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Abstractbook 6Ewvp.Pdf
6th European Workshop on Vertebrate Palaeontology - Florence and Montevarchi (Italy) - September 19-22, 2001 The organizing team welcomes the participants in the 6th European Workshop of Vertebrate Paleontology in Florence and expresses its deepest thanks to the many colleagues that enthusiastically answered to our call making this issue possible. The organizers hope the participants will find Florence not only that jewel-case of art celebrated all over the world, but also an appropriate place for discussing crumbled fossil bones. May the meeting come up to everybody’s best expectations! The 6th European Workshop on Vertebrate Paleontology has been made possible, thanks to the support and collaboration obtained from the Tethys Cultural Association, the Section of Geology and Paleontology of the Museum of Natural History of Florence, the Department of Earth Sciences of Florence and the Museum of Plaeontology of the Accademia Valdarnese del Poggio of Montevarchi. The organizers would like to thank the administration of the Section of Geology and Paleontology of the Museum of Natural History of Florence and the Accademia Valdarnese del Poggio for granting their facilities, and all the volunteers for their generous donation of time and talent. Without their dedication and tireless efforts, this issue would have been impossible. Special thanks are due to Maria Cristina Andreani, manager of the display department of the Section of Geology and Paleontology of the Museum of Natural History of Florence, for her assistance and for creating the logo and producing the panels of explanation of the evolution of the Upper Valdarno. The organizers are also grateful to the Comune of Montevarchi for offering the conference lunch and to Tiziana Vitali for arranging the tea party. -
1 Published in Journal of South American Earth Sciences, 31:414
Published in Journal of South American Earth Sciences, 31:414-425, 2011 (This is a prepublication version, with larger illustrations) A high resolution stratigraphic framework for the remarkable fossil cetacean assemblage of the Miocene/Pliocene Pisco Formation, Peru Leonard Brand a,*, Mario Urbina b, Arthur Chadwick c, Thomas J. DeVries d, Raul Esperante e, a Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, CA 92350 b Museo de Historia Natural, Lima 14, Peru c Southwestern Adventist University, Keene, TX 76059 d Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195 e Geoscience Research Institute, Loma Linda, CA 92350 Abstract The Miocene/Pliocene Pisco Formation of Peru contains a rich marine vertebrate fossil record, providing a unique opportunity for the study of paleoecology and evolution, along with the sedimentological context of the fossils. The lack of a high-resolution stratigraphic framework has hampered such study. In this paper we develop the needed stratigraphy for the areas in the Pisco Formation where most of the vertebrate paleontological research is occurring. In the Ica Valley and in the vicinity of Lomas, series of lithologically or paleontologically unique marker beds were identified. These were walked out and documented with GPS technology. Measured sections connecting these marker beds provide a stratigraphic framework for the areas studied. GPS locations, maps of the marker beds on aerial photographs, and outcrop photographs allow field determination of the stratigraphic positions of study areas. Keywords: Stratigraphy, Miocene, Pliocene, Pisco, Peru * Corresponding author. FAX 909-558-0259 E-mail address: [email protected] (Leonard Brand) 1. -
Fossil Bovidae from the Malay Archipelago and the Punjab
