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Foucault's Darwinian Genealogy
genealogy Article Foucault’s Darwinian Genealogy Marco Solinas Political Philosophy, University of Florence and Deutsches Institut Florenz, Via dei Pecori 1, 50123 Florence, Italy; [email protected] Academic Editor: Philip Kretsedemas Received: 10 March 2017; Accepted: 16 May 2017; Published: 23 May 2017 Abstract: This paper outlines Darwin’s theory of descent with modification in order to show that it is genealogical in a narrow sense, and that from this point of view, it can be understood as one of the basic models and sources—also indirectly via Nietzsche—of Foucault’s conception of genealogy. Therefore, this essay aims to overcome the impression of a strong opposition to Darwin that arises from Foucault’s critique of the “evolutionistic” research of “origin”—understood as Ursprung and not as Entstehung. By highlighting Darwin’s interpretation of the principles of extinction, divergence of character, and of the many complex contingencies and slight modifications in the becoming of species, this essay shows how his genealogical framework demonstrates an affinity, even if only partially, with Foucault’s genealogy. Keywords: Darwin; Foucault; genealogy; natural genealogies; teleology; evolution; extinction; origin; Entstehung; rudimentary organs “Our classifications will come to be, as far as they can be so made, genealogies; and will then truly give what may be called the plan of creation. The rules for classifying will no doubt become simpler when we have a definite object in view. We possess no pedigrees or armorial bearings; and we have to discover and trace the many diverging lines of descent in our natural genealogies, by characters of any kind which have long been inherited. -
Joachim 8Arrande (1819) 1799-1883 Pierre Pavot (44) Et Jean-Maurice Poutiers, Attaché Au Muséum National D'histoire Naturelle De Paris
LIBRES PROPOS • Bicentenaire d'un ancien plus célèbre à Prague qu'à Paris, Joachim 8arrande (1819) 1799-1883 Pierre Pavot (44) et Jean-Maurice Poutiers, attaché au Muséum national d'histoire naturelle de Paris Prague honorera cet été le bicentenaire de la naissance de ce savant géologue par une exposition et un symposium international. E Il AOÛT 1799 naissait dans la région de Saugues CHaute-Loire) L un garçon qui s'intéressera très tôt à la nature, à la technique et aux machines. Grâce à la solide aisance de ses parents, le jeune Joachim peut poursuivre ses études dans un éta blissement renommé de Paris, le col lège Stanislas. Entré à l'École poly technique en 1819, il en sort major en 1821 puis termine sa formation aux Ponts et Chaussées en 1824. Son intérêt personnel pour les sciences naturelles le conduit à suivre des cours et conférences des plus grands naturalistes de l'époque comme Georges Cuvier, Alexandre Brongniart, Alcide d'Orbigny .. Évoluant dans la société parisienne et aussi à la cour royale, il est remar qué par le dauphin, le duc d'An goulême, pour son intelligence excep tionnelle, son ardeur au travail et sa probité. À la fin des années 1820, Charles X l'appelle à être le précep- m )UIN1UILLET 1999 LA JAUNE ET LA ROUG E TRILOBITES Depuis cette époque, la Bohême est devenue un terrain classique d'études de l'ère primaire, connu de tous les géologues et naturalistes érudits. Par ses études et ses recherches, Barrande a débordé le domaine étroit de la Bohême en établissant des cor rélations avec les autres régions du monde grâce à une documentation considérable. -
George P. Merrill Collection, Circa 1800-1930 and Undated
