DOCSLIB.ORG

The Tectonic Setting of the Caribbean Region: Key in the Radical Late Cretaceous-Early Paleocene South American Land-Mammal Turnover

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Tectonic Setting of the Caribbean Region: Key in the Radical Late Cretaceous-Early Paleocene South American Land-Mammal Turnover E. Díaz-Martínez e I. Rábano (Eds.), 4th European Meeting on the Palaeontology and Stratigraphy of Latin America Cuadernos del Museo Geominero, nº 8. Instituto Geológico y Minero de España, Madrid, 2007. ISBN 978-84-7840-707-1 © Instituto Geológico y Minero de España THE TECTONIC SETTING OF THE CARIBBEAN REGION: KEY IN THE RADICAL LATE CRETACEOUS-EARLY PALEOCENE SOUTH AMERICAN LAND-MAMMAL TURNOVER E. Ortiz-Jaureguizar and R. Pascual Facultad de Ciencias Naturales y Museo, Paseo del Bosque s/n, B1900FWA La Plata, Argentina. [email protected], [email protected] Keywords: Mesozoic, Cenozoic, paleogeography, mammal turnover, immigration, extinction. INTRODUCTION Earlier the Caribbean Region, and later Central America, has played a crucial role in the mutual bio- geography and evolution of the North and South American faunas. Emplacement of the Panamanian isth- mian bridge some 3 Ma ago was the essential geological event that triggered the so called Great American Biotic Interchange (GABI; see Stehli and Webb, 1985). Today we know that with the exception of the caviomorph rodents and platyrrhine primates (arrived from Africa during Late Eocene-Early Oligocene) the mammals recorded in South America before the GABI (i.e., marsupials, xenarthrans, and “ungulates”) were endemic from South America but descendant of North American immigrants. They arrived from the Late Cretaceous on, during the successive stages of the Caribbean and Central American differentiation (see Pascual and Ortiz-Jaureguizar, in press, and references therein). The historical knowledge of those sup- posed oldest (Paleogene and partially Neogene) South American mammals was first reviewed by Simpson (1940, 1950, 1980 and references therein). But neither Simpson nor contemporary authors noticed that those supposedly oldest South American mammals were representing just the last third of the South American mammal history. But in 1982, Bonaparte and colleagues discovered in Patagonia the first unquestionable Late Cretaceous mammals, together with hadrosaurs dinosaurian remains, which permit- ted to have the first approximated idea of the compositional status of a South American Cretaceous land- mammal.community (see Bonaparte, 1996 and references therein). Furthermore, these discoveries (as well as other discoveries in Patagonian Early Paleocene land-mammal bearing beds (see Pascual and Ortiz- Jaureguizar, in press and references therein) led Pascual (see 2006 and references therein) to recognized that the whole history of South American mammals can be divided into two quite distinct and unrelated episodes: The Gondwanan Episode (?Late Triassic-Late Cretaceous) and The South American Episode (Early Paleocene-Recent), represented by phylogenetically unrelated actors, that respectively dwelt in likewise dis- tinct sceneries. Those mammals of the Gondwanan Episode were almost exclusively Gondwanan non- and pre-tribosphenics mammals, while those characterizing the South American Episode were just Theria, most- ly immigrants from North America with a Laurasian history. Both Episodes were separated by a critical lat- est Cretaceous-earliest Paleocene hiatus, during which South American land-mammals communities expe- 301 E. Ortiz-Jaureguizar and R. Pascual rienced a notably evolutionary change: the almost complete extinction of the Gondwanan mammals, and the arrival and radiation of the North American marsupials and placentals (see Pascual, 2006; Pascual and Ortiz-Jaureguizar, in press, and references therein). On the basis of the last paleontological and geological evidence, in this communication we analyse the compositional changes recorded in the Late Cretaceous-Paleocene South American land-mammal faunas in the context of the tectonic setting of the Caribbean Region, as one very important contributing cause of latest Cretaceous-Early Paleocene total extinction of the South American Gondwanan land-mammals. THE SOUTH AMERICAN LAND-MAMMAL FAUNAS DURING THE LATE CRETACEOS-PALEOCENE SPAN The very