Cueva De Altamira, Cantabria): Microclima, Geomicrobiología Y Mecanismos De Interacción Cavidad/Exterior

Total Page:16

File Type:pdf, Size:1020Kb

Cueva De Altamira, Cantabria): Microclima, Geomicrobiología Y Mecanismos De Interacción Cavidad/Exterior DEPARTAMENTO DE GEOLOGÍA MUSEO NACIONAL DE CIENCIAS NATURALES CONSEJO SUPERIOR DE INVESTIGACIONES CIENTÍFICAS DEPARTAMENTO DE PETROLOGÍA Y GEOQUÍMICA FACULTAD DE CIENCIAS GEOLÓGICAS UNIVERSIDAD COMPLUTENSE DE MADRID Dinámica microambiental de un medio kárstico somero (Cueva de Altamira, Cantabria): microclima, geomicrobiología y mecanismos de interacción cavidad/exterior. Tesis Doctoral SOLEDAD CUEZVA ROBLEÑO Madrid, 2008 Directores: SERGIO SÁNCHEZ MORAL Departamento de Geología Museo Nacional de Ciencias Naturales Consejo Superior de Investigaciones Científicas JUAN CARLOS CAÑAVERAS JIMÉNEZ Departamento de Ciencias de la Tierra y del Medio Ambiente Facultad de Ciencias Universidad de Alicante Tutor: CARLOS ROSSI NIETO Departamento de Petrología y Geoquímica Facultad de Ciencias Geológicas Universidad Complutense de Madrid Dinámica microambiental de un medio kárstico somero (Cueva de Altamira, Cantabria): microclima, geomicrobiología y mecanismos de interacción cavidad/exterior. Esta Tesis Doctoral ha sido realizada en el Departamento de Geología del Museo Nacional de Ciencias Naturales (CSIC), con colaboración del Museo Nacional y Centro de Investigación de Altamira, y financiada por los pro- yectos de Investigación del Ministerio de Educación y Ciencia BTE2002-04492-CO2-02 (Inv. Principal S. Sánchez Moral), GL2006-11561 (Inv. Principal S. Sánchez Moral), la Acción Complementaria CGL2006-26147 (Inv. Principal S. Sánchez Moral) y dos Convenios de Colaboración entre la Dirección General de Bellas Artes y Bienes Culturales (MCu) y el Consejo Superior de Investigaciones Científicas (Inv. Principal S. Sánchez Moral). Esta Memoria es presentada por Soledad Cuezva Robleño para optar al grado de Doctor en Ciencias Geológicas. Madrid, mayo de 2008. El Doctorando, Soledad Cuezva Robleño Los Directores, Dr. Sergio Sánchez Moral Dr. Juan Carlos Cañaveras Jiménez Agradezco... Esta Tesis Doctoral no tiene un carácter estrictamente individual. La naturaleza multidisciplinar del trabajo ha requerido, para su desarrollo y consecución, la colaboración y el apoyo de numerosas personas y de diversas instituciones. Así, yo siento que, para ser justos, junto al nombre de la autora principal debería incluirse un amplio et al. Sergio Sánchez Moral y Juan Carlos Cañaveras Jiménez, directores de la tesis, son los indudables inspi- radores y promotores de este trabajo, coautores esenciales, y claves de que haya ocurrido y de que haya llegado a su fin. Son tremendos profesionales y magníficas personas, y he sido afortunada por tenerlos como mentores. El resultado de este trabajo es, además, fruto de una estrecha colaboración con otros grupos de investigación: • En el IRNAS-CSIC, Cesáreo Sáiz Jiménez y su equipo (Juan González Grau, Valme Jurado y Mª Carmen Portillo, etc.) han desarrollado los estudios microbiológicos, imprenscindibles para una correcta aproxi- mación geomicrobiológica. • En la Universidad de Granada, Andrew S. Kowalsky y Penélope Serrano Ortíz, han realizado el trata- miento de los datos de los flujos de CO2, fundamentales en el estudio de los procesos de comunica- ción cavidad/exterior. • En el Laboratorio de Petrología Aplicada de la Universidad de Alicante, David Benavente ha supervisa- do los análisis petrofísicos, que han permitido identificar el papel de las membranas de interconexión. En los laboratorios del Departamento de Geología del MNCN-CSIC se han realizado gran parte de los aná- lisis de materiales y aguas: los análisis mineralógicos y geoquímicos han sido realizados por Rafael González; la preparación de muestras y elaboración de láminas delgadas estuvo a cargo de Manuel Castillejo y José Mª Hontoria; Mª Angeles Fernández llevó a cabo los análisis granulométricos; los análi- sis hidrogeoquímicos fueron desarrollados por Mª Isabel Ruíz, Mª Asunción Vallejo y Roberto García. El extenso trabajo de microscopía electrónica se ha realizado con la ayuda técnica de Laura Tormo y Marta Furió, y con la permanente inspiración de Josefo Bedoya. Colaboraciones especiales, que han supuesto una gran aportación en este trabajo son las de: - Javier Elez, en los temas de SIG, 3D y trabajo de campo, entre otras muchas; - Marta Tárraga y Ángel