Discovery of the World's Highest-Dwelling Mammal
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Palaeoindian Occupation of the Atacama Desert, Northern Chile
Palaeoindian occupation of the Atacama Desert, northern Chile MARTIN GROSJEAN,1* LAUTARO NU´ N˜ EZ2 and ISABEL CARTAJENA3 1 National Center of Excellence in Research on Climate (NCCR Climate) and Institute of Geography, University of Bern, Bern, Switzerland 2 Instituto de Investigaciones Arqueolo´gicas y Museo, Universidad Cato´lica del Norte, San Pedro de Atacama, Chile 3 Departamento de Antropologı´a, Universidad de Chile, N˜ un˜oa, Santiago de Chile ABSTRACT: Palaeoindian occupation of the Atacama Desert in northern Chile has been found between 12 600 and 10 200 cal. yr BP. The new site at Salar Punta Negra (24 280S/60 530W/ 2976 m) includes about 1000 classifiable, mostly unifacial artefacts and, uniquely, three different diagnostic types of early projectile points. Two of the Lateglacial/early Holocene projectile types have wide distribution and are known from different geographical areas in South America: the Palaeoindian ‘Fell’ fish-tail point mainly from the southern cone of South America, and the triangular ‘Tuina’ points typical of the Puna of the south-central Andes in northern Chile and northwestern Argentina. In addition, we found a third type, a stemmed point typical for the Salar Punta Negra. Fill- ing a large geographical gap of ‘Fell’ occupation, the site at Salar Punta Negra provides evidence for generally much higher mobility and diversity of early cultures, and supports an Andean-Pacific route for early human exploration of South America to the south through the desert at intermediate alti- tudes. Contemporaneous high-amplitude climatic changes were fundamental preconditions to pro- vide adequate environments and habitats, and to make Palaeoindian hunting-gathering occupation possible in the Atacama Desert. -
The Taxonomic History of the South American Cricetid Genera Euneomys
AMERICAN MUSEUM NOVITATES Published by OF NATURAL HISTORT Number 541 THE AMERICAN NewMUSeUMYork City June 16, 1932 59.9, 32 C (8) THE TAXONOMIC HISTORY OF THE SOUTH AMERICAN CRICETID GENERA EUNEOMYS (SUBGENERA EUNEOMYS AND GALENOMYS), A ULISCOMYS, CHELEMYSCUS, CHIlNCHILLULA, PHYLLOTIS, PARALOMYS, GRAOMYS, ELIGMODONTIA AND HESPEROMYS BY G. H. H. TATE This is the second of a series of short papers on the systematic status of Neotropical mice. The intention is to concentrate in one article the scattered taxonomic information of the genera and species in question and to present it in such form that it is readily available for s ibsequent work. The genera treated are close allies and their histories interlock repeatedly. The history of each successive genus or subgenus is presented in chronological order, and placed after it is a summary setting forth the present status, based upon the opinions of recent writers, of all forms concerned, together with their type localities. HISTORICAL STATEMENT EUNEOMYS Coues Subgenus Euneomys Coues 1837. Waterhouse described (p. 17) Mus micropus (n. sp.) and placed it (p. 21) in Abrothrix, n. subg. of Mus. 1839. Waterhouse further described (p. 61) Mus micropus Waterhouse. He described (p. 72) Reithrodon chinchilloides (n. sp.) (later designated by Coues the type of Euneomys). He erected (p. 75) Hesperomys, n. g., to contain almost all forms of Cricetida of the Western Hemisphere. Micropus was presumably included in this genus. 1842. Lesson placed (p. 136) micropus in Mus (Abrothrix) and listed (p. 143) chinchilloides under Mus (Reithrodon). 1843. Wagner (p. 520) placed micropus in Hesperomys, subgenus of Habrothrix, and (p. -
Appendix A. Supplementary Material to the Manuscript