first steps of the history of South American mammals took origin ca.130 Ma, when the South American plate, still connected to the Antarctic Peninsula, began to drift away from the African-Indian plate. Most of the Mesozoic history of the South American mammals is still unknown, and we only have a very few and enigmatic taxa (i.e., a Jurassic Australosphenida and an Early Cretaceous Prototribosphenida) that pose more evolutionary and biogeographic questions that answers (Pascual and Ortiz-Jaureguizar, in press). The best known South American Mesozoic land-mammals were found in Late Cretaceous (Campanian-Maastrichtian) Patagonian beds. They are represented by several non- and pre-tribosphenic endemic genera (one “plagiaulacidan” multituberculate, two gondwanatherians, one docodont, one “tri- conodont”, one “symmetrodont” and ten dryolestoids), that are relict of pangeic lineages, which were extinct in coeval beds of Laurasia (see Kielan-Jaworowska et al., 2004; Pascual and Ortiz Jaureguizar, in press). The total absence of tribosphenic mammals in Patagonian Late Cretaceous beds (well diversified in coeval Laurasian beds), and the advanced morphology and endemism of non-tribosphenic and pre-tri- bosphenic ones was interpreted as an evidence of the long isolation of South America from the North American continent (see Bonaparte, 1996; Kielan-Jaworowska et al., 2004; Pascual, 2006; Pascual and Ortiz-Jaureguizar, in press). But the so recently finding of a new genus and species of a ?cimolodontan multituberculate, the first found in those Late Cretaceous Patagonian beds (Kielan-Jaworowska et al., 2007) could change, at least in part, the classic scenario of a completely isolated South American land- mammal fauna. According to Kielan-Jaworowska et al. (2007), the new multituberculate is a North American immi- grant that could be arrived to South America during Early Cretaceous or Late Cretaceous. The hypothesis of an Early Cretaceous arrival is supported by the presence of some morphological features that are shared with “Plagiaulacida”, a multituberculate suborder which did not cross the Early-Cretaceous-Late Cretaceous boundary. But there is not fossil evidence among the South American vertebrates of an arrival of North American immigrants during Early Cretaceous. Additionally, to us this is not the only cimolodon- tan multituberculate that shows a mosaic of plagiaulacidan (plesiomorphic) and cimolodontan (apomor- phic) characters. The “Paracimexomys group” (i.e., the most plesiomorphic, informal group of Cimolodonta) share some molar features with some “Plagiulacida” (i.e., Plagiaulacidae and Eobaataridae). They were recorded in Early Cretaceous (Aptian/Albian) to Late Cretaceous (Maastrichtian) beds of North America, as well as in Late Cretaceous (?Maastrichtian) ones of Europe. (Kielan-Jaworowska et al., 2004). Consequently, we can also suppose that the new Patagonian taxon was a South American representative of a clade of basal cimolodontans (not yet recorded in the “classical” Late Cretaceous North American 302 THE TECTONIC SETTING OF THE CARIBBEAN REGION: KEY IN THE RADICAL LATE CRETACEOUS-EARLY PALEOCENE SOUTH AMERICAN LAND-MAMMAL TURNOVER Figure 1. Cretaceous paleogeographic reconstruction of Caribbean region, mdified from Iturralde-Vinent (2004) and Iturralde- Vinent and McPhee (2004). A, Early Cretaceous (125-120 Ma); B, Late Cretaceous (ca. 70 Ma). References: Black areas: emerged lands; Grey areas: shallow sea; White areas: deep sea; White squares: volcanoes. mammal-bearing beds) that arrived to South America during Late Cretaceous. Additionally, all the paleo- geographic reconstructions of the Caribbean-“Central America” area (Fig. 1 and see below) favor a Late Cretaceous inter-American vetebrate exchange. The Late Cretaceous migratory events suggest that there was some kind of inter-American dry land connection by the end of the Cretaceous, which for sure was transitory (geologically speaking) and throughout the incipient Caribbean Sea. THE GEOLOGIC AND TECTONIC SETTING OF THE CARIBBEAN REGION The creation of the Caribbean Plate was probably the most important aspect of a timing sequence for a link between the North and South America land masses (Smith, 1985). The general geologic and tectonic setting of the Caribbean region is crucial to evaluating the very first