Mitidieri, M. Estudio De Patologías Óseas En Reptiles Marinos Mesozoicos De Patagonia Y Antártida

Total Page:16

File Type:pdf, Size:1020Kb

Mitidieri, M. Estudio De Patologías Óseas En Reptiles Marinos Mesozoicos De Patagonia Y Antártida ESTUDIO DE PATOLOGÍAS ÓSEAS EN REPTILES MARINOS MESOZOICOS DE PATAGONIA Y ANTÁRTIDA Trabajo Final Licenciatura en Paleontología (UNRN 2021) Universidad Nacional de Río Negro Autor: Matías Mitidieri Universidad Nacional de Río Negro EEUU 750, General Roca, Río Negro, Argentina. Directora: Marianella Talevi Instituto de Investigación en Paleobiología y Geología Universidad Nacional de Río Negro - CONICET Av. Roca 1242, General Roca, Río Negro, Argentina. Mitidieri, M. Estudio de patologías óseas en reptiles marinos mesozoicos de Patagonia y Antártida. 2021 AGRADECIMIENTOS A mis padres por haberme apoyado en cada etapa de mi vida y particularmente en la elección de mi carrera, así como al resto de mi familia (hermanos, tíos, primos y abuelos) por el interés mostrado en el desarrollo de esta Tesis. A mi directora, Dra. Marianella Talevi, por la lectura crítica de las sucesivas versiones de este Trabajo Final de Licenciatura, por los consejos dados y el apoyo incondicional durante el desarrollo del mismo. A la Universidad Nacional de Río Negro (UNRN), al Instituto de Investigación en Paleobiología y Geología (IIPG) y al Consejo Interuniversitario Nacional (CIN) por brindar el marco institucional y financiamiento necesarios para la realización de este trabajo. A mis amigos que me acompañaron durante el cursado de la Licenciatura en Paleontología: Gerardo, Lautaro, Lisandro, Lucas y Rocío. Finalmente, deseo agradecer a todos aquellos que, aunque no mencionados explícitamente, han colaborado de muchas maneras a lo largo de estos cinco años. 1 Mitidieri, M. Estudio de patologías óseas en reptiles marinos mesozoicos de Patagonia y Antártida. 2021 ÍNDICE RESUMEN………………………………………………………………….……...………4 ABSTRACT……………………………………………………………….……….…..…..6 CAPÍTULO 1 – INTRODUCCIÓN 1.1. Introducción……………………………………………………………….….....……8 1.2. Hipótesis de trabajo……………………………………………….……….……...…9 1.3. Objetivos………………………………………………………….………….….......10 1.4. Plesiosaurios…………………………………………………….…………….........10 1.5. Reseña histórica de estudios patológicos en plesiosauria…......………..…….12 1.5.1. Necrosis avascular…………………………….………………………..…….12 1.5.2. Necrosis séptica……………………………….………………………..….....13 1.5.3. Marcas de mordedura……………………….………………………….....….14 1.5.4. Nódulos de Schmorl……………………….…………………………...….....16 1.5.5. Artrosis……………………………………..………………………….............17 1.5.6. Fusiones vertebrales debido a traumatismos……………………….…......18 1.6. Mosasaurios…………………………………………………………………..….....20 1.7. Reseña histórica de estudios patológicos en mosasaurios.............................22 1.7.1. Necrosis avascular…………………………………………...…………….....22 1.7.2. Neoplasia (tumores)……………………………………..……………….......23 1.7.3. Fracturas óseas………………………………………………..…………......25 1.7.4. Fusiones vertebrales debido a infecciones óseas……………..…..……...27 1.7.5. Fusiones vertebrales debido a traumatismos……………………………...31 1.7.6. Osteomielitis………………………………………………………….…...…..33 1.7.7. Artritis……………………………………………………..…………….……...35 CAPÍTULO 2 – MATERIALES Y MÉTODOS 2.1. Marco geológico…………………………………………………………………….37 2.1.1. Ejemplar MML-PV 1305. Vértebra cervical de plesiosaurio…...…..……..37 2.1.2. Ejemplar MLP 87-II-7-1. Escápula izquierda de mosasaurio.....…………39 2 Mitidieri, M. Estudio de patologías óseas en reptiles marinos mesozoicos de Patagonia y Antártida. 2021 2.2. Elementos analizados……………………………………………………………...41 2.2.1. Plesiosaurio…………………………………………………………..………..41 2.2.2. Mosasaurio………………………………………………………..…………...41 2.3. Análisis y documentación……………………………………………………........42 2.3.1. Microtomografías computarizadas…………………………………...