DOCSLIB.ORG

Programm Und Kurzfassungen – Program and Abstracts

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Programm Und Kurzfassungen – Program and Abstracts 1 Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Paläontologie und Geologie 29 Paläontologie im Blickpunkt 80. Jahrestagung der Paläontologischen Gesellschaft 5. – 8. Oktober 2010 in München Programm und Kurzfassungen – Program and Abstracts München 2010 Zitteliana B 29 118 Seiten München, 1.10.2010 ISSN 1612-4138 2 Editors-in-Chief/Herausgeber: Gert Wörheide, Michael Krings Mitherausgeberinnen dieses Bandes: Bettina Reichenbacher, Nora Dotzler Production and Layout/Bildbearbeitung und Layout: Martine Focke, Lydia Geissler Bayerische Staatssammlung für Paläontologie und Geologie Editorial Board A. Altenbach, München B.J. Axsmith, Mobile, AL F.T. Fürsich, Erlangen K. Heißig, München H. Kerp, Münster J. Kriwet, Stuttgart J.H. Lipps, Berkeley, CA T. Litt, Bonn A. Nützel, München O.W.M. Rauhut, München B. Reichenbacher, München J.W. Schopf, Los Angeles, CA G. Schweigert, Stuttgart F. Steininger, Eggenburg Bayerische Staatssammlung für Paläontologie und Geologie Richard-Wagner-Str. 10, D-80333 München, Deutschland http://www.palmuc.de email: [email protected] Für den Inhalt der Arbeiten sind die Autoren allein verantwortlich. Authors are solely responsible for the contents of their articles. Copyright © 2010 Bayerische Staassammlung für Paläontologie und Geologie, München Die in der Zitteliana veröffentlichten Arbeiten sind urheberrechtlich geschützt. Nachdruck, Vervielfältigungen auf photomechanischem, elektronischem oder anderem Wege sowie die Anfertigung von Übersetzungen oder die Nutzung in Vorträgen, für Funk und Fernsehen oder im Internet bleiben – auch auszugsweise – vorbehalten und bedürfen der schriftlichen Genehmigung durch die Bayerische Staatssammlung für Paläontologie und Geologie, München. ISSN 1612-412X Druck: Gebr. Geiselberger GmbH, Altötting 3 Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Paläontologie und Geologie CONTENTS/INHALT EINFÜHRUNG 4 SPONSOREN 4 TAGUNGSORGANISATION UND STRUKTUR 5 LAGEPLAN DER VORTRAGSRÄUME 6 PROGRAMM UND ZEITPLAN 7 KURZFASSUNG DES ÖFFENTLICHEN ABENDVORTRAGS 11 KURZFASSUNGEN DER VORTRÄGE UND POSTER (alphabetisch nach Autoren) 13 LISTE ALLER POSTER, GEORDNET NACH SYMPOSIEN 111 VERZEICHNIS ALLER AUTOREN 114 Zitteliana B 29 118 Seiten München, 1.10.2010 ISSN 1612-4138 4 Einführung Sponsoren Die 80. Jahrestagung der Paläontologischen Gesellschaft Für die finanzielle Unterstützung bedanken wir uns bei: steht unter dem Motto „Paläontologie im Blickpunkt". Die Ergebnisse paläontologischer Forschung gewinnen zurzeit Deutsche Forschungsgemeinschaft (DFG), Bonn stark an Bedeutung für die Beantwortung einiger der zentra- len Fragen der Menschheit im 21. Jahrhundert. Nur durch Department für Geo- u. Umweltwissenschaften den Rückblick in die Erdgeschichte können die Folgen des (Fragile Earth Programm), LMU München derzeitigen Verlustes von Biodiversität bis hin zu den lokalen und globalen Auswirkungen des Klimawandels wirklich inter- Münchner Universitätsgesellschaft, München pretiert und verstanden werden. Das Fach Paläontologie rückt somit verstärkt ins Zentrum der öffentlichen Wahrnehmung. Fakultät für Geowissenschaften, LMU München Renommierte Keynote-Sprecher und Vortragende