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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. -
Triásico Superior-Jurásico Inferior) Y Efusivas De La Formación Nogontova (Macizo De Santander, Colombia)
vol. 43, n.° 1, enero-abril de 2021 ISSN impreso: 0120-0283 ISSN en línea: 2145-8553 Petrografía y geoquímica de las rocas piroclásticas y efusivas de la Formación Bocas (Triásico Superior- Jurásico Inferior) y efusivas de la Formación Nogontova (Macizo de Santander, Colombia) Luz Mary Toro-Toro1* ; John Jairo Cardona-Ríos1 ; Mario Moreno-Sánchez1 ; Arley de Jesús Gómez-Cruz1 Forma de citar: Toro-Toro, L.M.; Cardona-Ríos, J.J.; Moreno-Sánchez, M.; Gómez-Cruz, A. de J. (2021). Petrografía y geoquímica de las rocas piroclásticas y efusivas de la Formación Bocas (Triásico Superior-Jurásico Inferior) y efusivas de la Formación Nogontova (Macizo de Santander, Colombia). Boletín de Geología, 43(1), 53-75. https://doi.org/10.18273/revbol.v43n1-2021003 Resumen La secuencia de rocas volcánicas y volcano-sedimentarias reportadas en el segmento superior de la Formación Bocas, subyacen sedimentos rojos de la Formación Jordán, está constituida por derrames de lavas máficas a intermedias y rocas piroclásticas félsicas interestratificadas con lodolitas, areniscas y areniscas tobáceas. En este trabajo se exponen nuevos datos de campo, petrográficos y geoquímicos de una secuencia volcánica máfica y volcanoclástica félsica. En cercanías al corregimiento Las Bocas, las rocas básicas presentan bajos contenidos TiO2 (1,04 - 1,65% peso) y P2O5 (0,3 - 0,7% peso) y altos contenidos de Al2O3 (15,79 - 15,92% peso), dentro de las series toleíticas; estas rocas se caracterizan por tener un leve enriquecimiento de LREE, anomalías positivas en Th, U y Zr y anomalías negativas en Nb, Ta y Ti con tendencias de ambiente MORB. Las rocas félsicas que corresponden a rocas piroclásticas de composición riolítica están enriquecidas en álcalis y LREE con anomalías negativas Ba, Sr, Nb, Ta y Ti y enriquecimiento moderado en LREE con un patrón característicos de intraplaca. -
Late Jurassic Syn-Extensional Sedimentary Deposition and Cenozoic Basin Inversion As Recorded in the Girón Formation, Northern Andes of Colombia
Andean Geology 48 (2): 237-266. May, 2021 Andean Geology doi: 10.5027/andgeoV48n2-3264 www.andeangeology.cl Late Jurassic syn-extensional sedimentary deposition and Cenozoic basin inversion as recorded in The Girón Formation, northern Andes of Colombia *Diego Osorio-Afanador1, 2, Francisco Velandia1 1 Escuela de Geología, Universidad Industrial de Santander, Cra. 27 calle 9, Bucaramanga, Colombia. [email protected], [email protected] 2 Posgrado en Ciencias de La Tierra, Centro de Geociencias, Universidad Nacional Autónoma de México, Campus Juriquilla, Querétaro, México. [email protected] * Corresponding author: [email protected] ABSTRACT. The Yariguíes Anticlinorium, a regional structure located at the western flank of the Eastern Cordillera of Colombia, includes the thickest record of continental sedimentary rocks accumulated near to the Jurassic-Cretaceous boundary. The sedimentary rocks are lithoarenites and feldspathic arenites, grouped in the Girón Formation, and deposited in a Late Jurassic extensional basin interpreted in this work as a rift basin. We analysed the sedimentologic and compositional characteristics of two sections that accumulated in a complex rift system. We identified important thickness variations, from 3,350 m in the type section to at least 525 m in a reference section in the Zapatoca area, as well as petrographic and lithofacies changes. This led us to confirm that the Girón Formation encompasses all the continental facies, whose source rock correspond mainly to the exhumed blocks of the Santander Massif during the Late Jurassic. The synrift successions were segmented by transverse structures and regional longitudinal faults of the rift-shoulder, as the Suárez Fault. The tectonic frame of the study area shows the relevance of the W-E compressional regimes, explaining the local kinematics as a heritage of the former configuration and tectonic inversion of the basins. -
