The Great American Biotic Interchange a South American Perspective

Total Page:16

File Type:pdf, Size:1020Kb

The Great American Biotic Interchange a South American Perspective SPRINGER BRIEFS IN EARTH SYSTEM SCIENCES SOUTH AMERICA AND THE SOUTHERN HEMISPHERE Alberto Luis Cione Germán Mariano Gasparini Esteban Soibelzon Leopoldo Héctor Soibelzon Eduardo Pedro Tonni The Great American Biotic Interchange A South American Perspective 123 SpringerBriefs in Earth System Sciences South America and the Southern Hemisphere Series editors Jorge Rabassa, Ushuaia, Argentina Gerrit Lohmann, Bremen, Germany Justus Notholt, Bremen, Germany Lawrence A. Mysak, Montreal, Canada Vikram Unnithan, Bremen, Germany More information about this series at http://www.springer.com/series/10032 Pleistocene continental beds cropping out in the coastal cliffs south of Miramar, Buenos Aires Province. Note the chimango, a terrestrial bird at the left, and a gull, a marine bird at the right. Photo by Esteban Soibelzon Alberto Luis Cione · Germán Mariano Gasparini Esteban Soibelzon · Leopoldo Héctor Soibelzon Eduardo Pedro Tonni The Great American Biotic Interchange A South American Perspective 1 3 Alberto Luis Cione Leopoldo Héctor Soibelzon División Paleontología Vertebrados, División Paleontología Vertebrados, Museo de La Plata, Facultad de Museo de La Plata, Facultad de Ciencias Naturales y Museo Ciencias Naturales y Museo UNLP UNLP La Plata La Plata Argentina Argentina Germán Mariano Gasparini Eduardo Pedro Tonni División Paleontología Vertebrados, División Paleontología Vertebrados, Museo de La Plata, Facultad de Museo de La Plata, Facultad de Ciencias Naturales y Museo Ciencias Naturales y Museo UNLP UNLP La Plata La Plata Argentina Argentina Esteban Soibelzon División Paleontología Vertebrados, Museo de La Plata, Facultad de Ciencias Naturales y Museo UNLP La Plata Argentina ISSN 2191-589X ISSN 2191-5903 (electronic) SpringerBriefs in Earth System Sciences ISBN 978-94-017-9791-7 ISBN 978-94-017-9792-4 (eBook) DOI 10.1007/978-94-017-9792-4 Library of Congress Control Number: 2015934918 Springer Dordrecht Heidelberg New York London © The Author(s) 2015 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. The publisher, the authors and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made. Printed on acid-free paper Springer Science+Business Media B.V. Dordrecht is part of Springer Science+Business Media (www.springer.com) The most emblematic South American mammals are the guanaco, the tapir, and the spectacled bear. However, the closest ancestors of these animals did not originate in the continent: They were recent immigrants from North America. Yes, we got a problem: The evidence is at the bottom of the bottle and we are not drunks Preface The Great American Biotic Interchange (GABI) between North and South America is one of the most important events in the history of land mammals. The first authors that considered the interchange between the Americas were Wallace, Ameghino, and few others as early as the second half of the nineteenth century. Notwithstanding that a huge effort was made by thousands of paleontologists, zoologists, botanists, geologists, and professionals of other disciplines, we are far from having a precise panorama about one of the most important events in the his- tory of mammals. However, we are confident that a more complete survey of mammal bearing units in southern South America as well as discovering others in the central and northern Andes and Central America will give us the factual evidence for propos- ing, confirming, or rejecting many hypotheses. Moreover, the expanding molecular studies will provide the minimum age for the origin of many endemic clades of North American families whose first appearance is not adequately explained. In this book, we consider the extinction of megafauna in South America as a part of GABI. Several paleontologists (including the authors of this book) are commited to the study of the process that modified permanently the composi- tion and distribution of land mammals in South America. The entrance of hunter- gatherers at the end of the Pleistocene occasioned the spectacular extinction of megafauna. However, this