aus aller Welt haben zu einem anspruchsvollen und vielfältigen Prof. Dr. Axel von Hillebrandt, Berlin Programm der 80. Jahrestagung der Paläontologischen Ge- sellschaft beigetragen. Vorträge für 11 Symposien, für "Freie Prof. Dr. Dr. Dietrich Herm, München Themen", zahlreiche Poster, ein Öffentlicher Vortrag sowie ein Kompaktkurs, alle aus spannenden und hochaktuellen E. Schweizerbart'sche Verlagsbuchhandlung Forschungsfeldern, wurden angemeldet. Im Blickpunkt (Nägele & Obermiller), Stuttgart stehen aber nicht nur die Paläontologie und ihre Nachbar- disziplinen, sondern auch unsere Nachwuchsforscher/innen, GE Sensing & Inspection Technologies GmbH, denen mit dem "Zukunfts-Symposium" (Zukunftspreis für phoenixǀx-ray Computer-Tomographen junge Paläontologen) eine attraktive Plattform geboten wird. Das Zukunfts-Symposium, einmalig für die Jahrestagung der GeoBio-Center LMU München Paläontologischen Gesellschaft, wurde anlässlich der goldenen Doktorjubiläen von Prof. Dr. A. von Hillebrandt (Berlin) und unseres Ehrenmitglieds Prof. Dr. Dr. D. Herm (München) in- itiiert; das Preisgeld wurde von den beiden Jubilaren gestiftet. Der rege Zuspruch, den es erfahren hat (18 Vorträge!) zeigt das starke Interesse der Jungforscher/innen für unser Fach. Darüber hinaus bieten wir auch viel Zeit für Poster-Sessions und es besteht die Möglichkeit, das "beste Poster" zu wählen. Weiterhin wird auch wieder das Fossil des Jahres gewählt wer- den. Alle Preisverleihungen finden während des gemeinsamen Abendessens am Freitagabend statt. Wir freuen uns auf viele spannende Beiträge und Diskussionen! 5 Tagungsorganisation und Struktur Tagungsleitung & Tagungsassistenz Prof. Dr. Bettina Reichenbacher, Prof. Dr. Michael Krings, Prof. Dr. Gert Wörheide, Dr. Nora Dotzler, Ella Schönhofer, Ursula Bommhardt Tagungsbüro Ursula Bommhardt, Monika Brinkrolf, Dr. Nora Dotzler, Ella Schönhofer Studentische Hilfskräfte Saskia Börner, Stefan Gehring, Christoph Gierl, Nicola Heckeberg, Patrick Kotyla, Stefanie Penk (alle Bc. Sc.) Veranstalter Department für Geo- und Umweltwissenschaften, Paläontologie & Geobiologie, Ludwig-Maximilians-Universität München Bayerische Staatssammlung für Paläontologie und Geologie GeoBio-CenterLMU Tagungsort Paläontologisches Museum, Richard-Wagner Str. 10, D-80333 München Department für Geo- u. Umweltwissenschaften der LMU München, Richard-Wagner Str. 10, Luisenstr. 37, D-80333 München Wissenschaftliches Programm Das Vortrags- und Poster-Programm umfasst neben den Freien Themen die Symposien A-K mit insgesamt 10 Übersichtsvor- trägen, 112 Vorträgen und 81 Poster-Präsentationen sowie den Öffentlichen Abendvortrag (Prof. Dr. J. Thiede, Kopenhagen). Die Titel und Leiter der Symposien sind: A. Zukunftspreis für junge Paläontologen. - B. Reichenbacher, LMU München, M. Krings, BSPG & LMU München, G. Wörheide, BSPG & LMU München & GeoBio-CenterLMU. B. Hohe Diversität auf allen Ebenen - warum sind Mollusken so erfolgreich? - A. Nützel, BSPG & LMU München, M. Amler, LMU München. C. Fragile Earth - Riffe und Umwelt. - G. Wörheide, BSPG & LMU München & GeoBio-CenterLMU, M. Nose, BSPG. D. Freie Themen Paläobotanik/Palynologie (APP). - L. Kunzmann, Senckenberg Naturhistorische Sammlungen Dresden. E. Mesozoische Gymnospermen. - H. Kerp, Univ. Münster, L. Kunzmann, Senckenberg Dresden, M. Krings, BSPG & LMU