Gerardo A. Aymard C.1 & Lisa M. Campbell2 Caraipa Aublet
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Memorial to Carlos Schubert 1938-1994 THO M a S W
Memorial to Carlos Schubert 1938-1994 THO M A S W. DONNELLY Dept, o f Geological Sciences, State University o f New York, Binghamton, NY 13902-6000 Friends of Carlos Schubert Paetow were shocked and saddened upon hearing of his death in Caracas, Venezuela, on July 22, 1994, following an aneurism and a mesenteric stroke. Carlos, a longtime Fellow of the Geological Society of America, was one of the dominant figures of Venezuelan geology, specializing in his later years in neotectonics and in Quaternary geology. His untimely passing leaves a large void in Latin American—and in Quaternary—geology. His publications were voluminous and spanned a wide range of topics, but dominantly centered in Venezuelan studies. Carlos was bom in Hamburg, Germany, on October 9, 1938, and went to Caracas as an infant. He had a youthful interest in many subjects, but not especially in geology. His decision to pursue this field was the result of parental advice that geology and chemistry were the major fields of the future. Because he was uncom fortable with chemistry, he chose geology. Undoubtedly one of his important inspirations was the German explorer Alexander von Humboldt. Indeed, one of Carlos’s most prized possessions was his German 1815 edition of Humboldt’s Travels. In much of Carlos’s later work we can find a thread linking him to the founder of South American earth science. When he completed his high school studies in Caracas in 1957, he faced the problem that Pérez Jiménez, the president of Venezuela, had closed all Venezuelan universities. Fortunately, Carlos was awarded a scholarship from the Shell Oil Company to attend the University of Arizona, where he received his bachelor’s degree in geology in 1961. -
Mario Gomes1
Rodriguésia 63(4): 1157-1163. 2012 http://rodriguesia.jbrj.gov.br Nota Científica / Short Communication Kielmeyera aureovinosa (Calophyllaceae) – a new species from the Atlantic Rainforest in highlands of Rio de Janeiro state Kielmeyera aureovinosa (Calophyllaceae) - uma nova espécie da Mata Atlântica na região serrana do estado do Rio de Janeiro Mario Gomes1 Abstract Kielmeyera aureovinosa M. Gomes is a tree of the Atlantic Rainforest, endemic to the highlands of Rio de Janeiro state, occurring in riverine forest. The new species is distinguished in the genus by having a wine colored stem with metallic luster, peeling, with golden bands: it differs from other species of Kielmeyera section Callodendron by having leaves with sparse resinous corpuscles and flowers with ciliate margined sepals and petals. This paper provides a description of the species, illustrations and digital images; morphological and palynological features of Kielmeyera section Callodendron species are discussed and compared. Key words: Calophyllaceae, Kielmeyera aureovinosa, Atlantic Rainforest, riverine forest, Rio de Janeiro state. Resumo Kielmeyera aureovinosa M.Gomes é uma árvore da Mata Atlântica, endêmica da região serrana do estado do Rio de Janeiro, ocorrente em matas ciliares. A nova espécie é distinta das demais no gênero por ter caule de coloração vinoso-metálica, desfolhante, com faixas e nuances dourados; diferencia-se das demais espécies de Kielmeyera seção Callodendron por possuir folhas com corpúsculos resiníferos esparsos e flores com sépalas e pétalas de margens ciliadas. Este trabalho fornece descrição da espécie, estado de conservação, ilustrações esquemáticas e imagens digitais; características morfológicas e palinológicas das espécies de Kielmeyera seção Callodendron são discutidas e apresentadas em tabelas para comparação. -
The State of Venezuela's Forests
