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Business Bavaria Newsletter
Business Bavaria Newsletter Issue 07/08 | 2013 What’s inside 5 minutes with … Elissa Lee, Managing Director of GE Aviation, Germany Page 2 In focus: Success of vocational training Page 3 Bavaria in your Briefcase: Summer Architecture award for tourism edition Page 4 July/August 2013 incl. regional special Upper Franconia Apprenticeships – a growth market Bavaria’s schools are known for their well-trained school leavers. In July, a total of According to the latest education monitoring publication of the Initiative Neue 130,000 young Bavarians start their careers. They can choose from a 2% increase Soziale Marktwirtschaft, Bavaria is “top when it comes to school quality and ac- in apprenticeships compared to the previous year. cess to vocational training”. More and more companies are increasing the number of training positions to promote young people and thus lay the foundations for With 133,000 school leavers, 2013 has a sizeable schooled generation. Among long-term success. the leavers are approximately 90,000 young people who attended comprehensive school for nine years or grammar school for ten. Following their vocational train- The most popular professions among men and women are very different in Ba- ing, they often start their apprenticeships right away. varia: while many male leavers favour training as motor or industrial mechanics To ensure candidates and positions are properly matched, applicants and com- or retail merchants, occupations such as office manager, medical specialist and panies seeking apprentices are supported in their search by the Employment retail expert are the most popular choices among women. Agency. Between October 2012 and June 2013 companies made a total of 88,541 free, professional, training places available – an increase of 1.8% on the previ- www.ausbildungsoffensive-bayern.de ous year. -
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t t d d i i e e n n h h c c S S l l e e a a h h c c i i t a M M b o © © D The section of the Limes in Hesse that is approved as a world heritage The Upper German-Raetian Limes is Bavari a’ s most well known ground mo - o o k t t i o o r h h E P P © ranges from Heidenrod at the watchtower 2/35 «Am Laufenselder Weg» to nument and symbolizes the Roman ancient times from the 1st to the 3rd 3 8 / 9 P W f Mainhausen on the Main. The Limes runs across the wooded heights of the century A.D. Starting from the Wuerttembergian border the Limes runs o n o i t c u r t Taunus and encloses the fertile area of the Wetterau in a large arc. The across Middle Franconia, Upper Bavaria and ends at the Danube in Lowe r s n o c e r , b state of preservation of the 153 km long route with 18 big and 31 small forts Bavaria. Starting from 1892 the Limes got systematically researched due to a r G - h c a l r as well as 200 watchtowers differs due to the post-Roman usage of the the the Imperial Limes Commission, which was conducted in other states e ß o r G : e l t as well. Johann Turmair, named Aventinus (1477–1534) led the way to inter - i terrain. There is not much visible in agricultural areas while especially ram - T part and moat are still visible aboveground in the forests. -
Polskaakademianauk Instytutpaleobiologii
POLSKA AKADEMIA NAUK INSTYTUT PALEOBIOLOGII im. Romana Kozłowskiego SILURIAN AND DEVONIAN HETEROSTRACI FROM POLAND AND HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS Sylurskie i dewońskie Heterostraci z Polski oraz efektywność hydrodynamiczna psammosteidów Marek Dec Dissertation for degree of doctor of Earth and related environmental sciences, presented at the Institute of Paleobiology of Polish Academy of Sciences Rozprawa doktorska wykonana w Instytucie Paleobiologii Polskiej Akademii Nauk pod kierunkiem prof. dr hab. Magdaleny Borsuk-Białynickiej w celu uzyskania stopnia doktora w dyscyplinie Nauki o Ziemi oraz środowisku Warszawa 2020 CONTENTS ACKNOWLEDGMENTS…………………………………………………………….….... 3 STRESZCZENIE………………………………………………………………….....….. 4 SUMMARY……………………………………………………………………….…….. 8 CHAPTER I…………………………………………………………………………….. 