München. F. Advances in terrestrial vertebrate palaeontology: understanding large-scale processes in the Eurasian Neogene. - J. Prieto, BSPG & LMU München & Univ. Tübingen. G. Mikropaläontologie. - A.V. Altenbach, LMU München & GeoBio-CenterLMU. H. Potenzial Molekulare Paläobiologie. - G. Wörheide, G. Rößner, beide BSPG & LMU München & GeoBio-CenterLMU. I. Biologic Mineralisation: Paleoarchives, natural functional materials and bacterial mineralisation processes. - E. Griesshaber, W. Schmahl, beide LMU München & GeoBio-CenterLMU. J. Vertebrate diversity and evolution during the Early Mesozoic. - A. Lopez-Arbarello, BSPG, O. Rauhut, BSPG & LMU München, R. Butler, BSPG. K. Early Palaeozoic Ecosystems. - O. Lehnert, Univ. Erlangen. Im Vorfeld der Tagung werden die Exkursionen A-C durchgeführt: A) Jura der Frankenalb (Leitung: W. Werner, BSPG München), B) Obere Süßwassermolasse (Miozän) im bayerischen Alpenvorland (Leitung: G. Rößner, K. Heissig, beide BSPG & LMU München), C) Trias/Jura-Grenze in der Karwendelmulde (GSSP Kuhjoch) (Leitung: A. von Hillebrandt, TU Berlin, K. Kment, Bad Tölz). Im Anschluß an die Tagung (11.-15.10.2010) findet der Labor-KompaktkursMethoden der Molekularen Paläobiologie statt (Leitung: G. Wörheide, BSPG & LMU München & GeoBio-CenterLMU, D. Erpenbeck; LMU München & GeoBio-CenterLMU). 6 Lageplan der Vortragsräume im 1. OG der Richard-Wagner-Str. 10 7 Programm und Zeitplan Dienstag, 5.10.2010 8.00 Uhr Exkursionen A, B, C: ab Parkplatz Richard-Wagner-Str. 10 (hinter Museum) Tagungsbüro & Registration Sitzung von Vorstand & Beirat Anbringen der Poster 16:00 - 20:00, Raum 104 14:00 - 18:00, Raum 12 16:00 - 20:00, Raum 108 & 110 ab 18:00 Icebreaker-Party, Raum 10 Mittwoch, 6.10.2010 8:15 - 8:45 Eröffnung & Begrüßung (in Raum 230) 8:45 - 9:15 K. Remes (DFG Referent): Tipps und Neuigkeiten aus der DFG (in Raum 230) Raum 230 103 Symposium H: 09:15 - Symposium G: R. Asher: Data Integration and Reconstructing the 09:55 A. Altenbach: Holistic micropalaeontology; keynote Mammalian Tree of Life; keynote 09:55 - C. Larroux et al.: What can the sponge genome tell us A. von Hillebrandt: Wo kommen die planktonischen 10:15 about the metazoan last common ancestor? Foraminiferen her? O. Voigt, G. Wörheide: When morphology misleads: An M. Pippèrr, B. Reichenbacher: Planktonic foraminifera: proxies for 10:15 - example of problems with the taxonomy of extant palaeo-bathymetry and past sea-surface tempe-ratures? A case 10:35 Calcareous Sponges (Class Calcarea, Phylum Porifera) history from the early Miocene Upper Marine Molasse Sea 10:35 - 11:00 Kaffeepause / Coffee break (in 106) Symposium H: Symposium D: 11:00 - M. Dohrmann, D. Janussen, A.G. Collins, G. Wörheide: N. Dotzler et al.: Peronosporomycota (Oomycota) in the fossil 11:20 Glass, rocks and clocks: prospects and problems of record molecular dating in hexactinellid sponges 11:20 - D. Erpenbeck et al.:
Load more

Recommended publications
  • A Classification of Living and Fossil Genera of Decapod Crustaceans