process is being completed by modern man. For this, research on recent distribution of vertebrates in South America has to be accel- erated. During the last twentieth and twenty-first centuries, terrestrial and aquatic environments changed radically because modern human activities occasioned extinction, pseudoextinction, and alteration of distribution of many mammals. This disruption might make conventional and molecular studies of historical patterns and relationships between different lineages extremely difficult. However, fossils are still in the rocks. They are waiting for us to find them, unearth them, and make them drops of light for explaining the origin of a treasure in danger: the richest land mammal fauna of the world. vii viii Preface The authors thank Jorge Oscar Rabassa (Series Springer Editor for South America) for the invitation to publish this book and for critical review of an early draft of the manuscript; Jorge González for the drawings; Marcela Tomeo (Museo de La Plata) for the maps and figures; Mariano Donato, Jorge Morrone, Cecilia Deschamps, and Alfredo Zurita for valuable information; and Cecilia Deschamps (MLP) for language correction and revision of a former manuscript. We also thank Facultad de Ciencias Naturales y Museo (UNLP) and the Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET). This book was partially funded by PICT 2010-0804 and PIP 0436. Contents 1 Introduction ................................................ 1 References .................................................. 7 2 Continental Relationships, Chronostratigraphy, Climates, and Mammalian Biogeography of Southern South America Since Late Miocene .......................................... 9 2.1 General Continental Relationships of South America ............ 9 2.2 Evolution of the Physical Connection Between Central and South America ....................................... 12 2.3 History and Conceptual Framework of Mammal Stratigraphy of the Southern Cone of South America Since the Miocene ....... 14 2.3.1 The Stratigraphy of the Pampas ...................... 14 2.3.2 Comments on the Pampean Loess and Lithostratigraphic Units of the Pampean Region ........................ 19 2.4 The Late Cenozoic Mammals of the Pampean Region. A Biostratigraphical Point of View .......................... 20 2.4.1 Biozone of Macrochorobates scalabrinii ............... 21 2.4.2 Biozone of Eumysops Laeviplicatus ................... 23 2.4.3 Biozone of Paraglyptodon chapadmalensis ............. 23 2.4.4 Biozone of Platygonus scagliai ...................... 25 2.4.5 Biozone of Akodon (Akodon) lorenzinii ................ 25 2.4.6 Biozone of Ctenomys chapalmalensis ................. 26 2.4.7 Biozone of Mesotherium cristatum ................... 28 2.4.8 Biozone of Megatherium americanum ................. 29 2.4.9 Biozone of Equus (Amerhippus) neogaeus ............. 30 2.4.10 Biozone of Lagostomus maximus ..................... 32 2.4.11 An Alternative Scheme for the Late Miocene Based on Biochronology ........................... 35 ix x Contents 2.5 Paleoclimatology of the Southern Cone of South America Since the Miocene ....................................... 36 2.5.1 Climates in Patagonia Since the Miocene .............. 36 2.5.2 Climates in the Pampean Region from the Late Miocene to the Pliocene ................................... 38 2.5.3 Climates in the Pampean Region During the Quaternary ... 39 2.6 Biogeography of the Recent Mammals of South America ......... 44 2.6.1 Biogeography of Argentina ......................... 49 2.6.2 The Pampa Ecoregion. 51 2.6.3 Mammals Introduced by Man ....................... 53 References .................................................. 53 3 The GABI in Southern South America .......................... 71 3.1 Short History of the Interchange and the Great American Biotic Interchange (GABI) Concept. 71 3.2 The GABI Chronology and Dynamics ........................ 73 3.2.1 First Record of Taxa of North American Origin in Southern South America Gives the General Pattern but does not Explain the Details. 73 3.2.2 Integration of South American Mammalian Faunas: The Coexistence of Native and Immigrant Taxa ......... 78 References .................................................. 90 Index ......................................................... 97 Chapter 1 Introduction Abstract The Great American Biotic Interchange (GABI) between North and South America is one of the most important events in the history of land mam- mals. The interchange occurred in several phases during more than
