4 Department of Anatomy, New York a1111111111 Institute of Technology College of Osteopathic Medicine, Old Westbury, NY, United States of America, a1111111111 5 Department of Pediatrics, Alfred I. duPont Hospital for Children, Wilmington, DE, United States of America, a1111111111 6 Department of Paleontology, American Museum of Natural History, New York, NY, United States of a1111111111 America * [email protected] OPEN ACCESS Abstract Citation: Hou S, Cydylo M, Danowitz M, Solounias We are describing and figuring for the first time skulls of Schansitherium tafeli, which are N (2019) Comparisons of Schansitherium tafeli with Samotherium boissieri (Giraffidae, Mammalia) abundant in the Gansu area of China from the Late Miocene. They were animals about the from the Late Miocene of Gansu Province, China. size of Samotherium with shorter necks that had two pairs of ossicones that merge at the PLoS ONE 14(2): e0211797. https://doi.org/ base, which is unlike Samotherium. The anterior ossicones consist of anterior lineations, 10.1371/journal.pone.0211797 which may represent growth lines. They were likely mixed feeders similar to Samotherium. -
Ontogenetic Allometry of the Postcranial Skeleton of the Giraffe (Giraffa Camelopardalis), with Application to Giraffe Life History, Evolution and Palaeontology
Ontogenetic allometry of the postcranial skeleton of the giraffe (Giraffa camelopardalis), with application to giraffe life history, evolution and palaeontology By Sybrand Jacobus van Sittert Submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy (PhD) in the Department of Production Animal Studies Faculty of Veterinary Science University of Pretoria Supervisor: Prof Graham Mitchell Former supervisor (deceased): Prof John D Skinner Date submitted: October 2015 i Declaration I, Sybrand Jacobus van Sittert, declare that the thesis, which I hereby submit for the degree Doctor of Philosophy at the University of Pretoria is my own work and has not previously been submitted by me for a degree at this or any other tertiary institution. October 2015 ii Acknowledgements Including a list of people to whom I am grateful to in the acknowledgement section hardly does justice to the respective persons: A thesis is, in all honestly, only comprehensively read by very few people. Nevertheless, it occurred to me that even when I roughly skim through a thesis or dissertation for bits of information, I am always drawn into the acknowledgements. I suppose it is the only section where one can get a glimpse into the life of the researcher in an otherwise rather ‘cold’ academic work. Therefore, although not a large platform to say ‘thank you’, I wish to convey to everyone listed here that you are in the warmest part of my heart … and probably the most read part of my thesis. Prof Graham Mitchell for his patience with me, his guidance, enthusiasm and confidence. I consider myself lucky and honoured to have had you as a supervisor. -
I.—A Retrospect of Palaeontology in the Last Forty Years
THE GEOLOGICAL MAGAZINE. NEW SERIES. DECADE V. VOL. I. No. IV. —APRIL, 1904. ORIGI3STAL ARTICLES. I.—A KETROSPECT OF PALAEONTOLOGY IN TIIE LAST FOBTY YEABS. (Concluded from the March Number, p. 106.) EEPTILIA ET AVES.—Our two greatest Anatomists of the past century, Owen and Huxley, both contributed to this section of our palseozoological record. Owen (in 1865) described some remains of a small air-breathing vertebrate, Anihrakerpeton crassosteum, from the Coal-shales of Glamorganshire, corresponding with those described by Dawson from the Coal-measures of Nova Scotia ; and in 1870 he noticed some remains of Plesiosaurus Hoodii (Owen) from New Zealand, possibly of Triaasic age. Huxley made us acquainted with an armed Dinosaur from the Chalk-marl of Folkestone, allied to Scelidosaurus (Liassic), ITylao- saurus and Polacanthus (Wealden), the teeth and dermal spines of which he described and figured (1867), and