    RAFFLES BULLETIN OF ZOOLOGY 2009 Supplement No. 21: 1–109 Date of Publication: 15 Sep.2009 © National University of Singapore A CLASSIFICATION OF LIVING AND FOSSIL GENERA OF DECAPOD CRUSTACEANS Sammy De Grave1, N. Dean Pentcheff 2, Shane T. Ahyong3, Tin-Yam Chan4, Keith A. Crandall5, Peter C. Dworschak6, Darryl L. Felder7, Rodney M. Feldmann8, Charles H. J. M. Fransen9, Laura Y. D. Goulding1, Rafael Lemaitre10, Martyn E. Y. Low11, Joel W. Martin2, Peter K. L. Ng11, Carrie E. Schweitzer12, S. H. Tan11, Dale Tshudy13, Regina Wetzer2 1Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, United Kingdom [email protected] [email protected] 2Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, CA 90007 United States of America [email protected] [email protected] [email protected] 3Marine Biodiversity and Biosecurity, NIWA, Private Bag 14901, Kilbirnie Wellington, New Zealand [email protected] 4Institute of Marine Biology, National Taiwan Ocean University, Keelung 20224, Taiwan, Republic of China [email protected] 5Department of Biology and Monte L. Bean Life Science Museum, Brigham Young University, Provo, UT 84602 United States of America [email protected] 6Dritte Zoologische Abteilung, Naturhistorisches Museum, Wien, Austria [email protected] 7Department of Biology, University of Louisiana, Lafayette, LA 70504 United States of America [email protected] 8Department of Geology, Kent State University, Kent, OH 44242 United States of America [email protected] 9Nationaal Natuurhistorisch Museum, P. O. Box 9517, 2300 RA Leiden, The Netherlands [email protected] 10Invertebrate Zoology, Smithsonian Institution, National Museum of Natural History, 10th and Constitution Avenue, Washington, DC 20560 United States of America [email protected] 11Department of Biological Sciences, National University of Singapore, Science Drive 4, Singapore 117543 [email protected] [email protected] [email protected] 12Department of Geology, Kent State University Stark Campus, 6000 Frank Ave.
    [Show full text]
  • Updated Aragonian Biostratigraphy: Small Mammal Distribution and Its Implications for the Miocene European Chronology
    Geologica Acta, Vol.10, Nº 2, June 2012, 159-179 DOI: 10.1344/105.000001710 Available online at www.geologica-acta.com Updated Aragonian biostratigraphy: Small Mammal distribution and its implications for the Miocene European Chronology 1 2 3 4 3 1 A.J. VAN DER MEULEN I. GARCÍA-PAREDES M.A. ÁLVAREZ-SIERRA L.W. VAN DEN HOEK OSTENDE K. HORDIJK 2 2 A. OLIVER P. PELÁEZ-CAMPOMANES * 1 Faculty of Earth Sciences, Utrecht University Budapestlaan 4, 3584 CD Utrecht, The Netherlands. Van der Meulen E-mail: [email protected] Hordijk E-mail: [email protected] 2 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales MNCN-CSIC C/ José Gutiérrez Abascal 2, 28006 Madrid, Spain. García-Paredes E-mail: [email protected] Oliver E-mail: [email protected] Peláez-Campomanes E-mail: [email protected] 3 Netherlands Centre for Biodiversity-Naturalis Darwinweg 2, 2333 CR Leiden, The Netherlands. Van den Hoek Ostende E-mail: [email protected] 4 Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid. IGEO-CSIC C/ José Antonio Novais 2, 28040 Madrid, Spain. Álvarez-Sierra E-mail: [email protected] * Corresponding author ABSTRACT This paper contains formal definitions of the Early to Middle Aragonian (Late Early–Middle Miocene) small- mammal biozones from the Aragonian type area in North Central Spain. The stratigraphical schemes of two of the best studied areas for the Lower and Middle Miocene, the Aragonian type area in Spain and the Upper Freshwater Molasse from the North Alpine Foreland Basin in Switzerland, have been compared.