Fernández Cortés, en el tratamiento estadístico de los datos; y - Enrique Sanz Rubio, en la geología, en las correcciones de texto y en ni se sabe cuantas cosas más. Añadir a Ana y Rafa, laRana, artífices de la estética y el orden de este "tocho", y principales responsables de que haya quedado realmente bien. Agradezco profunda y sinceramente el esfuerzo y la calidad de todas estas personas y, por ello, deseo dejar constancia de su inestimable colaboración en este trabajo. En el ámbito del Museo Nacional y Centro de Investigación de Altamira agradezco la constante colabora- ción del director José Antonio Lasheras y la conservadora Carmen de las Heras. Asimismo, a los acompa- ñantes en las innumerables horas de trabajo en la cueva (MªLuisa, MªFe, Begoña, Isabel, Alfredo, Abelardo, etc.), a los de seguridad, y al personal de cafetería, agradezco su buena disposición, su ayuda y su amabilidad. El apoyo de los compañeros de cañas, de los compañeros de batalla y de diversas amistades de la vida, ha sido una fuente de energía constante e indispensable. Colaboradores indirectos son también mis seres más queridos, mis amigos del alma y mi pequeña gran familia. Hacia ellos siento una gratitud especial ya que, a pesar de mis prolongadas ausencias, me han brindado siempre sus afectos, una extrema comprensión y apoyo incondicional. Con todo mi cariño y un profundo agradecimiento a todos, doy pie al comienzo de esta Tesis Doctoral. Índice Prólogo ............................................................................................................................................................9 Capítulo 1. Introducción: contextualización y fundamentos del estudio ..........................................................................11 Karst ....................................................................................................................................................13 Cavidades kársticas someras y dinámica microambiental ............................................................................16 Perfil kárstico ..............................................................................................................................16 Intercambios de materia y energía..................................................................................................17 Definición del sistema geoquímico ..................................................................................................20 Factores físico-químicos y parámetros microambientales principales ..................................................22 a) CO2 (en aire y agua) ......................................................................................................22 b) Temperatura (aire, roca-suelo, agua) ................................................................................24 c) Presión ........................................................................................................................25 d) Humedad del aire............................................................................................................25 e) Concentración de 222Rn en aire ........................................................................................26 f) Las aguas de infiltración kárstica ......................................................................................26 g) La presencia de microorganismos en el ambiente kárstico ....................................................27 Vulnerabilidad de la cavidad kárstica frente a actividades antrópicas ..................................................29 Antecedentes de los estudios microambientales en cavidades kársticas someras.............................................32 Investigación y Conservación en Altamira. ................................................................................................37 Capítulo 2. Objetivos y métodos ..............................................................................................................................45 Objetivos del estudio...............................................................................................................................45 Métodos empleados ..............................................................................................................................48 Trabajo de campo. ........................................................................................................................48 