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The Mio-Pliocene European Primate Fossil Record: Dynamics and Habitat Tracking
Journal of Human Evolution 47 (2004) 323e341 The Mio-Pliocene European primate fossil record: dynamics and habitat tracking Jussi T. Eronena,*, Lorenzo Rookb aDepartment of Geology, P.O. Box 64, FIN-00014 University of Helsinki, Finland bDipartimento di Scienze della Terra, Universita di Firenze, Via G.La Pira 4, 59121 Firenze, Italy Received 16 September 2003; accepted 13 August 2004 Abstract We present here a study of European Neogene primate occurrences in the context of changing humidity. We studied the differences of primate localities versus non-primate localities by using the mammal communities and the ecomorphological data of the taxa present in the communities. The distribution of primates is influenced by humidity changes during the whole Neogene, and the results suggest that the primates track the changes in humidity through time. The exception to this is the Superfamily Cercopithecoidea which shows a wider range of choices in habitats. All primate localities seem to differ from non-primate localities in that the mammal community structure is more closed habitat oriented, while in non-primate localities the community structure changes towards open-habitat oriented in the late Neogene. The differences in primate and non-primate localities are stronger during the times of deep environmental change, when primates are found in their preferred habitats and non-primate localities have faunas better able to adapt to changing conditions. Ó 2004 Elsevier Ltd. All rights reserved. Keywords: fossil primates; Cercopithecoidea; herbivore humidity proxy; hypsodonty; community structure; habitat tracking; Late Neogene; Europe Introduction look at the paleoecological scenarios for the temporal and geographical variation of different The Primate record of Europe is comparatively primate families and genera (e.g. -
Unravelling the Positional Behaviour of Fossil Hominoids: Morphofunctional and Structural Analysis of the Primate Hindlimb
ADVERTIMENT. Lʼaccés als continguts dʼaquesta tesi queda condicionat a lʼacceptació de les condicions dʼús establertes per la següent llicència Creative Commons: http://cat.creativecommons.org/?page_id=184 ADVERTENCIA. El acceso a los contenidos de esta tesis queda condicionado a la aceptación de las condiciones de uso establecidas por la siguiente licencia Creative Commons: http://es.creativecommons.org/blog/licencias/ WARNING. The access to the contents of this doctoral thesis it is limited to the acceptance of the use conditions set by the following Creative Commons license: https://creativecommons.org/licenses/?lang=en Doctorado en Biodiversitat Facultad de Ciènces Tesis doctoral Unravelling the positional behaviour of fossil hominoids: Morphofunctional and structural analysis of the primate hindlimb Marta Pina Miguel 2016 Memoria presentada por Marta Pina Miguel para optar al grado de Doctor por la Universitat Autònoma de Barcelona, programa de doctorado en Biodiversitat del Departamento de Biologia Animal, de Biologia Vegetal i d’Ecologia (Facultad de Ciències). Este trabajo ha sido dirigido por el Dr. Salvador Moyà Solà (Institut Català de Paleontologia Miquel Crusafont) y el Dr. Sergio Almécija Martínez (The George Washington Univertisy). Director Co-director Dr. Salvador Moyà Solà Dr. Sergio Almécija Martínez A mis padres y hermana. Y a todas aquelas personas que un día decidieron perseguir un sueño Contents Acknowledgments [in Spanish] 13 Abstract 19 Resumen 21 Section I. Introduction 23 Hominoid positional behaviour The great apes of the Vallès-Penedès Basin: State-of-the-art Section II. Objectives 55 Section III. Material and Methods 59 Hindlimb fossil remains of the Vallès-Penedès hominoids Comparative sample Area of study: The Vallès-Penedès Basin Methodology: Generalities and principles Section IV. -
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. -
The Evolution of Neogene Terrestrial Ecosystems in Europe Edited by Jorge Agusti, Lorenzo Rook and Peter Andrews Index More Information
