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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. -
Astragalar Morphology of Selected Giraffidae
RESEARCH ARTICLE Astragalar Morphology of Selected Giraffidae Nikos Solounias1,2☯*, Melinda Danowitz1☯ 1 Department of Anatomy, New York Institute of Technology College of Osteopathic Medicine, Old Westbury, NY, United States of America, 2 Department of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, NY, United States of America ☯ These authors contributed equally to this work. * [email protected] Abstract The artiodactyl astragalus has been modified to exhibit two trochleae, creating a double pullied structure allowing for significant dorso-plantar motion, and limited mediolateral motion. The astragalus structure is partly influenced by environmental substrates, and cor- respondingly, morphometric studies can yield paleohabitat information. The present study establishes terminology and describes detailed morphological features on giraffid astragali. Each giraffid astragalus exhibits a unique combination of anatomical characteristics. The giraffid astragalar morphologies reinforce previously established phylogenetic relationships. We find that the enlargement of the navicular head is a feature shared by all giraffids, and that the primitive giraffids possess exceptionally tall astragalar heads in relation to the total astragalar height. The sivatheres and the okapi share a reduced notch on the lateral edge OPEN ACCESS of the astragalus. We find that Samotherium is more primitive in astragalar morphologies Citation: Solounias N, Danowitz M (2016) Astragalar than Palaeotragus, which is reinforced -
PALEONTOLOGICAL (PLANKTIC FORAMINIFER-OSTRACOD) INVESTIGATION of EOCENE SEQUENCE of KARAMAN REGION Ümit ŞAFAK* ABSTRACT
PALEONTOLOGICAL (PLANKTIC FORAMINIFER-OSTRACOD) INVESTIGATION OF EOCENE SEQUENCE OF KARAMAN REGION Ümit ŞAFAK* ABSTRACT.- The microfauna of Eocene sequence outcropping around Karaman have been investigated. These planktic foraminifers and ostracods were systematically described; also Acarinina bullbrooki planktic foraminifer zone belonging to Lutetian has been determined and this zone was compared with other Eocene planktic foraminifer zones over the world indicat- ing same level. In addition, ostracod species described were stratigraphically and paleogeographically compared with those of other basins. OSTRACOD AND FORAMINIFER ASSEMBLAGES OF TERTIARY SEDIMENTS AT W. BAKIRKÖY (ISTANBUL) Ümit ŞAFAK*. Niyazi AVŞAR* and Engin MERİÇ** ABSTRACT.- The drilling samples taken from the western part of the Bakırköy Basin were investigated, and the microplaeonto- logical data were evaluated. Pliocene, Late Miocene and Late Eocene aged sediments have been observed from top to bottom of drilling, at the results of the laboratory investigation. 14 genera and 25 species from the ostracods and 10 genera and 8 species of benthic foraminifera from the Pliocene sediments: 6 genera and 11 species of ostracods, 9 genera 9 species of ben- thic foraminifera from the Late Miocene deposits and 11 genera and 11 sepices of ostracods and 20 genera and 6 species of benthic foraminifera from the Late Eocene sediments were described. The microfauna of Pliocene sediments consists of Cyprideis seminulum (Reuss), C. pannonica (Mehes), C.anatolica Bassiouni, C. torosa (Jones). C. tuberculata(Mehes). C. tritu- berculata Kristic. C. pontica Kristic are rare, and characteristic for Pontic Basin. In addition, Loxoconcha sp., Semicytherura sp.. Xestoleberis margaritae Mauller, X. ventricosa Mueller. X, reymenti Ruggieri, X. communis Mueller. -
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. -
Chapter 1 - Introduction
EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed. -
Central African Republic Giraffe Conservation Status Report February 2020
Country Profile Central African Republic Giraffe Conservation Status Report February 2020 General statistics Size of country: 622,984 km² Size of protected areas / percentage protected area coverage: 13% Species and subspecies In 2016 the International Union for the Conservation of Nature (IUCN) completed the first detailed assessment of the conservation status of giraffe, revealing that their numbers are in peril. This was further emphasised when the majority of the IUCN recognised subspecies where assessed in 2018 – some as Critically Endangered. While this update further confirms the real threat to one of Africa’s most charismatic megafauna, it also highlights a rather confusing aspect of giraffe