recorded interchange of land verte- brates between North and South America during the Late Cretaceous. As Case et al. (2004) stated regard- ing the marsupials, and the contribution to an appraisal of mammalian dispersal of other groups of land vertebrates (e.g., the dispersal history of hadrosaurine dinosaurs and booid snakes; see Estes and Báez, 1985; Gayet et al., 1992), the window of dispersal seems to begin in the Campanian, to be most likely in the Maastrichtian, and to wane in the Paleocene. These authors, essentially based on the fossil evidence afforded by fossil marsupials, concluded that “…the dispersal probability is best proposed as having been a sweepstakes to a relatively strong filter”, as Simpson (1953) proposed. To them, the Aves Ridge could have provided the dried dispersal route for land vertebrates between North and South America during the Campanian-Maastrichtian span. On the contrary, Iturralde-Vinent and Mac Phee (1999, 2004) concluded that no permanent landmasses were present in the Caribbean prior to the middle Eocene. However, to these authors the NW margin of the Caribbean Plate was the area where emerged volcanic islands were aligned between North and South America
Load more

Recommended publications
  • Dome-Headed, Small-Brained Island Mammal from the Late Cretaceous of Romania
    Dome-headed, small-brained island mammal from the Late Cretaceous of Romania Zoltán Csiki-Savaa,1, Mátyás Vremirb, Jin Mengc, Stephen L. Brusatted, and Mark A. Norellc aLaboratory of Paleontology, Faculty of Geology and Geophysics, University of Bucharest, 010041 Bucharest, Romania; bDepartment of Natural Sciences, Transylvanian Museum Society, 400009 Cluj-Napoca, Romania; cDivision of Paleontology, American Museum of Natural History, New York, NY 10024; and dSchool of GeoSciences, Grant Institute, University of Edinburgh, EH9 3FE Edinburgh, United Kingdom Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved March 26, 2018 (received for review January 20, 2018) The island effect is a well-known evolutionary phenomenon, in describe the anatomy of kogaionids in detail, include them in a which island-dwelling species isolated in a resource-limited envi- comprehensive phylogenetic analysis, estimate their body sizes, ronment often modify their size, anatomy, and behaviors compared and present a reconstruction of their brain and sense organs. with mainland relatives. This has been well documented in modern This species exhibits several features that we interpret as re- and Cenozoic mammals, but it remains unclear whether older, more lated to its insular habitat, most notably a brain that is sub- primitive Mesozoic mammals responded in similar ways to island stantially reduced in size compared with close relatives and habitats. We describe a reasonably complete and well-preserved skeleton of a kogaionid, an enigmatic radiation of Cretaceous island- mainland contemporaries, demonstrating that some Mesozoic dwelling multituberculate mammals previously represented by frag- mammals were susceptible to the island effect like in more mentary fossils.
    [Show full text]
  • Enamel Ultrastructure of Multituberculate Mammals: an Investigation of Variability
    CO?JTRIBI!TIONS FROM THE MUSEUM OF PALEOK.1-OLOCiY THE UNIVERSITY OF MICHIGAN VOL. 27. NO. 1, p. 1-50 April I, 1985 ENAMEL ULTRASTRUCTURE OF MULTITUBERCULATE MAMMALS: AN INVESTIGATION OF VARIABILITY BY SANDRA J. CARLSON and DAVID W. KRAUSE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRlBUTlONS FROM THE MUSEUM OF PALEON I OLOGY Philip D. Gingerich, Director Gerald R. Smith. Editor This series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan, 48109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN Vol . 27, no. 1, p. 1-50, pub1 ished April 1, 1985, Sandra J. Carlson and David W. Krause (Authors) ERRATA Page 11, Figure 4 caption, first line, should read "(1050X)," not "(750X)." ENAMEL ULTRASTRUCTURE OF MULTITUBERCULATE MAMMALS: AN INVESTIGATION OF VARIABILITY BY Sandra J. Carlsonl and David W. Krause' Abstract.-The nature and extent of enamel ultrastructural variation in mammals has not been thoroughly investigated. In this study we attempt to identify and evaluate the sources of variability in enamel ultrastructural patterns at a number of hierarchic levels within the extinct order Multituberculata.