George P. Merrill Collection, circa 1800-1930 and undated Finding aid prepared by Smithsonian Institution Archives Smithsonian Institution Archives Washington, D.C. Contact us at [email protected] Table of Contents Collection Overview ........................................................................................................ 1 Administrative Information .............................................................................................. 1 Historical Note.................................................................................................................. 1 Descriptive Entry.............................................................................................................. 2 Names and Subjects ...................................................................................................... 3 Container Listing ............................................................................................................. 4 Series 1: PHOTOGRAPHS, CORRESPONDENCE AND RELATED MATERIAL CONCERNING INDIVIDUAL GEOLOGISTS AND SCIENTISTS, CIRCA 1800-1920................................................................................................................. 4 Series 2: PHOTOGRAPHS OF GROUPS OF GEOLOGISTS, SCIENTISTS AND SMITHSONIAN STAFF, CIRCA 1860-1930........................................................... 30 Series 3: PHOTOGRAPHS OF THE UNITED STATES GEOLOGICAL AND GEOGRAPHICAL SURVEY OF THE TERRITORIES (HAYDEN SURVEYS), CIRCA 1871-1877.............................................................................................................. -
Epilogue: Pattern Cladistics from Goethe to Brady
Epilogue: Pattern Cladistics From Goethe to Brady Most, if not all, ideas in science are recycled, rediscovered, or rehashed, either sur- reptitiously, through rereading and rediscovering old works, or simply (commonly?) through lack of knowledge of past achievements. The idea of transformation—that things might change, transform, convert into other things—for instance, has been proposed many times, by both evolutionists and non-evolutionists alike. Yet the notion of transformation is really a myth, a story which many scientists embrace, a story that tells of living things transforming into other living things, with their role to interpret its meaning and mechanism: The fall of Paradise to the untamed wild, the tamed landscape to the Biblical flood, the reigns of monarchs, a kingdom to a republic and the pastoral to the industrial—of transformations there are plenty. A deep desire to uncover what mechanism(s) lie behind these transformations has provided many explanations, from the acquisition of sin after the fall from grace, to God’s will, to progress, however construed. The belief that every transformation neatly fits a law or model by which nature abides has shaped our way of thinking. Yet concomitant with such thoughts is the recognition that Nature is complex, and that Nature’s complexity obeys no single law or theory that places it neatly into a box. For every law and theory, we are told, there are exceptions, which are given ad hoc explanations. Man may have toiled the soil to shape nature into his or her image of Eden, but complexity does not fit any man-made law. -
List of the Geological Society of London
m LIST OF THE GEOLOGICAL SOCIETY OF LONDON. November 1st, 1875. LIST THE GEOLOGICAL SOCIETY OP LONDON. November 1st, 1875. PEIXTED BT TAYLOR AND PEAXCIS, KED LION COUKT, FLEET STIiEET. OFFICERS AND COUNCIL.—1875. President. * John Evans, Esq., Y.P.E.S. Vice-Presidents. Prof! P. Martin Duncan, M.B., E.R.S. Sir P. de M. G. Egerton, Bart., M.P., F.E.S. Eobert Etheridge, Esq., E.R.S. Prof. A. C. Ramsay, LL.D., E.R.S. Secretaries. David Eorbes, Esq., E.R.S. Rev. T. AVUtshire, M.A. Foreign Secretary. Warington W. Smyth, Esq., M.A., E.R.S. Treasurer. J. Gwyn Jeffreys, LL.D., E.R.S. CounciL H. Bancrman, Esq. J. Gwyn Jeffreys, LL.D., E.R.S. W. Carruthers, Esq., E.R.S. C. J. A. Meyer, Esq. Frederic Drew, Esq. J. Carrick Moore, Esq., M.A., E.R.S. Prof. P. Martin Duncan, M.B., E.R.S. Prof. A. C. Ramsay, LL.D., E.R.S. Sir P.dc M. G. Egerton, Bart., M.P., Samuel Sharp, Esq., E.S.A. E.R.S. Warington W. Smyth, Esq., M.A., R. Etheridge, Esq., E.R.S. E.R.S. John Evans, Esq., Y.P.R.S., E.S.A. H. C. Sorby, Esq., E.R.S. David Eorbes, Esq., E.R.S. Prof. J. Tennaut, E.C.S. R. A. C. Godwin-Austen, Esq., E.R.S. W. Whitaker, Esq., B.A. Henry Hicks, Esq. Rev. T. Wiltshire, M.A., E.L.S. Prof T. McKenny Hughes, M.A. Henry Woodward, Esq., E.R.S. -