ArtePortada 25/06/2002 09:20 pm Page 1 GLOBAL FOREST WATCH (GFW) WORLD RESOURCES INSTITUTE (WRI) The State of Venezuela’s Forests ACOANA UNEG A Case Study of the Guayana Region PROVITA FUDENA FUNDACIÓN POLAR GLOBAL FOREST WATCH GLOBAL FOREST WATCH • A Case Study of the Guayana Region The State of Venezuela’s Forests. Forests. The State of Venezuela’s Págs i-xvi 25/06/2002 02:09 pm Page i The State of Venezuela’s Forests A Case Study of the Guayana Region A Global Forest Watch Report prepared by: Mariapía Bevilacqua, Lya Cárdenas, Ana Liz Flores, Lionel Hernández, Erick Lares B., Alexander Mansutti R., Marta Miranda, José Ochoa G., Militza Rodríguez, and Elizabeth Selig Págs i-xvi 25/06/2002 02:09 pm Page ii AUTHORS: Presentation Forest Cover and Protected Areas: Each World Resources Institute Mariapía Bevilacqua (ACOANA) report represents a timely, scholarly and Marta Miranda (WRI) treatment of a subject of public con- Wildlife: cern. WRI takes responsibility for José Ochoa G. (ACOANA/WCS) choosing the study topics and guar- anteeing its authors and researchers Man has become increasingly aware of the absolute need to preserve nature, and to respect biodiver- Non-Timber Forest Products: freedom of inquiry. It also solicits Lya Cárdenas and responds to the guidance of sity as the only way to assure permanence of life on Earth. Thus, it is urgent not only to study animal Logging: advisory panels and expert review- and plant species, and ecosystems, but also the inner harmony by which they are linked. Lionel Hernández (UNEG) ers. -
Calophyllaceae Da Bahia E Padrões De Distribuição De
AMANDA PRICILLA BATISTA SANTOS CALOPHYLLACEAE DA BAHIA E PADRÕES DE DISTRIBUIÇÃO DE KIELMEYERA NA MATA ATLÂNTICA FEIRA DE SANTANA – BAHIA 2015 UNIVERSIDADE ESTADUAL DE FEIRA DE SANTANA DEPARTAMENTO DE CIÊNCIAS BIOLÓGICAS PROGRAMA DE PÓS-GRADUAÇÃO EM BOTÂNICA CALOPHYLLACEAE DA BAHIA E PADRÕES DE DISTRIBUIÇÃO DE KIELMEYERA NA MATA ATLÂNTICA AMANDA PRICILLA BATISTA SANTOS Dissertação apresentada ao Programa de Pós- Graduação em Botânica da Universidade Estadual de Feira de Santana como parte dos requisitos para a obtenção do título de Mestre em Botânica. ORIENTADOR: PROF. DR. ALESSANDRO RAPINI (UEFS) FEIRA DE SANTANA – BAHIA 2015 Ficha Catalográfica – Biblioteca Central Julieta Carteado Santos, Amanda Pricilla Batista S233c Calophyllaceae da Bahia e padrões de distribuição de Kielmeyera na Mata Atlântica. – Feira de Santana, 2015. 121 f. : il. Orientador: Alessandro Rapini. Dissertação (mestrado) – Universidade Estadual de Feira de Santana, Programa de Pós-Graduação em Botânica, 2015. 1. Kielmeyera. 2. Calophyllaceae. 2. Florística – Bahia. I. Rapini, Alessandro, orient. II. Universidade Estadual de Feira de Santana. III. Título. CDU: 582(814.2) BANCA EXAMINADORA ________________________________________________________ Pedro Fiaschi ________________________________________________________ Daniela Santos Carneiro Torres ________________________________________________________ Prof. Dr. Alessandro Rapini Orientador e presidente da Banca FEIRA DE SANTANA – BAHIA 2015 Aos meus queridos pais, por todo apoio e incentivo, dedico. AGRADECIMENTOS -
The Venezuelan Hydrocarbon Habitat, Part 1: Tectonics, Structure, Palaeogeography and Source Rocks
Journal of Petroleum Geology, vo1.23(1), January 2000, pp 5-53. 5 THE VENEZUELAN HYDROCARBON HABITAT, PART 1: TECTONICS, STRUCTURE, PALAEOGEOGRAPHY AND SOURCE ROCKS K. H. James* Venezuela forms part of an important hydrocarbon province, defined by the presence of prolific Cretaceous source rocks, which extends across northern South America. By early 1997, the country had produced 53 billion barrels of oil. Reserves are estimated to total 73 billion barrels of oil and 146 TCF of gas with 250 billion barrels recoverable in the Heavy Oil Belt. Most reserves are located within the intermontane Maracaibo and foreland Barinas-Apure and Eastern Venezuela BasinxThey correspond to more than 1.5 trillion BOE originally in place. The province S hydrocarbon history began with a broad passive margin over which the sea transgressed throughout much ofthe Cretaceous. Limestones and shales followed basal sands and included rich source rocks. Convergence between the distal part of the area and the Caribbean Plate created an active margin that migrated southwards, so that flysch and wildflysch followed the transgressive facies. The process culminated in Lute Cretaceous to Middle Eocene orogeny with the emplacement of southward-vergent nappes and the development of northward-deepeningforedeeps. Flysch and wildflysch formed in the north while important deltaic - paralic reservoir sands accumulated in the south. Major phases of hydrocarbon generationfrom Jurassic-Cretaceoussource rocks occurred across the entire margin of northern South America during the orogeny. They are recorded by Jurassic - Middle Cretaceous graphitic marbles, schists and quartzites (metamorphosed, organic limestones and shales and oil-bearing sandstones) in the Coastal and Northern Ranges of Venezuela and Trinidad. -
