Università Deglistudidinapolifederico

Total Page:16

File Type:pdf, Size:1020Kb

Università Deglistudidinapolifederico UNIVERSITÀ DEGLI STUDI DI NAPOLI FEDERICO II THE PLIO -HOLOCENE LARGE MAMMALS OF THE WESTERN EURASIA : MACROECOLOGICAL AND EVOLUTIONARY ANALYSES OF THE FAUNAS Dr. Francesco Carotenuto Dottorato in Scienze della Terra, Geologia del Sedimentario XXII Ciclo Tutor Prof. Carmela Barbera Cotutori Dr. Pasquale Raia, Prof. Anastassios Kotsakis 2009 To Daniela and my family “The most erroneous stories are those we think we know best - and therefore never scrutinize or question.” Stephen J. Gould Index Preface ........................................................................................................................................... IV Chapter 1 - The Eurasian Paleocommunities ................................................................................. 1 1.1 Introduction ............................................................................................................................ 1 1.1.1 The italian Paleocommunities (PCOMs) ............................................................................ 2 1.1.2 The properties of the Italian Paleocommunities: Body size and occupancy ..................... 5 1.1.3 Species turnover, diversity trends, and prey-predator relationship ................................... 6 1.2 Materials and Methods ........................................................................................................ 10 1.2.1 The data employed ........................................................................................................... 10 1.2.2 Time ordering techniques ................................................................................................. 13 1.2.2.1 Spectral ordering ........................................................................................................... 13 1.2.2.2 The Maximum Likelihood Appearance Event Ordination (MLA EO) ............................. 15 1.2.3 The Bootstrapped Cluster Analysis .................................................................................. 17 1.2.3.1 The BCA applied to the Plio-Holocene Western Eurasia LFAs .................................... 19 1.3 Results ................................................................................................................................. 20 1.3.1 The time-ordering of the Local Faunal Assemblages ...................................................... 20 1.3.2 The EA PCOM .................................................................................................................. 22 1.3.3 The geographical distribution and composition of the EA PCOMs ................................. 24 1.4. Discussion .......................................................................................................................... 31 Chapter 2 -Macroecology of the fossil mammal assemblages: occupancy, range size and phylogeny ...................................................................................................................................... 32 2.1 Introduction .......................................................................................................................... 32 2.1.1 The body size and its geographical distribution ............................................................... 33 2.1.2 Occupancy ........................................................................................................................ 34 2.1.3 The abundance-occupancy relationship .......................................................................... 35 2.1.3.1 Occupancy in paleontological studies ........................................................................... 37 2.1.4 The range size .................................................................................................................. 39 2.1.4.1 The distribution of range sizes ...................................................................................... 40 2.1.4.2 The hereditability of the range size ............................................................................... 41 2.1.5 The inclusion of phylogenetic information in comparative studies .................................. 43 2.1.5.1 The structures of a phylogenetic tree and its properties .............................................. 46 2.1.5.2 The Brow nian motion model ......................................................................................... 46 I 2.1.5.3 The Ornstein-Uhlenbeck process (OU) and the accelerating and decelerating Brow nian evolution (ACDC) ....................................................................................................... 47 2.1.5.4 Phylogenetic influence on type I and II error estimations ............................................. 48 2.1.6 Phylogenetic comparative methods ................................................................................. 50 2.1.6.1 Independent contrasts ................................................................................................... 50 2.1.6.2 Detecting the phylogenetic signal: the K statistics ........................................................ 52 2.1.6.3 Pagel’s λ ........................................................................................................................ 54 2.2 Materials and methods ........................................................................................................ 55 2.2.1 Taxa occurrences and age estimation ............................................................................. 55 2.2.2 Body size and duration ..................................................................................................... 56 2.2.3 Species level and genus level phylogenies ..................................................................... 