    [Show full text]
  • Ischigualasto Formation. the Second Is a Sile- Diversity Or Abundance, but This Result Was Based on Only 19 of Saurid, Ignotosaurus Fragilis (Fig
    This article was downloaded by: [University of Chicago Library] On: 10 October 2013, At: 10:52 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 Vertebrate succession in the Ischigualasto Formation Ricardo N. Martínez a , Cecilia Apaldetti a b , Oscar A. Alcober a , Carina E. Colombi a b , Paul C. Sereno c , Eliana Fernandez a b , Paula Santi Malnis a b , Gustavo A. Correa a b & Diego Abelin a a Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan , España 400 (norte), San Juan , Argentina , CP5400 b Consejo Nacional de Investigaciones Científicas y Técnicas , Buenos Aires , Argentina c Department of Organismal Biology and Anatomy, and Committee on Evolutionary Biology , University of Chicago , 1027 East 57th Street, Chicago , Illinois , 60637 , U.S.A. Published online: 08 Oct 2013. To cite this article: Ricardo N. Martínez , Cecilia Apaldetti , Oscar A. Alcober , Carina E. Colombi , Paul C. Sereno , Eliana Fernandez , Paula Santi Malnis , Gustavo A. Correa & Diego Abelin (2012) Vertebrate succession in the Ischigualasto Formation, Journal of Vertebrate Paleontology, 32:sup1, 10-30, DOI: 10.1080/02724634.2013.818546 To link to this article: http://dx.doi.org/10.1080/02724634.2013.818546 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content.
    [Show full text]
  • University of Michigan University Library
    CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN VOL. XI NO.6, pp. 101-157 (12 pk., 1 map) MARCH25, 1953 TRILOBITES OF THE DEVONIAN TRAVERSE GROUP OF MICHIGAN BY ERWIN C. STUMM UNIVERSITY OF MICHIGAN PRESS ANN ARBOR CONTMBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN MUSEUM OF PALEONTOLOGY Director: LEWIS B. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and also to individuals upon request. Correspondence should be directed to the University of Michigan Press. A list of the separate papers in Volumes II-IX will be sent upon request. VOL. I. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian, by C. L. Fenton and M. A. Fenton. Pages xi+260. Cloth. $2.75. VOL. 11. Fourteen papers. Pages ix+240. Cloth. $3.00. Parts sold separately in paper covers. VOL. 111. Thirteen papers. Pages viii+275. Cloth. $3.50. Parts sold separately in paper covers. VOL. IV. Eighteen papers. Pages viiif295. Cloth. $3.50. Parts sold separately in paper covers, VOL. V. Twelve papers. Pages viii+318. Cloth. $3.50. Parts sold separately in paper covers. VOL. VI. Ten papers. Pages vii+336. Paper covers. $3.00. Parts sold separately. VOLS. VII-IX. Ten numbers each, sold separately. (Continued on inside back cover) VOL.
    [Show full text]
  • Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
    Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages.