Appendix A. Supplementary material to the manuscript: The role of crustal and eruptive processes versus source variations in controlling the oxidation state of iron in Central Andean magmas 1. Continental crust beneath the CVZ Country Rock The basement beneath the sampled portion of the CVZ belongs to the Paleozoic Arequipa- Antofalla terrain – a high temperature metamorphic terrain with abundant granitoid intrusions that formed in response to Paleozoic subduction (Lucassen et al., 2000; Ramos et al., 1986). In Northern Chile and Northwestern Argentina this Paleozoic metamorphic-magmatic basement is largely homogeneous and felsic in composition, consistent with the thick, weak, and felsic properties of the crust beneath the CVZ (Beck et al., 1996; Fig. A.1). Neodymium model ages of exposed Paleozoic metamorphic-magmatic basement and sediments suggest a uniform Proterozoic protolith, itself derived from intrusions and sedimentary rock (Lucassen et al., 2001). AFC Model Parameters Pervasive assimilation of continental crust in the Central Andean ignimbrite magmas is well established (Hildreth and Moorbath, 1988; Klerkx et al., 1977; Fig. A.1) and has been verified by detailed analysis of radiogenic isotopes (e.g. 87Sr/86Sr and 143Nd/144Nd) on specific systems within the CVZ (Kay et al., 2011; Lindsay et al., 2001; Schmitt et al., 2001; Soler et al., 2007). Isotopic results indicate that the CVZ magmas are the result of mixing between a crustal endmember, mainly gneisses and plutonics that have a characteristic crustal signature of high 87Sr/86Sr and low 145Nd/144Nd, and the asthenospheric mantle (low 87Sr/86Sr and high 145Nd/144Nd; Fig. 2). In Figure 2, we model the amount of crustal assimilation required to produce the CVZ magmas that are targeted in this study. -
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. -
Volcán Lascar
Volcán Lascar Región: Antofagasta Provincia: El Loa Comuna: San Pedro de Atacama Coordenadas: 21°22’S – 67°44’O Poblados más cercanos: Talabre – Camar – Socaire Tipo: Estratovolcán Altura: 5.592 m s.n.m. Diámetro basal: 8.9 km Área basal: 62.2 km2 Volumen estimado: 28.5 km3 Última actividad: 2015 Última erupción mayor: 1993 Volcán Lascar. Vista desde el norte Ranking de riesgo (Fotografía: Gabriela Jara, SERNAGEOMIN) 14 específico: Generalidades El volcán Láscar corresponde a un estratovolcán compuesto, elongado en dirección este-oeste, activo desde hace unos 240 ka y emplazado en el margen oeste de la planicie altiplánica. Está conformado por lavas andesíticas, que alcanzan más de 10 km de longitud, y por potentes lavas dacíticas que se extienden hasta 5 km, las que fueron emitidas desde los flancos NO a SO. La lava más reciente se estima en 7 mil años de antigüedad. En los alrededores del volcán se reconocen depósitos de flujo y caída piroclástica, además de numerosos cráteres de impacto asociados a la eyección de bombas durante erupciones plinianas y subplinianas. El principal evento eruptivo durante su evolución se denomina Ignimbrita Soncor, generado hace unos 27 ka al oeste del volcán y con un volumen estimado cercano a los 10 km3. En la cima de este volcán se observan seis cráteres, algunos anidados, y el central de estos se encuentra activo. Registro eruptivo Este volcán ha presentado alrededor de 30 erupciones explosivas desde el siglo XIX, lo que lo convierte en el volcán más activo del norte de Chile. Estos eventos han consistido típicamente en erupciones vulcanianas de corta duración, con emisión de ceniza fina y proyecciones balísticas en un radio de 5 km, donde el último evento de este tipo ocurrió el 30 de octubre del 2015. -
Integrative Taxonomy of the Southernmost Tucu-Tucus in the World: Differentiation of the Nominal Forms Associated with Ctenomys