Recommended publications
  • 1.1 První Chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2
    MASARYKOVA UNIVERZITA PŘÍRODOVĚDECKÁ FAKULTA ÚSTAV GEOLOGICKÝCH VĚD Jakub Březina Rešerše k bakalářské práci Využití mikrostruktur klů neogenních chobotnatců na příkladu rodu Zygolophodon Vedoucí práce: doc. Mgr. Martin Ivanov, Dr. Brno 2012 OBSAH 1. Současný pohled na evoluci chobotnatců 3 1.1 První chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2. Kly chobotnatců a jejich mikrostruktura 9 2.1 Přírůstky v klech chobotnatců 11 2.1.1 Využití přírůstků v klech chobotnatců 11 2.2 Schregerův vzor 12 2.2.1 Stavba Schregerova vzoru 12 2.2.2 Využití Schregerova vzoru 12 2.3 Dentinové kanálky 15 3 Sedimenty s nálezy savců v okolí Mikulova 16 3.1 Baden 17 3.2 Pannon a Pont 18 1. Současný pohled na evoluci chobotnatců Současná systematika chobotnatců není kompletně odvozena od jejich fylogeneze, rekonstruované pomocí kladistických metod. Diskutované skupiny tak mnohdy nepředstavují monofyletické skupiny. Přestože jsou taxonomické kategorie matoucí (např. Laurin 2005), jsem do jisté míry nucen je používat. Některým skupinám úrovně stále přiřazeny nebyly a zde této skutečnosti není přisuzován žádný význam. V této rešerši jsem se zaměřil hlavně na poznatky, které následovaly po vydání knihy; The Proboscidea: Evolution and Paleoecology of Elephants and Their Relatives, od Shoshaniho a Tassyho (1996). Chobotnatci jsou součástí skupiny Tethytheria společně s anthracobunidy, sirénami a desmostylidy (Shoshani 1998; Shoshani & Tassy 1996; 2005; Gheerbrant & Tassy 2009). Základní klasifikace sestává ze dvou skupin. Ze skupiny Plesielephantiformes, do které patří čeledě Numidotheriidae, Barytheriidae a Deinotheridae a ze skupiny Elephantiformes, do které patří čeledě Palaeomastodontidae, Phiomiidae, Mammutida, Gomphotheriidae, tetralofodontní gomfotéria, Stegodontidae a Elephantidae (Shoshani & Marchant 2001; Shoshani & Tassy 2005; Gheerbrant & Tassy 2009).
    [Show full text]
  • Snakes of the Siwalik Group (Miocene of Pakistan): Systematics and Relationship to Environmental Change
    Palaeontologia Electronica http://palaeo-electronica.org SNAKES OF THE SIWALIK GROUP (MIOCENE OF PAKISTAN): SYSTEMATICS AND RELATIONSHIP TO ENVIRONMENTAL CHANGE Jason J. Head ABSTRACT The lower and middle Siwalik Group of the Potwar Plateau, Pakistan (Miocene, approximately 18 to 3.5 Ma) is a continuous fluvial sequence that preserves a dense fossil record of snakes. The record consists of approximately 1,500 vertebrae derived from surface-collection and screen-washing of bulk matrix. This record represents 12 identifiable taxa and morphotypes, including Python sp., Acrochordus dehmi, Ganso- phis potwarensis gen. et sp. nov., Bungarus sp., Chotaophis padhriensis, gen. et sp. nov., and Sivaophis downsi gen. et sp. nov. The record is dominated by Acrochordus dehmi, a fully-aquatic taxon, but diversity increases among terrestrial and semi-aquatic taxa beginning at approximately 10 Ma, roughly coeval with proxy data indicating the inception of the Asian monsoons and increasing seasonality on the Potwar Plateau. Taxonomic differences between the Siwalik Group and coeval European faunas indi- cate that South Asia was a distinct biogeographic theater from Europe by the middle Miocene. Differences between the Siwalik Group and extant snake faunas indicate sig- nificant environmental changes on the Plateau after the last fossil snake occurrences in the Siwalik section. Jason J. Head. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC 20013-7012, USA. [email protected] School of Biological Sciences, Queen Mary, University of London, London, E1 4NS, United Kingdom. KEY WORDS: Snakes, faunal change, Siwalik Group, Miocene, Acrochordus. PE Article Number: 8.1.18A Copyright: Society of Vertebrate Paleontology May 2005 Submission: 3 August 2004.