    [Show full text]
  • Sedimentology, Taphonomy, and Palaeoecology of a Laminated
    Palaeogeography, Palaeoclimatology, Palaeoecology 243 (2007) 92–117 www.elsevier.com/locate/palaeo Sedimentology, taphonomy, and palaeoecology of a laminated plattenkalk from the Kimmeridgian of the northern Franconian Alb (southern Germany) ⁎ Franz Theodor Fürsich a, , Winfried Werner b, Simon Schneider b, Matthias Mäuser c a Institut für Paläontologie, Universität Würzburg, Pleicherwall 1, 97070 Würzburg, Germany LMU b Bayerische Staatssammlung für Paläontologie und Geologie and GeoBio-Center , Richard-Wagner-Str. 10, D-80333 München, Germany c Naturkunde-Museum Bamberg, Fleischstr. 2, D-96047 Bamberg, Germany Received 8 February 2006; received in revised form 3 July 2006; accepted 7 July 2006 Abstract At Wattendorf in the northern Franconian Alb, southern Germany, centimetre- to decimetre-thick packages of finely laminated limestones (plattenkalk) occur intercalated between well bedded graded grainstones and rudstones that blanket a relief produced by now dolomitized microbialite-sponge reefs. These beds reach their greatest thickness in depressions between topographic highs and thin towards, and finally disappear on, the crests. The early Late Kimmeridgian graded packstone–bindstone alternations represent the earliest plattenkalk occurrence in southern Germany. The undisturbed lamination of the sediment strongly points to oxygen-free conditions on the seafloor and within the sediment, inimical to higher forms of life. The plattenkalk contains a diverse biota of benthic and nektonic organisms. Excavation of a 13 cm thick plattenkalk unit across an area of 80 m2 produced 3500 fossils, which, with the exception of the bivalve Aulacomyella, exhibit a random stratigraphic distribution. Two-thirds of the individuals had a benthic mode of life attached to hard substrate. This seems to contradict the evidence of oxygen-free conditions on the sea floor, such as undisturbed lamination, presence of articulated skeletons, and preservation of soft parts.
    [Show full text]
  • (Echinodermata: Holothuroidea) from the Latest Cretaceous Of
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universität München: Elektronischen Publikationen 285 Zitteliana 89 Short Communication First report of sea cucumbers (Echinodermata: Holothuroidea) from the latest Cretaceous of Paläontologie Bayerische Bavaria,GeoBio- Germany & Geobiologie Center Staatssammlung 1,2,3 LMU München für Paläontologie und Geologie LMUMike MünchenReich 1 n München, 01.07.2017 SNSB - Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, 80333 Munich, Germany 2 n Manuscript received Ludwig-Maximilians-Universität München, Department für Geo- und Umweltwissenschaften, 30.12.2016; revision ac- Paläontologie und Geobiologie, Richard-Wagner-Straße 10, 80333 Munich, Germany 3 cepted 21.01.2017 GeoBio-Center der Ludwig-Maximilians-Universität München, Richard-Wagner-Straße 10, 80333 Munich, Germany n ISSN 0373-9627 E-mail: [email protected] n ISBN 978-3-946705-00-0 Zitteliana 89, 285–289. Key words: fossil Holothuroidea; Cretaceous; Maastrichtian; Bavaria; Germany Schüsselwörter: fossile Holothuroidea; Kreide; Maastrichtium; Bayern; Deutschland The Bavarian Gerhardtsreit Formation (‶Gerhardts- 1993; Smith 2004) due to different reasons (Reich reiter Mergel″ / ‶Gerhardtsreiter Schichten″; cf. 2013). There are nearly 1,700 valid extant sea cucum- Böhm 1891; Hagn 1960; Wagreich et al. 2004), also ber species (Smiley 1994; Kerr 2003; Paulay pers. known as Gerhartsreit Formation (‶Gerhartsreiter comm.) known worldwide. The fossil record (since Schichten″; Hagn et al. 1981, 1992; Schwarzhans the Middle Ordovician; Reich 1999, 2010), by con- 2010; Pollerspöck & Beaury 2014) or ‶Gerhards- trast, is discontinuous in time and recorded ranges reuter Schichten″ (Egger 1899; Hagn & Hölzl 1952; of species with around 1,000 reported forms (Reich de Klasz 1956; Herm 1979, 2000) is exposed in Up- 2013, 2014, 2015b) since the early 19th century.