Mammalian Biology https://doi.org/10.1007/s42991-020-00015-z ORIGINAL ARTICLE Integrative taxonomy of the southernmost tucu‑tucus in the world: diferentiation of the nominal forms associated with Ctenomys magellanicus Bennett, 1836 (Rodentia, Hystricomorpha, Ctenomyidae) Pablo Teta1 · Guillermo D’Elía2 · Juan C. Opazo2 Received: 19 July 2019 / Accepted: 23 January 2020 © Deutsche Gesellschaft für Säugetierkunde 2020 Abstract We reviewed the alpha taxonomy of the genus Ctenomys Blainville, 1826 in southernmost South America, with emphasis on those nominal forms previously associated with C. magellanicus Bennett, 1836. We integrate distinct lines of evidence, including variation of mtDNA sequences, and the assessment of quantitative and qualitative traits of skins and skulls; when available, karyotypic data was also considered. Phylogenetic analysis of molecular markers shows low levels of divergence among specimens from southern South American mainland and the island of Tierra del Fuego (ca. 0.4%). This evidence plus the results of the multivariate analysis of metric data suggest that the nominal forms C. colburni J. A. Allen, 1903, C. fueginus Philippi, 1880, C. osgoodi J. A. Allen, 1905, C. m. dicki Osgood, 1943, and C. m. obscurus Texera, 1975 are subjective junior synonyms of C. magellanicus. In addition, we reviewed the status of C. fodax Thomas, 1910, a nominal form that have been alternatively considered as a valid species or related to C. magellanicus by previous researchers. Based on quantitative and qualitative morphological traits, we preliminarily regard C. fodax at the species level while citing it for the frst time to Chile. Keywords Caviomorpha · Octodontoidea · Taxonomy · Patagonia · Tierra del Fuego Introduction With ca. -
Camelid Domestication on the Western Slope of the Puna De Atacama, Northern Chile
Camelid domestication on the western slope of the Puna de Atacama, northern Chile Isabel CARTAJENA Departamento de Antropología Universidad de Chile Ignacio Carrera Pinto 1045, CL-Santiago Chile (Chili) [email protected] Lautaro NÚÑEZ Instituto de Investigaciones Arqueológicas y Museo R.P. Gustavo Le Paige Universidad Católica del Norte Le Paige s/n, CL-San Pedro de Atacama Chile (Chili) [email protected] Martin GROSJEAN Nacional Center of Excellence in Research on Climate (NCCR) and Institute of Geography University of Bern Erlachstrasse 9a, CH-Bern 3012 (Switzerland) [email protected] Cartajena I., Núñez L. & Grosjean M. 2007. – Camelid domestication on the western slope of the Puna de Atacama, northern Chile. Anthropozoologica 42 (2): 155-173. ABSTRACT Archaeofaunal records from the Early Archaic to the Early Formative sites (11000-2400 BP) on the western slope of the Puna de Atacama region (22ºS- 24ºS) were analysed in order to understand the process of camelid domestication. The remains were recovered from rock shelters and open sites reflecting an extended occupational sequence, starting with the first human occupations in the Early Archaic (11000-8000). During the Late Archaic (5000-3800 BP), the mobile hunting/gathering tradition had changed into a cultural system characterised by large campsites, hunting activities being present along with the first evidence of camelid domestication in favourable mid-Holocene sites (Quebrada Tulán and Puripica), which evolved during the Early Formative to complex camelid husbandry-based societies about 3100 BP. Although osteometrical evidence is mainly used, we incorporate pathologies, palaeoenvironmental information, the material culture and the archaeological context. Our intent is to identify the environmental scenario and the importance of environmental variables in desert areas, as well as to understand the emergence of camelid domestication in relation to ANTHROPOZOOLOGICA • 2007 • 42 (2) © Publications Scientifiques du Muséum national d’Histoire naturelle, Paris. -
Novltatesamerican MUSEUM PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET, NEW YORK, N.Y