FOSSIL BOVIDAE FROM THE MALAY ARCHIPELAGO AND THE PUNJAB by Dr. D. A. HOOIJER (Rijksmuseum van Natuurlijke Historie, Leiden) with pls. I-IX CONTENTS Introduction 1 Order Artiodactyla Owen 8 Family Bovidae Gray 8 Subfamily Bovinae Gill 8 Duboisia santeng (Dubois) 8 Epileptobos groeneveldtii (Dubois) 19 Hemibos triquetricornis Rütimeyer 60 Hemibos acuticornis (Falconer et Cautley) 61 Bubalus palaeokerabau Dubois 62 Bubalus bubalis (L.) subsp 77 Bibos palaesondaicus Dubois 78 Bibos javanicus (d'Alton) subsp 98 Subfamily Caprinae Gill 99 Capricornis sumatraensis (Bechstein) subsp 99 Literature cited 106 Explanation of the plates 11o INTRODUCTION The Bovidae make up a very large portion of the Dubois collection of fossil vertebrates from Java, second only to the Proboscidea in bulk. Before Dubois began his explorations in Java in 1890 we knew very little about the fossil bovids of that island. Martin (1887, p. 61, pl. VII fig. 2) described a horn core as Bison sivalensis Falconer (?); Bison sivalensis Martin has al• ready been placed in the synonymy of Bibos palaesondaicus Dubois by Von Koenigswald (1933, p. 93), which is evidently correct. Pilgrim (in Bron- gersma, 1936, p. 246) considered the horn core in question to belong to a Bibos species closely related to the banteng. Two further horn cores from Java described by Martin (1887, p. 63, pl. VI fig. 4; 1888, p. 114, pl. XII fig. 4) are not sufficiently well preserved to allow of a specific determination, although they probably belong to Bibos palaesondaicus Dubois as well. In a preliminary faunal list Dubois (1891) mentions four bovid species as occurring in the Pleistocene of Java, viz., two living species (the banteng and the water buffalo) and two extinct forms, Anoa spec. -
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A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases. -
Checklist of Fish and Invertebrates Listed in the CITES Appendices
JOINTS NATURE \=^ CONSERVATION COMMITTEE Checklist of fish and mvertebrates Usted in the CITES appendices JNCC REPORT (SSN0963-«OStl JOINT NATURE CONSERVATION COMMITTEE Report distribution Report Number: No. 238 Contract Number/JNCC project number: F7 1-12-332 Date received: 9 June 1995 Report tide: Checklist of fish and invertebrates listed in the CITES appendices Contract tide: Revised Checklists of CITES species database Contractor: World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge, CB3 ODL Comments: A further fish and invertebrate edition in the Checklist series begun by NCC in 1979, revised and brought up to date with current CITES listings Restrictions: Distribution: JNCC report collection 2 copies Nature Conservancy Council for England, HQ, Library 1 copy Scottish Natural Heritage, HQ, Library 1 copy Countryside Council for Wales, HQ, Library 1 copy A T Smail, Copyright Libraries Agent, 100 Euston Road, London, NWl 2HQ 5 copies British Library, Legal Deposit Office, Boston Spa, Wetherby, West Yorkshire, LS23 7BQ 1 copy Chadwick-Healey Ltd, Cambridge Place, Cambridge, CB2 INR 1 copy BIOSIS UK, Garforth House, 54 Michlegate, York, YOl ILF 1 copy CITES Management and Scientific Authorities of EC Member States total 30 copies CITES Authorities, UK Dependencies total 13 copies CITES Secretariat 5 copies CITES Animals Committee chairman 1 copy European Commission DG Xl/D/2 1 copy World Conservation Monitoring Centre 20 copies TRAFFIC International 5 copies Animal Quarantine Station, Heathrow 1 copy Department of the Environment (GWD) 5 copies Foreign & Commonwealth Office (ESED) 1 copy HM Customs & Excise 3 copies M Bradley Taylor (ACPO) 1 copy ^\(\\ Joint Nature Conservation Committee Report No. -
Did Adria Rotate Relative to Africa?