13 TRAQUAIRASPIDIDAE AND CYATHASPIDIDAE (HETEROSTRACI) FROM LOWER DEVONIAN OF POLAND CHAPTER II……………………………………………………………………….…… 24 A NEW TOLYPELEPIDID (AGNATHA, HETEROSTRACI) FROM THE LATE SILURIAN OF POLAND CHAPTER III…………………………………………………………………………... 41 REVISION OF THE EARLY DEVONIAN PSAMMOSTEIDS FROM THE “PLACODERM SANDSTONE” - IMPLICATIONS FOR THEIR BODY SHAPE RECONSTRUCTION CHAPTER IV……………………………………………………………………….….. 82 NEW MIDDLE DEVONIAN (GIVETIAN) PSAMMOSTEID FROM HOLY CROSS MOUNTAINS (POLAND) CHAPTER V……………………………………………………………………………109 HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS: NEW INSIGHTS FROM COMPUTATIONAL FLUID DYNAMICS SIMULATIONS 2 ACKNOWLEDGMENTS First and foremost I would like to say thank you to my supervisor Magdalena -
UNIVERSITY of CALIFORNIA Los Angeles
UNIVERSITY OF CALIFORNIA Los Angeles Evolution of the boxfish carapace: functional consequences of shape A thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Biology by Tina Ashley Marcroft 2015 ABSTRACT OF THE THESIS Evolution of the boxfish carapace: functional consequences of shape by Tina Ashley Marcroft Master of Science in Biology University of California, Los Angeles, 2015 Professor Michael Edward Alfaro, Chair Boxfishes are a group of heavily armored Tetraodontiform fishes that are highly variable in shape. Disparification of shape could be driven by a simple performance trade-off between its two hypothesized primary functions: protection from predation and maneuverability. Alternatively, disparification could be driven by many-to-one mapping of shape to performance, where a relaxation in morphological constraint where many of morphologies have the same performance. We tested this by isolating the major features of the boxfish carapace shape and tested for their correlation to performance, as well as for a negative correlation between performances. We found that some features were correlated but very weakly, and that the two performances did trade-off but also weakly. This weak correlation primarily suggests that many- to-one mapping of shape to performance is driving disparification, which was unobserved in continuous 3D shape systems until this study. ii The thesis of Tina Ashley Marcroft is approved. Blaire Van Valkenburgh David K. Jacobs Michael Edward Alfaro, Committee Chair University of California, Los Angeles 2015 iii I dedicate this thesis to Carrie Umetsu, Joseph Aprill, Mai Nguyen, Princess Gilbert, Francisca Wufu, Deb Pires, Jonathan Chang, Herbert Icasiano, and many others, without whose unwavering emotional and professional support I would not have completed this text. -
SILURIAN TIMES NEWSLETTER of the INTERNATIONAL SUBCOMMISSION on SILURIAN STRATIGRAPHY (ISSS) (INTERNATIONAL COMMISSION on STRATIGRAPHY, ICS) No
SILURIAN TIMES NEWSLETTER OF THE INTERNATIONAL SUBCOMMISSION ON SILURIAN STRATIGRAPHY (ISSS) (INTERNATIONAL COMMISSION ON STRATIGRAPHY, ICS) No. 27 (for 2019) Edited by ZHAN Renbin INTERNATIONAL UNION OF GEOLOGICAL SCIENCES President: CHENG Qiuming (Canada) Vice-Presidents: Kristine ASCH (Germany) William CAVAZZA (Italy) Secretary General: Stanley C. FINNEY (USA) Treasurer: Hiroshi KITAZATO (Japan) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: David A.T. HARPER (UK) Vice-Chairman: Brian T. HUBER (USA) Secretary General: Philip GIBBARD (UK) SUBCOMMISSION ON SILURIAN STRATIGRAPHY Chairman: Petr ŠTORCH (Czech Republic) Vice-Chairman: Carlo CORRADINI (Italy) Secretary: ZHAN Renbin (China) Other titular members: Anna ANTOSHKINA (Russia) Carlton E. BRETT (USA) Bradley CRAMER (USA) David HOLLOWAY (Australia) Jisuo JIN (Canada) Anna KOZŁOWSKA (Poland) Jiří KŘÍŽ (Czech Republic) David K. LOYDELL (UK) Peep MÄNNIK (Estonia) Michael J. MELCHIN (Canada) Axel MUNNECKE (Germany) Silvio PERALTA (Argentina) Thijs VANDENBROUCKE (Belgium) WANG Yi (China) Živilė ŽIGAITĖ (Lithuania) Silurian Subcommission website: http://silurian.stratigraphy.org 1 CONTENTS CHAIRMAN’S CORNER 3 ANNUAL REPORT OF SILURIAN SUBCOMMISSION FOR 2019 7 INTERNATIONAL COMMISSION ON STRATGRAPHY STATUTES 15 REPORTS OF ACTIVITIES IN 2019 25 1. Report on the ISSS business meeting 2019 25 2. Report on the 15th International Symposium on Early/Lower Vertebrates 28 3. Report on the 13th International Symposium on the Ordovician System in conjunction with the 3rd Annual Meeting of IGCP 653 32 GUIDELINES FOR THE ISSS AWARD: KOREN' AWARD 33 ANNOUNCEMENTS OF MEETINGS and ACTIVITIES 34 1. Lithological Meeting: GEOLOGY OF REEFS 34 SILURIAN RESEARCH 2019: NEWS FROM THE MEMBERS 36 RECENT PUBLICATIONS ON THE SILURIAN RESEARCH 67 MEMBERSHIP NEWS 77 1. List of all Silurian workers and interested colleagues 77 2. -