Técnicas de monitorización microambiental ......................................................................................49 > Procesado y análisis de los datos. Tratamiento estadístico.....................................................52 Técnicas hidroquímicas ................................................................................................................53 Estudio y tratamiento de materiales ................................................................................................54 > Estudio sedimentológico ..................................................................................................54 > Técnicas petrográficas ......................................................................................................55 • Microscopía óptica convencional • Microscopía óptica de alta resolución > Técnicas mineralógicas ....................................................................................................56
Recommended publications
  • 40 000 Years in the Greater Eastern Cape, South Africa
    Late Quaternary environmental phases in the Eastern Cape and adjacent Plettenberg Bay-Knysna region and Little Karoo, South Africa Colin A. Lewis Department of Geography, Rhodes University, Grahamstown 6140, South Africa Tel: +27 46 6222416, Fax: +27 46 6361199 e-mail: [email protected] ABSTRACT Four major climato-environmental phases have been identified in the Eastern Cape, Plettenberg Bay-Knysna region and Little Karoo between somewhat before ~ 40 000 cal. a BP and the present: the Birnam Interstadial from before 40 000 cal. a BP until ~ 24 000 cal. a BP; the Bottelnek Stadial (apparently equating with the Last Glacial Maximum) from ~24 000 cal. a BP until before ~ 18 350 cal. a BP; the Aliwal North (apparently equating with the Late Glacial) from before ~ 18 350 cal. a BP until ~ 11 000 cal. a BP; the Dinorben (apparently equating with the Holocene) from ~ 11 000 cal. a BP until the present. The evidence for, and the characteristics of, these phases is briefly described. Key words Palaeoclimate. Southern Africa. Late Quaternary. Last Glacial Maximum. Late Glacial. Holocene. 1. Introduction 1.1. Purpose of this paper and use of proxy data The purpose of this paper is to summarise the evidence for, and describe the characteristics of, the major climato-environmental phases that have occurred in the Eastern Cape and adjacent Plettenberg Bay-Knysna region and Little Karoo during the last ~ 40 000 a (Fig. 1). The age of these phases has been established mainly by radiocarbon dating. Events predating ~ 40 000 cal. a BP are effectively beyond the range of radiocarbon dating and are not considered in this paper.
    [Show full text]
  • Cave Research Foundation
    CAVE RESEARCH FOUNDATION QUARTERLY NEWSLETTER FEBRUARY 2 005 VOLUME 33, NO. 1 SPOTLIGHT ON MAMMOTH CAVE See Mammoth Cave Expedition Reports, pages 6-11 2 CRF NEWSLETTER Annual Report Submission Guidelines for 2004 Volume 33, No.I The Cave Research Foundation solicits reports established 1973 from CRF operations areas, research expeditions, pro­ Send all articles and reports for submission to: jects, and sponsored scientific and historical research William Payne, Editor projects for the 2004 Annual Report. The deadline for 5213 Brazos Midland, TX 79707-3161 submissions is March 1, 2005. Maps, photos, line drawings, charts, tables and The CRF Newsletter is a quarterly publication of the other images are an important part of the report and Cave Research Foundation, a non-profit organization should be chosen and prepared with the goal of com­ incorporated in 1957 under the laws of Kentucky for the municating significant achievements and discoveries purpose of furthering research, conservation, and during 2004. education about caves and karst. A new feature for the 2004 Annual Report will be Newsletter Submissions & Deadlines: the limited inclusion of color photos. High quality, Original articles and photographs are welcome. If intending to jointly submit material to another publication, please in­ high-resolution photos will be needed for the front and form the CRF editor. Publication cannot be guaranteed, espe­ back covers. If enough high-quality submissions are cially if submitted elsewhere. All material is subject to revi­ received and the printing budget warrants it, there may sion unless the author specifically requests otherwise. For be a color plate insert in the report.