……..42 2.3.2. Fotogrametría………………………………………………………………....42 2.4. Abreviaturas institucionales……………………………………………………….43 2.5. Abreviaturas anatómicas…………………………………………………...…......44 CAPÍTULO 3 – RESULTADOS 3.1. Ejemplar MML-PV 1305. Vértebra cervical de plesiosaurio…………...……....45 3.1.1. Descripción general……………………………………………………...…...45 3.1.2. Análisis macroscópico………………………………………………………..46 3.1.3. Análisis de las microtomografías computarizadas…………...…………...47 3.2. Ejemplar MLP 87-II-7-1. Escápula izquierda de mosasaurio…………............49 3.2.1. Descripción general………………………………………………….............49 3.2.2. Análisis macroscópico……………………………………………….…….....49 3.2.3. Análisis de las microtomografías computarizadas………………………...50 3.3. Fotogrametría de los materiales……………………………………………..……51 CAPÍTULO 4 – DISCUSIÓN Y CONCLUSIONES 4.1. Diagnosis Patológica del ejemplar MML-PV 1305………………………..........54 4.2. Diagnosis Patológica del ejemplar MLP 87-II-7-1.……….…………….............57 4.3. Conclusiones……………….………...…………………………………..…………59 REFERENCIAS BIBLIOGRÁFICAS………………………………………..…………61 3 Mitidieri, M. Estudio de patologías óseas en reptiles marinos mesozoicos de Patagonia y Antártida. 2021 RESUMEN Los estudios paleopatológicos se han utilizado para comprender la historia de lesiones y enfermedades en el registro fósil, y permiten deducir el tipo de daño esquelético que ocurre en ejemplares fósiles, su causa aparente y por los aspectos relacionados con la paleoecología y de comportamiento. El análisis de las características patológicas de los reptiles marinos mesozoicos de Patagonia y Antártida, se presenta como un vasto campo de estudio aun escasamente explorado, y capaz de ofrecer información novedosa. El objetivo principal del trabajo es analizar elementos óseos de un plesiosaurio y un mosasaurio recuperados de Patagonia y Antártida respectivamente, los cuales presentan indicios de diversas paleopatologías. Los elementos de los ejemplares se analizaron macroscópicamente así como también mediante microtomografías computarizadas. Asimismo, a través de la técnica de fotogrametría se realizó una reconstrucción en 3D de los elementos, que luego fueron impresos mediante una impresora 3D (Creality Ender 3). El primer ejemplar (MML-PV 1305) consta de una vértebra cervical perteneciente a un plesiosaurio adulto, recuperado del Maastrichtiano superior de Patagonia (Bajo de Santa Rosa, Río Negro). Éste representa el primer informe de una paleopatología ósea en un reptil marino de Argentina. El análisis macroscópico reveló en la cara articular anterior del centro vertebral la presencia un nódulo de Schmorl acompañado de osteofitos en el borde inferior izquierdo del centro vertebral. El análisis de las microtomografías permitió evidenciar una depresión en la región central del centro vertebral, seguida de una erosión que se extendió internamente hasta la región media del mismo. Todas estas características observadas en el ejemplar resultan consistentes con el diagnóstico de un trauma por estrés mecánico, generado por esfuerzos de torsión y compresión producidos por la propia longitud del cuello o en momentos de alimentación. Esta condición patológica pudo generar dificultades en el movimiento y ocasionar dolores recurrentes en la región cervical del individuo. El segundo ejemplar (MLP 87-II-7-1) consta de una escápula izquierda perteneciente a un mosasaurio juvenil, recuperado del Maastrichtiano superior de Antártida (Isla Marambio), que representa el primer informe de una patología ósea en un reptil marino de Antártida. 4 Mitidieri, M. Estudio de patologías óseas en reptiles marinos mesozoicos de Patagonia y Antártida. 