    [Show full text]
  • Multituberculate Mammals from the Wahweap
    MULTITUBERCULATE MAMMALS FROM THE WAHWEAP (CAMPANIAN, AQUILAN) AND KAIPAROWITS (CAMPANIAN, JUDITHIAN) FORMATIONS, WITHIN AND NEAR GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, SOUTHERN UTAH Jeffrey G. Eaton Department of Geosciences Weber State University Ogden, UT 84408-2507 phone: (801) 626-6225 fax: (801) 626-7445 e-mail: [email protected] Cover photo by author: Powell Point in “The Blues,” the early Tertiary Claron Formation on the horizon and the Kaiparowits Formation in the foreground. ISBN 1-55791-665-9 Reference to any specific commercial product by trade name, trademark, or manufacturer does not constitute endorsement or recommendation by the Utah Geological Survey MISCELLANEOUS PUBLICATION 02-4 UTAH GEOLOGICAL SURVEY a division of 2002 Utah Department of Natural Resources STATE OF UTAH Michael O. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Robert Morgan, Executive Director UTAH GEOLOGICAL SURVEY Richard G. Allis, Director UGS Board Member Representing Robert Robison (Chairman) ...................................................................................................... Minerals (Industrial) Geoffrey Bedell.............................................................................................................................. Minerals (Metals) Stephen Church .................................................................................................................... Minerals (Oil and Gas) E.H. Deedee O’Brien .......................................................................................................................
    [Show full text]
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • Lhiwanj[Fuseum
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by American Museum of Natural History Scientific... >lhiwanJ[fuseum PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2 2 26 AUGUST I7, I 965 First Evidence of Tooth Replacement in the Subclass Allotheria (Mammalia) BY FREDERICK S. SZALAY1 INTRODUCTION Multituberculates (the only known order of the subclass Allotheria) are abundantly represented in Mesozoic and Paleocene mammal locali- ties. Of the relatively large number of multituberculate mandibles and maxillae known up to the summer of 1963, not one showed a tooth in the process of replacement. Young specimens were known with less fully erupted teeth (Jepsen, 1940, p. 245; Clemens, 1963, p. 34), but it has not been possible before to demonstrate diphyodonty in multituberculates. With a now-standardized washing technique used for obtaining ver- tebrate microfossils (Hibbard, 1949; McKenna, 1962), a vertebrate paleontology field party of the American Museum of Natural History collected a large assemblage of vertebrate fossils during the summer of 1963. The collection was of approximately Torrejonian age from the eastern part of the Washakie Basin in southern Wyoming.2 Among the large number of multituberculates represented, a fragmentary left man- dible (A.M.N.H. No. 83003) is one of the two specimens described in the present paper that supply the first direct evidence of allotherian tooth replacement. The deciduous lower incisor is still present in the mandible, 1 Department of Zoology, Columbia University, New York, New York.
    [Show full text]
  • Mammals from the Mesozoic of Mongolia
    Mammals from the Mesozoic of Mongolia Introduction and Simpson (1926) dcscrihed these as placental (eutherian) insectivores. 'l'he deltathcroids originally Mongolia produces one of the world's most extraordi- included with the insectivores, more recently have narily preserved assemblages of hlesozoic ma~nmals. t)een assigned to the Metatheria (Kielan-Jaworowska Unlike fossils at most Mesozoic sites, Inany of these and Nesov, 1990). For ahout 40 years these were the remains are skulls, and in some cases these are asso- only Mesozoic ~nanimalsknown from Mongolia. ciated with postcranial skeletons. Ry contrast, 'I'he next discoveries in Mongolia were made by the Mesozoic mammals at well-known sites in North Polish-Mongolian Palaeontological Expeditions America and other continents have produced less (1963-1971) initially led by Naydin Dovchin, then by complete material, usually incomplete jaws with den- Rinchen Barsbold on the Mongolian side, and Zofia titions, or isolated teeth. In addition to the rich Kielan-Jaworowska on the Polish side, Kazi~nierz samples of skulls and skeletons representing Late Koualski led the expedition in 1964. Late Cretaceous Cretaceous mam~nals,certain localities in Mongolia ma~nmalswere collected in three Gohi Desert regions: are also known for less well preserved, but important, Bayan Zag (Djadokhta Formation), Nenlegt and remains of Early Cretaceous mammals. The mammals Khulsan in the Nemegt Valley (Baruungoyot from hoth Early and Late Cretaceous intervals have Formation), and llcrmiin 'ISav, south-\vest of the increased our understanding of diversification and Neniegt Valley, in the Red beds of Hermiin 'rsav, morphologic variation in archaic mammals. which have heen regarded as a stratigraphic ecluivalent Potentially this new information has hearing on the of the Baruungoyot Formation (Gradzinslti r't crl., phylogenetic relationships among major branches of 1977).