    [Show full text]
  • TITLE PAGE.Wpd
    Proceedings of BAT GATE DESIGN: A TECHNICAL INTERACTIVE FORUM Held at Red Lion Hotel Austin, Texas March 4-6, 2002 BAT CONSERVATION INTERNATIONAL Edited by: Kimery C. Vories Dianne Throgmorton Proceedings of Bat Gate Design: A Technical Interactive Forum Proceedings of Bat Gate Design: A Technical Interactive Forum held March 4 -6, 2002 at the Red Lion Hotel, Austin, Texas Edited by: Kimery C. Vories Dianne Throgmorton Published by U.S. Department of Interior, Office of Surface Mining, Alton, Illinois and Coal Research Center, Southern Illinois University, Carbondale, Illinois U.S. Department of Interior, Office of Surface Mining, Alton, Illinois Coal Research Center, Southern Illinois University, Carbondale, Illinois Copyright 2002 by the Office of Surface Mining. All rights reserved. Printed in the United States of America 8 7 6 5 4 3 2 1 Library of Congress Cataloging-in-Publication Data Bat Gate Design: A Technical Interactive Forum (2002: Austin, Texas) Proceedings of Bat Gate Design: Red Lion Hotel, Austin, Texas, March 4-6, 2002/ edited by Kimery C. Vories, Dianne Throgmorton; sponsored by U.S. Dept. of the Interior, Office of Surface Mining and Fish and Wildlife Service, Bat Conservation International, the National Cave and Karst Management Symposium, USDA Natural Resources Conservation Service, the National Speleological Society, Texas Parks and Wildlife, the Lower Colorado River Authority, the Indiana Karst Conservancy, and Coal Research Center, Southern Illinois University at Carbondale. p. cm. Includes bibliographical references. ISBN 1-885189-05-2 1. Bat ConservationBUnited States Congresses. 2. Bat Gate Design BUnited States Congresses. 3. Cave Management BUnited State Congresses. 4. Strip miningBEnvironmental aspectsBUnited States Congresses.
    [Show full text]
  • Bat Caves in Fiji
    Bat caves in Fiji Status and conservation of roosting caves of the Fiji blossom bat (Notopteris macdonaldi), the Pacific sheath-tailed bat (Emballonura semicaudata) and the Fiji free-tailed bat (Chaerephon bregullae). Joanne Malotaux NatureFiji-MareqetiViti July 2012 Bat caves in Fiji Status and conservation of roosting caves of the Fiji blossom bat (Notopteris macdonaldi), the Pacific sheath-tailed bat (Emballonura semicaudata) and the Fiji free-tailed bat (Chaerephon bregullae). Report number: 2012-15 Date: 27th June 2012 Prepared by: Joanne Malotaux, intern at NatureFiji-MareqetiViti NatureFiji-MareqetiViti 14 Hamilton-Beattie Street Suva, Fiji Cover page picture: Wailotua cave. © Joanne Malotaux. 1 CONTENTS Introduction ............................................................................................................................................. 3 Chapter 1. Cave-dwelling bat species...................................................................................................... 4 Fiji blossom bat .................................................................................................................................... 4 Pacific sheath-tailed bat ...................................................................................................................... 5 Fiji free-tailed bat ................................................................................................................................ 6 Chapter 2. General recommendations ...................................................................................................