2021 El análisis macroscópico reveló una expansión de la articulación glenohumeral, la cual se encontraba profundamente erosionada y remodelada, y un seno de drenaje a la altura del cuello escapular, el cual se encontraba rodeado de un delgado margen de hueso perióstico nuevo. El análisis de las microtomografías reveló tejido trabecular desorganizado y dos senos de drenaje. Todas estas características observadas en el ejemplar resultan consistentes con el diagnóstico de una artritis infecciosa. La articulación de la escápula y el húmero fue interrumpida por la erosión de la fosa glenoidea, comprometiendo su función normal. Aunque no está directamente relacionada con la muerte del mosasaurio, esta condición pudo haber contribuido a reducir su efectividad para obtener alimento o aumentar su susceptibilidad a enfermedades fatales, lesiones adicionales o incluso depredación. Los resultados obtenidos a partir del trabajo realizado complementan el estado de conocimiento sobre patologías actuales en formas extintas y su prospección evolutiva, así como aspectos paleoecológicos de los organismos estudiados. Palabras clave: Patología. Reptiles marinos. Cretácico. Patagonia. Antártida. 5 Mitidieri, M. Estudio de patologías óseas en reptiles marinos mesozoicos de Patagonia y Antártida. 2021 ABSTRACT Paleopathological studies have been used to understand the history of injuries and diseases in the fossil record, and allow deducing the type of skeletal damage that occurs in fossil specimens, its apparent cause, and aspects related to palaeoecology and behavior. The analysis of the pathological characteristics of the Mesozoic marine reptiles of Patagonia and Antarctica, is presented as a vast field of study still scarcely explored, and capable of offering novel information. The main objective of the work is to analyze bone elements of a plesiosaur and a mosasaur recovered from Patagonia and Antarctica which show signs of various paleopathologies. The elements of the specimens were analyzed macroscopically as well as by computerized microtomography. Also, through the photogrammetry technique, a 3D reconstruction of the elements was made, which were then printed using a 3D printer (Creality Ender 3). The first specimen (MML-PV 1305) consists of a cervical vertebra belonging to an adult plesiosaur, recovered from the upper Maastrichtian
Recommended publications
  • Upper Cretaceous), Northern James Ross Island, Antarctic Peninsula
    Cretaceous Research 56 (2015) 550e562 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Calcareous nannofossils from the Santa Marta Formation (Upper Cretaceous), northern James Ross Island, Antarctic Peninsula * Rodrigo do Monte Guerra a, , Andrea Concheyro b, c, Jackie Lees d, Gerson Fauth a, Marcelo de Araujo Carvalho e, Renato Rodriguez Cabral Ramos e a ITT Fossil, Instituto Tecnologico de Micropaleontologia, Universidade do Vale do Rio dos Sinos (UNISINOS), Av. UNISINOS, 950, B. Cristo Rei/CEP: 93.022- 000, Sao~ Leopoldo, RS, Brazil b Instituto Antartico Argentino (IAA), Buenos Aires, Argentina c IDEAN-CONICET, Departamento de Ci^encias Geologicas, Universidad de Buenos Aires, Pabellon II, Ciudad Universitaria, 1428, Buenos Aires, Argentina d Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK e Museu Nacional e Universidade Federal do Rio de Janeiro, Brazil article info abstract Article history: This study reports on the most stratigraphically extensive nannofloras yet recovered from the Lachman Received 26 March 2015 Crags Member of the Santa Marta Formation, James Ross Island, Antarctic Peninsula. The productive Received in revised form samples are dated as early Campanian. These ages are in accord with those provided by ammonites, 15 June 2015 foraminifera, ostracods and radiolarians from the same locality. The consistent and relatively abundant Accepted in revised form 16 June 2015 presence of Gephyrobiscutum diabolum throughout the productive part of the section, a species that has Available online 11 July 2015 previously only been documented from the Falkland Plateau, extends its geographic distribution to higher latitudes, at least to the Antarctic Peninsula area.