    [Show full text]
  • Larvae of Marine Bivalves and Echinoderms
    V.L. KflSVflNOV>G.fl. KRVUCHKOVfl VAKUUKOVfl-LAIVICDVCDevn Scientific Cditor Dovid L pQiuson LARVAE OF MARINE BIVALVES AND ECHINODERMS V.L. KASYANOV, G.A. KRYUCHKOVA, V.A. KULIKOVA AND L. A. MEDVEDEVA Scientific Editor David L. Pawson SMITHSONIAN INSTITUTION LIBRARIES Washington, D.C. 1998 Smin B87-101 Lichinki morskikh dvustvorchatykh moUyuskov i iglokozhikh Akademiya Nauk SSSR Dal'nevostochnyi Nauchnyi Tsentr Institut Biologii Morya Nauka Publishers, Moscow, 1983 (Revised 1990) Translated from the Russian © 1998, Oxonian Press Pvt. Ltd., New Delhi Library of Congress Cataloging-in-Publication Data Lichinki morskikh dvustvorchatykh moUiuskov i iglokozhikh. English Larvae of marine bivalves and echinodermsA^.L. Kasyanov . [et al.]; scientific editor David L. Pawson. p. cm. Includes bibliographical references. 1. Bivalvia — Larvae — Classification. 2. Echinodermata — Larvae — Classification. 3. Mollusks — Larvae — Classification. 4. Bivalvia — Lar- vae. 5. Echinodermata — Larvae. 6. Mollusks — Larvae. I. Kas'ianov, V.L. II. Pawson, David L. (David Leo), 1938-III. Title. QL430.6.L5313 1997 96-49571 594'.4139'0916454 — dc21 CIP Translated and published under an agreement, for the Smithsonian Institution Libraries, Washington, D.C., by Amerind Publishing Co. Pvt. Ltd., 66 Janpath, New Delhi 110001 Printed at Baba Barkha Nath Printers, 26/7, Najafgarh Road Industrial Area, NewDellii-110 015. UDC 591.3 This book describes larvae of bivalves and echinoderms, living in the Sea of Japan, which are or may be economically important, and where adult forms are dominant in benthic communities. Descriptions of 18 species of bivalves and 10 species of echinoderms are given, and keys are provided for the iden- tification of planktotrophic larvae of bivalves and echinoderms to the family level.
    [Show full text]
  • From the Upper Triassic (Norian) of Northern Carnic Pre-Alps (Udine, Northeastern Italy)
    GORTANIA. Geologia,GORTANIA Paleontologia, Paletnologia 35 (2013) Geologia, Paleontologia, Paletnologia 35 (2013) 11-18 Udine, 10.IX.2014 ISSN: 2038-0410 Alessandro Garassino ACANTHOCHIRANA TRIASSICA N. SP. Günter Schweigert Giuseppe Muscio AND ANTRIMPOS COLETTOI N. SP. (DECAPODA: AEGERIDAE, PENAEIDAE) FROM THE UPPER TRIASSIC (NORIAN) OF NORTHERN CARNIC PRE-ALPS (UDINE, NORTHEASTERN ITALY) Acanthochirana TRIASSICA N. SP. E AntrimPOS COLETTOI N. SP. (DECAPODA: AEGERIDAE, PENAEIDAE) DAL TRIASSICO SUPERIORE (NORICO) DELLA PREALPI CARNICHE SETTENTRIONALI (UDINE, ITALIA NORDORIENTALE) Riassunto breve - I crostacei decapodi del Triassico superiore (Norico) della Dolomia di Forni sono stati descritti da Ga- rassino et al. (1996). La recente scoperta di un piccolo campione, rivenuto nella Valle del Rio Seazza e in quella del Rio Rovadia, ha permesso un aggiornamento relativo ai crostacei decapodi delle Prealpi Carniche. Gli esemplari studiati sono stati assegnati a Acanthochirana triassica n. sp. (Aegeridae Burkenroad, 1963) e Antrimpos colettoi n. sp. (Penaeidae Rafinesque, 1815). Acanthochirana triassica n. sp. estende il range