in the following year he figured and determined two new genera of Triassic reptilia, Saurosternon Bainii and Pristerodon McKayi, from the Dicynodont beds of South Africa. E. Etheridge recorded (in 1866) the discovery by Dr. E. P. Wright and Mr. Brownrig of several new genera of Labyrinthodonts in the Coal-shales of Jarrow Colliery, Kilkenny, Ireland, com- municated by Huxley to the Royal Irish Academy, an account of which appeared later on in the GEOLOGICAL MAGAZINE in the same year by Dr. E. P. Wright (p. 165), the genera given being Urocordylus, Ophiderpeton, Ichthyerpeton, Keraterpeton, Lepterpeton, and Anthracosaurus. Besides these genera there were indications of the existence of several others (not described), making at that time a total of thirteen genera from the Carboniferous formation in general. -
Liebe ID-Freunde
[Back to internetlibrary.html] Wolf-Ekkehard Lönnig 8 May 2007 (last update 16 October 2010), updates 27 Oct. 2007 with Appendix on Cameron & du Toit 2007: "Winning by a Neck…" pp .62-78; 5 Oct. 2008 some language corrections and a brief comment on Brown et al. 2007: "Extensive population genetic structure in the giraffe" on p. 79. The Evolution of the Long-Necked Giraffe (Giraffa camelopardalis L.) What do we really know? (Part 2) As for Part 1, see http://www.weloennig.de/Giraffe.pdf Some Questions, Facts and Quotations to Supplement Part 1 Repetitio est mater studiorum –Repetition is the best teacher (literally: the mother of studies) Summary Introduction: the story which is commonly taught in high schools about the evolution of the long- necked giraffe by natural selection (feeding-competition-hypothesis) fails to explain, among other things, the size differences between males and females. Giraffe cows are up to 1.5 meters shorter than the giraffe bulls, not to mention the offspring. The wide migration range of the giraffe and the low heights of the most common plants in their diet likewise argue against the dominant selection hypothesis. Now to the main points: 1) The fossil „links“, which according to the theory should appear successively and replace each other, usually exist simultaneously for long periods of time. 2) Evolutionary derivations based on similarities rely on circular reasoning (to refer once more to Kuhn's statement) 3) The giraffe has eight cervical vertebrae. Although the 8th vertebra displays almost all the characteristics of a neck vertebra, as an exception to the rule the first rib pair is attached there. -
Africa's Giraffe
AFRICA’S GIRAFFE A CONSERVATION GUIDE CONTENTS Introduction 1 Evolution 2 Giraffe & humans 2 Giraffe facts 3 Taxonomy & species 5 Distribution & habitat 7 Masai giraffe 9 Northern giraffe 10 Kordofan giraffe 10 Nubian giraffe 11 West African giraffe 12 Reticulated giraffe 13 Southern giraffe 14 Angolan giraffe 14 South African giraffe 15 Conservation 17 Status & statistics 17 IUCN Red List 17 Species & numbers 18 CITES & CMS 20 Stakeholders 20 Threats 21 Limiting factors 22 Significance of giraffe 24 Economic 24 Ecological 24 The future 25 Giraffe Conservation Foundation 26 Bibliography 27 BILLY DODSON In order to address this, the Giraffe Conservation Foundation (GCF) has drafted an Africa-wide Giraffe Strategic Framework, which provides a road-map for giraffe conservation throughout Africa, and supports several governments in developing their first National Giraffe Conservation Strategies and Action Plans. Now is the time to act for giraffe, before time runs out. Evolution Helladotherium, a three-metre-tall antelope-like animal, which once WIKIMEDIA COMMONS roamed the plains and forests of Asia and Europe between the Eocene and Oligocene epochs 30-50 million years ago, is the forefather of the two remaining members of the Giraffidae family: the giraffe we know today, and the okapi. To date, more than ten fossil genera have been discovered, revealing that by the Miocene epoch, 6-20 million years ago, early deer-like These giraffe images, which are carved life-size and with incredible detail into rock, are believed giraffids were yet to develop the characteristic long neck of today’s giraffe. to date back 9,000 years to a time when the Sahara was wet and green. -