57 2.2.4 Geographical distances betw een taxa ............................................................................. 58 2.2.5 Occupancy computation and trajectory ............................................................................ 59 2.2.6 Geographic range computation and its trajectory ............................................................ 60 2.2.7 The hereditability of the traits ........................................................................................... 61 2.3 Results ................................................................................................................................. 62 2.3.1 Occupancy and Area trajectories ..................................................................................... 62 2.3.2 Tests for phylogenetic signal and PICs correlations ........................................................ 63 2.3.3 Range position and phylogeny ......................................................................................... 64 2.4 Discussion ........................................................................................................................... 67 Chapter 3 -Macroecology of the fossil mammal assemblages: the species accumulation over space and time .............................................................................................................................. 70 3.1 Introduction .......................................................................................................................... 70 3.1.2 The species-area relationship .......................................................................................... 71 3.1.2.1 The hypotheses about the species-area relationship ................................................... 73 3.1.2.2 Combining the “area per se” and habitat heterogeneity influences in the species-area relationship: species-energy and the choros models ................................................................ 77 3.1.3 The species-time relationship .......................................................................................... 79 3.1.3.1 The factors that shape the pattern ................................................................................ 81 3.1.4 STAR model: combining the effects of both area and time in species accumulation ..... 82 3.2 Material and Methods .......................................................................................................... 85 3.2.1 Setting the data for the analyses ...................................................................................... 85 3.2.2 STR calculation and the application of the correction factors ......................................... 87 3.2.3 Comparing slopes at different time periods ..................................................................... 88 II 3.2.4 The computation of the SAR ............................................................................................ 89 3.2.5 The STAR model .............................................................................................................. 90 3.3 Results ................................................................................................................................. 91 3.3.1 The SAR and the STR ...................................................................................................... 91 3.3.2 Slopes per time ................................................................................................................. 91 3.3.3 STAR models .................................................................................................................... 92 3.4 Discussion ........................................................................................................................... 96 3.4.1 The STR and SA R models .............................................................................................
Recommended publications
  • Mammalia, Cervidae) During the Middle Holocene in the Cave of Bizmoune (Morocco, Essaouira Region
    Quaternary International xxx (2015) 1e14 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint The last occurrence of Megaceroides algericus Lyddekker, 1890 (Mammalia, Cervidae) during the middle Holocene in the cave of Bizmoune (Morocco, Essaouira region) * Philippe Fernandez a, , Abdeljalil Bouzouggar b, c, Jacques Collina-Girard a, Mathieu Coulon d a Aix Marseille Universite, CNRS, MCC, LAMPEA UMR 7269, 13094, Aix-en-Provence, France b Institut National des Sciences de l'Archeologie et du Patrimoine, Rabat, Morocco c Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, D-04103 Leipzig, Germany d Aix Marseille Universite, CNRS, LAMES UMR 7305, 13094, Aix-en-Provence, France article info abstract Article history: During the course of archaeological test excavations carried out in 2007 in the cave of Bizmoune Available online xxx (Essaouira region, Morocco), seven archaeological layers yielding Pleistocene and Holocene artefacts and faunal remains were identified. In the layers C4, C3 and C2, respectively from the oldest to the most Keywords: recent, terrestrial Helicidae mollusk shells (Helix aspersa) were dated by 14C. These layers also contained Giant deer many fragments of eggshell, belonging to Struthio cf. camelus, associated with mammal remains such as Extinction Oryctolagus/Lepus, Gazella sp., Sus scrofa, Ammotragus lervia, Alcelaphus buselaphus, Equus sp., Pha- Holocene cochoerus aethiopicus and an undetermined Caprini. Among these remains, an incomplete mandible of North Africa Speciation Megaceroides algericus Lydekker, 1890 with M1 and M2 was found in layer C3. The 6641 to 6009 cal BP Palaeoecology time range attributed to this layer has provided the most recent date known so far for M.
    [Show full text]
  • 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.