    [Show full text]
  • A Partial Short-Faced Bear Skeleton from an Ozark Cave with Comments on the Paleobiology of the Species
    Blaine W. Schubert and James E. Kaufmann - A partial short-faced bear skeleton from an Ozark cave with comments on the paleobiology of the species. Journal of Cave and Karst Studies 65(2): 101-110. A PARTIAL SHORT-FACED BEAR SKELETON FROM AN OZARK CAVE WITH COMMENTS ON THE PALEOBIOLOGY OF THE SPECIES BLAINE W. SCHUBERT Environmental Dynamics, 113 Ozark Hall, University of Arkansas, Fayetteville, AR 72701, and Geology Section, Research and Collections, Illinois State Museum, Springfield, IL 62703 USA JAMES E. KAUFMANN Department of Geology and Geophysics, University of Missouri-Rolla, Rolla, MO 65409 USA Portions of an extinct giant short-faced bear, Arctodus simus, were recovered from a remote area with- in an Ozark cave, herein named Big Bear Cave. The partially articulated skeleton was found in banded silt and clay sediments near a small entrenched stream. The sediment covered and preserved skeletal ele- ments of low vertical relief (e.g., feet) in articulation. Examination of a thin layer of manganese and clay under and adjacent to some skeletal remains revealed fossilized hair. The manganese in this layer is con- sidered to be a by-product of microorganisms feeding on the bear carcass. Although the skeleton was incomplete, the recovered material represents one of the more complete skeletons for this species. The stage of epiphyseal fusion in the skeleton indicates an osteologically immature individual. The specimen is considered to be a female because measurements of teeth and fused postcranial elements lie at the small end of the size range for A. simus. Like all other bears, the giant short-faced bear is sexually dimorphic.
    [Show full text]
  • Análisis Litoestratigráfico De La Formación Cerro Azul (Mioceno Superior) En La Provincia De La Pampa
    Revista de la Asociación Geológica Argentina 67 (2): 257 - 265 (2010) 257 ANÁLISIS LITOESTRATIGRÁFICO DE LA FORMACIÓN CERRO AZUL (MIOCENO SUPERIOR) EN LA PROVINCIA DE LA PAMPA Graciela VISCONTI1, Ricardo N. MELCHOR1,2, Claudia I. MONTALVO1, Aldo M. UMAZANO1,2 y Elena E. DE ELORRIAGA1 1 Universidad Nacional de La Pampa, Facultad de Ciencias Exactas y Naturales. E-mail: [email protected] 2 INCITAP (CONICET-UNLPam) RESUMEN La Formación Cerro Azul fue definida en 1980 para incluir a las sedimentitas continentales pliocenas (limolitas arenosas y are- niscas limosas) que afloran de manera discontinua en casi todo el ámbito de la provincia de La Pampa. No obstante, varias in- vestigaciones paleontológicas realizadas a partir de la segunda mitad de la década del 80’ han permitido ubicar geocronológi- camente a la unidad en el intervalo 10 Ma a 5,8-5,7 Ma. El objetivo del trabajo es realizar un análisis de las características li- toestratigráficas de la Formación Cerro Azul de acuerdo al Código Argentino de Estratigrafía. Se propone un lectoestratoti- po para la unidad, consistente en el perfil de Algarrobo del Águila y un perfil auxiliar en cerro El Morro. También se estable- cieron las relaciones estratigráficas con otras formaciones. Se interpreta un paleoambiente depositacional de llanura, donde alter- nan depósitos de loess con numerosos paleosuelos, detectándose escasos depósitos lacustres en la base y pocos cursos fluviales. Palabras clave: Formación Cerro Azul, Mioceno, Huayqueriense, La Pampa. ABSTRACT: Lithostratigrafic analysis of Cerro Azul Formation (Upper Miocene), La Pampa. Cerro Azul Formation was defined in 1980 to include the Pliocene continental sedimentary rocks (sandy silt and silty sand) that appear in discontinuous outcrops in al- most all La Pampa province.
    [Show full text]
  • Revised Stratigraphy of Neogene Strata in the Cocinetas Basin, La Guajira, Colombia
    Swiss J Palaeontol (2015) 134:5–43 DOI 10.1007/s13358-015-0071-4 Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia F. Moreno • A. J. W. Hendy • L. Quiroz • N. Hoyos • D. S. Jones • V. Zapata • S. Zapata • G. A. Ballen • E. Cadena • A. L. Ca´rdenas • J. D. Carrillo-Bricen˜o • J. D. Carrillo • D. Delgado-Sierra • J. Escobar • J. I. Martı´nez • C. Martı´nez • C. Montes • J. Moreno • N. Pe´rez • R. Sa´nchez • C. Sua´rez • M. C. Vallejo-Pareja • C. Jaramillo Received: 25 September 2014 / Accepted: 2 February 2015 / Published online: 4 April 2015 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2015 Abstract The Cocinetas Basin of Colombia provides a made exhaustive paleontological collections, and per- valuable window into the geological and paleontological formed 87Sr/86Sr geochronology to document the transition history of northern South America during the Neogene. from the fully marine environment of the Jimol Formation Two major findings provide new insights into the Neogene (ca. 17.9–16.7 Ma) to the fluvio-deltaic environment of the history of this Cocinetas Basin: (1) a formal re-description Castilletes (ca. 16.7–14.2 Ma) and Ware (ca. 3.5–2.8 Ma) of the Jimol and Castilletes formations, including a revised formations. We also describe evidence for short-term pe- contact; and (2) the description of a new lithostratigraphic riodic changes in depositional environments in the Jimol unit, the Ware Formation (Late Pliocene). We conducted and Castilletes formations. The marine invertebrate fauna extensive fieldwork to develop a basin-scale stratigraphy, of the Jimol and Castilletes formations are among the richest yet recorded from Colombia during the Neogene.