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Solid Earth Discuss., 6, 937–983, 2014 Open Access www.solid-earth-discuss.net/6/937/2014/ Solid Earth doi:10.5194/sed-6-937-2014 Discussions © Author(s) 2014. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal Solid Earth (SE). Please refer to the corresponding final paper in SE if available. Did Adria rotate relative to Africa? D. J. J. van Hinsbergen1, M. Mensink1, C. G. Langereis1, M. Maffione1, L. Spalluto2, M. Tropeano2, and L. Sabato2 1Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands 2Dipartimento di Scienze della Terra e Geoambientali, Universitá degli Studi “Aldo Moro” di Bari, Via E. Orabona 4, 70125, Bari, Italy Received: 17 March 2014 – Accepted: 18 March 2014 – Published: 28 March 2014 Correspondence to: D. J. J. van Hinsbergen ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 937 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract The first and foremost boundary condition for kinematic reconstructions of the Mediter- ranean region is the relative motion between Africa and Eurasia, constrained through reconstructions of the Atlantic Ocean. The Adria continental block is in a downgoing 5 plate position relative to the strongly curved Central Mediterranean subduction-related orogens, and forms the foreland of the Apennines, Alps, Dinarides, and Albanides- Hellenides. It is connected to the African plate through the Ionian Basin, likely with lower Mesozoic oceanic lithosphere. If the relative motion of Adria vs. Africa is known, its po- sition relative to Eurasia can be constrained through the plate circuit, and hard bound- 10 ary conditions for the reconstruction of the complex kinematic history of the Mediter- ranean are obtained. -
Investigating Sexual Dimorphism in Ceratopsid Horncores
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-01-25 Investigating Sexual Dimorphism in Ceratopsid Horncores Borkovic, Benjamin Borkovic, B. (2013). Investigating Sexual Dimorphism in Ceratopsid Horncores (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26635 http://hdl.handle.net/11023/498 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Investigating Sexual Dimorphism in Ceratopsid Horncores by Benjamin Borkovic A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2013 © Benjamin Borkovic 2013 Abstract Evidence for sexual dimorphism was investigated in the horncores of two ceratopsid dinosaurs, Triceratops and Centrosaurus apertus. A review of studies of sexual dimorphism in the vertebrate fossil record revealed methods that were selected for use in ceratopsids. Mountain goats, bison, and pronghorn were selected as exemplar taxa for a proof of principle study that tested the selected methods, and informed and guided the investigation of sexual dimorphism in dinosaurs. Skulls of these exemplar taxa were measured in museum collections, and methods of analysing morphological variation were tested for their ability to demonstrate sexual dimorphism in their horns and horncores. -
Evidence of Predation on Epipelagic Fish for a Stem Beaked Whale
Electronic Supplementary Material for No deep diving: evidence of predation on epipelagic fish for a stem beaked whale from the late Miocene of Peru Olivier Lambert*, Alberto Collareta, Walter Landini, Klaas Post, Benjamin Ramassamy, Claudio Di Celma, Mario Urbina, Giovanni Bianucci *To whom correspondence should be addressed. E-mail: [email protected] Content: 1. Supplementary Figures p. 2 2. Size and Weight Estimates for Messapicetus gregarius p. 7 3. Size and Weight Estimates for Sardinops sp. cf S. sagax p. 8 4. Comparison of Cervical Vertebrae Ankylosis and Size among Ziphiidae p. 12 5. Comparison of Relative Humeral Length among Ziphiidae p. 18 6. Abbreviations for Institutions p. 20 7. Supplementary References p. 22 2 1. SUPPLEMENTARY FIGURES Figure S1. A, B: Two different sets of imbricated cycloid scales. Note the presence of tubercular protuberances in the centre of the scales and the curved radii-like lines in their lateral fields; nowadays, these two features are typical of large scales belonging to mature individuals of the extant Pacific pilchard (Sardinops sagax). 