    [Show full text]
  • Growth, Learning, Play and Attachment in Neanderthal Children
    This is a repository copy of The Cradle of Thought : Growth, Learning, Play and Attachment in Neanderthal children. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/83027/ Version: Submitted Version Article: Spikins, Penny orcid.org/0000-0002-9174-5168, Hitchens, Gail, Rutherford, Holly et al. (1 more author) (2014) The Cradle of Thought : Growth, Learning, Play and Attachment in Neanderthal children. Oxford Journal of Archaeology. pp. 111-134. ISSN 0262-5253 https://doi.org/10.1111/ojoa.12030 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ THE CRADLE OF THOUGHT: GROWTH, LEARNING, PLAY AND ATTACHMENT IN NEANDERTHAL CHILDREN Penny Spikins, Gail Hitchens, Andy Needham and Holly Rutherford Department of Archaeology University of York King’s Manor York YO1 7EP SUMMARY Childhood is a core stage in development, essential in the acquisition of social, practical and cultural skills. However, this area receives limited attention in archaeological debate, especially in early prehistory.
    [Show full text]
  • Bibliography
    Bibliography Many books were read and researched in the compilation of Binford, L. R, 1983, Working at Archaeology. Academic Press, The Encyclopedic Dictionary of Archaeology: New York. Binford, L. R, and Binford, S. R (eds.), 1968, New Perspectives in American Museum of Natural History, 1993, The First Humans. Archaeology. Aldine, Chicago. HarperSanFrancisco, San Francisco. Braidwood, R 1.,1960, Archaeologists and What They Do. Franklin American Museum of Natural History, 1993, People of the Stone Watts, New York. Age. HarperSanFrancisco, San Francisco. Branigan, Keith (ed.), 1982, The Atlas ofArchaeology. St. Martin's, American Museum of Natural History, 1994, New World and Pacific New York. Civilizations. HarperSanFrancisco, San Francisco. Bray, w., and Tump, D., 1972, Penguin Dictionary ofArchaeology. American Museum of Natural History, 1994, Old World Civiliza­ Penguin, New York. tions. HarperSanFrancisco, San Francisco. Brennan, L., 1973, Beginner's Guide to Archaeology. Stackpole Ashmore, w., and Sharer, R. J., 1988, Discovering Our Past: A Brief Books, Harrisburg, PA. Introduction to Archaeology. Mayfield, Mountain View, CA. Broderick, M., and Morton, A. A., 1924, A Concise Dictionary of Atkinson, R J. C., 1985, Field Archaeology, 2d ed. Hyperion, New Egyptian Archaeology. Ares Publishers, Chicago. York. Brothwell, D., 1963, Digging Up Bones: The Excavation, Treatment Bacon, E. (ed.), 1976, The Great Archaeologists. Bobbs-Merrill, and Study ofHuman Skeletal Remains. British Museum, London. New York. Brothwell, D., and Higgs, E. (eds.), 1969, Science in Archaeology, Bahn, P., 1993, Collins Dictionary of Archaeology. ABC-CLIO, 2d ed. Thames and Hudson, London. Santa Barbara, CA. Budge, E. A. Wallis, 1929, The Rosetta Stone. Dover, New York. Bahn, P.