Map and Database of Quaternary Faults in Venezuela and Its Offshore Regions
U.S. Department of the Interior U.S. Geological Survey Map and Database of Quaternary Faults in Venezuela and its Offshore Regions By Franck A. Audemard M., Michael N. Machette, Jonathan W. Cox, Richard L. Dart, and Kathleen M. Haller Open-File Report 00-018 (paper edition) This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards nor with the North American Stratigraphic Code. Any use of trade names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. 2000 Map and Database of Quaternary Faults in Venezuela and its Offshore Regions A project of the International Lithosphere Program Task Group II-2, Major Active Faults of the World Data and map compiled by 1 FRANCK A. AUDEMARD M., 2 MICHAEL N. MACHETTE, 2 JONATHAN W. COX, 2 RICHARD L. DART, AND 2 KATHLEEN M. HALLER 1 Fundación Venezolana de Investigaciones Sismológicas (FUNVISIS) Dpto. Ciencias de la Tierra, Prolongacion Calle Mara, El Llanito Caracas 1070-A, Venezuela 2 U.S. Geological Survey (USGS) Central Geologic Hazards Team MS 966, P.O. Box 25046 Denver, Colorado, USA Regional Coordinator for Central America CARLOS COSTA Universidad Nacional de San Luis Departmento de Geologia Casilla de Correo 320 San Luis, Argentina ILP Task Group II-2 Co-Chairman, Western Hemisphere MICHAEL MACHETTE U.S. Geological Survey (USGS) Central Geologic Hazards Team MS 966, P.O. Box 25046 Denver, Colorado, USA January 2000 version i TABLE OF CONTENTS PAGE INTRODUCTION...............................................................................................................................................................1 -
Tetonic Inheritance and Structural Styles in the Merida
Third ISAG, St Malo (France), 17-19/9/1996 TECTONIC INHERITANCE AND STRUCTURAL STYLES IN THE MERIDA ANDES (WESTERN VENEZUELA). Bernard COLLETTA( l ) , Franqois ROURE( l) Bruno DE TONI(~),Daniel LOLTREIRO(~)Herminio PASSALACQUA(~)~~~Yves GOU(~). (I hnstitut Franqais du PCtrole, BP3 1 1, 92506 Rueil-Malmaison, France (2)~ntevep,Apartado 76343, Caracas 1070-A, Venezuela (3)~eicipFranlab, 92506 Rueil-Malmaison, France KEY WORDS: Venezuela, Merida Andes, tectonic inversion, crustal scale balanced sections INTRODUCTION Unlike the adjacent Caribbean and Central Andean orogens, the Merida Andes (Fig. 1) do not relate to direct interactions between the South American craton and either arc terranes or oceanic domains, but represent only minor intraplate readjustements between the Eastern Cordillera in the south and the South Caribbean transform margin in the north.Although no deep seismic profiling has yet been attempted across the Venezuelan Andes, a large set of conventional seismic reflection profiles has been recorded by the petroleum industry in the Maracaibo and Barinas-Apure basins, respectively along the North and South Andean foothills. In addition, isolated refraction and magnetotelluric data are available. However, only the gravimetric coverage is really complete, thus providing a relatively coherent image of the basement architecture. STRUCTURE OF THE SOUTH ANDEAN FLANK The Barinas-Apure basin extends from the Andean foothills in the northwest to the Guyana shield in the southeast, thus encompassing most of the drainage area of the Rio Apure, a tributary of the Orinoco River. Southwards, it connects directly with the Llanos basin in Colombia. The Barinas basin hardly compares with a flexural basin. It is largely dominated by either north- or south-verging basement- involved structures. -
Late Quaternary Deglacial History of the Mérida Andes, Venezuela
JOURNAL OF QUATERNARY SCIENCE (in press) Copyright ß 2007 John Wiley & Sons, Ltd. Published online in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/jqs.1109 Correspondence the terminal and lateral moraines of the El Caballo and Reply: Late Quaternary deglacial La Mucuchache glaciers. A chemically untreated organic history of the Me´rida Andes, sample from 1.5 m above the base of the section yielded a conventional age of 22 750 cal. yr BP (19 000 14C yr BP), Venezuela: response whereas a peat sample immediately below the top of the section yielded an age of 19 960 cal. yr BP (16 500 14C yr BP). to comment We recognise that other workers (e.g. Mahaney et al., 2001, 2004; Dirszowsky et