Cambridge University Press 0521640970 - The Evolution of Neogene Terrestrial Ecosystems in Europe Edited by Jorge Agusti, Lorenzo Rook and Peter Andrews Index More information Index Abies, 382, 383 Albanensia grimmi, 157, 158 Abruzzi-Apulia palaeobioprovince, 191–3, Albanohyus, 403 197 Albanohyus pygmaeus, 119 Aceraceae, 184 Alcelaphini, 444 Aceratherium, 217, 221, 223 algal symbionts, 282–3, 311, 315 Aceratherium incivisum, 167, 170 Alicornops alfambrense, 119, 173 Aceratherium kiliasi, 212 Alicornops simorrense, 114, 119 Aceritherium incisivum, 119 Alilepus, 145, 198–9 Aceritherium tetradactylum, 119 Allohyaena kadici, 173 Acerorhinus, 253, 261 Allosoricinae, 392, 394 Acteocemas, 96, 98 Allospalax, 152 Adcrocuta, 104, 114, 209, 212 alluvial sediments Adcrocuta eximia, 118, 167, 173, 209, 211, NE Spain, 398–9 214, 215, 218, 220, 222, 230, 449 Sinap, 243–7 Aden, Gulf of, Pliocene tephra correlation, Tuscany, 365–8 24, 31, 31–51 Alpine foredeep, 13, 15 Aegean, rodent faunas, 17 altitudinal position, 89–90 aeolian deposits, Upper Valdarno basin, altitudinal trees, 379, 383 363–5 Altomiramys,96 Aepycerotini, 444 Alveolinella, 291 Afghanistan, Miocene primate taxa, 458 Amblycoptus, 267, 268, 270, 393 Africa American mammal immigration to Europe climate, 62–4 9, 13, 17, 446;, see also Bering climate/vegetation relationship, 64–8, landbridge 290, 292 American shrews, 392, 393, 394–5 correspondence analysis, recent faunas, Ammonia, 291 419–29 Amphechinus, 265 palaeoenvironment reconstruction, 290, amphibians, Italy, 191 292 Amphicyon, 14, 103 -
Fossil Primates
AccessScience from McGraw-Hill Education Page 1 of 16 www.accessscience.com Fossil primates Contributed by: Eric Delson Publication year: 2014 Extinct members of the order of mammals to which humans belong. All current classifications divide the living primates into two major groups (suborders): the Strepsirhini or “lower” primates (lemurs, lorises, and bushbabies) and the Haplorhini or “higher” primates [tarsiers and anthropoids (New and Old World monkeys, greater and lesser apes, and humans)]. Some fossil groups (omomyiforms and adapiforms) can be placed with or near these two extant groupings; however, there is contention whether the Plesiadapiformes represent the earliest relatives of primates and are best placed within the order (as here) or outside it. See also: FOSSIL; MAMMALIA; PHYLOGENY; PHYSICAL ANTHROPOLOGY; PRIMATES. Vast evidence suggests that the order Primates is a monophyletic group, that is, the primates have a common genetic origin. Although several peculiarities of the primate bauplan (body plan) appear to be inherited from an inferred common ancestor, it seems that the order as a whole is characterized by showing a variety of parallel adaptations in different groups to a predominantly arboreal lifestyle, including anatomical and behavioral complexes related to improved grasping and manipulative capacities, a variety of locomotor styles, and enlargement of the higher centers of the brain. Among the extant primates, the lower primates more closely resemble forms that evolved relatively early in the history of the order, whereas the higher primates represent a group that evolved more recently (Fig. 1). A classification of the primates, as accepted here, appears above. Early primates The earliest primates are placed in their own semiorder, Plesiadapiformes (as contrasted with the semiorder Euprimates for all living forms), because they have no direct evolutionary links with, and bear few adaptive resemblances to, any group of living primates. -
Middle and Late Miocene Terrestrial Vertebrate Localities And