    [Show full text]
  • A Bibliography of Klamath Mountains Geology, California and Oregon
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY A bibliography of Klamath Mountains geology, California and Oregon, listing authors from Aalto to Zucca for the years 1849 to mid-1995 Compiled by William P. Irwin Menlo Park, California Open-File Report 95-558 1995 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. PREFACE This bibliography of Klamath Mountains geology was begun, although not in a systematic or comprehensive way, when, in 1953, I was assigned the task of preparing a report on the geology and mineral resources of the drainage basins of the Trinity, Klamath, and Eel Rivers in northwestern California. During the following 40 or more years, I maintained an active interest in the Klamath Mountains region and continued to collect bibliographic references to the various reports and maps of Klamath geology that came to my attention. When I retired in 1989 and became a Geologist Emeritus with the Geological Survey, I had a large amount of bibliographic material in my files. Believing that a comprehensive bibliography of a region is a valuable research tool, I have expended substantial effort to make this bibliography of the Klamath Mountains as complete as is reasonably feasible. My aim was to include all published reports and maps that pertain primarily to the Klamath Mountains, as well as all pertinent doctoral and master's theses.
    [Show full text]
  • Lithium Extraction in Argentina: a Case Study on the Social and Environmental Impacts
    Lithium extraction in Argentina: a case study on the social and environmental impacts Pía Marchegiani, Jasmin Höglund Hellgren and Leandro Gómez. Executive summary The global demand for lithium has grown significantly over recent years and is expected to grow further due to its use in batteries for different products. Lithium is used in smaller electronic devices such as mobile phones and laptops but also for larger batteries found in electric vehicles and mobility vehicles. This growing demand has generated a series of policy responses in different countries in the southern cone triangle (Argentina, Bolivia and Chile), which together hold around 80 per cent of the world’s lithium salt brine reserves in their salt flats in the Puna area. Although Argentina has been extracting lithium since 1997, for a long time there was only one lithium-producing project in the country. In recent years, Argentina has experienced increased interest in lithium mining activities. In 2016, it was the most dynamic lithium producing country in the world, increasing production from 11 per cent to 16 per cent of the global market (Telam, 2017). There are now around 46 different projects of lithium extraction at different stages. However, little consideration has been given to the local impacts of lithium extraction considering human rights and the social and environmental sustainability of the projects. With this in mind, the current study seeks to contribute to an increased understanding of the potential and actual impacts of lithium extraction on local communities, providing insights from local perspectives to be considered in the wider discussion of sustainability, green technology and climate change.
    [Show full text]
  • Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,***
    Woodburne, M.O.; Cione, A.L.; and Tonni, E.P., 2006, Central American provincialism and the 73 Great American Biotic Interchange, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Ad- vances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic In- terchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 73–101. CENTRAL AMERICAN PROVINCIALISM AND THE GREAT AMERICAN BIOTIC INTERCHANGE Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,*** ABSTRACT The age and phyletic context of mammals that dispersed between North and South America during the past 9 m.y. is summarized. The presence of a Central American province of cladogenesis and faunal differentiation is explored. One apparent aspect of such a province is to delay dispersals of some taxa northward from Mexico into the continental United States, largely during the Blancan. Examples are recognized among the various xenar- thrans, and cervid artiodactyls. Whereas the concept of a Central American province has been mentioned in past investigations it is upgraded here. Paratoceras (protoceratid artio- dactyl) and rhynchotheriine proboscideans provide perhaps the most compelling examples of Central American cladogenesis (late Arikareean to early Barstovian and Hemphillian to Rancholabrean, respectively), but this category includes Hemphillian sigmodontine rodents, and perhaps a variety of carnivores and ungulates from Honduras in the medial Miocene, as well as peccaries and equids from Mexico. For South America, Mexican canids and hy- drochoerid rodents may have had an earlier development in Mexico. Remarkably, the first South American immigrants to Mexico (after the Miocene heralds; the xenarthrans Plaina and Glossotherium) apparently dispersed northward at the same time as the first Holarctic taxa dispersed to South America (sigmodontine rodents and the tayassuid artiodactyls).