The Nineteenth Century Engagement Between Geological and Adventist Thought and Its Bearing on the Twentieth Century Flood Geology Movement
Avondale College ResearchOnline@Avondale Theses PhD Theses 12-2016 The Nineteenth Century Engagement Between Geological and Adventist Thought and its Bearing on the Twentieth Century Flood Geology Movement Cornelis Siebe Bootsman Avondale College of Higher Education, [email protected] Follow this and additional works at: https://research.avondale.edu.au/theses_phd Part of the Physical Sciences and Mathematics Commons Recommended Citation Bootsman, C. S. (2016). The nineteenth century engagement between geological and Adventist thought and its bearing on the twentieth century flood geology movement (Doctoral dissertation, Avondale College of Higher Education, Cooranbong, Australia). Retrieved from https://research.avondale.edu.au/ theses_phd/7 This Thesis is brought to you for free and open access by the Theses at ResearchOnline@Avondale. It has been accepted for inclusion in Theses PhD by an authorized administrator of ResearchOnline@Avondale. For more information, please contact [email protected]. The Nineteenth Century Engagement Between Geological and Adventist Thought and its Bearing on the Twentieth Century Flood Geology Movement Cornelis Siebe Bootsman BSc, MSc (Vrije Universiteit Amsterdam), PhD (Witwatersrand) Thesis submitted in fulfilment of the requirements for the degree of Doctor of Philosophy Discipline of Science and Mathematics Avondale College of Higher Education September 2016 Statement of Original Authorship I declare that the work contained in this thesis has not been submitted previously for a degree or diploma at this institution, an Australian or overseas university or any other institution of higher education. To the best of my knowledge and belief, this thesis contains no material previously published or written by another person except where due reference is made. -
Foundations of Systematics and Biogeography David M
Foundations of Systematics and Biogeography David M. Williams · Malte C. Ebach Foundations of Systematics and Biogeography Foreword by Gareth Nelson David M. Williams Malte C. Ebach Dept. Botany Botanischer Garten und Natural History Museum Botanisches Museum Berlin-Dahlem Cromwell Road Freie Universität Berlin London SW7 5BD Königin-Luise-Str. 6–8 United Kingdom 14191 Berlin Germany ISBN: 978-0-387-72728-8 e-ISBN: 978-0-387-72730-1 Library of Congress Control Number: 2007938218 c 2008 Springer Science+Business Media, LLC All rights reserved. This work may not be translated or copied in whole or in part without the written permission of the publisher (Springer Science+Business Media, LLC., 233 Spring Street, New York, NY10013, USA), except for brief excerpts in connection with reviews or scholarly analysis. Use in connection with any form of information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed is forbidden. The use in this publication of trade names, trademarks, service marks, and similar terms, even if they are not identified as such, is not to be taken as an expression of opinion as to whether or not they are subject to proprietary rights. Printed on acid-free paper 987654321 springer.com Dedicated to Agnes Arber (1879–1960) Adolf Naef (1883–1949) Léon Croizat (1894–1982) Lars Brundin (1907–1993) Rainer Zangerl (1912–2004) Colin Patterson (1933–1998) Ronald H. Brady (1937–2003) Foreword “But where shall wisdom be found? and where is the place of understanding?” Job 28: 12 Where, indeed? Today in systematics and biogeography, DNA is revered as the source of all. -
Charles Lapworth's "The Moffat Series", 1878