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 2006 Band/Volume: 30 Autor(en)/Author(s): Nargolwalla Mariam C., Hutchison Matt P., Begun David R. Artikel/Article: Middle and Late Miocene Terrestrial Vertebrate Localities and Paleoenvironments in the Pannonian Basin 347-360 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 30:347-360, Wien 2006 Middle and Late Miocene Terrestrial Vertebrate Localities and Paleoenvironments in the Pannonian Basin by Mariam C. N a r g o l w a l l a *),Matt P. H u t c h is o n & David R. B e g u n Nargolwalla , M.C., H utchison , M.P. & Begun , D.R., 2006. Middle and Late Miocene Terrestrial Vertebrate Localities and Paleoenvironments in the Pannonian Basin. — Beitr. Palaont., 30:347-360, Wien. Abstract Crisis,’ in addition to the paleoenvironmental evidence for the location and timing of potential corridors for The Pannonian Basin, surrounded by the Carpathians, faunal interchange. Alps and Dinarides, has long been known as a sedimen tary catchment area rich in information on the environ Key words: Miocene, Pannonian Basin, Lake Pannon, fos mental and biological evolution of Central Europe in the sil, vertebrate, paleoenvironment, paleogeography Miocene. We present here the results of an integrative study using GIS to synthesize the findings from our last three years of survey and excavation of new terrestrial Kurzfassung vertebrate fossil localities of Miocene age, together with the most recent paleogeographic reconstructions of the Das Pannonische Becken, umgeben von den Karpaten, region and published faunal and environmental data, Alpen und Dinariden, ist schon lange bekannt für seinen with the purpose of presenting a revised, comprehensive Sedimentreichtum und für seine Informationen bezüglich history of the paleogeography and paleobiogeography der Umweltentwicklung und der biologischen Evolution of the Pannonian Basin. -
A New Dryopithecine Mandibular Fragment from the Middle Miocene
Journal of Human Evolution 145 (2020) 102790 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Short Communications A new dryopithecine mandibular fragment from the middle Miocene of Abocador de Can Mata and the taxonomic status of ‘Sivapithecus’ occidentalis from Can Vila (Valles-Pened es Basin, NE Iberian Peninsula) * David M. Alba a, , Josep Fortuny a, Josep M. Robles a, Federico Bernardini b, c, Miriam Perez de los Ríos d, Claudio Tuniz c, b, e, Salvador Moya-Sol a a, f, g, * Clement Zanolli h, a Institut Catala de Paleontologia Miquel Crusafont, Universitat Autonoma de Barcelona, Edifici ICTA-ICP, Carrer de les Columnes s/n, Campus de la UAB, Cerdanyola del Valles, Barcelona, 08193, Spain b Centro Fermi, Museo Storico della Fisica e Centro di Studi e Ricerche ‘Enrico Fermi’, Piazza del Viminale 1, Roma, 00184, Italy c Multidisciplinary Laboratory, The ‘Abdus Salam’ International Centre for Theoretical Physics, Via Beirut 31, Trieste, 34151, Italy d ~ Departamento de Antropología, Facultad de Ciencias Sociales, Universidad de Chile, Ignacio Carrera Pinto, 1045, Nunoa,~ Santiago, Chile e Center for Archaeological Science, University of Wollongong, Northfields Ave, Wollongong, NSW, 2522, Australia f Unitat d'Antropologia Biologica, Department de Biologia Animal, Biologia Vegetal i Ecologia, Universitat Autonoma de Barcelona, Campus de la UAB, Cerdanyola del Valles, Barcelona, Spain g Institucio Catalana de Recerca i Estudis Avançats (ICREA), Pg. Lluís Companys 23, Barcelona, 08010, Spain h Laboratoire PACEA, UMR 5199 CNRS, Universite de Bordeaux, allee Geoffroy Saint Hilaire, 33615 Pessac Cedex, France article info Article history: 2012; Alba et al., 2018). -
A New Dryopithecine Mandibular Fragment from the Middle Miocene
A new dryopithecine mandibular fragment from the middle Miocene of Abocador de Can Mata and the taxonomic status of ‘Sivapithecus’ occidentalis from Can Vila (Vallès-Penedès Basin, NE Iberian Peninsula) David Alba, Josep Fortuny, Josep Robles, Federico Bernardini, Miriam Pérez de los Ríos, Claudio Tuniz, Salvador Moyà-Solà, Clément Zanolli To cite this version: David Alba, Josep Fortuny, Josep Robles, Federico Bernardini, Miriam Pérez de los Ríos, et al.. A new dryopithecine mandibular fragment from the middle Miocene of Abocador de Can Mata and the tax- onomic status of ‘Sivapithecus’ occidentalis from Can Vila (Vallès-Penedès Basin, NE Iberian Penin- sula). Journal of Human Evolution, Elsevier, 2020, 145, pp.102790. 10.1016/j.jhevol.2020.102790. hal-03002540 HAL Id: hal-03002540 https://hal.archives-ouvertes.fr/hal-03002540 Submitted on 12 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. Postprint of: Alba, D. M., Fortuny, J., Robles, J. M., Bernardini, F., Pérez de los Ríos, M., Tuniz, C., Moyà-Solà, S., & Zanolli, C. (2020). A new dryopithecine mandibular fragment from the middle Miocene of Abocador de Can Mata and the taxonomic status of ‘Sivapithecus’ occidentalis from Can Vila (Vallès-Penedès Basin, NE Iberian Peninsula). -