NovltatesAMERICAN MUSEUM PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 3085, 39 pp., 17 figures, 6 tables December 27, 1993 A New Genus for Hesperomys molitor Winge and Holochilus magnus Hershkovitz (Mammalia, Muridae) with an Analysis of Its Phylogenetic Relationships ROBERT S. VOSS1 AND MICHAEL D. CARLETON2 CONTENTS Abstract ............................................. 2 Resumen ............................................. 2 Resumo ............................................. 3 Introduction ............................................. 3 Acknowledgments ............... .............................. 4 Materials and Methods ..................... ........................ 4 Lundomys, new genus ............... .............................. 5 Lundomys molitor (Winge, 1887) ............................................. 5 Comparisons With Holochilus .............................................. 11 External Morphology ................... ........................... 13 Cranium and Mandible ..................... ........................ 15 Dentition ............................................. 19 Viscera ............................................. 20 Phylogenetic Relationships ....................... ...................... 21 Character Definitions ................... .......................... 23 Results .............................................. 27 Phylogenetic Diagnosis and Contents of Oryzomyini ........... .................. 31 Natural History and Zoogeography -
Actualización Plan Director De Infraestructura Mop
REPÚBLICA DE CHILE MINISTERIO DE OBRAS PÚBLICAS DIRECCIÓN DE PLANEAMIENTO ACTUALIZACIÓN PLAN DIRECTOR DE INFRAESTRUCTURA MOP Informe Final Región de Antofagasta Chile, Noviembre de 2009 INECON, Ingenieros y Economistas Consultores S.A. ÍNDICE 1. CARACTERÍSTICAS DE LA REGIÓN DE ANTOFAGASTA ............................ 1 1.1. Características generales. ............................................................................. 1 1.2. Características económicas. .......................................................................... 1 1.3. Características de la población. ..................................................................... 2 1.4. Gasto histórico en infraestructura por parte del MOP. ...................................... 2 2. IMAGEN OBJETIVO DE LA REGIÓN DE ANTOFAGASTA ............................ 3 2.1. Diagnósticos, objetivos estratégicos y visiones pertinentes. .............................. 3 2.1.1. Estrategia de Desarrollo Regional (EDR) ................................................... 3 2.1.2. Visión 2020- Talleres MOP ..................................................................... 4 2.1.3. Reconocimiento Territorial ...................................................................... 4 2.2. Oportunidades y restricciones de la región. ..................................................... 5 2.2.1. Oportunidades ...................................................................................... 5 2.2.2. Restricciones ....................................................................................... -
Chigger Mites (Acariformes: Trombiculidae) of Chiloé Island, Chile, with Descriptions of Two New Species and New Data on the Genus Herpetacarus
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/346943842 Chigger Mites (Acariformes: Trombiculidae) of Chiloé Island, Chile, With Descriptions of Two New Species and New Data on the Genus Herpetacarus Article in Journal of Medical Entomology · December 2020 DOI: 10.1093/jme/tjaa258 CITATIONS READS 2 196 8 authors, including: Carolina Silva Alexandr A Stekolnikov Universidad Austral de Chile Russian Academy of Sciences 42 PUBLICATIONS 162 CITATIONS 98 PUBLICATIONS 666 CITATIONS SEE PROFILE SEE PROFILE Thomas Weitzel Esperanza Beltrami University of Desarrollo Universidad Austral de Chile 135 PUBLICATIONS 2,099 CITATIONS 12 PUBLICATIONS 18 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: THE ROLE OF RODENTS IN THE DISTRIBUTION OF TRICHINELLA SP. IN CHILE View project Fleas as potential vectors of pathogenic bacteria: evaluating the effects of diversity and composition community of fleas and rodent on prevalence of Rickettsia spp. and Bartonella spp. in Chile View project All content following this page was uploaded by Esperanza Beltrami on 11 December 2020. The user has requested enhancement of the downloaded file. applyparastyle "fig//caption/p[1]" parastyle "FigCapt" applyparastyle "fig" parastyle "Figure" Journal of Medical Entomology, XX(X), 2020, 1–12 doi: 10.1093/jme/tjaa258 Morphology, Systematics, Evolution Research Chigger Mites (Acariformes: Trombiculidae) of Chiloé Island, Chile, With Descriptions of Two New Species and New Data on the Genus Herpetacarus Downloaded from https://academic.oup.com/jme/advance-article/doi/10.1093/jme/tjaa258/6020011 by guest on 11 December 2020 María Carolina Silva-de la Fuente,1 Alexandr A. -