    [Show full text]
  • ARTICLES Definition of Late Cretaceous Stage Boundaries In
    ARTICLES De®nition of Late Cretaceous Stage Boundaries in Antarctica Using Strontium Isotope Stratigraphy J. M. McArthur, J. A. Crame,1 and M. F. Thirlwall2 Department of Geological Sciences, University College London, Gower Street, London WC1E 6BT, United Kingdom (e-mail: [email protected]) ABSTRACT New 87Sr/86Sr analyses of macrofossils from 13 key marker horizons on James Ross and Vega Islands, Antarctica, allow the integration of the Antarctic Late Cretaceous succession into the standard biostratigraphic zonation schemes of the Northern Hemisphere. The 87Sr/86Sr data enable Late Cretaceous stage boundaries to be physically located with accuracy for the ®rst time in a composite Southern Hemisphere reference section and so make the area one of global importance for documenting Late Cretaceous biotic evolution, particularly radiation and extinction events. The 87Sr/86Sr values allow the stage boundaries of the Turonian/Coniacian, Coniacian/Santonian, Santonian/Campanian, and Campanian/Maastrichtian, as well as other levels, to be correlated with both the United Kingdom and United States. These correlations show that current stratigraphic ages in Antarctica are too young by as much as a stage. Immediate implications of our new ages include the fact that Inoceramus madagascariensis, a useful fossil for regional austral correlation, is shown to be Turonian (probably Late Turonian) in age; the ªMytiloidesº africanus species complex is exclusively Late Coniacian in age; both Baculites bailyi and Inoceramus cf. expansus have a Late Con- iacian/Early Santonian age range; an important heteromorph ammonite assemblage comprising species of Eubostry- choceras, Pseudoxybeloceras, Ainoceras, and Ryugasella is con®rmed as ranging from latest Coniacian to very earliest Campanian.
    [Show full text]
  • First Description of Scleractinian Corals from the Santa Marta and Snow Hill Island (Gamma Member) Formations, Upper Cretaceous, James Ross Island, Antarctica
    • Article • Advances in Polar Science doi: 10.13679/j.advps.2020.0013 September 2020 Vol. 31 No. 3: 205-214 First description of scleractinian corals from the Santa Marta and Snow Hill Island (Gamma Member) formations, Upper Cretaceous, James Ross Island, Antarctica Roberto VIDEIRA-SANTOS1,2*, Sandro Marcelo SCHEFFLER1, Luiza Corral Martins de Oliveira PONCIANO3, Luiz Carlos WEINSCHÜTZ4, Rodrigo Giesta FIGUEIREDO5, Taissa RODRIGUES6, Juliana Manso SAYÃO7,8, Douglas Santos RIFF9 & Alexander Wilhelm Armin KELLNER8 1 Laboratório de Paleoinvertebrados, Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista, s/n, 20940-040, Rio de Janeiro, RJ, Brazil; 2 Universidade Federal Rural do Rio de Janeiro, BR-465, Km 07, s/n, 23890-000, Seropédica, RJ, Brazil; 3 Laboratório de Tafonomia e Paleoecologia Aplicadas – LABTAPHO, Departamento de Ciências Naturais – DCN, Universidade Federal do Estado do Rio de Janeiro – UNIRIO, Av. Pasteur, 458, 22290-250, Rio de Janeiro, RJ, Brasil; 4 Centro Paleontológico de Mafra – CENPALEO, Universidade do Contestado, Av. Pres. Nereu Ramos,1071, 89300-000, Mafra, SC, Brazil; 5 Departamento de Biologia, Universidade Federal do Espírito Santo – UFES, Alto Universitário s/n, Guararema, Alegre, ES, Brazil; 6 Laboratório de Paleontologia, Departamento de Ciências Biológicas, Centro de Ciências Humanas e Naturais, Universidade Federal do Espírito Santo – UFES, Avenida Fernando Ferrari, 514, Goiabeiras, 29075-910, Vitória, ES, Brazil; 7 Laboratório de Paleobiologia
    [Show full text]
  • Method for the Systematic Identification of Globally Important Geological Sites in Antarctica