Leeds Thesis Template
Middle to Late Miocene terrestrial biota and climate by Matthew James Pound M.Sci., Geology (University of Bristol) Submitted in accordance with the requirements for the degree of Doctor of Philosophy The University of Leeds School of Earth and Environment September 2012 - 2 - Declaration of Authorship The candidate confirms that the work submitted is his/her own, except where work which has formed part of jointly-authored publications has been included. The contribution of the candidate and the other authors to this work has been explicitly indicated below. The candidate confirms that appropriate credit has been given within the thesis where reference has been made to the work of others. Chapter 2 has been published as: Pound, M.J., Riding, J.B., Donders, T.H., Daskova, J. 2012 The palynostratigraphy of the Brassington Formation (Upper Miocene) of the southern Pennines, central England. Palynology 36, 26-37. Chapter 3 has been published as: Pound, M.J., Haywood, A.M., Salzmann, U., Riding, J.B. 2012. Global vegetation dynamics and latitudinal temperature gradients during the mid to Late Miocene (15.97 - 5.33 Ma). Earth Science Reviews 112, 1-22. Chapter 4 has been published as: Pound, M.J., Haywood, A.M., Salzmann, U., Riding, J.B., Lunt, D.J. and Hunter, S.J. 2011. A Tortonian (Late Miocene 11.61-7.25Ma) global vegetation reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology 300, 29-45. This copy has been supplied on the understanding that it is copyright material and that no quotation from the thesis may be published without proper acknowledgement. © 2012, The University of Leeds, British Geological Survey and Matthew J. -
Palaeontological Highlights of Austria
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Mitt. Österr. Geol. Ges. ISSN 0251-7493 92 (1999) 195-233 Wien, Juli 2000 Palaeontological Highlights of Austria WERNER E. PILLER1, GUDRUN DAXNER-HÖCK2, DARYL P DOMNING3, HOLGER C. FORKE4, MATHIAS HARZHAUSER2, BERNHARD HUBMANN1, HEINZ A. KOLLMANN2, JOHANNA KOVAR-EDER2, LEOPOLD KRYSTYN5, DORIS NAGEL5, PETER PERVESLER5, GERNOT RABEDER5, REINHARD ROETZEL6, DIETHARD SANDERS7, HERBERT SUMMESBERGER2 28 Figures and 1 Table Introduction Besides Zeapora gracilis, distinguished by large rounded cortical filaments, Pseudolitanaia graecensis and Pseu The oldest known fossils in Austria date back into the dopalaeoporella lummatonensis occur (Fig. 3). Pseudolitan Ordovician. From this time on a broadly continuous fossil aia graecensis is built up of straight thalli containing club- record is preserved up to the Holocene. Since an encyclo shaped filaments and Pseudopalaeoporella lummatonensis paedic or monographic presentation is impossible within is characterized by a typically poorly-calcified medullar this volume, nine case studies of different stratigraphic lev zone and delicate cortical filaments. els (Fig. 1) were selected to call attention to this remarkably There are two localities known with autochthonous algal good fossil documentation. These case studies include occurrences in the Graz Palaeozoic. One is characterized records on invertebrate fossils from several time slices from by Pseudopalaeoporella lummatonensis with dispersed the Late Palaeozoic to the Miocene, as well as on verte thalli of Pseudolitanaia. Contrary to all expectations, these brates from the Miocene and Pleistocene and on plant algae are found in marly lithologies suggesting very bad fossils from the Devonian and Early Miocene. This selection environmental conditions for photoautotrophic organisms. -
Macaques at the Margins: the Biogeography and Extinction of Macaca Sylvanus in Europe. Sarah Elton1 and Hannah J. O'regan2 1D