3 Figure S2. A: Four fully articulated fish vertebral column segments embedded in bony and dermal fish remains. B: Detail of A showing a vertebral column segment contoured by imbricated, large cycloid scales. C: Fully articulated clupeid pelvic girdle, comprising the proximal portion of some fin rays. 4 Figure S3. A, B: Two clupeid preopercles packed with other partly disarticulated, although still interconnected, collapsed skull bones. A partial bivalve shell can be seen in A, while in B some characteristic cycloid scales appear. C, D: Detail of the dolomite concretion including the skull and mandibles of Messapicetus gregarius, showing the hamular processes of the pterygoids, the posteroventral portions of the mandibles, two articulated bivalve shells, and a fragment of fossilized wood. -
GC University Lahore
GC University Lahore PALAEOENVIRONMENTAL STUDY OF PAKISTAN SIWALIKS Name: MUHAMMAD TARIQ Session: 2007-2010 Roll No: 05-GCU-PHD-Z-07 Supervisor: Prof. Dr. Nusrat Jahan Department: Zoology PALAEOENVIRONMENTAL STUDY OF PAKISTAN SIWALIKS Submitted to GC University Lahore in fulfillment of the requirements for the award of Degree of Doctor of Philosophy in Zoology by Name: MUHAMMAD TARIQ Session: 2007-2010 Roll No: 05-GCU-PHD-Z-07 Department of Zoology GC University Lahore DEDICATION This work is dedicated to MY LOVING PARENTS (Gulzar Ahmad and Sugran Abdullah) through whom I acquired indefatigable temperament, morality, and determination for achieving objectives in every walk of life MY YOUNGER BROTHERS (Muhammad Yasin and Muhammad Noor-ul-Amin) who gave hope and strength to meet with the challenges of life MY YOUNGER SISTERS Zainab Gulzar, Shahida Gulzar and Shakeela Gulzar for their care, affection and cooperation MY DEAREST DAUGHTER (Kashaf Tariq) who proved great blessing for achieving goals of my life ALL GREAT SOULS who pursue their dreams with persistent efforts to make this world a better place to live in DECLARATION I, Mr. Muhammad Tariq Roll No. 05-GCU-PHD-Z-07 student of PhD in the subject of Zoology session: 2007-2010, hereby declare that the matter printed in the thesis titled “Palaeoenvironmental Study of Pakistan Siwaliks” is my own work and has not been printed, published and submitted as research work, thesis or publication in any form in any University, Research Institution etc in Pakistan or abroad. ________________ _____________________ Dated Signatures of Deponent RESEARCH COMPLETION CERTIFICATE Certified that the research work contained in this thesis titled “Palaeoenvironmental Study of Pakistan Siwaliks” has been carried out and completed by Mr. -
Abstract (Pdf)
2 Congresso GeoSed 25-26 Settembre 2008 Aula Magna Palazzo di Scienze della Terra Campus Universitario Via E. Orabona 4 BARI Atti del Congresso a cura di: Massimo Moretti ORGANIZZAZIONE Coordinamento Luisa Sabato Segreteria Luigi Spalluto Comitato organizzatore Salvatore Gallicchio Massimo Moretti Luisa Sabato Luigi Spalluto Marcello Tropeano Collaboratori Alessia Barchetta Elisa Costantini Antonietta Cilumbriello Antonio Grippa Michele Labriola Rosanna Laragione Stefania Lisco Vincenzo Onofrio Mariangela Pepe Patrocinio e Contributo Università degli Studi di Bari Dipartimento di Geologia e Geofisica Dottorato di Scienze della Terra Regione Puglia Regione Basilicata Provincia di Bari Comune di Bari Commissione Italiana “Anno Internazionale del Pianeta Terra” 4 INDICE DEL VOLUME G. Aiello, A. Conforti, B. D’Argenio Regional marine geologic cartography of the Naples Bay (scale 1:10.000): the geological map n. 465 “Procida” pag. 1 G. Aiello, E. Marsella, S. Passaro The continental slopes off the Ischia island (Naples Bay): submarine gravity instability processes investigated by means of marine geological and geophysical data pag. 4 M. Aldinucci, I. Martini, F. Sandrelli The Pliocene deposits of the northern Siena Basin (Tuscany, Italy) revised through unconformity-bounded stratigraphic units pag. 6 A. Alfarano, M. Delle Rose, L. Orlanducci, F. Resta Rapporti stratigrafici tra pietra leccese, piromafo e Calcareniti di Andrano (area urbana e periferia est di Lecce) pag. 8 S. Andreucci, V. Pascucci, M. D. Bateman Record of three peaks during the Marine Isotopic Stage MIS5 along the Alghero coast, NW Sardinia, Italy: Sea level implication pag. 10 A. Barchetta, L. Spalluto Stratigrafia e caratteri di facies delle successioni carbonatiche affioranti nell’area compresa tra Binetto e Grumo Appula (Murge baresi, Puglia) pag. -