    [Show full text]
  • (Im) Pulse Caprovis Savinii (Bovidae, Mammalia) Rediscovered: Horn Core
    Netherlands Journal of Geosciences — Geologie en Mijnbouw | 85 - 3 | 239 - 243 | 2006 Geo (Im) pulse Caprovis savinii (Bovidae, Mammalia) rediscovered: horn core finds of an Early Pleistocene antelope from the North Sea floor B. De Wilde Bochtenstraat 47, 9270 Laarne, Belgium. Email: [email protected] Manuscript received: March 2006; accepted: August 2006 Abstract For more than 120 years since the name Caprovis savinii was founded on the basis of a bovid horn core from the 'Forest Bed' at Overstrand (Norfolk, UK), only one other find has been assigned to this species. Recently, two horn cores and one horn core fragment of the species have been discovered at two sand and gravel sorting centres in the Netherlands. The bone-bearing sediments are exposed on the North Sea floor, just off the coast of Great Yarmouth (Norfolk, UK). By comparing fossil and extant taxa, a classification within the bovid tribe Antilopini is proposed. Based on the accompa­ nying fauna from the specific dredging area and the litho- and chronostratigraphy at Overstrand, C. savinii is placed within the Early Pleistocene. Keywords: bovid, dredging, Forest Bed, Yarmouth Roads Formation Introduction Newton (1882) founded the species Caprovis savinii on the basis of a single right horn core with part of the frontal bone, obtained from the 'Forest Bed' at Overstrand (Norfolk, UK). The horn core was in the collection of Mr. A.C. Savin, of which a large part is now stored in the Natural History Museum, London. It took nearly 90 years before another specimen was assigned to this species. Spencer (1970) mentions briefly his Harlingen discovery of a rolled left horn core of Caprovis savinii in a box full of broken bones collected by Mr.
    [Show full text]
  • Neogene and Quaternary Mammal Faunas of Thessaly*
    NEOGENE AND QUATERNARY MAMMAL FAUNAS OF THESSALY* by A. ATHANASSIOU ** I. INTRODUCTION The Province of Thessaly is situated in Central Greece. It is a mainly plain geographical area (the most extensive low relief area in the Greek peninsula), delimited in the North by Olympus Mountain, in the West by Pfndos mountain range, in the East by the Aegean Sea and in the South by Orthrys mountain range. Alluvial deposits that form extensive plains cover most of the eastern and central part of the region. A hill range made of tertiary gravel beds and directed NW-SE, divides these plains into two regions: the plain of Larissa in the East and the plain of Trfkala-Kardftsa in the West. Two smaller basins, those of Volos and Almyros, extend in SE Thessaly. The westernmost part of the province is mountainous, formed by alpine and molassic formations of Mesozoic and Neogene age respectively. In the southwestern part the long peninsula of P61ion Mountain forms the wide and rather closed Pagassetic Gulf. 11. GEOLOGY The Thessalian mountain ranges are placed in the Pelagonic and Pfndos geotectonic zones, which have a NW-SE direction. The Pelagonic is a very wide zone that covers a very extensive area of Northern and Central Greece. It is usually divided to several minor zones, either metamorphic or not. Most of those zones are of Triassic-lurassic age and they are covered by a transgression series that begins in Late Cretaceous (Cenomanian). The stratigraphic columns of the Pelagonic zone consist of Late Palaeozoic and Mesozoic metamorphic, semimetamorphic or sedimentary rocks, as gneiss, amphibolites, slates and limestones.
    [Show full text]
  • La Préhistoire : Les Premiers Humains En « France »
    h Chapitre 1 La préhistoire : les premiers humains en « France » Ce que vous allez apprendre • La présence de l’être humain en France est très ancienne : plus de 1,5 million d’années. • L’histoire de la préhistoire est née en France au XIXe siècle. • La France est riche de sites préhistoriques célèbres, de Lascaux à Carnac. • Les sociétés préhistoriques ont modifié la faune, la flore et les paysages. I. À LA DÉCOUVERTE D’UN MONDE LONGTEMPS IGNORÉ : LA PRÉHISTOIRE Histoire des découvertes préhistoriques Si l’existence des hommes de la préhistoire est aujourd’hui une évidence pour la grande majorité de nos contemporains, de même que l’ancienneté de l’humanité en millions d’années, ces connaissances sont fort récentes à l’échelle de la longue durée des sociétés humaines. Jusqu’au milieu du XIXe siècle, à de rares exceptions, les Européens n’imaginent même pas la possibilité d’une humanité antérieure à la Genèse (premier livre de la Bible). L’histoire de l’humanité est vieille de 4 000 à 5 000 ans, et pas davantage, estiment alors les savants. Les Églises chrétiennes, tout comme d’ailleurs le judaïsme et l’islam, s’en tiennent rigoureusement à ce qu’enseignent les textes sacrés sur les origines du monde et de l’humanité : la Torah pour les juifs, la Bible pour les chrétiens, le Coran pour les musulmans. Les trois religions monothéistes enseignent que l’univers, la Terre, le monde vivant et le genre humain ont été créés par Dieu, en fort peu de temps. L’idée d’une évolution de la vie et notamment de l’humanité sur des millions ou des milliards d’années est littéralement inconcevable pour les hommes de religion et pour les Européens jusqu’au milieu du XIXe siècle.