Macaques at the margins: the biogeography and extinction of Macaca sylvanus in Europe. Sarah Elton1 and Hannah J. O’Regan2 1Department of Anthropology, Durham University, Durham, DH1 3LE 2Department of Archaeology, University of Nottingham, University Park Nottingham, NG7 2RD. KEYWORDS Miocene, Pliocene, Pleistocene, primate, fossil, modelling, Eurasia, time budgets ABSTRACT The genus Macaca (Primates: Cercopithecidae) originated in Africa, dispersed into Europe in the Late Miocene and resided there until the Late Pleistocene. In this contribution, we provide an overview of the evolutionary history of Macaca in Europe, putting it into context with the wider late Miocene, Pliocene and Pleistocene European monkey fossil record (also comprising Mesopithecus, Paradolichopithecus, Dolichopithecus and Theropithecus). The Pliocene and Pleistocene European Macaca fossil material is largely regarded as Macaca sylvanus, the same species as the extant Barbary macaque in North Africa. The M. sylvanus specimens found at West Runton in Norfolk (53°N) during the Middle Pleistocene are among the most northerly euprimates ever discovered. Our simple time-budget model indicates that short winter day lengths would have imposed a significant constraint on activity at such relatively high latitudes, so macaque populations in Britain may have been at the limit of their ecological tolerance. Two basic models using climatic and topographic data for the Last Interglacial and the Last Glacial Maximum alongside Middle and Late Pleistocene fossil 1 distributions indicate that much of Europe may have been suitable habitat for macaques. The models also indicate that areas of southern Europe in the present day have a climate that could support macaque populations. However, M. sylvanus became locally extinct in the Late Pleistocene, possibly at a similar time as the straight-tusked elephant, Palaeoloxodon antiquus, and narrow-nosed rhinoceros, Stephanorhinus hemitoechus. -
Kingdom =Animalia Phylum =Chordata Subphylum =Vertebrata Class =Mammalia Order =Primates I. PARTIAL
Kingdom =Animalia '' Phylum =Chordata '' Subphylum =Vertebrata '' Class =Mammalia '' Order =Primates 130-132 I. PARTIAL TAXONOMIC CLASSIFICATION OF PREHISTORIC AND CONTEMPORARY PRIMATES 176-187 197-198/Lab 7.II. Suborder Infraorder Superfamily Family Genus Species Common Name Prosimii [tree shrew = insectivore] (Strepsirhini) lemur 132-134 aye-aye 188-191 loris and bush baby tarsier Anthropoidea Platyrrhini *Parapithecus (basal anthropoid) (Haplorhini) 134-136 *Apidium (basal anthropoid) 134-138 Ceboidea New World monkey 188-191 Catarrhini *Propliopithecus (basal catarrhine) 136-138 *Aegyptopithecus (basal catarrhine) Cercopithecoidea Cercopithecidae Old World monkey 124-126 Macaca macaque Papio baboon Colobidae Colobus colobus monkey Presbytis langur Hominoidea *Proconsulidae *Proconsul 138-143 191-193 Lab 7. II. D. *Oreopithecidea *Oreopithecus Hylobatidae Hylobates gibbon *Pliopithecidae *Pliopithecus Pongidae *Dryopithecus *dryopithecus *Sivapithecus *ramapithecus *kenyapithecus *ouranopithecus *Gigantopithecus Pongo orangutan Panidae Pan traglodytes chimpanzee Pan paniscus bonobo (“pygmy chimpanzee”) Pan ? Gorilla gorilla Mountain gorilla Gorilla Western lowland g. 202-204 Hominidae *Ardipithecus *ramidus 213-218 1 228-237 *Australopithecus *anamensis 241-245 *afarensis Lucy / First Family Lab 8 *africanus southern ape *garhi *[aka Paranthropus]1 *aethiopicus *boisei Zinj *robustus *Kenyanthropus *platyops 1 237-238 Homo *rudolfensis ER-1470 245-247 *habilis human Ch. 11 *erectus Java / Peking “Man” Lab 10 sapiens Mary / John Chs. 12-13 Lab 12 An * marks groups known only through fossils. Compare: FIGURE 6-7 Primate taxonomic classification, p. 131 FIGURE 6-8 Revised partial classification of the primates, p. 132 FIGURE 8-1 Classification chart, modified from Linnaeus p. 177 FIGURE 8-15 Major events in early primate evolution, p. 191 Virtual Lab 1, section II, parts A-D Primate Classification 1(Note: Australopithecus and Paranthropus make up a “Subfamily” called Australopithecinae, more commonly known as Australopithecines.