Cytogenetics of Some Mammal Species from Central
CYTOGENETICS OF SOME MAMMAL SPECIES FROM CENTRAL ARGENTINA by SERGIO I. TIRANTl, B.S. A THESIS IN ZOOLOGY Submitted to the Gradúate Faculty of Texas Tech University in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE Approved August, 1996 ^f5 'f\\iV 30- Ho i^'í> "h Copyright 1996, Sergio I. Tiranti ACKNOWLEDGMENTS My special thanks go to Robert J. Baker, my committee chairman, for his encouragement and support throughout my stay at Texas Tech. Committee members Robert D. Bradley and Michael R. Willig, offered comments and suggestions that benefited the final outcome of this thesis. Portions of this thesis were reviewed by John Bickham, Meredith J. Hamilton, Steve Kasper, Karen McBee and Lara E. Wiggins, thus contributing to its improvement. My work in La Pampa Province, Argentina, was supported by the Subsecretaría de Cultura, where Norma Durango, Gustavo Siegenthaler and Eduardo Fiorucci contributed in many ways to the accomplishment of this research project. Numerous localities visited in this study were sampled as part of La Pampa Province Vertébrate Survey. My stay at TTU is supported in part by the Dirección Nacional de Cooperación Internacional, Ministerio de Cultura y Educación, Argentina and the Universidad Nacional de La Pampa, Argentina. Finally, I am heartedly indebted to my parents, Iván and Irene, for their neverending encouragement and support. 11 TABLE OF CONTENTS ACKNOWLEDGMENTS ü ABSTRACT v LIST OF TABEES vi LIST OF FIGURES vii CHAPTER I. INTRODUCTION 1 II. THE KARYOTYPE OFMYQTIS.LEYIS (CHIROPTERA, VESPERTILIONIDAE). 7 Introduction...... 7 Material and Methods . 7 Results and Discussion .... 9 III. CHROMOSOMAL POLYMORPHISM VARL\TION IN THE SCRUB MOUSE AKODON MOLINAE (RODENTL\: SIGMODONTINAE) IN CENTRAL ARGENTINA 11 Abstract. -
MATERIAL SUPLEMENTARIO ONLINE Tabla S1. NMI, %NMI E Índices De Diversidad Para Seis Localidades De La Selva Pedemontana De
MATERIAL SUPLEMENTARIO ONLINE Tabla S1. NMI, %NMI e índices de diversidad para seis localidades de la Selva Pedemontana de las Yungas. S= Riqueza de especies, D= Índice de dominancia de Simpson, α= Índice alpha de Fisher, H’= Índice de equitatividad de Shannon-Wiener, Chao-1= estimador Chao1. RU ISP EAS LR SG LH Localidades NMI %NMI NMI %NMI NMI %NMI NMI %NMI NMI %NMI NMI %NMI Especies Thylamys cf. T. sponsorius/venustus - - - - 1 1.639 - - - - 9 1.844 Thylamys sp. - - - - - 3 0.319 1 1.333 - - Abrothrix illutea 6 0.977 - - - - - - - - - - Akodon caenosus - - - - - - - - 4 5.333 94 19.26 Akodon simulator 5 0.814 10 5.952 3 4.918 16 1.700 7 9.333 67 13.73 Akodon spegazzinii 45 7.329 14 8.333 6 9.836 110 11.70 - - - - Akodon sylvanus - - - - - - - - 2 2.667 7 1.434 Necromys lasiurus 2 0.326 8 4.762 - - 28 2.976 - - - - Oxymycterus paramensis - - - - - - - - - - 8 1.639 Euryoryzomys legatus - - - - - - - - - - 1 0.205 Andinomys edax 2 0.327 - - - - - - - - - - Holochilus chacarius - - 5 2.976 - - 2 0.213 - - 1 0.205 Oligoryzomys brendae 92 14.99 16 9.524 6 9.836 33 3.507 14 18.67 131 28.84 Oligoryzomys cf. O. occidentalis 66 10.75 38 22.62 10 16.39 36 3.826 11 14.67 53 10.86 Calomys cf. C. fecundus/venustus 113 18.40 65 38.70 20 32.79 478 50.71 29 38.67 96 19.67 Calomys cf. C. laucha/musculinus 282 45.93 6 3.571 15 24.90 226 24.02 2 2.667 1 0.205 Graomys domorum - - - - - - - - - - 3 0.615 Rhipidomys austrinus - - - - - - - - 3 4.000 11 2.254 Rattus sp.