194 Classic Paper Classic Paper in the History of Geology Charles Lapworth's "The Moffat Series", 1878 The investigation of the geol- quent repetition of beds. By working in the same meticulous way as ogy of the Southern Uplands, he had done in the south, and applying what he had read of discover- which form the border region ies in the Alps, he worked out the succession and structures, and between Scotland and Eng- again stimulated the Survey and others to re-map the area and revise land, has played an important their thinking. role in the history of geological research, from the time of Hut- ton, through the nineteenth century, and to the present. The problems in the geology of the The 1878 paper, the 'Moffat Series' by Charles Lapworth Southern Uplands (see Figure 1) was a major part in the development of the According to William Watts, writing an appreciation of Charles Lap- understanding of the geology worth in 1921, the problems in the understanding of the Lower Pal- of the area. Dealing with a aeozoic of the Southern Uplands was similar to those of the Lower region of complex deforma- Palaeozoic elsewhere. Trilobites and brachiopods had been used for tion, he worked out the bio- correlation, but had led to contradictions and inconsistencies. There stratigraphy and structure, was little or no confidence in graptolites as a stratigraphic tool. The using a hitherto largely main body of the Southern Uplands were considered to be virtually neglected fossil group, the barren and to have a total thickness of greywackes, with shale bands, Figure 1 Charles Lapworth. -
The Presently Best-Preserved Specimen Of
The presently best-preserved specimen of Lower Devonian Dalmanitid Trilobite of the Prague Basin (Czech Republic), with articulated hypostome Petr Budil, Catherine Crônier, Oldřich Fatka, Jessie Cuvelier To cite this version: Petr Budil, Catherine Crônier, Oldřich Fatka, Jessie Cuvelier. The presently best-preserved specimen of Lower Devonian Dalmanitid Trilobite of the Prague Basin (Czech Republic), with articulated hypos- tome. Annales de la Société Géologique du Nord, 2012, 19 (2ème série), pp.137 - 143. hal-02403133 HAL Id: hal-02403133 https://hal.archives-ouvertes.fr/hal-02403133 Submitted on 18 Feb 2020 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. Ann. Soc. Géol. du Nord. T.19 (2ème série), p. 137-143, Octobre 2012. THE PRESENTLY BEST-PRESERVED SPECIMEN OF LOWER DEVONIAN DALMANITID TRILOBITE OF THE PRAGUE BASIN (CZECH REPUBLIC), WITH ARTICULATED HYPOSTOME Le spécimen actuellement le mieux préservé, avec son hypostome articulé, de trilobite dalmanitide du Dévonien inférieur du Bassin de Prague (République Tchèque) by Petr BUDIL (*), Catherine CRÔNIER (**), Oldřich FATKA (***) and Jessie CUVELIER (**) (Planche IX) Abstract. — A rare, complete specimen of Zlichovaspis (Zlichovaspis) rugosa rugosa (Hawle & Corda, 1847) with in situ articulated hypostome is described from the locality Tetín Hill near Beroun (Bohemia). -
Darwin's Muses Behind His 1859 Diagram
ARBOR Ciencia, Pensamiento y Cultura Vol. 189-763, septiembre-octubre 2013, a072 | ISSN-L: 0210-1963 doi: http://dx.doi.org/10.3989/arbor.2013.763n5009 VARIA / VARIA LAS MUSAS DE DARWIN TRAS DARWIN’S MUSES BEHIND HIS EL DIAGRAMA DE 1859 1859 DIAGRAM Erica Torrens y Ana Barahona Grupo de Estudios Sociales de la Ciencia, Facultad de Ciencias, Universidad Nacional Autónoma de México [email protected] Citation/Cómo citar este artículo: Torrens, E. y Barahona, Copyright: © 2013 CSIC. This is an open-access article distribu- A. (2013). “Darwin’s muses behind his 1859 diagram”. ted under the terms of the Creative Commons Attribution-Non Arbor, 189 (763): a072. doi: http://dx.doi.org/10.3989/ Commercial (by-nc) Spain 3.0 License. arbor.2013.763n5009 Recibido: 30 abril 2013. Aceptado: 29 julio 2013. RESUMEN: En este artículo queremos mostrar mediante una re- ABSTRACT: This article uses a review of a number of tree visión de algunos diagramas en forma de árbol, que el hecho de diagrams to highlight how the fact that Darwin was to choose que Darwin escogiera la metáfora de un árbol para representar the metaphor of a tree to describe evolutionary relationships relaciones evolutivas entre los organismos no resulta enteramen- between organisms should come as no great surprise, as the te sorpresivo, ya que la figura arbórea ya guardaba una posición tree already occupied an important position in European ico- importante en la tradición iconográfica europea. En la revisión nography. In the review of some of the uses of a “tree” to de algunos usos del “árbol” para representar diferentes clases represent different types of relationships in the pre-Darwinian de relaciones en la época pre-darwiniana, queremos ilustrar dos age, we want to illustrate two basic issues. -