Online First Article
Pakistan J. Zool., pp 1-10, 2021. DOI: https://dx.doi.org/10.17582/journal.pjz/20180805150835 New Fossil Remains of Giraffids from the Lower Siwaliks of Punjab, Pakistan: Evolution, Systematics and Biogeography Amin Arif1, Khizar Samiullah1*, Riffat Yasin2, Bilal Rasool1, Shakila Naz1, Xijun Ni3 and Saleem Akhtar1 1 Department of Zoology, GC University, Faisalabad, Pakistan Article Information 2Faculty of Veterinary and Animal Sciences, Muhammad Nawaz Sharif University of Received 05 August 2018 Revised 29 May 2019 Agriculture, Multan, Punjab, Pakistan Accepted 05 November 2020 3Institute of Vertebrate Palaeontology and Palaeoanthropology, Beijing, China Available online 09 February 2021 Authors’ Contribution ABSTRACT KS, RY and XN presented the concept and designed the study. AA, Taxonomic study from a late Miocene Fossil locality Dhok Bun Ameer Khatoon, Lower Siwalik Hills SA and SN helped in collection and of Pakistan has been conducted. New fossil remains belong to family Giraffidae which include right and preparation of fossils. KS and BR drafted the manuscript. left maxilla, isolated upper premolars and molars. After morphological and comparative analysis, the collection is attributed to Giraffokeryx punjabiensis and Giraffa priscilla. Size variation in dentition is Key words taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct Miocene, Giraffidae, Lower siwaliks, this study at this specific site to add additional information about family Giraffidae. The fossil site has well Chinji formation exposed Chinji and Nagri Formation and has dated approximately 14.2-9.5 Ma. In this study, different aspects of evolution, taxonomy and biogeographic distribution as well as the relation of Giraffidae with Procerotidae have been discussed comprehensively. -
The Numerical Inversion of the Laplace Transform
▼ Journal of Research (Science), Bahauddin Zakariya University, Multan, Pakistan. Vol.13, No.2, December 2002, pp. 139-144 ISSN 1021-1012 A NEW INDRATHERIUM FOSSIL GIRAFFE INDRATHERIUM COMPRESSUS SP. NOV. FROM SIWALIK FORMATIONS OF PAKISTAN Aleem Ahmed Khan1 and Muhammad Sarwar2 1Zoology Division, Institute of Pure and Applied Biology, Bahauddin Zakariya University, Multan, Pakistan. 2Zoology Department, University of the Punjab, New Campus, Lahore, Pakistan. Abstract: The specimen P.U. P.C. No.87/13 is excellently preserved upper third premolar of the upper right side and is found from Sardhok, district Gujrat, Punjab, Pakistan. It belongs to the Pinjorian of the upper Siwalik formations. The P3 is very large, transversely elongated, triangular and with pronounced para- and mesostyles. The upper premolars of the species under study were extremely compressed and the parastylic fold was highly pronounced. Indratherium is distinguished from other genera due to the striking excess of breadth over length in the molars. This feature must have been shown by its premolars as well. In other larger genera of the giraffidae, this feature is not exhibited. The specimen under study is fairly wider transversely than longer. The specialized characters of P.U.P.C. No. 87/13 warrant the erection of a new species Indratherium compressus sp. nov. Keywords:- Giraffidae, Indratherium, para- and mesostyles, Siwaliks. INTRODUCTION First scientific mention of the Siwalik giraffes goes back to 1836 when Falconer and Cautley described a large massive giraffe, Sivatherium giganteum from the Upper Siwaliks. Since that time, a number of genera and species have been recorded from various formations of the Siwaliks by different workers such as Lydekker [1876, 1878], Pilgrim [1910] and Matthew [1929].