Calcium Stable Isotopes Place Devonian Conodonts As First Level Consumers V
Calcium stable isotopes place Devonian conodonts as first level consumers V. Balter, J.E. Martin, T. Tacail, G. Suan, Sabrina Renaud, Catherine Girard To cite this version: V. Balter, J.E. Martin, T. Tacail, G. Suan, Sabrina Renaud, et al.. Calcium stable isotopes place Devonian conodonts as first level consumers. Geochemical Perspectives Letters, European Assoication of Geochemistry, 2019, 10, pp.36-39. 10.7185/geochemlet.1912. hal-02112869 HAL Id: hal-02112869 https://hal.archives-ouvertes.fr/hal-02112869 Submitted on 27 Apr 2019 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. © 2019 The Authors Published by the European Association of Geochemistry Calcium stable isotopes place Devonian conodonts as first level consumers V. Balter1*, J.E. Martin1, T. Tacail2, G. Suan1, S. Renaud3, C. Girard4 Abstract doi: 10.7185/geochemlet.1912 Conodont animals are an extinct group of jawless vertebrates whose hard parts, also known as conodont elements, represent the earliest evidence of a mineralised skeleton in the vertebrate lineage. Conodont elements are interpreted as parts of a feeding apparatus, which together with the presence of eyes and microwear patterns, support the controversial hypothesis that conodont animals were macrophagous predators and/or scavengers. -
Conodont Stratigraphy of a Highly Tectonised Silurian-Devonian Section in the San Basilio Area (SE Sardinia, Italy)
Bollettino della Societa Paleontologica Italiana 40 (3), 2001 ISSN 0375-7633 Modena, Dicembre 2001 Conodont stratigraphy of a highly tectonised Silurian-Devonian section in the San Basilio area (SE Sardinia, Italy) Carlo CORRADINI F rancesco LEONE Alfredo Loi Enrico SERPAGLI Dipartimento del Museo di Paleobiologia Dipartimento di Scienze della Terra Dipartimento del Museo di Paleobiologia e dell'Orto Botanico Universita di Cagliari e dell'Orto Botanico Universidt di Modena e Reggio Emilia Universita di Modena e Reggio Emilia KEYWORDS- Conodonts, Biostratigraphy, Tectonics, Silurian, Devonian, SE Sardinia. ABSTRACT- Several conodont species belonging to five "late Silurian biozones (Ancoradella ploeckensis, Polygnathoides siluricus, Ozarkodina crispa, Ozarkodina remscheidensis, Oulodus elegans detortus) and four Early and Late Devonian biozones (delta, pesavis, kitabicus-excavatus and Late rhenana) allow a better interpretation of stratigraphy and tectonics of the San Basilio area in western Gerrei. Frasnian sediments are documented for the first time in SE Sardinia. RIASSUNTO- [Stratigrafia a conodonti di una sezione forremente tettonizzata di eta Siluriano-Devoniano nell'area di San Basilio (Sardegna SE)] - Grazie alla biostratigrafia a conodonti viene interpretata la complessa tettonica di una sezione nell'area di San Basilio (Sardegna sud-orientale) e viene ricostruita la successione originaria. Sono documentate cinque biozone a conodonti del Siluriano superiore (Ancoradella eioeckensis, Polygnathoides siluricus, Ozarkodina crispa, -
View of What Is Now Known About
A PHASE OF THE UPPER DEVONIAN OF WESTERN HIGHLAND COUNTY, VIRGINIA By Helen F. Pulver A. B., Berea College, 1946 A thesis submitted to the Faculty of Oberlin College in partial fulfillment of the requirements for the Degree of Master of Arts in the Department of Geology 1948 PLATE I Chemung formation, Alleghany Mountain locality, 3145 A fossiliferous bed of arenaceous shale, containing predominantly Douvillina cayuta; Schizophoria stria tula in the upper and lower right hand corners, and a part of Tylothyris mesacostalis and Camarotoeehia eximia in the center. PLATE 1 PREFACE '!his paper is a study of the Brallier and Chemung formations - of west Highland County, Virginia. '!he limits of the Brallier forma t.ion are determined on the basis ot faunal and lithological evidence, and correlations made with format.ions in New York, Pennsylvania, Maryland and West Virginia. 