Los Mamíferos Del Plioceno Y Pleistoceno De La Península Ibérica
94 investigación Los mamíferos del Plioceno y Pleistoceno de la Península Ibérica Bienvenido Martínez-Navarro | IPHES, Institut Català de Paleoecologia Humana i Evolució Social, Àrea de Prehistòria, Universitat Rovira i Virgili (URV), ICREA Sergio Ros-Montoya, María-Patrocinio Espigares | Dpto. de Ecología y Geología, Facultad de Ciencias, Universidad de Málaga Joan Madurell-Malapeira | Institut Català de Paleontologia Miquel Crusafont Paul Palmqvist | Dpto. de Ecología y Geología, Facultad de Ciencias, Universidad de Málaga URL de la contribución <www.iaph.es/revistaph/index.php/revistaph/article/view/4203> RESUMEN España es el país con mayor número de yacimientos bien conservados, cantidad y calidad de fósiles de todo el continente europeo. Aquí se describe el patrimonio paleobiológico correspondiente al Plio-Pleistoceno (últimos 5,3 millones de años) registrado en los principales yacimientos con presencia de fósiles de grandes mamíferos de la Península Ibérica. Ningún otro país de nuestro entorno al norte del Mediterráneo ofrece mayores posibilidades para el estudio y disfrute de los registros paleontológicos del Plioceno y Pleistoceno. En este contexto destacan las principales cuencas sedimentarias como las de Besalú-Bañolas, Vallés, Calatayud-Teruel, o ya en el sur las cuencas intrabéticas, donde merece especial interés la de Baza y Guadix, con localidades emblemáticas como Baza 1 para el Plioceno, y como los yacimientos de Orce (Fuente Nueva 1 y 3, Venta Micena o Barranco León, entre otros) para el Pleistoceno inferior. También se hace referencia a otro tipo de yacimientos, como son los maares volcánicos pliocénicos del Camp dels Ninots en Cataluña, o el de las Higueruelas en la Mancha, a las terrazas fósiles de los grandes ríos peninsulares, así como a los extraordinarios registros kársticos, donde destaca el de Atapuerca en Burgos. -
Hemibos (Bovini, Bovidae, Mammalia) from the Pinjor Formation of Pakistan
The Journal of Animal & Plant Sciences 19(2): 2009, Pages: 98-100 ISSN: 1018-7081 HEMIBOS (BOVINI, BOVIDAE, MAMMALIA) FROM THE PINJOR FORMATION OF PAKISTAN M. A. Khan, M. Iqbal* and M. Akhtar** Department of Zoology, Government College University, Faisalabad, Punjab, Pakistan. * Department of Zoology, Government Science College Wahdat Road, Lahore, Pakistan ** Department of Zoology, University of the Punjab, Lahore, 54590, Pakistan *Correspondence author: [email protected] ABSTRACT The dental material of Hemibos from the Plio-Pleistocene of the Pinjor Formation (2.6 – 0.6 Ma) in the Upper Siwaliks (Pakistan) is reported here. The new specimens consist of two fragmentary maxillae. The comparative morphological and matric study of Hemibos dental fossils provide interesting information about individual variation. Key words: Hemibos, Bovine, Pinjor Formation, Upper Siwaliks, Plio-Pleistocene. INTRODUCTION 73°34´55 E), district Jhelum and Pir Jaffar (32°46´44 N, 74°05´01 E), district Gujrat from the Pinjor Formation of Bovines (clade Bovini) are widespread group Pakistan (Fig. 1). The anatomy of the specimens confirms including extant wild and domesticated species such as that it is a member of the genus Hemibos, the ancestor of the African Cape buffalo, the American bison, the Asian the water buffalo Bubalus. water buffalo, kouprey, banteng, gaur, anoa, and yak, as well as the progenitor of domesticated cattle, the auroch (Bibi, 2007) as well as extinct species such as Bos namadicus, B. acutifrons, Leptobos falconeri, Proleptobos birmanicus, Hemibos spp., Bison spp., Bubalus spp., Bucapra daviesii and Proamphibos spp. (Pilgrim, 1937, 1939; Hooijer, 1958; Nanda, 2008, Khan et al., 2009). Bovines display a suite of craniodental characters that has facilitated their identification in the archaeological and fossil records (Bibi, 2007).