al., 2005) have re-analysed the Pedregal fan complex. For example, the sedimentology was described in detail by Dirszowsky et al. (2005). However, the chronology in We welcome the opportunity to respond to Mahaney et al.’s these papers is questionable and not useful for constraining the critique of our article on the deglacial history of the LGM. All of the recently published dates are on refractory Venezuelan Andes (Stansell et al., 2005). The source of our organic matter isolated using a cellulose extraction technique disagreement appears to stem primarily from differences in which concentrates refractory carbon, resulting in ages research strategies and methodology. Our work in the between 47 000 and 60 000 14C yr BP. These ages include mul- Venezuelan Andes employs lake sediment archives that record tiple reversals and are at the very edge of interpretability as continuous sedimentary sequences and can be dated using finite radiocarbon ages; nonetheless, the authors have inter- accelerator mass spectrometry (AMS) radiocarbon dating of preted them as valid ages. -
Andean Venezuelan
Venezuelan Andean Spanish Intonation Venezuelan Andean Spanish Intonation* Lluïsa Astruca, Elsa Morab and Simon Rewc The Open University and The University of Cambridgea Universidad de Los Andesb The University of Cambridgec 1. Introduction Lying in western Venezuela, the state of Mérida is traversed by the eastern branch of the northern Andes and has an area of 11,300 km2, which corresponds to approximately 1.2% of the national territory. The main economic activities of the region are agriculture and tourism. The city of Mérida itself has 300,000 inhabitants (2001 census) and constitutes a national cultural and university centre. The Universidad de Los Andes is a major source of employment in the region, specifically in the areas of teaching, research and services. The structure of this chapter is as follows. Section 1 first offers an overview of past intonational research in Venezuelan Spanish and especially in Venezuelan Andean Spanish and then describes the methodological procedure used in the present study. Section 2 presents an inventory of pitch accents and boundary tones found in the Mérida dialect. Section 3 analyses the basic intonation contours found in the Mérida corpus. Finally, Section 4 summarises the nuclear patterns in the different sentence types. The study of intonation does not have a long history in Venezuela and, furthermore, the rather scant research has been mostly oriented towards dialectology. The first study of the intonation of Venezuelan Spanish was published in the phonetics section of El habla de Caracas (Mosonyi 1971). A decade later, Obregón (1981) carried out a dialectal study in which he analysed the distribution of certain characteristic patterns (which he called construcciones entonativas) and which led him to propose a division into five dialectal areas: Mérida and Táchira (southwest), Maracaibo (northwest), Nueva Esparta and Sucre (east), Apure and Guárico (south) and the rest of the country (centre). -
Spring Shorebird Migration Through Central Venezuela
Wilson Bull., 99(4), 1987, pp. 571-578 SPRING SHOREBIRD MIGRATION THROUGH CENTRALVENEZUELA BETSY TRENT THOMAS ’ AnsrnAcr.-Nearctic-breeding shorebirds regularly migrate through the llanos of central Venezuela in the spring (March-May). At a single site, consisting of three feeding areas with a total of 3-5 ha, 10 species were recorded. Four migrating Least Sandpipers (Culidris minutilla) banded at this site were recaptured there in subsequent years. White-rumped Sandpipers (C. fusicollis) dyed and flagged in the Venezuelan llanos were observed a few weeks later, one in Texas and two in Kansas. Shorebird weights, numbers, passage times, and lengths of stay at the study site are given. Nearly all shorebirds had recently completed molt of remiges and rectrices, but none were in distinctive breeding plumages or colors. Received27 Jan. 1987, accepted4 June 1987. Although shorebird migration routes are relatively well known in North America, their passage routes in South America, where most species spend over half of their lives, are poorly understood. Recently, interest has increased in the welfare of migrant nearctic-breeding shorebirds because feeding and resting sites are limited and declining in both number and quality (Myers 1983, Senner and Howe 1984). I briefly sampled spring shorebirds on migration at a single site in 1982 and 1983. In 1983 I recaptured one of the 2 1 Least Sandpipers (Calidris minutilla) banded in the previous year. Because of this I decided to study in detail shorebird passage in 1984. Here, I give data on species, passage times, numbers, weights, molt, length of stay, and returns. STUDY AREA AND METHODS The site of most observations and all mist-netting was a 4000-ha cattle ranch, Fundo Pecuario Masaguaral, approximately central in the llanos of Venezuela (08”3 lN,’ 67”35W).’ A description of the vegetation of this ranch is in Troth (1979). -
