Доминиканский Янтарь Dominikanischer Bernstein Dominican Amber
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A New Macrolepidopteran Moth (Insecta, Lepidoptera, Geometridae) in Miocene Dominican Amber
ZooKeys 965: 73–84 (2020) A peer-reviewed open-access journal doi: 10.3897/zookeys.965.54461 RESEARCH ARTICLE https://zookeys.pensoft.net Launched to accelerate biodiversity research A new macrolepidopteran moth (Insecta, Lepidoptera, Geometridae) in Miocene Dominican amber Weiting Zhang1,2, Chungkun Shih3,4, YuHong Shih5, Dong Ren3 1 Hebei GEO University, 136 Huaiandonglu, Shijiazhuang 050031, China 2 State Key Laboratory of Pal- aeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, CAS, Nanjing 210008, China 3 College of Life Sciences and Academy for Multidisciplinary Studies, Capital Normal University, 105 Xisan- huanbeilu, Haidian District, Beijing 100048, China 4 Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20013-7012, USA 5 Laboratorio Dominicano De Ambar Y Gemas, Santo Domingo, Dominican Republic Corresponding author: Weiting Zhang ([email protected]) Academic editor: Gunnar Brehm | Received 19 May 2020 | Accepted 12 August 2020 | Published 3 September 2020 http://zoobank.org/05E273DB-B590-42D1-8234-864A787BE6A0 Citation: Zhang W, Shih C, Shih YH, Ren D (2020) A new macrolepidopteran moth (Insecta, Lepidoptera, Geometridae) in Miocene Dominican amber. ZooKeys 965: 73–84. https://doi.org/10.3897/zookeys.965.54461 Abstract A new genus and species of fossil moth, Miogeometrida chunjenshihi Zhang, Shih & Shih, gen. et sp. nov., assigned to Geometridae, is described from Miocene Dominican amber dating from 15–20 Mya. The new genus is characterized by the forewing without a fovea, R1 not anastomosing with Sc, no areole formed by veins R1 and Rs, R1 and Rs1 completely coincident, M2 arising midway between M1 and M3, anal veins 1A and 2A fused for their entire lengths; and the hind wing with Rs running close to Sc + R1 and M2 absent. -
Reglas De Congo: Palo Monte Mayombe) a Book by Lydia Cabrera an English Translation from the Spanish
THE KONGO RULE: THE PALO MONTE MAYOMBE WISDOM SOCIETY (REGLAS DE CONGO: PALO MONTE MAYOMBE) A BOOK BY LYDIA CABRERA AN ENGLISH TRANSLATION FROM THE SPANISH Donato Fhunsu A dissertation submitted to the faculty of the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of English and Comparative Literature (Comparative Literature). Chapel Hill 2016 Approved by: Inger S. B. Brodey Todd Ramón Ochoa Marsha S. Collins Tanya L. Shields Madeline G. Levine © 2016 Donato Fhunsu ALL RIGHTS RESERVED ii ABSTRACT Donato Fhunsu: The Kongo Rule: The Palo Monte Mayombe Wisdom Society (Reglas de Congo: Palo Monte Mayombe) A Book by Lydia Cabrera An English Translation from the Spanish (Under the direction of Inger S. B. Brodey and Todd Ramón Ochoa) This dissertation is a critical analysis and annotated translation, from Spanish into English, of the book Reglas de Congo: Palo Monte Mayombe, by the Cuban anthropologist, artist, and writer Lydia Cabrera (1899-1991). Cabrera’s text is a hybrid ethnographic book of religion, slave narratives (oral history), and folklore (songs, poetry) that she devoted to a group of Afro-Cubans known as “los Congos de Cuba,” descendants of the Africans who were brought to the Caribbean island of Cuba during the trans-Atlantic Ocean African slave trade from the former Kongo Kingdom, which occupied the present-day southwestern part of Congo-Kinshasa, Congo-Brazzaville, Cabinda, and northern Angola. The Kongo Kingdom had formal contact with Christianity through the Kingdom of Portugal as early as the 1490s. -
Lithology and Geochemistry of the Guadalupe Group Base Around Tunja, This Work Is Distributed Under the Creative Commons Attribution 4.0 License