'Ihe field work was carried on during the lat ter part of the summer of 1947 and the identification and correlations worked out in the winter of 1947 and the spring of 1948. I wish to thank Mr. Minor B. Long and 1fr. Bruce Weber for help in measuring .the section of the field. I am. grateful to Dr. E. C. Stumm for his interest and original suggestion of the problem. ~ Dr. C.W• .Carlston I should like to express my thanks for valuable suggestions in the field and in the preparation of this manuscript. Above all I should. like to express my deep appreeiation to Dr. Fred Foreman under whose direction this problem was completed, for his continued encouragement and constant assistance. -
Abstract Book
Ber. Inst. Erdwiss. K.-F.-Univ. Graz ISSN 1608-8166 Band 19 Graz 2014 IGCP 596 & 580, Joint Meeting Mongolia Ulaanbaatar, 5-18th August 2014 Berichte des Institutes für Erdwissenschaften, Karl-Franzens-Universität Graz, Band 19 IGCP 596 & IGCP 580 Joint Meeting and Field-Workshop International Symposium in Mongolia Ulaanbaatar, Mongolia 5-18th August 2014 ABSTRACT VOLUME Editorial: KIDO, E., WATERS, J.A., ARIUNCHIMEG, YA., SERSMAA, G., DA SILVA, A.C., WHALEN, M., SUTTNER, T.J. & KÖNIGSHOF, P. Impressum: Alle Rechte für das In- und Ausland vorbehalten. Copyright: Institut für Erdwissenschaften, Bereich Geologie und Paläontologie, Karl-Franzens-Universität Graz, Heinrichstrasse 26, A-8010 Graz, Österreich Medieninhaber, Herausgeber und Verleger: Institut für Erdwissenschaften, Karl-Franzens-Universität Graz, homepage: www.uni-graz.at Druck: Medienfabrik Graz GmbH, Dreihackengasse 20, 8020 Graz 1 Ber. Inst. Erdwiss. K.-F.-Univ. Graz ISSN 1608-8166 Band 19 Graz 2014 IGCP 596 & 580, Joint Meeting Mongolia Ulaanbaatar, 5-18th August 2014 2 Ber. Inst. Erdwiss. K.-F.-Univ. Graz ISSN 1608-8166 Band 19 Graz 2014 IGCP 596 & 580, Joint Meeting Mongolia Ulaanbaatar, 5-18th August 2014 Organization Organizing Committee Johnny A. Waters - Appalachian State University (USA) Ariunchimeg Yarinpil - Palaeontological Centre, Mongolian Academy of Sciences (Mongolia) Sersmaa Gonchigdorj - Mongolian University of Science and Technology (Mongolia) Anne-Christine da Silva - University of Liège (Belgium) Michael Whalen - University of Alaska Fairbanks (USA) Erika Kido - University of Graz (Austria) Thomas J. Suttner - University of Graz (Austria) Peter Königshof - Senckenberg Forschungsinstitut und Naturmuseum (Germany) Scientific Committee Johnny A. Waters Ariunchimeg Yarinpil Sersmaa Gonchigdorj Anne-Christine da Silva Michael Whalen Erika Kido Thomas J. -
SGSI 7 013-034 Amler.Indd 13 11-11-10 08:47 14 Amler
Late Devonian (Frasnian) bivalves from the Nocedo Formation – the results of Wilhelm Kegel’s 1927 field trip to northern Spain Michael R.W. Amler Amler, M.R.W. Late Devonian (Frasnian) bivalves from the Nocedo Formation – the results of Wil- helm Kegel’s 1927 field trip to northern Spain. Scripta Geologica Special Issue, 7: 13-34, 9 figs., Leiden, December 2010. Michael R.W. Amler, Department für Geo- und Umweltwissenschaften, Sektion Geologie, and Geo- Biocenter Munich, Ludwig-Maximilians-Universität München, Luisenstr. 37, D-80333 München, Ger- many ([email protected]), and Institut für Geologie und Paläontologie im Fachbereich Geographie der Philipps-Universität Marburg, Hans-Meerwein-Str., D-35032 Marburg, Germany ([email protected]). Key words — Bivalvia, Rhenish Facies, Nocedo Formation, Frasnian, Cantabrian Mountains, Iberia, Wilhelm Kegel. During a field trip to the Peña-Corada Unit of the southernmost Esla region of the Cantabrian Moun- tains in 1927, the German stratigrapher Wilhelm Kegel sampled brachiopods and bivalves from a section in the Laoz valley near La Ercina. The stratigraphic position is believed to be part of the No- cedo Formation of Frasnian age. This fauna includes poorly preserved steinkerns of a near-shore bi- valve fauna that was prepared for publication including labels and proposed names, but never pub- lished. The fauna represents only a very small and random part of the former community. But as in- formation on Frasnian bivalves is scarce, the few specimens add important information on the distri- bution and palaeogeographic occurrence of near-shore, that is, Rhenish Facies bivalves within the south Laurussian – Rheic Ocean Realm. -