Jurassic Evolution of the Northwestern Corner Published Online 28 April 2020 of Gondwana: Present Knowledge and Future
Volume 2 Quaternary Chapter 5 Neogene https://doi.org/10.32685/pub.esp.36.2019.05 Jurassic Evolution of the Northwestern Corner Published online 28 April 2020 of Gondwana: Present Knowledge and Future Challenges in Studying Colombian Jurassic Rocks Paleogene Germán BAYONA1* , Camilo BUSTAMANTE2 , Giovanny NOVA3 , 1 [email protected] Corporación Geológica ARES 4 and Ana Milena SALAZAR–FRANCO Calle 26 n.° 69C–03 Torre C Of. 904 Bogotá, Colombia Cretaceous Abstract This chapter summarizes knowledge (published up to February 2019) of meta- 2 [email protected] Universidad EAFIT morphic, plutonic, volcanic, carbonate, and clastic sedimentary Jurassic rocks that are Carrera 49 n.° 7 sur–50 exposed from northern Perú to Venezuela. This compilation allows an evaluation of Medellín, Colombia 3 [email protected] three tectonic models that have been proposed for the evolution of the northwestern Corporación Geológica ARES Jurassic corner of Gondwana: an extensional model, a subduction–dominated model, and the Calle 26 n.° 69C–03 Torre C Of. 904 Bogotá, Colombia along–marginal migration of blocks model, that last of which considers the interaction of 4 [email protected] western subduction and the north–south separation of continental blocks. We conclude Corporación Geológica ARES Calle 26 n.° 69C–03 Torre C Of. 904 that (1) the Jurassic evolution of this orthogonal margin cannot be represented in a single Bogotá, Colombia paleogeographic map that represents a dominant geodynamic process; (2) future anal- * Corresponding author Triassic yses must -
Évolution Néogène De La Partie Centrale Des Andes De Mérida (Venezuela): Analyse Structurale, Modélisation Géologique Et N
Évolution Néogène de la partie centrale des Andes de Mérida (Venezuela) : analyse structurale, modélisation géologique et numérique d’un système en échappement Bernard Monod To cite this version: Bernard Monod. Évolution Néogène de la partie centrale des Andes de Mérida (Venezuela) : analyse structurale, modélisation géologique et numérique d’un système en échappement. Géologie appliquée. Université de Pau et des Pays de l’Adour, 2009. Français. tel-00492032 HAL Id: tel-00492032 https://tel.archives-ouvertes.fr/tel-00492032 Submitted on 14 Jun 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Num´ero d’attribution `ala biblioth`eque | | | | | | | | | | | UNIVERSITE DE PAU ET DES PAYS DE L’ADOUR ECOLE DOCTORALE DES SCIENCES EXACTES ET DE LEURS APPLICATIONS THESE DE DOCTORAT Pr´esent´ee pour l’obtention du grade de DOCTEUR de l’Universit´ede Pau et des Pays de l’Adour (Sp´ecialit´eSciences de la Terre) par Bernard MONOD EVOLUTION NEOGENE DE LA PARTIE CENTRALE DES ANDES DE MERIDA (VENEZUELA) : ANALYSE STRUCTURALE, MODELISATION GEOLOGIQUE ET NUMERIQUE D’UN SYSTEME EN ECHAPPEMENT Soutenue publiquement le 3 novembre 2009 devant le jury compos´ede : M. Damien Dhont Maˆıtre de Conf´erences (HDR), Universit´ede Pau et Pays de l’Adour Directeur de th`ese M. -
Structural Evolution of the Northernmost Andes, Colombia