Trees and Networks Before and After Darwin Mark a Ragan
Biology Direct BioMed Central Review Open Access Trees and networks before and after Darwin Mark A Ragan Address: The University of Queensland, Institute for Molecular Bioscience and Australian Research Council Centre of Excellence in Bioinformatics, 306 Carmody Rd, St Lucia, Brisbane, Queensland 4072, Australia Email: Mark A Ragan - [email protected] Published: 16 November 2009 Received: 24 October 2009 Accepted: 16 November 2009 Biology Direct 2009, 4:43 doi:10.1186/1745-6150-4-43 This article is available from: http://www.biology-direct.com/content/4/1/43 © 2009 Ragan; licensee BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Abstract It is well-known that Charles Darwin sketched abstract trees of relationship in his 1837 notebook, and depicted a tree in the Origin of Species (1859). Here I attempt to place Darwin's trees in historical context. By the mid-Eighteenth century the Great Chain of Being was increasingly seen to be an inadequate description of order in nature, and by about 1780 it had been largely abandoned without a satisfactory alternative having been agreed upon. In 1750 Donati described aquatic and terrestrial organisms as forming a network, and a few years later Buffon depicted a network of genealogical relationships among breeds of dogs. In 1764 Bonnet asked whether the Chain might actually branch at certain points, and in 1766 Pallas proposed that the gradations among organisms resemble a tree with a compound trunk, perhaps not unlike the tree of animal life later depicted by Eichwald. -
Plant Diversity of the Mid Silurian (Lower Wenlock, Sheinwoodian) Terrestrial Vegetation Preserved in Marine Sediments from the Barrandian Area, the Czech Republic
FOSSIL IMPRINT • vol. 74 • 2018 • no. 3–4 • pp. 327–333 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) PLANT DIVERSITY OF THE MID SILURIAN (LOWER WENLOCK, SHEINWOODIAN) TERRESTRIAL VEGETATION PRESERVED IN MARINE SEDIMENTS FROM THE BARRANDIAN AREA, THE CZECH REPUBLIC MILAN LIBERTÍN 1, JIŘÍ KVAČEK1,*, JIŘÍ BEK2, PETR ŠTORCH2 1 Department of Palaeontology, National Museum, Prague, Václavské náměstí 68, 110 00 Prague 1, the Czech Republic; e-mail: [email protected], [email protected]. 2 Institute of Geology of the Czech Academy of Sciences, v.v.i., Rozvojová 269, 165 00 Prague 6, the Czech Republic; e-mail: [email protected], [email protected]. * corresponding author Libertín, M., Kvaček, J., Bek, J., Štorch, P. (2018): Plant diversity of the mid Silurian (lower Wenlock, Sheinwoodian) terrestrial vegetation preserved in marine sediments from the Barrandian area, the Czech Republic. – Fossil Imprint, 74(3-4): 327–333, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: Plant mega- and microfossils are described from the middle Sheinwoodian of the Barrandian area. The material comes from the Loděnice locality and the same horizon as the earliest unequivocal land plant, Cooksonia barrandei LIBERTÍN, J.KVAČEK, BEK, ŽÁRSKÝ et ŠTORCH. Its age (432 Myr) is inferred from the associated graptolite fauna, including the zonal index graptolite Monograptus belophorus. Megafossils have clear similarity with Cooksonia, due to their dichotomised axes with slightly widened subtending axes bearing putative sporangia. They document some of the plant diversity that was in place when the fi rst proven representative of the genus Cooksonia appeared, and together with dispersed spores they provide strong and important evidence that a diversifi ed terrestrial ecosystem had developed on the Barrandian volcanic archipelago in the peri-Gondwanan realm by the end of the Sheinwoodian Stage of the Silurian Period.