    [Show full text]
  • Replica a Los Comentarios De Canudo Et Al. a «Asociacion
    Estudios Geol., 60: 53-59 (2004) REPLICA A LOS COMENTARIOS DE CANUDO ET AL. A «ASOCIACION FAUNISTICA DE VERTEBRADOS MESOZOICOS DE LA LOCALIDAD DE GALVE (TERUEL)>> [ESTUDIOS GEOL., 58 (2002), 189-193] B. Sánchez Hernández * Una vez analizados los Comentarios a mi artículo lizó en el año 1958, difícilmente pudo llevarse a realizados por Canudo, Ruiz-Omeñaca, Barco, cabo el trabajo de campo, selección del área correc­ Cuenca-Bescós y Royo, sorprende el exceso de celo ta de prospección, estudio del material hallado y para descalificar un artículo que nunca pretendió excavación de la zona atendiendo a los resultados otra cosa -como se especifica claramente en su de las etapas anteriores señaladas, estudio del mate­ introducción- que ser una actualización temporal rial hallado, redacción del artículo y publicación de de la «Lista faunística de los vertebrados de Galve éste en ese mismo año. Parece razonable que todo (Teruel)>> realizada por los investigadores Buscalio­ ese trabajo le llevara un poco más de tiempo, posi­ ni y Sanz (1987). En esta publicación se pretende blemente años. Cabe señalar que algunos de estos clarificar algunas afirmaciones contenidas en dichos mismos autores aceptaban fechas aún anteriores Comentarios. para esa actividad, como se puede comprobar en la Guía del Parque Paleontológico de Galve (Teruel), cuyos autores son J. 1. Canudo, G. Cuenca Bescós y Fecha de inicio del estudio de los yacimientos de J. 1. Ruiz Omeñaca (1996), en donde señalan «Este Galve yacimiento (el de Las Zabacheras) lo encontró José María (se refieren a D. José M.ª Herrero, antiguo Canudo et al. afirman que es incorrecta mi afir­ propietario de la colección Herrero donada al mación del comienzo de los estudios sobre los Museo de Galve) a la orilla de la carretera de depósitos de Galve a principios del siglo xx, así entrada al pueblo, construida sobre el año 1934, y como la fecha de 1950 para el comienzo de las cuyo trazado cortó el yacimiento y cuantos materia­ excavaciones.
    [Show full text]
  • A Aardvark, 96 Abderites, 15, 162 Abderitidae, 11, 159, 200 Aboriginal, 15, 17 Adamantina, 79, 83 Africa, 79, 96, 116, 127, 130
    Index A Antarctic Circumpolar Current (ACC), 126, Aardvark, 96 188, 210 Abderites, 15, 162 Antarctic Counter Current, 104 Abderitidae, 11, 159, 200 Antarctic Peninsula, 12, 80, 83, 97, 109, Aboriginal, 15, 17 113–116, 165, 187, 216 Adamantina, 79, 83 Antarctic Region, 113, 133 Africa, 79, 96, 116, 127, 130, 141 Antarctodonas, 110 Afrotemperate Region, 133 Antechinus, 56 Afrothere, 96 Aonken Sea, 139 Afrotheria, 96, 97 Aptian, 79, 98, 129 Alamitan, 83, 90, 95, 141, 211 Aquatic, 130 Alchornea, 113 Araceae, 113 Alcidedorbignia, 94 Araucaria, 130 Alisphenoid, 10, 11 Arboreal, 6, 12, 38, 58–61, 64, 65 Allen, 80 Archaeodolops, 195 Allenian, 211 Archaeohyracidae, 143 Allotherian, 212 Archaeonothos, 109 Allqokirus, 95, 214 Arctodictis, 166 Alphadelphian, 214 Arecaceae, 113 Altiplano, 127 Argentina, 13, 17, 19, 22, 61, 80, 83, 95, 107, Altricial, 203 112, 116, 130, 135, 136, 138, 157 Ameghinichnus, 140 Argentodites, 212 Ameridelphia, 157, 165, 166, 186, 192, 195 Argyrolagidae, 13, 158, 196, 220 Ameridelphian, 91, 95, 106, 107, 110, 157, Argyrolagoidea, 13, 143, 195, 201, 220 166, 200, 213, 215, 216 Argyrolagus, 158, 220 Amphidolops, 195, 200 Arid diagonal, 135, 136, 138 Anachlysictis, 23, 161 Arminiheringia, 166, 194 Andean Range, 133 A1 scenario, 138 Andean Region, 127, 132, 133, 135, 136 Ascending ramus, 170 Andes, 12, 127 Asia, 6, 127, 156, 202 Andinodelphys, 95, 157, 159 Astragalar, 10 Angiosperm, 114, 115, 129, 190 Astrapotheria, 3 Angular process, 10, 11, 171, 175 Atacama Desert, 130, 133, 136 Animalivore, 47 Atlantic Forest, 61, 130 Animalivorous, 47 Atlantic Ocean, 137 Ankle bone, 96, 107 Atlantogenata, 97 Antarctica, 8, 12, 79, 98–100, 104, 109, 112, Australasia, 218 115, 116, 126, 127, 133, 135, 137, 210, 220 © Springer Science+Business Media Dordrecht 2016 227 F.J.