    Attachment A Method for the systematic identification of globally important geological sites in Antarctica Introduction and concepts The SCAR Action Group on Geological Heritage and Geoconservation discussed methods to identify sites of globally important geological value at its 2nd meeting held during the SCAR/IASC Open Science Conference in Davos, Switzerland, 17 July 2018. It was agreed that the procedure for the identification of Antarctic sites of exceptional geological value should follow the methods of the Global Geosites Project (which is promoted and co-sponsored by UNESCO and the International Union of Geological Sciences (IUGS), and focusses on the identification of geological heritage), but adapted for the unique situation and specific circumstances found in Antarctica. One benefit of this approach is that the process would be comparable with that used globally, and would allow the many unique processes that have occurred within Antarctica to be understood within a global context. The objective of the proposed method for Antarctica is to select the most important sites for geological science, taking a global perspective and using a comparative review, resulting in the selection of geological sites worthy of international recognition. The method, has two steps, as follows (see Figure 1): 1. The systematic classification of Antarctica’s geological past into defined geological themes through the identification of a list of Geological Frameworks. SCAR has already completed this process with the initial identification of nine Geological Frameworks that represent the most significant events in Antarctic’s geological past (see Annex 1). 2. The subsequent identification of Antarctic sites of exceptional geological importance (known as Antarctic Geosites) within each of the identified Geological Frameworks.
    [Show full text]
  • Análisis Comparativo De La Microestructura Ósea Y
    Garat, L.M. Análisis comparativo de la microestructura ósea y paleohistología en diferentes secciones de la 2019 columna vertebral de un plesiosaurio (elasmosáurido) del Cretácico Superior de Antártida. AGRADECIMIENTOS En primer lugar, quiero expresar mi gratitud hacia mis directores. A la Dra. Marianella Talevi, por su paciencia, tenacidad y dedicación en la dirección de este trabajo, el cual no vería la luz sin su apoyo. Al Dr. Patricio José O’Gorman, por sus aportes y sugerencias que han ayudado a mejorar el manuscrito. También deseo agradecer al Dr. Ignacio Alejandro Cerda por compartir su tiempo e instruirme en esta disciplina que he aprendido a amar. A mi madre por su apoyo incondicional y su eterno cariño. A mis amigos y compañeros de la Y.I.K.G.A. a quienes considero mi segunda familia. Por último quisiera agradecer a los docentes y a la comunidad de la Universidad Nacional de Río Negro (U.N.R.N.) que me formaron como profesional, al Consejo Interuniversitario Nacional (C.I.N.) por el financiamiento de este trabajo de grado y al Instituto de Investigación en Paleobiología y Geología (I.I.P.G.) y a su director Silvio Casadío por haber brindado el espacio y los instrumentos del Laboratorio de Microscopia para el análisis de las muestras. 1 Garat, L.M. Análisis comparativo de la microestructura ósea y paleohistología en diferentes secciones de la 2019 columna vertebral de un plesiosaurio (elasmosáurido) del Cretácico Superior de Antártida. ÍNDICE RESUMEN……………………………………………………………………………..4 ABSTRACT…………………………………………………………………………... 6 CAPÍTULO 1 – INTRODUCCIÓN 1.1. Introducción……………………………………………………………………. 8 1.2. Hipótesis de trabajo…………………………………………………………..12 1.3.