    [Show full text]
  • The Stable Isotope Setting of Australopithecus Sediba at Malapa
    Research Article Malapa cave stable isotopes Page 1 of 9 The stable isotope setting of Australopithecus AUTHORS: sediba at Malapa, South Africa Emily Holt1 Paul Dirks1,2,3 13 18 Christa Placzek1 We report δ C and δ O results from carbonate-cemented cave sediments at Malapa in South Africa. Lee Berger2 The sediments were deposited during a short-period magnetic reversal at 1.977±0.003 Ma, immediately preceding deposition of Facies D sediments that contain the type fossils of Australopithecus sediba. Values AFFILIATIONS: of δ13C range between -5.65 and -2.09 with an average of -4.58±0.54‰ (Vienna Pee Dee Belemnite, 1Department of Geosciences, VPDB) and values of δ18O range between -6.14 and -3.84 with an average of -4.93±0.44‰ (VPDB). College of Science and Despite signs of diagenetic alteration from metastable aragonite to calcite, the Malapa isotope values are Engineering, James Cook University, Queensland, Australia similar to those obtained in two previous studies in South Africa for the same relative time period. Broadly, 13 2Evolutionary Studies Institute, the Malapa δ C values provide constraints on the palaeovegetation at Malapa. Because of the complex DST/NRF Centre of Excellence in nature of the carbonate cements and mixed mineralogy in the samples, our estimates of vegetation type Palaeosciences, University of the (C -dominant) must be regarded as preliminary only. However, the indication of a mainly C landscape is in Witwatersrand, Johannesburg, 4 4 contrast to the reported diet of A. sediba, and suggests a diverse environment involving both grassland and South Africa riparian woodland.
    [Show full text]
  • Some Unintended Results of Blanket Cave Closures: a Story About Fern Cave Jennifer Pinkley
    Some Unintended Results of Blanket Cave Closures: a Story about Fern Cave Jennifer Pinkley The first time I visited Alabama’s Fern Along the way, explorers found beauti- Grotto members about gray bats and the Cave, I thought of the Mines of Moria in ful and rare helictites, gypsum crystals that need to avoid disturbing them. The Grotto JRR Tolkien’s Middle Earth: vast beyond look like giant corn flakes, huge dogtooth started to get the word out that cavers should imagining. As I moved through the cave, it spar calcite formations, rimstone dams, stay out of the approximately three miles of seemed that around every corner I discovered towering flowstone, giant rooms, deep pits, Morgue passage of the cave in the winter. another passage, another canyon, another cave pearls, and stream passage. In obscure Cavers complied. The bats thrived. path to explore. On that first bewildering rooms, cavers found bones of extinct animals trip, I visited Helictite Heaven, one of the that roamed the earth over 13,000 years MAnAgeMent under tHe us FisH And most beautiful and bizarre rooms not only in ago, including giant-sized varieties of cave WiLdLiFe serviCe Fern, but in any cave I’ve ever visited. Weird bears, armadillos, and lions. Hidden in the In 1980, the US Fish and Wildlife rock forms sprout out of the floors, walls and mud were also jaguar teeth, a horse tooth, Service (FWS) purchased all of the entrances ceilings like mutant, sparkling coral bushes. and a 2,400-year-old human jawbone. to Fern, except Surprise Pit, to protect the After that trip, I was hooked.
    [Show full text]
  • Site Management Plan, Medford District BLM
    TABLE OF CONTENTS I. Background ............................................................................................................................... 3 II. Life History .............................................................................................................................. 4 Habitat Associations ................................................................................................................... 4 Roosting Ecology ........................................................................................................................ 4 Foraging Behavior, Habitat, and Diet ......................................................................................... 6 Reproduction and Development ................................................................................................. 6 Behavioral ecology ..................................................................................................................... 7 III. Threats..................................................................................................................................... 7 IV. General Management Direction for Townsend’s Big-eared Bat Roost Sites ........................ 8 V. Grants Pass Resource Area Sites .......................................................................................... 10 Oak Mine .................................................................................................................................. 10 Gopher / Baby / Lamb Mine ....................................................................................................