stratigrafico di questo genere nel Triassico superiore, mentre Antrimpos colettoi n. sp. rappresenta la seconda specie di questo genere segnalata nel Triassico superiore d’Italia. La scoperta di queste due nuove specie incrementa il numero delle specie di peneidi conosciuti nel Norico dell’alta Val Ta- gliamento (Prealpi Carniche settentrionali). Parole chiave: Crustacea, Decapoda, Aegeridae, Penaeidae, Triassico superiore, Prealpi Carniche. Abstract - The decapod crustaceans from the Upper Triassic (Norian) of the Dolomia di Forni Formation were reported by Garassino et al. (1996). The recent discovery of a small sample from this Formation between Seazza and Rovadia brooks allowed updating the decapod assemblages from the Norian of Carnic Pre-Alps.
    [Show full text]
  • Chapter 1 - Introduction
    EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed.
    [Show full text]
  • Available Generic Names for Trilobites
    AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites.
    [Show full text]
  • Decapod Crustaceans from the Middle Jurassic Opalinus Clay of Northern Switzerland, with Comments on Crustacean Taphonomy
    0012-9402/04/030381-12 Eclogae geol. Helv. 97 (2004) 381–392 DOI 10.1007/s00015-004-1137-2 Birkhäuser Verlag, Basel, 2004 Decapod crustaceans from the Middle Jurassic Opalinus Clay of northern Switzerland, with comments on crustacean taphonomy WALTER ETTER Key words: Decapoda, Peracarida, Jurassic, Switzerland, ecology, crustacean taphonomy ABSTRACT ZUSAMMENFASSUNG Four species of decapod crustaceans from the Middle Jurassic Opalinus Clay Aus dem Opalinuston (Mittlerer Jura, Aalenian) der Nordschweiz werden vier (Aalenian) of Northern Switzerland are described. Of these, Mecochirus cf. Arten von decapoden Krebsen beschrieben. Von Aeger sp., Eryma cf. bedelta eckerti is the most common one, while Eryma cf. bedelta, Glyphea sp. and und Glyphaea sp. wurden nur ganz wenige Exemplaren gefunden, während Aeger sp. were present as individuals, or only a few specimens. The preserva- Mecochirus cf. eckerti etwas häufiger ist. Die Erhaltungsbedingungen waren tion of these crustaceans ranges from moderate to excellent, reflecting the während der Ablagerung des Opalinustones günstig, was sich in einer geringen favourable taphonomic conditions of the depositional environment. An inter- Disartikulations- und Fragmentationsrate der Krebse widerspiegelt. Ein in- esting aspect of the taphocoenosis in the Opalinus Clay is that the decapod teressanter Aspekt der Taphocoenose ist die deutliche Dominanz der Klein- crustaceans are by far outnumbered by small peracarid crustaceans (isopods krebse (Peracarida: Isopoden und Tanaidaceen). Dies dürfte die Zahlenver- and tanaids). This is interpreted as reflecting the original differences in abun- hältnisse der ehemaligen Lebensgemeinschaft widerspiegeln. In den meisten dance. Yet this distribution is not frequently encountered in sedimentary se- Ablagerungen dominieren jedoch die decapoden Krebse, wogegen Peracarida quences where decapods (although rare) are far more common than isopods äusserst selten sind.
    [Show full text]