    [Show full text]
  • Abstract Book
    4th Interdisciplinary Antarctic Earth Sciences Conference Oct. 13-15, 2019 Antarctic deep field camp planning workshop Oct. 15-16, 2019 Camp Cedar Glen, Julian, CA Thanks to those who make our science possible and many others... AGENDA 2019 Interdisciplinary Antarctic Earth Sciences Conference Saturday, Oct. 12 4:00 pm Earliest possible check in at Camp Cedar Glen 5:00 8:00 Badge pick up @ Camp Cedar Glen, dinner and social at Julian Brewing Co. (Participants pay) Rides available. See Christine Kassab to load Sunday presentations. Sunday, Oct. 13 start End notes Title Authors 8:00 9:00 Breakfast with Safety Orientation from Camp staff. Badge pick up and load talks in Griffin Hall 9:00 9:10 Welcome Organizing Committee: B. Adams, B. Goehring, J. Isbell, K. Licht, K. Panter, L. Stearns, K. Tinto 9:10 9:20 NSF remarks Mike Jackson 9:20 9:35 Processes acting on Antarctic mantle: Implications for James M.D. Day flexure and volcanism 9:35 9:50 Sub-Ice Thermal Anomaly Mapping Using Phil Wannamaker, G. Hill, V. Magnetotellurics. Considering the U.S. Great Basin as Maris, J. Stodt, Y. Ogawa an Analog 9:50 10:10 INVITED: Pre-glacial and glacial uplift and incision Stuart N. Thomson, P. W. Reiners, history of the central Transantarctic Mountains J. He, S. R. Hemming, K.J. Licht reevaluated using multiple low-temperature thermochronometers 10:10 10:25 New single-crystal age determinations for basement K.W. Parsons, Willis Hames, S. rocks in the Miller Range of the Ross Orogen, Central Thomson Transantarctic Mountains 10:25 10:45 Break 10:45 11:05 INVITED: Antarctic Subglacial Limnology: John E.
    [Show full text]
  • Calcareous Nannoplankton As Paleoceanographic And
    Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2009 Calcareous Nannoplankton as Paleoceanographic and Biostratigraphic Proxies: Examples from the Mid-Cretaceous Equatorial Atlantic (ODP Leg 207) and Pleistocene of the Antarctic Peninsula (NBP0602A) and North Atlantic (IODP Exp. 306) Denise Kay Kulhanek Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES CALCAREOUS NANNOPLANKTON AS PALEOCEANOGRAPHIC AND BIOSTRATIGRAPHIC PROXIES: EXAMPLES FROM THE MID-CRETACEOUS EQUATORIAL ATLANTIC (ODP LEG 207) AND PLEISTOCENE OF THE ANTARCTIC PENINSULA (NBP0602A) AND NORTH ATLANTIC (IODP EXP. 306) By DENISE KAY KULHANEK A Dissertation submitted to the Department of Geological Sciences in partial fulfillment of the requirements for the degree of Doctor of Philosophy Degree Awarded: Fall Semester, 2009 Copyright © 2009 Denise Kay Kulhanek All Rights Reserved The members of the committee approve the dissertation of Denise Kay Kulhanek defended on August 6, 2009. __________________________________ Sherwood W. Wise, Jr. Professor Directing Dissertation __________________________________ Philip N. Froelich, Jr. Outside Committee Member __________________________________ William C. Parker Committee Member __________________________________ Yang Wang Committee Member The Graduate School has verified and approved the above-named committee members. ii To my husband Simon iii ACKNOWLEDGEMENTS This dissertation would not have been possible without the help and encouragement of many, many people. First and foremost, I would like to thank my advisor, Dr. Sherwood “Woody” Wise, who encouraged me to take advantage of many different opportunities while I was a doctoral student. Without his support I would not have had the chance to sail as a calcareous nannofossil paleontologist on Integrated Ocean Drilling Program Expedition 306 to the North Atlantic.