    [Show full text]
  • Cave Research Foundation Annual Report - 2001-2003
    Cave Research Foundation Annual Report - 2001-2003 1 Cave Research Foundation Annual Report - 2001-2003 2 Cave Research Foundation Annual Report - 2001-2003 Annual Reports 2001-2003 Cave Research Foundation 177 Hamilton Valley Road Cave City, Kentucky 42127 Cave Research Foundation Cave Research 3 Cave Research Foundation Annual Report - 2001-2003 The Cave Research Foundation (CRF) is a private non-profit organization incorporated in 1957 under the laws of the Commonwealth of Kentucky. Its purpose is to: Facilitate research, management, and interpretation of caves and karst resources Form partnerships to study, protect and preserve cave resources and karst areas Promote the long-term conservation of caves and karst resources Editors: Patricia Kambesis Elizabeth Winkler Hoffman Environmental Research Institute 238 Tyler Court Western Kentucky University Smiths Groves, Kentucky 42171 1906 College Heights Blvd. Bowling Green, Kentucky 42101 Hawkins River at the Amos Hawkins Formation, Mammoth Cave Cover layout and photo: Gary Berdeaux Cave Research Foundation 2001-2003 Annual Report c by the Cave Research Foundation, Inc. Permission is granted to reproduce this material for scientific and educational use only. For information contact CRF, 177 Hamilton Valley Road, Cave City, KY 42127-45424 ISBN 978-0-939748-59-4 Published by Cave Books 4700 Amberwood Drive Dayton, Ohio 45424 4 Cave Research Foundation Annual Report - 2001-2003 Table of Contents Cave Research Foundation Activities 2001 2001 Highlights ..............................................................................................................................................................
    [Show full text]
  • Humanity from African Naissance to Coming Millennia” Arises out of the World’S First G
    copertina2 12-12-2000 12:55 Seite 1 “Humanity from African Naissance to Coming Millennia” arises out of the world’s first J. A. Moggi-Cecchi Doyle G. A. Raath M. Tobias V. P. Dual Congress that was held at Sun City, South Africa, from 28th June to 4th July 1998. “Dual Congress” refers to a conjoint, integrated meeting of two international scientific Humanity associations, the International Association for the Study of Human Palaeontology - IV Congress - and the International Association of Human Biologists. As part of the Dual Congress, 18 Colloquia were arranged, comprising invited speakers on human evolu- from African Naissance tionary aspects and on the living populations. This volume includes 39 refereed papers from these 18 colloquia. The contributions have been classified in eight parts covering to Coming Millennia a wide range of topics, from Human Biology, Human Evolution (Emerging Homo, Evolving Homo, Early Modern Humans), Dating, Taxonomy and Systematics, Diet, Brain Evolution. The book offers the most recent analyses and interpretations in diff rent areas of evolutionary anthropology, and will serve well both students and specia- lists in human evolution and human biology. Editors Humanity from African Humanity Naissance from to Coming Millennia Phillip V. Tobias Phillip V. Tobias is Professor Emeritus at the University of the Witwatersrand, Johannesburg, where he Michael A. Raath obtained his medical doctorate, PhD and DSc and where he served as Chair of the Department of Anatomy for 32 years. He has carried out researches on mammalian chromosomes, human biology of the peoples of Jacopo Moggi-Cecchi Southern Africa, secular trends, somatotypes, hominin evolution, the history of anatomy and anthropology.
    [Show full text]
  • Agency Guide to Cave and Mine Gates 2009
    Agency Guide to Cave and Mine Gates 2009 Jerry Fant, American Cave Conservation Association Jim Kennedy, Bat Conservation International Roy Powers, Jr., American Cave Conservation Association William Elliott, Missouri Department of Conservation Agency Guide to Cave and Mine Gates August 2009 Jerry Fant (ACCA) Jim Kennedy (BCI) Roy Powers, Jr. (ACCA) William Elliott (MDC) Sponsored by: American Cave Conservation Association Bat Conservation International Missouri Department of Conservation Contents: Introduction 1 Why gate? 2 Placement of gates and variations on the standard design 4 Gate Design Specifications 8 Construction timing 10 Gate Contractors 11 Post-gating Actions 12 Resources 13 Selected reading live 15 Introduction This guide is not intended to become a how-to manual on building gates to protect cave and mine resources, or to reduce liability at those sites, particularly abandoned mines. It is, however, intended to guide resource managers in making the best decisions on why, how, when, and who should build such gates. Over the years many hundreds, if not thousands, of gates have been constructed across the United States to secure cave and mine entrances. Some are good, being both secure and ecologically transparent. Others, poorly planned and designed, have had severe detrimental effects on the very resources they were built to protect. Over the years, much research by the American Cave Conservation Association, Bat Conservation International, and the US Fish and Wildlife Service has helped aid in the evolution of cave and mine gates, to the point where we now know what features are essential. An “industry standard” design with variations is now widely accepted by the National Park Service, US Fish and Wildlife Service, Bureau of Land Management, US Forest Service, NGOs such as The Nature Conservancy and the National Speleological Society, and many state wildlife agencies and conservation departments.