Boletín Geológico, 47, 35-65, 2020 https://doi.org/10.32685/0120-1425/ boletingeo.47.2020.494 Lithology and geochemistry of the Guadalupe Group base around Tunja, This work is distributed under the Creative Commons Attribution 4.0 License. Boyacá, Colombia Received: May 12, 2020 Revised: July 27, 2020 Accepted: September 17, 2020 Litología y geoquímica de la base del Grupo Guadalupe, en los Published online: December 28, 2020 alrededores de Tunja, Boyacá, Colombia German Martínez Aparicio1, Pedro Patarroyo2 and Roberto Terraza Melo1 1. Servicio Geológico Colombiano, (SGC), Bogotá, Colombia. 2. Universidad Nacional de Colombia, (UNAL), Bogotá, Colombia. Corresponding author: German Martínez Aparicio, [email protected] Abstract The base of the Guadalupe Group, in the Tunja area of Colombia, contains cherts, porcellanites, mudstones, and siltstones with subordinate quartz arenites. The lithostratigraphic description of two stratigraphic sections showed that the dominant facies have fine granular textures and siliceous compositions, which considerably differ from those of the prevailing sandy terrigenous facies described in the type locality in the Eastern Hills of Bogotá, in the Arenisca Dura Formation, the basal unit of the Guadalupe Group in this sector. The units that form the Guadalupe Group (base of the Guadalupe Group, Plaeners, and Arenisca Tierna) markedly differ from each other morphologically, which facilitates their mapping because the base and top units generate a steep morphology, and the intermediate units form surface depressions or valleys, similar to the morphology of the Guadalupe Group in its type locality in the Eastern Hills of Bogotá. The base of the Guadalupe Group consists of cherts and porcellanites toward the NW of the study area (Alto del Gavilán section), with mudstones, siltstones, quartz arenites, and to a lesser extent porcellanites and cherts prevailing toward the SE (Vereda Salitre section). -
Rock Art of Latin America & the Caribbean
World Heritage Convention ROCK ART OF LATIN AMERICA & THE CARIBBEAN Thematic study June 2006 49-51 rue de la Fédération – 75015 Paris Tel +33 (0)1 45 67 67 70 – Fax +33 (0)1 45 66 06 22 www.icomos.org – [email protected] THEMATIC STUDY OF ROCK ART: LATIN AMERICA & THE CARIBBEAN ÉTUDE THÉMATIQUE DE L’ART RUPESTRE : AMÉRIQUE LATINE ET LES CARAÏBES Foreword Avant-propos ICOMOS Regional Thematic Studies on Études thématiques régionales de l’art Rock Art rupestre par l’ICOMOS ICOMOS is preparing a series of Regional L’ICOMOS prépare une série d’études Thematic Studies on Rock Art of which Latin thématiques régionales de l’art rupestre, dont America and the Caribbean is the first. These la première porte sur la région Amérique latine will amass data on regional characteristics in et Caraïbes. Ces études accumuleront des order to begin to link more strongly rock art données sur les caractéristiques régionales de images to social and economic circumstances, manière à préciser les liens qui existent entre and strong regional or local traits, particularly les images de l’art rupestre, les conditions religious or cultural traditions and beliefs. sociales et économiques et les caractéristiques régionales ou locales marquées, en particulier Rock art needs to be anchored as far as les croyances et les traditions religieuses et possible in a geo-cultural context. Its images culturelles. may be outstanding from an aesthetic point of view: more often their full significance is L’art rupestre doit être replacé autant que related to their links with the societies that possible dans son contexte géoculturel. -
Fossil Resins–Constraints from Portable and Laboratory Near-Infrared Raman Spectrometers
Article Fossil Resins–Constraints from Portable and Laboratory Near-infrared Raman Spectrometers Beata Naglik 1,*, Maja Mroczkowska-Szerszeń 2, Magdalena Dumańska-Słowik 3, Lucyna Natkaniec-Nowak 3, Przemysław Drzewicz 4, Paweł Stach 3 and Grażyna Żukowska 5 1 Polish Geological Institute-National Research Institute, Upper Silesian Branch, 1 Królowej Jadwigi Str., 41-200 Sosnowiec, Poland 2 Oil and Gas Institute-National Research Institute, 25A Lubicz Str., 31-503 Krakow, Poland; [email protected] 3 Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, 30 Mickiewicz Av., 30-059 Krakow, Poland; [email protected] (M.D.-S.); [email protected] (L.N.