    [Show full text]
  • Libro Antartida.Indd
    COMPILADOR Colaboradores Editoriales Prof. Maria Josefa Fioriti Prof. Gabriela Rouiller Diseño Tapa Diseñadora Gráfica Lorena Vago Instituto Nacional del Agua Diagramación interior Diseñador Gráfico Mariano Masariche Foto tapa Ing. Patxi Elichiry Humedales Subpolares de la Cuenca del Arroyo Matías, Península Potter, Isla 25 de Mayo (King George), Schetland del Sur Antártida. Los autores se responsabilizan de la información y los trabajos edita- dos en la presente obra El agua en el norte de la península antártica / Adrían Angel Busso...[el al.]; compilado por Adrían Angel Busso - 1a ed. - Buenos Aires: Fundación de Historia Natu- ral Félix de Azara, 2009. 168 p. ; 24x17 cm. ISBN 978-987-22121-8-6 1. Hidrología. 1. Busso, Adrían Angel II. Busso, Adrían Angel, comp. CDD 551.3 El Compilador de este trabajo agradece a las autoridades de la SubSecretaría de Recursos Hídricos de la Nación y de la Dirección Nacional del Antártico. En particular a las siguientes Instituciones que permitieron la participación de los diversos autores: Instituto Nacional del Agua, In- stituto Antártico Argentino y al Dpto. de Cs. Geológicas, FCEyN, Universidad Buenos Aires. En general extend- emos nuestro agradecimiento a las Fuerzas Armadas del República Argentina dado que su apoyo logístico perma- nente hace posible la realización de nuestro trabajo en el continente. En términos particulares, agradezco en primer lugar al Dr. Carlos Rinaldi que inicailemnte apoyó la investigación hi- drológica e hidrogeológica en el Continente Antártico, a la Prof. María Josefa Fioriti por su colaboración, al Cap. de Corveta Beltrán (Servicio de Hidrografía Naval) y fi- nalmente a los evaluadores, autores, colegas y amigos que han participado con su tiempo, sugerencias y voluntad en la realización de esta publicación.
    [Show full text]
  • Palaeomagnetic, 40Ar/39Ar, and Stratigraphical Correlation Of
    Antarctic Science 17 (3), 409–417 (2005) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102005002853 Palaeomagnetic, 40Ar/39Ar, and stratigraphical correlation of Miocene–Pliocene basalts in the Brandy Bay area, James Ross Island, Antarctica LEÓ KRISTJÁNSSON1*, MAGNÚS T. GUDMUNDSSON1, JOHN L. SMELLIE2, WILLIAM C. MCINTOSH3 and RICHARD ESSER3 1 Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland 2British Antarctic Survey, NERC, High Cross, Madingley Rd, Cambridge CB3 0ET, UK 3New Mexico Geochronology Research Laboratory, New Mexico Institute of Mining and Technology, Socorro, NM 87801, USA *[email protected] Abstract: A revised stratigraphy of Cenozoic volcanic outcrops in the Brandy Bay area on James Ross Island is obtained by combining palaeomagnetic and stratigraphical anlysis with 40Ar/39Ar dating. The fieldwork was carried out between January and March 2002. Oriented palaeomagnetic samples were obtained from 17 volcanic units, the majority of samples being from lava-fed deltas. Individually the deltas are a few to several hundred metres thick and were formed during voluminous basaltic eruptions within an ice sheet or in a marine setting. Out of the sampled units, 15 carry a stable primary magnetization; six were of normal polarity and nine were reversely magnetized. Our 40Ar/39Ar dating constrains the emplacement of most of the Brandy Bay basalts to the Gilbert chron, with the youngest dated unit having an age of 3.95 Ma and the oldest 6.16 Ma. The mean palaeomagnetic field direction from 14 units has an inclination I = -76° α and declination D = 352°, 95 = 7°. The results further suggest that the lava caps on some of the deltas have high remanent intensity and should generate recognizable aeromagnetic anomalies.