    [Show full text]
  • The Record of Miocene Impacts in the Argentine Pampas
    Meteoritics & Planetary Science 41, Nr 5, 749–771 (2006) Abstract available online at http://meteoritics.org The record of Miocene impacts in the Argentine Pampas Peter H. SCHULTZ1*, Marcelo Z¡RATE2, Willis E. HAMES3, R. Scott HARRIS1, T. E. BUNCH4, Christian KOEBERL5, Paul RENNE6, and James WITTKE7 1Department of Geological Sciences, Brown University, Providence, Rhode Island 02912–1846, USA 2Facultad de Ciencias Exactas y Naturales, Universidad Nacional de La Pampa, Avda Uruguay 151, 6300 Santa Rosa, La Pampa, Argentina 3Department of Geology, Auburn University, Auburn, Alabama 36849, USA 4Department of Geology, Northern Arizona University, Flagstaff, Arizona 86011, USA 5Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria 6Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, California 94709, USA 7Department of Geology, Northern Arizona University, Flagstaff, Arizona 86011, USA *Corresponding author. E-mail: [email protected] (Received 02 March 2005; revision accepted 14 December 2005) Abstract–Argentine Pampean sediments represent a nearly continuous record of deposition since the late Miocene (∼10 Ma). Previous studies described five localized concentrations of vesicular impact glasses from the Holocene to late Pliocene. Two more occurrences from the late Miocene are reported here: one near Chasicó (CH) with an 40Ar/39Ar age of 9.24 ± 0.09 Ma, and the other near Bahía Blanca (BB) with an age of 5.28 ± 0.04 Ma. In contrast with andesitic and dacitic impact glasses from other localities in the Pampas, the CH and BB glasses are more mafic. They also exhibit higher degrees of melting with relatively few xenoycrysts but extensive quench crystals. In addition to evidence for extreme heating (>1700 °C), shock features are observed (e.g., planar deformation features [PDFs] and diaplectic quartz and feldspar) in impact glasses from both deposits.
    [Show full text]
  • Orthoptera, Acrididae) at Non-Outbreaking and Outbreaking Situations
    SHORT COMMUNICATION Longevity and fecundity of Dichroplus maculipennis (Orthoptera, Acrididae) at non-outbreaking and outbreaking situations Yanina Mariottini1, María Laura De Wysiecki1 & Carlos Ernesto Lange1,2 1Centro de Estudios Parasitológicos y de Vectores (UNLP- CCT La Plata- CONICET). Calle 2 Nº 584, Código postal 1900, La Plata, Argentina. [email protected], [email protected] 2Comisión de Investigaciones Científicas provincia de Buenos Aires. [email protected] ABSTRACT. Longevity and fecundity of Dichroplus maculipennis (Orthoptera, Acrididae) at non-outbreaking and outbreaking situations. Dichroplus maculipennis is one of the most characteristic and damaging grasshopper species of Argentina, mainly in areas of the Pampas and Patagonia regions. We estimated and compared the longevity and fecundity of adult female D. maculipennis under controlled conditions (30°C, 14L:10D, 40% RH) from individuals collected as last instar nymphs (VI) in the field and with a known recent history of low and high density conditions. Densities of D. maculipennis at the collecting sites were 0.95 individuals per m2 in 2006 and 46 ind/m2 in 2009, representing non-outbreaking and outbreaking situations, respectively. Adult female longev- ity in 2006 (67.96 ± 3.2 days) was significantly higher (p < 0.05) than in 2009 (37.44 ± 1.98 days). The number of egg-pods per female was 3.32 ± 0.44 for 2006 and 1.62 ± 0.26 for 2009. The average fecundity in 2006 (89.29 ± 11.9 eggs/female) was signifi- cantly greater (p < 0.05) than that in 2009 (36.27 ± 5.82 eggs/female). While it was observed that the oviposition rate was higher in 2006, this difference was not significant (p > 0.05).