Brachiopods from the Mobarak Formation, North Iran
GeoArabia, 2011, v. 16, no. 3, p. 129-192 Gulf PetroLink, Bahrain Tournaisian (Mississippian) brachiopods from the Mobarak Formation, North Iran Maryamnaz Bahrammanesh, Lucia Angiolini, Anselmo Alessandro Antonelli, Babak Aghababalou and Maurizio Gaetani ABSTRACT Following detailed stratigraphic work on the Mississippian marlstone and bioclastic limestone of the Mobarak Formation of the Alborz Mountains in North Iran, forty-eight of the most important brachiopod taxa are here systematically described and illustrated. The ranges of the taxa are given along the Abrendan and Simeh Kuh stratigraphic sections, located north of Damgham. The examined brachiopod species date the base of the Mobarak Formation to the Tournaisian, in absence of age-diagnostic foraminifers. Change in brachiopod settling preferences indicates a shift from high energy, shallow-water settings with high nutrient supply in the lower part of the formation to quieter, soft, but not soppy substrates, with lower nutrient supply in the middle part of the Mobarak Formation. Brachiopod occurrence is instead scanty at its top. The palaeobiogeographic affinity of the Tournaisian brachiopods from North Iran indicates a closer relationship to North America, Western Europe and the Russian Platform than to cold-water Australian faunas, confirming the affinity of the other biota of the Alborz Mountains. This can be explained by the occurrence of warm surface-current gyres widely distributing brachiopod larvae across the Palaeotethys Ocean, where North Iran as other peri- Gondwanan blocks acted as staging-posts. INTRODUCTION The Mississippian Mobarak Formation of the Alborz Mountains (North Iran) has been recently revised by Brenckle et al. (2009) who focused mainly on its calcareous microfossil biota and refined its biostratigraphy, chronostratigraphy and paleogeography. -
Devonian and Carboniferous Pre-Stephanian Rocks from the Pyrenees
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repositorio da Universidade da Coruña 1 Published In García-López, S. and Bastida, F. (eds). Palaeozoic conodonts from northern Spain: Eight International Conodont Symposium held in Europe. Instituto Geológico y Minero de España, Serie Cuadernos del Museo Geominero 1, (2002), pp. 367-389. Madrid (438p.). ISBN: 84-74840-446-5. Devonian and Carboniferous pre-Stephanian rocks from the Pyrenees J. SANZ-LÓPEZ Facultad de Ciencias de la Educación. Universidad de A Coruña. Paseo de Ronda 47, 15011 A Coruña (Spain). [email protected] ABSTRACT A stratigraphic description of the Devonian and Carboniferous pre-Variscan rocks of the Pyrenees is presented. The successions are grouped into sedimentary domains that replace the “facies areas” proposed by previous authors for areas with homogeneous stratigraphy. The description of the sedimentary filling is divided into temporal intervals, where the previous stratigraphic correlation, based on lithological criteria, is supplemented by faunal data, especially conodont findings. A simple palaeogeographic model of the sedimentation during the Upper Palaeozoic and data related to southern boundary between the Pyrenean basin and the Cantabro-Ebroian Massif are discussed. Keywords: Devonian, Carboniferous, conodonts, Pyrenees, stratigraphy. RESUMEN Se ha realizado una descripción estratigráfica de las rocas devónicas y carboníferas pre- variscas de los Pirineos. Las sucesiones son agrupadas en dominios sedimentarios que sustituyen a las “áreas de facies” propuestas por los autores previos para zonas con una estratigrafía homogénea. La descripción del relleno sedimentario está dividida en intervalos de tiempo, donde la correlación estratigráfica basada en criterios litológicos está incrementada por los datos faunísticos, sobre todo los hallazgos de conodontos.