    [Show full text]
  • Report of the Ad Hoc Subcommittee on the U.S. Antarctic Program's
    National Science Foundation Office of Polar Programs Advisory Committee Report of the Ad Hoc Subcommittee on the U.S. Antarctic Program’s Research Vessel Procurement August 14, 2019 Members Kim S. Bernard, Oregon State University Amy Leventer, Colgate University Jonathan Michael Prince, Moss Landing Marine Laboratories, SJSU/CSU Randy Sliester, British Antarctic Survey James H. Swift, UCSD Scripps Institution of Oceanography (Chair) Tom Weingartner (member and OPP/AC liaison) Tim McGovern, National Science Foundation - OPP liaison PART I. Summary _____________________________________________________________________________________ 8 A. Executive Summary ______________________________________________________________________________ 8 B. Impetus and Approach __________________________________________________________________________ 14 B.1 Synopsis of Issues _____________________________________________________________________________________ 14 B.2 Subcommittee Charge and Scope of Activities ______________________________________________________ 15 B.3 General Approach _____________________________________________________________________________________ 16 B.4 Acknowledgements ___________________________________________________________________________________ 16 C. Relationship of the Analyses to Strategic Science and Logistics Planning ______________ 17 C.1 Strategic planning and future polar science initiatives _____________________________________________ 17 C.1.1 National Science Board 2020 Vision for the National Science Foundation
    [Show full text]
  • Drepanocladus Longifolius As a Case Study
    Organisms Diversity & Evolution (2018) 18:263–278 https://doi.org/10.1007/s13127-018-0372-8 ORIGINAL ARTICLE Do Antarctic populations represent local or widespread phylogenetic and ecological lineages? Complicated fate of bipolar moss concepts with Drepanocladus longifolius as a case study Marta Saługa1 & Ryszard Ochyra1 & Jan Żarnowiec2 & Michał Ronikier1 Received: 2 March 2018 /Accepted: 30 July 2018 /Published online: 9 August 2018 # The Author(s) 2018 Abstract Bipolar moss species, extreme examples of large and disjunctive geographical ranges, belong to the most important components of the vegetation cover in Antarctica. Their appropriate taxonomic interpretations are essential for fine-scale biogeographical considerations but our knowledge on their phylogenetic affinities still remains limited. Here, we address the history of the Antarctic populations of Drepanocladus longifolius, a moss species widely considered a bipolar taxon. First, based on a worldwide sampling, we verify its assumed bipolar status. Then, we ask whether its current Antarctic populations have persisted throughout at least the last major glaciation in situ or, alternatively, are they a recent, postglacial element. Phylogenetic analyses together with investigation of morphological characters were used to infer relationships among accessions representing the whole distribution range of the taxon. Morphological and phylogenetic data strictly segregated specimens from the Southern and the Northern Hemisphere, with an exception of Australian populations that were included in the latter group. The Antarctic, sub- Antarctic and South American populations belong to a single clade and are treated as D. longifolius s. str., which consequently is not a bipolar taxon. All Northern Hemisphere populations and the ones from Australia represent D.
    [Show full text]
  • Geological Exploration of Cockburn Island, Antarctic Peninsula
    vol. 23, no. 1, pp. xxx–xxx, 2002 Geological exploration of Cockburn Island, Antarctic Peninsula JEFFREY D. STILWELL School of Earth Sciences, James Cook University, Townsville, Queensland 4811, Australia <[email protected]> ABSTRACT: Cockburn Island is one of the most historically significant places on the Ant− arctic continent. The isle was first surveyed in early 1843 during Captain James Ross’ fa− mous expedition, but the early explorers failed to recognise its geological and palaeonto− logical significance. Cockburn Island is exceptional for it has the only succession of Upper Cretaceous, Eocene and Miocene–Pliocene rocks on the continent, which is now known to contain an admirable and diverse fossil record of fauna and flora. These fossil assemblages are providing exciting new information on the evolutionary history of Antarctica. At least 22 species of Late Cretaceous macroinvertebrates and vertebrates have been recognised, whereas the Eocene record is slightly more diverse at 28 macroinvertebrate taxa recorded. The Pliocene macrofossil record is depauperateatsome 11 species, butmicrofossils (dia− toms, ostracods, foraminifera) are represented by at least 94 taxa. The palaeoecologic and palaeobiogeographic significance of fossil assemblages is explored in this paper. Further, a checklist of fossils is presented herein, for the first time, as is a bibliography of the geology and palaeontology of the island. Key words: Antarctica, Cockburn Island, geology, palaeontology, history, bibliography. Introduction Cockburn Island (Figs 1, 2, 12), a small butprominentisle some 5 km northof Cape Bodman on Seymour Island at the boundary of Admiralty Sound and Erebus and Terror Gulf at latitude 64°13’S and longitude 56°50’E, has the honourable dis− tinction of being one the first places to be visited by early Antarctic explorers dur− ing the first half of the nineteenth century.
    [Show full text]