-N.); [email protected] (P.S.) 4 Polish Geological Institute-National Research Institute, 4 Rakowiecka Str., 00-975 Warsaw, Poland; [email protected] 5 Faculty of Chemistry, Warsaw University of Technology, 3 Noakowskiego Str., 00-664 Warsaw, Poland; [email protected] * Correspondence: [email protected] Received: 6 December 2019; Accepted: 17 January 2020; Published: 25 January 2020 Abstract: Comparative studies of fossil resins of various ages, botanical sources, geological environments, and provenience were provided via a handheld portable Near-Infrared (NIR)-Raman spectrometer and benchtop instrument both working with laser line 1064 nm. The recorded Raman spectra of individual fossil resins were found to be sufficiently similar irrespective to the device type applied, i.e., handheld or benchtop. Thus, the portable equipment was found to be a sufficient tool for the preliminary identification of resins based on botanical and geographical origin criteria. The observed height ratio of 1640/1440 cm−1 Raman bands did not correlate well with the ages of fossil resins. -
Molecular Phylogenetics and Evolution 82 (2015) 358–374
Molecular Phylogenetics and Evolution 82 (2015) 358–374 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev Biogeography in deep time – What do phylogenetics, geology, and paleoclimate tell us about early platyrrhine evolution? Richard F. Kay Department of Evolutionary Anthropology & Division of Earth and Ocean Sciences, Duke University, Box 90383, Durham, NC 27708, United States article info abstract Article history: Molecular data have converged on a consensus about the genus-level phylogeny of extant platyrrhine Available online 12 December 2013 monkeys, but for most extinct taxa and certainly for those older than the Pleistocene we must rely upon morphological evidence from fossils. This raises the question as to how well anatomical data mirror Keywords: molecular phylogenies and how best to deal with discrepancies between the molecular and morpholog- Platyrrhini ical data as we seek to extend our phylogenies to the placement of fossil taxa. Oligocene Here I present parsimony-based phylogenetic analyses of extant and fossil platyrrhines based on an Miocene anatomical dataset of 399 dental characters and osteological features of the cranium and postcranium. South America I sample 16 extant taxa (one from each platyrrhine genus) and 20 extinct taxa of platyrrhines. The tree Paraná Portal Anthropoidea structure is constrained with a ‘‘molecular scaffold’’ of extant species as implemented in maximum par- simony using PAUP with the molecular-based ‘backbone’ approach. The data set encompasses most of the known extinct species of platyrrhines, ranging in age from latest Oligocene ( 26 Ma) to the Recent. The tree is rooted with extant catarrhines, and Late Eocene and Early Oligocene African anthropoids. -
Caribbean Geological Conference 18Th
18 th Caribbean Geological Conference Santo Domingo · República Dominicana March 24th – 29th, 2008 Post Conference Field Trip # 4 Field trip Guide to the Median Belt and subduction zone rocks, Dominican Republic Compiled by Grenville Draper and John Lewis with contributions by R. A. Abbott, J. Escuder-Viruete, M. Krebs, W.V. Maresch, P. Schertl, A. Perez-Estaun, and J. P. Pindell IGCP 546 “Subduction zones of the Caribbean” We are celebrating 2008 INTERNATIONAL YEAR OF PLANET EARTH urhter information: Fwww.sodogeo.org www.dgm.gov.do www.ugr.es/~agcasco/igcp546/ >> Activities >> Dominican Rep 2008 Field trip Guide to the Median Belt and subduction zone rocks, Dominican Republic Compiled by Grenville Draper 1 and John Lewis 2 With contributions by R. A. Abbott, 3, J. Escuder-Viruete. 4, M. Krebs, 5 W.V. Maresch, 5 P. Schertl 5, A. Perez-Estaun,. 6 and J. P. Pindell 7 1 Department of Earth Sciences, Florida International University, Miami, FL 33199, USA; [email protected] 2 Dept of Earth and Environmental Science, The George Washington University, Washington D.C. 20052 3 Department of Geology, Appalachian State University, Boone, North Carolina 28608, USA 4 Instituto Geológico y Minero de España, Ríos Rosas 23, 28003 Madrid, Spain 5 Institute of Geology, Mineralogy and Geophysics, Ruhr-University Bochum, 44780 Bochum, Germany 6 I.C.T. Jaume Almera-CSIC, Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain 7 Tectonic Analysis, Ltd, Cokes Barn, West Burton, Sussex RH20 1HD England INTRODUCTION This three day field excursion is designed to give participants at the Caribbean Conference an opportunity to examine two of the most significant structural-petrological features in the northern Caribbean. -