conservation: how many species/subspecies of giraffe are there? The IUCN currently recognises one species (Giraffa camelopardalis) and nine subspecies of giraffe (Muller et al. 2016) historically based on outdated assessments of their morphological features and geographic ranges. The subspecies are thus divided: Angolan giraffe (G. c. angolensis), Kordofan giraffe (G. c. antiquorum), Masai giraffe (G. c. tippleskirchi), Nubian giraffe (G. c. camelopardalis), reticulated giraffe (G. c. reticulata), Rothschild’s giraffe (G. c. rothschildi), South African giraffe (G. c. giraffa), Thornicroft’s giraffe (G. c. thornicrofti) and West African giraffe (G. c. peralta). However, over the past decade GCF together with their partner Senckenberg Biodiversity and Climate Research Centre (BiK-F) have performed the first-ever comprehensive DNA sampling and analysis (genomic, nuclear and mitochondrial) from all major natural populations of giraffe throughout their range in Africa. As a result, an update to the traditional taxonomy now exists. This study revealed that there are four distinct species of giraffe and likely five subspecies (Fennessy et al. -
The Late Miocene Mammalian Fauna of Chorora, Awash Basin
The late Miocene mammalian fauna of Chorora, Awash basin, Ethiopia: systematics, biochronology and 40K-40Ar ages of the associated volcanics Denis Geraads, Zeresenay Alemseged, Hervé Bellon To cite this version: Denis Geraads, Zeresenay Alemseged, Hervé Bellon. The late Miocene mammalian fauna of Chorora, Awash basin, Ethiopia: systematics, biochronology and 40K-40Ar ages of the associated volcanics. Tertiary Research, 2002, 21 (1-4), pp.113-122. halshs-00009761 HAL Id: halshs-00009761 https://halshs.archives-ouvertes.fr/halshs-00009761 Submitted on 24 Mar 2006 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. The late Miocene mammalian fauna of Chorora, Awash basin, Ethiopia: systematics, biochronology and 40K-40Ar ages of the associated volcanics Denis GERAADS - EP 1781 CNRS, 44 rue de l'Amiral Mouchez, 75014 PARIS, France Zeresenay ALEMSEGED - National Museum, P.O.Box 76, Addis Ababa, Ethiopia Hervé BELLON - UMR 6538 CNRS, Université de Bretagne Occidentale, BP 809, 29285 BREST CEDEX, France ABSTRACT New whole-rock 40K-40Ar ages on lava flows bracketing the Chorora Fm, Ethiopia, confirm that its Hipparion-bearing sediments must be in the 10-11 Ma time-range. The large Mammal fauna includes 10 species. -
Giraffe Stature and Neck Elongation: Vigilance As an Evolutionary Mechanism
biology Review Giraffe Stature and Neck Elongation: Vigilance as an Evolutionary Mechanism Edgar M. Williams Faculty of Life Sciences and Education, University of South Wales, Wales CF37 1DL, UK; [email protected]; Tel.: +44-1443-483-893 Academic Editor: Chris O’Callaghan Received: 1 August 2016; Accepted: 7 September 2016; Published: 12 September 2016 Abstract: Giraffe (Giraffa camelopardalis), with their long neck and legs, are unique amongst mammals. How these features evolved is a matter of conjecture. The two leading ideas are the high browse and the sexual-selection hypotheses. While both explain many of the characteristics and the behaviour of giraffe, neither is fully supported by the available evidence. The extended viewing horizon afforded by increased height and a need to maintain horizon vigilance, as a mechanism favouring the evolution of increased height is reviewed. In giraffe, vigilance of predators whilst feeding and drinking are important survival factors, as is the ability to interact with immediate herd members, young and male suitors. The evidence regarding giraffe vigilance behaviour is sparse and suggests that over-vigilance has a negative cost, serving as a distraction to feeding. In woodland savannah, increased height allows giraffe to see further, allowing each giraffe to increase the distance between its neighbours while browsing. Increased height allows the giraffe to see the early approach of predators, as well as bull males. It is postulated that the wider panorama afforded by an increase in height and longer neck has improved survival via allowing giraffe to browse safely over wider areas, decreasing competition within groups and with other herbivores. -
ΓΕΩΡΓΙΟΣ ΗΛΙΟΠΟΥΛΟΣ Phd University of Leicester