    [Show full text]
  • Fossil Deer Assemblage from Sea Bottom of Bisan
    "FOSSIL DEER ASSEMBLAGE FROM SEA BOTTOM OF BISAN-SETO AREA WITH SPECIAL REFERENCE TO THEIR STRATIGRAPHIC POSITIONS (PLEISTOCENE DEER FAUNA IN SETO INLAND SEA, ----PART III)" 著者 "OTSUKA Hiroyuki" journal or 鹿児島大学理学部紀要. 地学・生物学 publication title volume 22 page range 55-87 別言語のタイトル 備讃瀬戸の海底に於ける鹿類化石群集-特にその産 出相に関連して (瀬戸内海の第四期鹿類化石群-そ の3) URL http://hdl.handle.net/10232/5980 FOSSIL DEER ASSEMBLAGE FROM SEA BOTTOM OF BISAN-SETO AREA WITH SPECIAL REFERENCE TO THEIR STRATIGRAPHIC POSITIONS (PLEISTOCENE DEER FAUNA IN SETO INLAND SEA, ----PART III) 著者 OTSUKA Hiroyuki journal or 鹿児島大学理学部紀要. 地学・生物学 publication title volume 22 page range 55-87 別言語のタイトル 備讃瀬戸の海底に於ける鹿類化石群集-特にその産 出相に関連して (瀬戸内海の第四期鹿類化石群-そ の3) URL http://hdl.handle.net/10232/00001718 Rep. Fac. Sci., Kagoshima Univ.,(Earth Sci. & Biol.) No. 22, p.55-87, 1989. FOSSIL DEER ASSEMBLAGE FROM SEA BOTTOM OF BISAN-SETO AREA WITH SPECIAL REFERENCE TO THEIR STRATIGRAPHIC POSITIONS PLEISTOCENE DEER FAUNA IN SETO INLAND SEA, 一一-PART I Hiroyuki Otsuka (Received August 30, 1989) Abstract This paper presents the results of paleontological and geological studies of fossil deer fauna collected from the sea bottom of the Bisan-seto area, in the eastern part of the Seto Inland Sea, West Japan. The fossil deer assemblages in this area are associated with abundant mammals of forest- to grassland habitats such as Naumann's elephant (Palaeoloxodon naumanni) and also with a few Stegodon, wild ox, rhino and water buffalo specimens. As a result of the present study, nine species fossil deer belonging to the family Cervidae were distinguished, among which six species are referred to the genus Cervus and others to the genus Elaphurus and SinamegaFeros.