    [Show full text]
  • Iguanid and Varanid CAMP 1992.Pdf
    CONSERVATION ASSESSMENT AND MANAGEMENT PLAN FOR IGUANIDAE AND VARANIDAE WORKING DOCUMENT December 1994 Report from the workshop held 1-3 September 1992 Edited by Rick Hudson, Allison Alberts, Susie Ellis, Onnie Byers Compiled by the Workshop Participants A Collaborative Workshop AZA Lizard Taxon Advisory Group IUCN/SSC Conservation Breeding Specialist Group SPECIES SURVIVAL COMMISSION A Publication of the IUCN/SSC Conservation Breeding Specialist Group 12101 Johnny Cake Ridge Road, Apple Valley, MN 55124 USA A contribution of the IUCN/SSC Conservation Breeding Specialist Group, and the AZA Lizard Taxon Advisory Group. Cover Photo: Provided by Steve Reichling Hudson, R. A. Alberts, S. Ellis, 0. Byers. 1994. Conservation Assessment and Management Plan for lguanidae and Varanidae. IUCN/SSC Conservation Breeding Specialist Group: Apple Valley, MN. Additional copies of this publication can be ordered through the IUCN/SSC Conservation Breeding Specialist Group, 12101 Johnny Cake Ridge Road, Apple Valley, MN 55124. Send checks for US $35.00 (for printing and shipping costs) payable to CBSG; checks must be drawn on a US Banlc Funds may be wired to First Bank NA ABA No. 091000022, for credit to CBSG Account No. 1100 1210 1736. The work of the Conservation Breeding Specialist Group is made possible by generous contributions from the following members of the CBSG Institutional Conservation Council Conservators ($10,000 and above) Australasian Species Management Program Gladys Porter Zoo Arizona-Sonora Desert Museum Sponsors ($50-$249) Chicago Zoological
    [Show full text]
  • Onetouch 4.0 Scanned Documents
    / Chapter 2 THE FOSSIL RECORD OF BIRDS Storrs L. Olson Department of Vertebrate Zoology National Museum of Natural History Smithsonian Institution Washington, DC. I. Introduction 80 II. Archaeopteryx 85 III. Early Cretaceous Birds 87 IV. Hesperornithiformes 89 V. Ichthyornithiformes 91 VI. Other Mesozojc Birds 92 VII. Paleognathous Birds 96 A. The Problem of the Origins of Paleognathous Birds 96 B. The Fossil Record of Paleognathous Birds 104 VIII. The "Basal" Land Bird Assemblage 107 A. Opisthocomidae 109 B. Musophagidae 109 C. Cuculidae HO D. Falconidae HI E. Sagittariidae 112 F. Accipitridae 112 G. Pandionidae 114 H. Galliformes 114 1. Family Incertae Sedis Turnicidae 119 J. Columbiformes 119 K. Psittaciforines 120 L. Family Incertae Sedis Zygodactylidae 121 IX. The "Higher" Land Bird Assemblage 122 A. Coliiformes 124 B. Coraciiformes (Including Trogonidae and Galbulae) 124 C. Strigiformes 129 D. Caprimulgiformes 132 E. Apodiformes 134 F. Family Incertae Sedis Trochilidae 135 G. Order Incertae Sedis Bucerotiformes (Including Upupae) 136 H. Piciformes 138 I. Passeriformes 139 X. The Water Bird Assemblage 141 A. Gruiformes 142 B. Family Incertae Sedis Ardeidae 165 79 Avian Biology, Vol. Vlll ISBN 0-12-249408-3 80 STORES L. OLSON C. Family Incertae Sedis Podicipedidae 168 D. Charadriiformes 169 E. Anseriformes 186 F. Ciconiiformes 188 G. Pelecaniformes 192 H. Procellariiformes 208 I. Gaviiformes 212 J. Sphenisciformes 217 XI. Conclusion 217 References 218 I. Introduction Avian paleontology has long been a poor stepsister to its mammalian counterpart, a fact that may be attributed in some measure to an insufRcien- cy of qualified workers and to the absence in birds of heterodont teeth, on which the greater proportion of the fossil record of mammals is founded.
    [Show full text]