    [Show full text]
  • High Resolution
    2 CRF NEWSLETTER CRF Benefits from Amazon Volume 49, No. 3 Donation Program established 1973 Send all articles and reports for submission to: By: Bob Hoke, CRF Treasurer Laura Lexander, Editor Amazon.com now has a program, called Am- [email protected] azonSmile, that allows customers to specify a 21551 SE 273rd Ct., Maple Valley, WA 98038 charity that will receive a donation of 0.5% of the purchase price of many products purchased The CRF Newsletter is a quarterly publication of the Cave on Amazon.com. CRF is registered with Ama- Research Foundation, a non-profit organization incorpo- zonSmile so you can specify that CRF receive a rated in 1957 under the laws of Kentucky for the purpose donation if your purchase is eligible. The dona- of furthering research, conservation, and education about tion is made by Amazon and is not added to the caves and karst. cost of your purchase. Newsletter Submissions & Deadlines: CRF became part of the AmazonSmile pro- Original articles and photographs are welcome. If intend- gram in mid -2014 and as of May 2021, we have ing to jointly submit material to another publication, please received a total of $1,158 from it. The money is inform the CRF editor. Publication cannot be guaranteed, used to offset some of the Foundations adminis- especially if submitted elsewhere. All material is subject to trative expenses. revision unless the author specifically requests otherwise. To enable donations for your purchases, go For timely publication, please observe these deadlines: to Smile.Amazon.com instead of Amazon.com. The first time you will be asked to select a char- February issue by December 1 it y so just enter “Cave Research Foundation, May issue by March 1 Inc.” and select it.
    [Show full text]
  • Concerning a Cupule Sequence on the Edge of the Kalahari Desert in South Africa
    Rock Art Research 2015 - Volume 32, Number 2, pp. 163-177. P. B. BEAUMONT and R. G. BEDNARIK 163 KEYWORDS: Cupule – Age estimate – Palaeoenvironment – Tswalu Kalahari Reserve – South Africa CONCERNING A CUPULE SEQUENCE ON THE EDGE OF THE KALAHARI DESERT IN SOUTH AFRICA Peter B. Beaumont and Robert G. Bednarik Abstract. The Tswalu Reserve in the southern Kalahari is an arid place, the present occupation of which is only made possible by means of boreholes that tap patches of fossil water, while semi-permanent surface sources of ~65 m2 extent are confined to three localities within an investigated area of over 1000 km2. Lithic evidence indicates that this vicinity was abandoned by humans during even drier Ice Age intervals, when rainfall fell at times to ~40% of present values, thereby providing a way to refer petroglyphs there to interglacials of known age and intensity in terms of regional and global paleaoclimatic data. By such means, together with microerosion measurements, it then becomes possible to identify three regional cupule production intervals: the earliest with cupules only at ~410–400 ka bp, the next with cupules and outline circles at ~130–115 ka ago, and the most recent, with cupules, geometric motifs and iconic images, at ~8–2 ka bp. Introduction then, but the later dating of various regional sites (Miller Cupules are manmade, roughly semi-hemispherical 1971; Sampson 1974) placed the artefact level between depressions, not normally more than ~8 cm in diame- ~25 and 13 cal ka ago (Weninger and Jöris 2008), and it ter, that were produced on hard rock surfaces by is consequently considered probable that the Chifubwa hammerstone percussion (Kumar and Krishna 2014), petroglyphs were made at some time within that reportedly supplemented or replaced on softer stones interval (Clark 1958).
    [Show full text]