A Study on the Formation Environment of the La Cumbre Amber Deposit, from Santiago Province, the Northwestern Dominican Republic
minerals Article A Study on the Formation Environment of the La Cumbre Amber Deposit, from Santiago Province, the Northwestern Dominican Republic Paweł Stach 1,* , Lucyna Natkaniec-Nowak 1, Marian Wagner 1, Magdalena Duma ´nska-Słowik 1 , Maja Mroczkowska-Szersze ´n 2 , Aleksandra Wesełucha-Birczy ´nska 3, Przemysław Drzewicz 4 , Carlos George 5 and Edwin Garcia 6 1 Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, 30 Mickiewicza Av., 30-059 Krakow, Poland; [email protected] (L.N.-N.); [email protected] (M.W.); [email protected] (M.D.-S.) 2 Oil and Gas Institute–National Research Institute, 25 Lubicz Str., 31-503 Krakow, Poland; [email protected] 3 Faculty of Chemistry, Jagiellonian University, 2 Gronostajowa Str., 30-387 Krakow, Poland; [email protected] 4 The Polish Geological Institute–National Research Institute, 4 Rakowiecka Str., 00-975 Warsaw, Poland; [email protected] 5 Dirección General de Minería, L. Navarro Av., Santo Domingo 10201, Dominican Republic; [email protected] 6 Faculty of Engineering and Natural Resources, UTECO La Universidad Tecnologica del Cibao Oriental, Ave Universitaria No. 100, Cotuí 43000, Dominican Republic; [email protected] * Correspondence: [email protected] Received: 18 July 2020; Accepted: 12 August 2020; Published: 21 August 2020 Abstract: The amber-bearing coaly shale from the La Cumbre deposit (Cordillera Septentrional, Dominican Republic) contains a large quantity of altered, coalified plant detritus. The coals in these shales are in the transition stage from meta-lignite to subbituminous coals. They are composed mainly of inertinite macerals such as fusinite, semifusinite, macrinite and secretinite. -
Checklist of Fossil Liverworts Suitable for Calibrating Phylogenetic Reconstructions
Bry. Div. Evo. 043 (1): 014–071 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.6 Checklist of fossil liverworts suitable for calibrating phylogenetic reconstructions KATHRin FELDBERG1,*, S. ROBBERT GRADSTEin2, CARSTEN GRÖHN3, JOCHEN HEinRicHS4,†, MATT VON KONRAT5, YURiy S. MAMONTOV6, MATT A. M. REnnER7, MADITA ROTH1, ALFOns SCHÄFER-VERWimp8, PHIANGPHAK SUkkHARAK9 & ALEXANDER R. SCHmiDT1 1Department of Geobiology, University of Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany; �[email protected]; https://orcid.org/0000-0002-9431-7193 �[email protected]; https://orcid.org/0000-0001-5426-4667 2Department of Systematics, Biodiversity and Evolution of Plants, Albrecht von Haller Institute for Plant Sciences, University of Göttingen, 37073 Göttingen, Germany; Muséum National d’Histoire Naturelle, Institute de Systematique, Évolution, Biodiversité (UMR 7205), 75005 Paris, France; �[email protected]; https://orcid.org/0000-0002-3849-6457 3Amber Study Group, c/o Geological-Palaeontological Institute and Museum (CeNak) of the University of Hamburg, Bundesstraße 55, 20146 Hamburg, Germany; �[email protected] 4Department of Biology I, Systematic Botany and Mycology, Geobio-Center, University of Munich (LMU), Menzinger Straße 67, 80638 Munich, Germany 5Gantz Family Collections Center, Science & Education, Field Museum, 1400 South Lake Shore Drive, Chicago, -
Zuckmücken (Chironomidae) Und Ihre Syninklusen in Dominikanischem
Zuckmücken(Chironomidae) und ihre Syninklusenin Dominikanischem Bernstein. Eine Analyse der Diversität, Biogeographie, Paläoökologie und Stabilität der fossilenFauna und Vergleichmit der heutigen Lebewelt. Dissertation zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) an der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität Bonn vorgelegt von Martin Grund aus Köln Juni 2006 Erster Gutachter: Prof. Dr. Jes Rust Zweiter Gutachter: PD Dr. Martin Sander Die mündliche Prüfung fand am 9. August 2006 statt. Diese Dissertation ist auf dem Hochschulschriftenserver der ULB Bonn http://hss.ulb.uni-bonn.de/diss_online elektronisch publiziert. Erscheinungsjahr: 2006 Danksagung Ich sage Dank an Prof. Dr. Jes Rust, dessen Engagement mir diese Arbeit ermöglichte. Dank für die Bestimmung von Fossilien schulde ich folgenden Kolleginnen und Kollegen: Dr. David Penney (Araneae) Monica Solórzeno Kraemer (Isoptera) Prof. Dr. Rüdiger Wagner (Psychodidae) Dr. Sonja Wedmann (Apidae) Prof. Dr. Wilfried Wichard (Trichoptera) Prof. Dr. Wolfgang Böhme (Iguanidae) Besonders bedanke ich mich für die gute Zusammenarbeit bei Prof. Dr. Jes Rust, Monica Solórzeno Kraemer, Dr. Fabian Seredszus, Prof. Dr. Wilfried Wichard und Dr. Bradley J. Sinclair. 1 Einleitung 1 1.1 Chironomiden 1 1.2 Dominikanischer Bernstein 1 1.3 Rekonstruktion und Stabilität fossiler Ökosysteme 2 1.4 Ökologie der Chironomidae 4 1.4.1 Ökologie der Unterfamilien der Chironomidae 4 1.4.2 Ökologie der Chironomidae in tropischen Bergbächen -