    [Show full text]
  • La Cantalera: an Exceptional Window Onto the Vertebrate Biodiversity of the Hauterivian-Barremian Transition in the Iberian Peninsula
    ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 36 (2) 2010: 205-224 doi:10.5209/rev_JIGE.2010.v36.n2.8 La Cantalera: an exceptional window onto the vertebrate biodiversity of the Hauterivian-Barremian transition in the Iberian Peninsula La Cantalera: una excepcional ventana a la biodiversidad del tránsito Hauteriviense- Barremiense en la Península Ibérica J.I. Canudo1, J.M. Gasca1, M. Aurell2, A. Badiola1, H.-A. Blain3, P. Cruzado-Caballero1, D. Gómez- Fernández1, M. Moreno-Azanza1, J. Parrilla1, R. Rabal-Garcés1, J. I. Ruiz-Omeñaca1,4 1Grupo Aragosaurus (http://www.aragosaurus.com). Universidad de Zaragoza. 50009 Zaragoza, Spain. [email protected], [email protected], [email protected], [email protected], [email protected], [email protected], [email protected] 2Estratigrafía. Universidad de Zaragoza. 50009 Zaragoza. Spain. [email protected] 3Institut Català de Paleoecologia Humana y Evolució Social (Unitat asociada al CSIC). Universitat Rovira i Virgili. 43005 Tarragona. Spain. [email protected] 4Museo del Jurásico de Asturias (MUJA). 33328 Colunga. Asturias. Spain. [email protected] Received: 15/11/09 / Accepted: 30/06/10 Abstract La Cantalera is an accumulation site for fossil vertebrates consisting mainly of teeth and isolated postcranial remains. It has the greatest vertebrate biodiversity of any site from the Hauterivian-Barremian transition in the Iberian Peninsula. Up to now, 31 vertebrate taxa have been recognized: an osteichthyan (Teleostei indet.), two amphibians (Albanerpetonidae indet. and Discoglos- sidae indet.), a chelonian (Pleurosternidae? indet.), a lizard (Paramacellodidae? indet.), four crocodylomorphs (cf. Theriosuchus sp., Bernissartiidae indet., Goniopholididae indet., cf.
    [Show full text]
  • Patagonian Bats
    Mammalia 2020; 84(2): 150–161 Analía Laura Giménez* and Mauro Ignacio Schiaffini Patagonian bats: new size limits, southernmost localities and updated distribution for Lasiurus villosissimus and Myotis dinellii (Chiroptera: Vespertilionidae) https://doi.org/10.1515/mammalia-2019-0024 (i.e. intra and interspecific interactions) and abiotic Received March 10, 2019; accepted June 7, 2019; previously published factors (i.e. temperature, altitude, precipitation and pro- online July 16, 2019 ductivity), together with dispersal ability capacities and the evolutionary history of each lineage (Gaston 2003, Cox Abstract: Vespertilionid species are widely distributed and Moore 2005, Soberón and Peterson 2005). As abiotic in South America. They are highly diverse, with physio- factors are not evenly distributed in space or time, they logical and behavioral adaptations which allow them to shape the borders of species’ distributions trough extreme extend their distributions into temperate areas. In Patago- values (e.g. minimum or maximum temperatures, dry or nia, this family is represented by seven species in three humid areas), which in turn influence resource availabil- genera (Histiotus, Lasiurus and Myotis). In this study, we ity and impose limits to reproduction and survival (Mackey analyzed the distribution of two vespertilionid species, and Lindenmayer 2001, Gaston 2003). In this way, those Lasiurus villosissimus and Myotis dinellii, including new areas with more favorable abiotic (and biotic) conditions southernmost records, and their relationship with envi- will show the highest relative abundance, while records ronmental variables. Two different spatial scales were will become more scarce and more far away from each analyzed: a continental approach for species distribu- other toward the borders of a species’ distribution (Brown tion analyses (South America), and local trapping of bats 2003 and references therein).