    [Show full text]
  • New Data on the Equus Stenonis Cocchi, 1867 from the Late Pliocene Locality of Sésklo (Thessaly, Greece)
    New data on the Equus stenonis Cocchi, 1867 from the late Pliocene locality of Sésklo (Thessaly, Greece) Athanassios ATHANASSIOU University of Athens, Department of Historical Geology and Palaeontology, Panepistimiopolis, 157 84 Athens (Greece) [email protected] Athanassiou A. 2001. — New data on the Equus stenonis Cocchi, 1867 from the late Pliocene locality of Sésklo (Thessaly, Greece). Geodiversitas 23 (3): 439-469. ABSTRACT The equid material from the late Pliocene locality of Sésklo (Thessaly, Greece) is described and compared in this article. It belongs to a large and KEY WORDS fairly stout Equus stenonis form, which shares many morphological characters Mammalia, with the species samples from Saint-Vallier, La Puebla de Valverde and Perissodactyla, Equidae, Olivola, as well as with already known Equus stenonis samples from other Equus stenonis, Greek localities (Dafneró, Vólax). Its main features are the big skull and late Pliocene, limbs, the short protocones and the very simple enamel plication in the teeth. Villafranchian, Thessaly, Large sized and relatively robust stenonid horses are common elements of the Greece. late Pliocene faunas of Greece. RÉSUMÉ Nouvelles données sur l ’Equus stenonis Cocchi, 1867 de la localité pliocène de Sésklo (Thessalie, Grèce). Dans l’article présent, l’équidé de la localité pliocène de Sésklo (Thessalie, Grèce) est décrit et comparé. Il appartient à une forme d’Equus stenonis large MOTS CLÉS et assez robuste, qui a des caractères morphologiques communs avec les Mammalia, échantillons de Saint-Vallier, La Puebla de Valverde et Olivola, ainsi qu’avec Perissodactyla, Equidae, des échantillons déjà connus d’autres localités grecques (Dafneró et Vólax).
    [Show full text]
  • An Early Modern Human Outside Africa
    City University of New York (CUNY) CUNY Academic Works Publications and Research Lehman College 2019 An early modern human outside Africa Eric Delson CUNY Lehman College How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/le_pubs/307 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] RESEARCH NEWS & VIEWS are too incomplete for their status as H. sapiens to be certain. Could molecular approaches be Apidima Denisova Neanderthal used to determine the species they are from? Greece Russia presence Jinniushan 210 kyr (Earliest known 195–52 kyr It is not always possible to recover DNA from 450–35 kyr China European H. sapiens) 147–91 kyr ancient fossils. However, analysing ancient 250–150 kyr 170 kyr proteins preserved in fossils, a method termed Misliya palaeo proteomics, is starting to be used to Israel Xiahe 194–177 kyr China Dali identify species (see go.nature.com/2xkosom). 160 kyr China Jebel Irhoud Compared with analysis of ancient DNA, 250–150 kyr Morocco Zuttiyeh palaeo proteomics requires less specialized Israel 315 kyr Hualongdong handling of the fossil to prevent contamination. 500–200 kyr China It was recently used14 to analyse a fossilized 300 kyr Olorgesailie Hathnora jaw found in China that is approximately Kenya India 160,000 years old, enabling the specimen to Stone tools 250–100 kyr 320 kyr be identified as an enigmatic hominin called a Denisovan, whose scarce fossils have also been Florisbad found at Denisova Cave in Siberia.
    [Show full text]
  • An Anthropological Assessment of Neanderthal Behavioural Energetics
    DEPARTMENT OF ARCHAEOLOGY, CLASSICS & EGYPTOLOGY An Anthropological Assessment of Neanderthal Behavioural Energetics. Thesis submitted in accordance with the requirements of the University of Liverpool for the Degree of Doctor in Philosophy by Andrew Shuttleworth. April, 2013. TABLE OF CONTENTS……………………………………………………………………..i LIST OF TABLES……………………………………………………………………………v LIST OF FIGURES…………………………………………………………………………..vi ACKNOWLEDGMENTS…………………………………………………………………...vii ABSTRACT…………………………………………………………………………………viii TABLE OF CONTENTS 1. INTRODUCTION...........................................................................................................1 1.1. Introduction..............................................................................................................1 1.2. Aims and Objectives................................................................................................2 1.3. Thesis Format...........................................................................................................3 2. THE NEANDERTHAL AND OXYEGN ISOTOPE STAGE-3.................................6 2.1. Discovery, Geographic Range & Origins..............................................................7 2.1.1. Discovery........................................................................................................7 2.1.2. Neanderthal Chronology................................................................................10 2.2. Morphology.............................................................................................................11
    [Show full text]
  • 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.
    [Show full text]