ΓΕΩΡΓΙΟΣ ΗΛΙΟΠΟΥΛΟΣ PhD University of Leicester Επίκουρος Καθηγητής Τμήματος Γεωλογίας Πανεπιστημίου Πατρών Βιογραφικό Σημείωμα Σπουδές – Τίτλοι – Δημοσιεύσεις, Ερευνητικό και Εκπαιδευτικό Έργο ΠΑΤΡΑ, ΜΑΡΤΙΟΣ 2018 1 ΠΕΡΙΕΧΟΜΕΝΑ Α. Βιογραφικά στοιχεία............................................................................................. 3 I. Προσωπικά στοιχεία……………………………………......…………….…….......3 II. Σπουδές – Τίτλοι……..……………………………………………......................... 3 III. Διδακτορική Διατριβή……………………..…………………………….................. 3 IV. Υποτροφίες – Ακαδημαϊκά βραβεία……….……..……………….…………........ 4 V. Ξένες γλώσσες……….….……………………………………….……………........ 4 VI. Επαγγελματική εξέλιξη..……………………..……………………………............. 4 VII. Διοικητικό έργο………..…………...………………………………………….......... 5 VIII. Άλλες δραστηριότητες……………………………………………..……................ 5 Β. Διδακτική δραστηριότητα......................................................................................6 I. Πανεπιστήμιο Πατρών……………………………………….……….........………. 6 II. Πανεπιστήμιο Κρήτης..…………………………………..…………………..........12 III. University College Northampton.………………………….………………..........14 IV. University of Leicester…………..………………………………………...............14 V. Εθνικό & Καποδιστριακό Πανεπιστήμιο Αθηνών…………..……………...…....14 Γ. Ερευνητική δραστηριότητα..................................................................................15 I. Τομείς έρευνας………………………...………………….……….........………... 15 II. Τρέχουσα ερευνητική δραστηριότητα...……………….………………….......… 15 III. Συμμετοχή σε ερευνητικά προγράμματα……………….………………………. -
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. -
4. Palaeontology
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2015 Palaeontology Klug, Christian ; Scheyer, Torsten M ; Cavin, Lionel Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-113739 Conference or Workshop Item Presentation Originally published at: Klug, Christian; Scheyer, Torsten M; Cavin, Lionel (2015). Palaeontology. In: Swiss Geoscience Meeting, Basel, 20 November 2015 - 21 November 2015. 136 4. Palaeontology Christian Klug, Torsten Scheyer, Lionel Cavin Schweizerische Paläontologische Gesellschaft, Kommission des Schweizerischen Paläontologischen Abhandlungen (KSPA) Symposium 4: Palaeontology TALKS: 4.1 Aguirre-Fernández G., Jost J.: Re-evaluation of the fossil cetaceans from Switzerland 4.2 Costeur L., Mennecart B., Schmutz S., Métais G.: Palaeomeryx (Mammalia, Artiodactyla) and the giraffes, data from the ear region 4.3 Foth C., Hedrick B.P., Ezcurra M.D.: Ontogenetic variation and heterochronic processes in the cranial evolution of early saurischians 4.4 Frey L., Rücklin M., Kindlimann R., Klug C.: Alpha diversity and palaeoecology of a Late Devonian Fossillagerstätte from Morocco and its exceptionally preserved fish fauna 4.5 Joyce W.G., Rabi M.: A Revised Global Biogeography of Turtles 4.6 Klug C., Frey L., Rücklin M.: A Famennian Fossillagerstätte in the eastern Anti-Atlas of Morocco: its fauna and taphonomy 4.7 Leder R.M.: Morphometric analysis of teeth of fossil and recent carcharhinid selachiens -
Issn: 2250-0588 Fossil Mammals
IJREISS Volume 2, Issue 8 (August 2012) ISSN: 2250-0588 FOSSIL MAMMALS (RHINOCEROTIDS, GIRAFFIDS, BOVIDS) FROM THE MIOCENE ROCKS OF DHOK BUN AMEER KHATOON, DISTRICT CHAKWAL, PUNJAB, PAKISTAN 1Khizar Samiullah* 1Muhammad Akhtar, 2Muhammad A. Khan and 3Abdul Ghaffar 1Zoology department, Quaid-e-Azam campus, Punjab University, Lahore, Punjab, Pakistan 2Zoology Department, GC University, Faisalabad, Punjab, Pakistan 3Department of Meteorology, COMSATS Institute of Information Technology (CIIT), Islamabad ABSTRACT Fossil site Dhok Bun Ameer Khatoon (32o 47' 26.4" N, 72° 55' 35.7" E) yielded a significant amount of mammalian assemblage including two families of even-toed fossil mammal (Giraffidae, and Bovidae) and one family of odd-toed (Rhinocerotidae) of the Late Miocene (Samiullah, 2011). This newly discovered site has well exposed Chinji and Nagri formation and has dated approximately 14.2-9.5 Ma. This age agrees with the divergence of different mammalian genera. Sedimentological evidence of the site supports that this is deposited in locustrine or fluvial environment, as Chinji formation is composed primarily of mud-stone while the Nagri formation is sand dominated. Palaeoenvironmental data indicates that Miocene climate of Pakistan was probably be monsoonal as there is now a days. Mostly the genera recovered from this site resemble with the overlying younger Dhok Pathan formation of the Siwaliks while the size variation in dentition is taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct this study at this specific site to add additional information in the field of Palaeontology. A detailed study of fossils mammals found in Miocene rocks exposed at Dhok Bun Ameer Khatoon was carried out.