    [Show full text]
  • «How to Write a Scientific Paper»
    The following material is part of the On-line Workshop «How to write a scientific paper» The workshop contains 24 h of video-recorded classes, with numerous practical examples that will help you publish an outstanding scientific paper. Visit: http://www.casadestudiselpont.eu/sciencelandingeng.html Casa de Lletres Academic Editing Services [email protected] www.casadelletres.eu Hypothesis- testing paper Casa de Lletres Academic Editing Services [email protected] www.casadelletres.eu Evolution of herbivory in Drosophilidae linked to loss of behaviors, antennal responses, odorant receptors, and ancestral diet Benjamin Goldman-Huertasa, Robert F. Mitchellb,c, Richard T. Lapointa,c, Cécile P. Faucherb,d, John G. Hildebrandb,1, and Noah K. Whitemana,1 Departments of aEcology and Evolutionary Biology and bNeuroscience, and cCenter for Insect Science, University of Arizona, Tucson, AZ 85721; and dLife Science Solutions, Thermo Fisher Scientific, 64293 Darmstadt, Germany Contributed by John G. Hildebrand, January 4, 2015 (sent for review August 29, 2014; reviewed by Ewald Grosse-Wilde, Benjamin Prud’homme, and Michael G. Ritchie) Herbivory is a key innovation in insects, yet has only evolved in one- been rarely shown but occurs in nematodes, although their olfactory third of living orders. The evolution of herbivory likely involves systems are distinct from insects (14). Families of mammalian ol- major behavioral changes mediated by remodeling of canonical factory receptor proteins have been remodeled during transitions to chemosensory modules. Herbivorous flies in the genus Scaptomyza flight, aquatic lifestyles, and frugivory (15–18). Similarly, the evo- (Drosophilidae) are compelling species in which to study the geno- lution of diet specialization in Drosophila species correlates with mic architecture linked to the transition to herbivory because they chemoreceptor gene losses (19–21), and hematophagous flies have recently evolved from microbe-feeding ancestors and are closely lost gustatory receptors that detect sweet compounds (22).
    [Show full text]
  • English Style, from the Late 18Th Century)
    WHC-99/CONF.204/INF.7 UNESCO WORLD HERITAGE CONVENTION BUREAU OF THE WORLD HERITAGE COMMITTEE 23rd session (5 - 10 July 1999) Paris (France) EVALUATIONS OF CULTURAL PROPERTIES Prepared by the International Council on Monuments and Sites (ICOMOS) The IUCN and ICOMOS evaluations are made available to members of the Bureau and the World Heritage Committee. A small number of additional copies are also available from the secretariat. Thank you. 1999 Mountains and down to the valley floors. Both rock art and Greater Blue Mountains (Australia) tracks are intact and authentic. The exceptional circumstances of the Greater Blue Mountains are the scale, intensity, and longevity of the No 917 cultural association. It is a place where ancient custodianship over the million hectares of dissected plateaux has been replaced by another, more recent, form of custodianship, significant nonetheless. The intense inter-relationship of nature and people over tens of thousands of years make the Greater Blue Mountains a Identification classic example of the nature-culture continuum, which has exercised the minds of the World Heritage Committee over Nomination The Greater Blue Mountains Area recent years and was given expression in its Global Strategy meeting of March 1998. Cultural criterion vi Location State of New South Wales State Party Australia Category of property Date 30 June 1998 In terms of the categories of cultural property set out in Article 1 of the 1972 World Heritage Convention, this is a site. Note This property is nominated under both natural and History and Description cultural criteria as a mixed site. In this evaluation only that History information from the dossier relating to nomination under the cultural criteria are taken into account.
    [Show full text]