COLOR PHENOMENA of BLUE AMBER Yan Liu, Guanghai Shi, and Shen Wang
NOTES & NEW TECHNIQUES COLOR PHENOMENA OF BLUE AMBER Yan Liu, Guanghai Shi, and Shen Wang Although resinites of different ages exist, avail- able biostratigraphic and paleogeographic data sug- The greenish blue color observed in some amber gest that the main amber deposits in the Dominican from the Dominican Republic and Indonesia is Republic (including those famous for yielding biolog- actually fluorescence stimulated by ultraviolet ical inclusions) were formed in a single sedimentary (UV) light. A previous study described the color basin during the late Early Miocene through early as iridescence over a yellow background, but it Middle Miocene (15 to 20 million years ago). There is in fact a surface fluorescence. Since this amber is little evidence of extensive reworking or redeposi- can be considered a long-wavelength pass filter tion of the ambers. Before the studies of Iturralde-Vi- with a half-pass wavelength at about 530 nm in nent and MacPhee (1996), amber from the northern its spectral transmittance, it does not transmit ei- area was thought to have formed during the Early ther UV or short-wave visible light. As this mate- Eocene to Early Miocene epochs (Baroni-Urbani and rial completely absorbs light in the UV range and Saunders, 1982; Lambert et al., 1985; Poinar and Can- strongly absorbs light in the short-wave visible natella, 1987; Grimaldi, 1996), while published esti- range, the stimulated blue color is confined ex- mates for the eastern area ranged from the Cretaceous clusively to the surface.The amber from this study to Holocene epochs (Burleigh and Whalley, 1983; also showed the Usambara effect, the phenome- Poinar and Cannatella, 1987; Grimaldi, 1996). -
Fossil Resins–Constraints from Portable and Laboratory Near-Infrared Raman Spectrometers
minerals Article Fossil Resins–Constraints from Portable and Laboratory Near-infrared Raman Spectrometers Beata Naglik 1,*, Maja Mroczkowska-Szersze ´n 2 , Magdalena Duma ´nska-Słowik 3 , Lucyna Natkaniec-Nowak 3, Przemysław Drzewicz 4 , Paweł Stach 3 and Gra˙zyna Zukowska˙ 5 1 Polish Geological Institute-National Research Institute, Upper Silesian Branch, 1 Królowej Jadwigi Str., 41-200 Sosnowiec, Poland 2 Oil and Gas Institute-National Research Institute, 25A Lubicz Str., 31-503 Krakow, Poland; [email protected] 3 Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, 30 Mickiewicz Av., 30-059 Krakow, Poland; [email protected] (M.D.-S.); [email protected] (L.N.-N.); [email protected] (P.S.) 4 Polish Geological Institute-National Research Institute, 4 Rakowiecka Str., 00-975 Warsaw, Poland; [email protected] 5 Faculty of Chemistry, Warsaw University of Technology, 3 Noakowskiego Str., 00-664 Warsaw, Poland; [email protected] * Correspondence: [email protected] Received: 6 December 2019; Accepted: 17 January 2020; Published: 25 January 2020 Abstract: Comparative studies of fossil resins of various ages, botanical sources, geological environments, and provenience were provided via a handheld portable Near-Infrared (NIR)-Raman spectrometer and benchtop instrument both working with laser line 1064 nm. The recorded Raman spectra of individual fossil resins were found to be sufficiently similar irrespective to the device type applied, i.e., handheld or benchtop. Thus, the portable equipment was found to be a sufficient tool for the preliminary identification of resins based on botanical and geographical 1 origin criteria. The observed height ratio of 1640/1440 cm− Raman bands did not correlate well with the ages of fossil resins.