Structural Evolution of the Northernmost Andes, Colombia GEOLOGICAL SURVEY PROFESSIONAL PAPER 846 Prepared in coopeTation ·with the lnstituto Nacional de Investigaciones Geologico-MineTas under the auspices of the Government of Colombia and the Agency for International Development) United States DepaTtment of State Structural Evolution of the Northernmost Andes, Colombia By EARL M. IRVING GEOLOGICAL SURVEY PROFESSIONAL PAPER 846 Prepared in cooperation ·with the lnstituto Nacional de Investigaciones Geologico-Min eras under the auspices of the Government of Colombia and the Agency for International Development) United States Department of State An interpretation of the geologic history of a complex mountain system UNITED STATES GOVERNlVIENT PRINTING OFFICE, vVASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Irving, Earl Montgomery, 1911- Structural evolution of the northernmost Andes, Columbia. (Geological Survey professional paper ; 846) Bibliography: p Includes index. Supt. of Docs. no.: I 19.16:846 1. Geology-Colombia. 2. Geosynclines----Colombia. I. Instituto Nacional de Investigaciones Geologico Mineras.. II. Title. III. Series: United States. Geological Survey. Professional paper ; 846. QE239.175 558.61 74-600149 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $1.30 (paper cover) Stock Number 2401-02553 CONTENTS Page Pasre Abstract ---------------------------------------- -
The Millipedes and Centipedes of Chiapas Amber
14 4 ANNOTATED LIST OF SPECIES Check List 14 (4): 637–646 https://doi.org/10.15560/14.4.637 The millipedes and centipedes of Chiapas amber Francisco Riquelme1, Miguel Hernández-Patricio2 1 Laboratorio de Sistemática Molecular. Escuela de Estudios Superiores del Jicarero, Universidad Autónoma del Estado de Morelos, Jicarero C.P. 62909, Morelos, Mexico. 2 Subcoordinación de Inventarios Bióticos, Comisión Nacional para el Conocimiento y Uso de la Biodiversidad, Tlalpan C.P. 14010, Mexico City, Mexico. Corresponding author: Francisco Riquelme, [email protected] Abstract An inventory of fossil millipedes (class Diplopoda) and centipedes (class Chilopoda) from Miocene Chiapas amber, Mexico, is presented, with the inclusion of new records. For Diplopoda, 34 members are enumerated, for which 31 are described as new fossil records of the orders Siphonophorida Newport, 1844, Spirobolida Bollman, 1893, Polydesmida Leach, 1895, Stemmiulida Pocock, 1894, and the superorder Juliformia Attems, 1926. For Chilopoda 8 fossils are listed, for which 3 are new records of the order Geophilomorpha Pocock, 1895 and 2 are of the order Scolopendromorpha Pocock, 1895. Key words Miocene, Mexico, Diplopoda, Chilopoda. Academic editor: Peter Dekker | Received 14 May 2018 | Accepted 26 July 2018 | Published 10 August 2018 Citation: Riquelme F, Hernández-Patricio F (2018) The millipedes and centipedes of Chiapas amber. Check List 14 (4): 637–646. https://doi. org/10.15560/14.4.637 Introduction Diplopoda fossil record worldwide (Edgecombe 2015). Two other centipedes have been reported in Ross et al. The extant species of millipedes and centipedes distributed (2016). Other records of millipedes have been mentioned across Mexico have been studied since the initial reports in the literature but are questionable because of a lack of Brand (1839) and Persbosc (1839). -
Multi-Gene Phylogeny and Divergence Estimations for Evaniidae (Hymenoptera)
A peer-reviewed version of this preprint was published in PeerJ on 4 April 2019. View the peer-reviewed version (peerj.com/articles/6689), which is the preferred citable publication unless you specifically need to cite this preprint. Sharanowski BJ, Peixoto L, Dal Molin A, Deans AR. 2019. Multi-gene phylogeny and divergence estimations for Evaniidae (Hymenoptera) PeerJ 7:e6689 https://doi.org/10.7717/peerj.6689 Multi-gene phylogeny and divergence estimations for Evaniidae (Hymenoptera) Barbara J Sharanowski 1 , Leanne Peixoto 2 , Anamaria Dal Molin 3 , Andrew R Deans Corresp. 4 1 Department of Biology, University of Central Florida, Orlando, Florida, United States 2 Department of Agroecology, Aarhus University, Aarhus, Denmark 3 Departamento de Ciências Biológicas, Universidade Federal do Espírito Santo, Vitória, ES, Brazil 4 Frost Entomological Museum, Department of Entomology, Pennsylvania State University, University Park, PA, United States Corresponding Author: Andrew R Deans Email address: [email protected] Ensign wasps (Hymenoptera: Evaniidae) develop as predators of cockroach eggs (Blattodea), have a wide distribution and exhibit numerous interesting biological phenomena. The taxonomy of this lineage has been the subject of several recent, intensive efforts, but the lineage lacked a robust phylogeny. In this paper we present a new phylogeny, based on increased taxonomic sampling and data from six molecular markers (mitochondrial 16S and COI, and nuclear markers 28S, RPS23, CAD, and AM2), the latter used for the first time in phylogenetic reconstruction. Our intent is to provide a robust phylogeny that will stabilize and facilitate revision of the higher-level classification. We also show the continued utility of molecular motifs, especially the presence of an intron in the RPS23 fragments of certain taxa, to diagnose evaniid clades and assist with taxonomic classification. -
A Study of the Biology and Life History of Prosevania
A STUDY OF THE BIOLOGY AND LIFE HISTORY OF PROSEVANIA PUNCTATA (BRULLE) WITH NOTES ON ADDITIONAL SPECIES (HYMENOPTERA : EVANilDAE) DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Lafe R^ Edmunds,n 77 B.3., M.S. The Ohio State University 1952 Approved by: Adviser Table of Contents Introduction...................................... 1 The Family Evaniidae.............................. *+ Methods of Study...... 10 Field Studies. ........... .»..... 10 Laboratory Methods......... l*f Culturing of Blattidae.............. lU- Culturing of Evaniidae.............. 16 Methods of Studying the Immature Stages of Evaniidae............... 18 Methods for Handling Parasites Other than Evaniidae.............. 19 Biology of the Evaniidae.......................... 22 The Adult......................... 22 Emergence from the Ootheca.......... 22 Mating Behavior......... 2b Oviposition. ............ 26 Feeding Habits of Adults............ 29 Parthenogenetic Reproduction......... 30 Overwintering and Group Emergence.... 3b The Evaniidae as Household Pests*.... 36 General Adult Behavior.............. 37 The Immature Stages.......... 39 The Egg..... *f0 Larval Stages........... *+1 Pupal Stages ....... b$ 1 S29734 Seasonal Abundance. ••••••••••••••••...... ^9 Effect of Parasitism on the Host................. 52 Summary..................................... ...... 57 References. ...................... 59 Plates .......... 63 Biography........................................ -
Our New, Bolder Newsletter President's Report
Hamuli The Newsletter of the International Society of Hymenopterists volume 1, issue 1 2 August 2010 Our new, bolder newsletter In this issue... By: Andy Deans, North Carolina State University President’s report (Woolley) 1 Well, here it is—the inaugural issue of our new Soci- Webmaster/Archivist report (Seltmann) 3 ety newsletter, Hamuli. Before I dive too deeply into the Publishing on Hymenoptera (Agosti et al.) 4 details I want to acknowledge my associate editor, Trish Reflections on the future (Masner) 4 Mullins, who helped organize the newsletter, and especial- Report on the 7th ICH (Melika) 5 ly the talented contributors, who provided content. Thanks A student’s impression of 7th ICH (Talamas) 5 for helping make this enterprise happen! Australian checklist (Austin & Jennings) 5 Hamuli is an effort to revive the spirit of newsletters Sawfly research in China (Wei) 6 past—e.g., Sphecos, IchNews, Proctos, and Melissa— Sweeping Shrinkies (Heraty & Mottern) 7 an enthusiasm for communication that, if you’ve had Hints on scaning to PDF (Noyes) 8 the good fortune to read recent project newsletters, like Evaniid oviposition behaviors (Mullins & Bertone) 10 Skaphion and TIGER, still permeates through our com- Collecting in Măcin Mountains (Mitroiu) 11 munity. We anticipate publishing two issues per year, one Collecting in Kauai (Carpenter) 12 in January, and another in July, and we’re always accept- Collecting in China (Niu & Wei) 13 ing submissions that are relevant to ISH and Hymenoptera Jesus Santiago Moure (Dal Molin) 15 research more broadly, including member news (updates Member News 16 on projects, student opportunities, recent collecting ef- 7th ICH photos 18 forts), opinion and methods pieces, notes and photos from Membership information 19 the field, from museum visits, and from meetings, and just about any other content you can think of. -
Aportes Al Conocimiento Del Plutonismo Del Arco Mocoa- Santa Marta Durante El Jurásico Temprano-Medio, En La Margen Noroccidental De Los Andes, Colombia
vol. 42, n.° 3, septiembre-diciembre de 2020 ISSN impreso: 0120-0283 ISSN en línea: 2145-8553 Aportes al conocimiento del plutonismo del Arco Mocoa- Santa Marta durante el Jurásico Temprano-Medio, en la margen noroccidental de los Andes, Colombia Gabriel Rodríguez-García1* ; Juan Pablo Zapata1 ; Ana María Correa-Martínez1 ; Diego Armando Ramírez1 ; Gloria Obando1 Forma de citar: Rodríguez-García, G.; Zapata, J.P.; Correa-Martínez, A.M.; Ramírez, D.A.; Obando, G. (2020). Aportes al conocimiento del plutonismo del Arco Mocoa-Santa Marta durante el Jurásico Temprano-Medio, en la margen noroccidental de los Andes, Colombia. Boletín de Geología, 42(3), 15-50. https://doi.org/10.18273/revbol.v42n3-2020001 Material suplementario: Este artículo contiene Material suplementario (Tablas TS1, TS2, TS3, TS4, TS5, TS6 y TS7). Resumen A partir de la integración de información de campo, con datos petrográficos, geoquímicos de roca total, isotópicos y geocronológicos, se realizó la comparación de los diferentes segmentos que conforman el Arco Mocoa-Santa Marta (AMSM). Este arco, que aflora en el Valle Superior del Magdalena, la Serranía de San Lucas, la Sierra Nevada de Santa Marta y la Alta Guajira, se emplazó en un basamento Neo-proterozoico y en granitoides de un arco Pérmico, los cuales fueron posteriormente dispersados a lo largo de la Paleomargen Suramericana. El plutonismo del AMSM se caracteriza por la migración composicional en sentido W-E, con la formación de intrusivos de cuarzomonzonita, monzonita, charnoquita, tonalita y granodiorita hacia el occidente y la formación de plutones de monzogranito y sienogranito hacia el oriente; también existe un enriquecimiento en SiO2 en sentido S-N. -
Jahresbericht 2012
Staatliches Museum für Naturkunde Stuttgart Jahresbericht Sammeln Bewahren Forschen Vermitteln 12 Impressum Herausgeber Prof. Dr. Johanna Eder Direktorin Staatliches Museum für Naturkunde Stuttgart Rosenstein 1 70191 Stuttgart Redaktion M.Sc. Lena Kempener Staatliches Museum für Naturkunde Stuttgart Jahresbericht/Dokumentarische Ausgabe ISSN 2191-7817 Berichtsjahr 2012, erschienen 2013 Copyright Diese Zeitschrift ist urheberrechtlich geschützt. Eine Verwertung ist nur mit schriftlicher Genehmigung des Herausgebers gestattet. Inhaltsverzeichnis 2 INHALTSVERZEICHNIS EDITORIAL 4 1 FORSCHUNG 6 1.1 Forschungsprojekte 6 1.1.1 Drittmittel-finanziert 6 1.1.2 Nicht Drittmittel-finanziert 7 1.2 Umfangreiche Freilandarbeiten, Grabungen 13 1.3 Studienaufenthalte 14 1.4 Tagungsbeiträge 14 1.4.1 International 14 1.4.2 National 16 1.5 Sonstige wissenschaftliche Vorträge 17 1.6 Organisation von Tagungen und Workshops 18 1.7 Organisierte wissenschaftliche Exkursionen 19 1.8 Gastforscher 19 1.8.1 National 19 1.8.2 International 21 2 SAMMLUNG UND BIBLIOTHEK 24 2.1 Bedeutende Sammlungsarbeiten 24 2.1.1 Wissenschaftliche Arbeiten 24 2.1.2 Präparatorische und konservatorische Arbeiten 26 2.1.3 Elektronische Sammlungserfassung 28 2.2 Bedeutende Sammlungszugänge 28 2.3 Führungen hinter die Kulissen 30 2.4 Bibliothek und Archiv 32 3 BILDUNG UND ÖFFENTLICHKEITSARBEIT 32 3.1 Führungen und Projekte 32 3.1.1 Dauerausstellung 32 3.1.2 Sonderausstellung 33 3.1.3 Neues Begleitmaterial 33 3.2 Vorträge 33 3.2.1 Populärwissenschaftliche Vorträge 33 3.2.2 Vorträge an anderen