Master in Biodiversity and Conservation in Tropical Regions
Master in Biodiversity and Conservation in Tropical Regions Biogeography and Conservation Status of Diurnal Raptors in Venezuela By Adrian Naveda-Rodríguez A thesis submitted In partial fulfillment of the requirements for the degree of Master of Science Advisor: Keith L. Bildstein, Ph.D. Academic year 2012 – 2013 ACKNOWLEDGMENTS This work was possible thanks to logistical and financial support provided by the Spanish Research Council (CSIC), Hawk Mountain Sanctuary, The Peregrine Fund and Wild4Ever. I wish to thank all those who contributed throughout the course of this work. I am absolutely indebted to my lovely wife Gabriela Lugo, my parents Maritza Rodriguez and Rafael Naveda who supported me in this process. I am very grateful to Dr. Keith Bildstein for introducing me to raptor conservation sciences and for all the opportunities he has given me since 2006. I am also grateful to Dr. Hernán Vargas and Dr. Gary Riggs for their confidence and support for this project. Marcial Quiroga-Carmona, José Gustavo León, Tony Crease, Alan Highton and Christian Olaciregui provided valuable information on raptors of Venezuela and Colombia. I sincerely appreciate the efforts of Marcial Quiroga-Carmona, Jorge Peralta and Bayron Calles for their help with statistical analyses. I appreciate the improvements in English usage made by Phillip Schwabl I kindly appreciate Francisco Bisbal, Alexis Araujo, Miguel Lentino, Jurahimar Gamboa, Marcos Salcedo, Carlos Rengifo and Rosana Calchi for providing information on voucher specimens in ornithological collections under their care. ABSTRACT Aim: Natural history data is crucial to monitor the vulnerability of birds of prey. In Venezuela, this information is non-existent for almost all species of raptors. -
Systematics and Biogeography of the Clusioid Clade (Malpighiales) Brad R
Eastern Kentucky University Encompass Biological Sciences Faculty and Staff Research Biological Sciences January 2011 Systematics and Biogeography of the Clusioid Clade (Malpighiales) Brad R. Ruhfel Eastern Kentucky University, [email protected] Follow this and additional works at: http://encompass.eku.edu/bio_fsresearch Part of the Plant Biology Commons Recommended Citation Ruhfel, Brad R., "Systematics and Biogeography of the Clusioid Clade (Malpighiales)" (2011). Biological Sciences Faculty and Staff Research. Paper 3. http://encompass.eku.edu/bio_fsresearch/3 This is brought to you for free and open access by the Biological Sciences at Encompass. It has been accepted for inclusion in Biological Sciences Faculty and Staff Research by an authorized administrator of Encompass. For more information, please contact [email protected]. HARVARD UNIVERSITY Graduate School of Arts and Sciences DISSERTATION ACCEPTANCE CERTIFICATE The undersigned, appointed by the Department of Organismic and Evolutionary Biology have examined a dissertation entitled Systematics and biogeography of the clusioid clade (Malpighiales) presented by Brad R. Ruhfel candidate for the degree of Doctor of Philosophy and hereby certify that it is worthy of acceptance. Signature Typed name: Prof. Charles C. Davis Signature ( ^^^M^ *-^£<& Typed name: Profy^ndrew I^4*ooll Signature / / l^'^ i •*" Typed name: Signature Typed name Signature ^ft/V ^VC^L • Typed name: Prof. Peter Sfe^cnS* Date: 29 April 2011 Systematics and biogeography of the clusioid clade (Malpighiales) A dissertation presented by Brad R. Ruhfel to The Department of Organismic and Evolutionary Biology in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of Biology Harvard University Cambridge, Massachusetts May 2011 UMI Number: 3462126 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted.