Jahresbericht 2014
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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. -
Jahresbericht 2016 Und Mitteilungen
der Bayerischen Staatssammlung für Paläontologie und Historische Geologie München e.V. Jahresbericht 2016 und Mitteilungen 45 Verlag Dr. Friedrich Pfeil München 2017 ISSN 0942-5845 ISBN 978-3-89937-222-9 der Bayerischen Staatssammlung für Paläontologie und Historische Geologie München e.V. Jahresbericht 2016 und Mitteilungen 45 Verlag Dr. Friedrich Pfeil München 2017 ISSN 0942-5845 ISBN 978-3-89937-222-9 Bibliografische Information der Deutschen Nationalbibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.dnb.de abrufbar. Redaktion: Martin Nose, Oliver Rauhut, & Winfried Werner Anschrift des Vereins Freunde der Bayerischen Staatssammlung für Paläontologie und Historische Geologie München e.V. Richard-Wagner-Str. 10, D-80333 München Tel (089) 2180-6630 Fax: (089) 2180-6601 E-Mail: [email protected] Homepage: www.palmuc.de/bspg Postbank München IBAN: DE75 7001 0080 0281 2128 03 BIC: PBNKDEFF Deutsche Kreditbank (DKB) AG IBAN: DE09 1203 0000 1004 4185 78 BIC: BYLADEM1001 Sonderkonto »Exkursionen«: Postbank München IBAN: DE23 7001 0080 0482 6128 02 BIC: PBNKDEFF Titelbild: Koralle Montlivaltia sp. aus dem Oberjura von Saal bei Kelheim; SNSB-BSPG 2016 XX1 21 (Sammlung J. Sylla). Durchmesser 2,5 cm. Foto: M. Schellenberger. Copyright © 2017 by Verlag Dr. Friedrich Pfeil, München Dr. Friedrich Pfeil, Wolfratshauser Straße 27, 81379 München www.pfeil-verlag.de Alle Rechte vorbehalten Druckvorstufe: Verlag Dr. Friedrich Pfeil, München Druck: PBtisk a.s., Prˇíbram I – Balonka Printed in the European Union – gedruckt auf chlorfrei gebleichtem Papier – ISSN 0942-5845 – ISBN 978-3-89937-222-9 Inhalt Vereinsgremien .......................................................................................... 4 Grußwort der Sammlungsdirektion ...................................................... -
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. -
Die Raupenfliegen (Diptera: Tachinidae) Mitteleuropas: Bestimmungstabellen Und Angaben Zur Verbreitung Und Ökologie Der Einzelnen Arten
5 download Biodiversity Heritage Library, http://www.biodiversitylibrary.org/ Stuttgarter Beiträge zur Naturkunde Serie A (Biologie) Herausgeber: 4fr für Naturkunde, RosensteinV 70 19 l; , Staatliches Museum 1, D- r Stuttgart Stuttgarter Beitr. Naturk. Ser. A Nr. 506 170 S ,4. 9. 19.94 Professor Dr. Bernhard Ziegler zum 65. Geburtstag Die Raupenfliegen (Diptera: Tachinidae) Mitteleuropas: Bestimmungstabellen und Angaben zur Verbreitung und Ökologie der einzelnen Arten The Tachinids (Diptera: Tachinidae) of Central Europe: Identification Keys for the Species and Data on Distribution and Ecology Von Hans-Peter Tschorsnig und Benno Herting, Stuttgart Mit 291 Abbildungen Summary Keys are given for all central and northern European species of Tachinidae (Diptera). The most important data on distribution and ecology (mainly habitat, phenology, and host-range) are listed for the central European species. Zuammenfassung Es werden Bestimmungsschlüssel für alle in Mittel- und Nordeuropa vorkommenden Arten der Tachinidae (Diptera) gegeben. Für jede mitteleuropäische Art werden die wichtigsten Kenndaten zur Verbreitung und Ökologie (vor allem Habitat, Flugzeit und Wirtskreis) aufge- listet. Inhalt 1. Einleitung 2 2. Beg'iff.c erklärungen 4 2.1. Allgemeines 4 2.2. Kopf 5 2.3. Thorax 7 2.4. Flügel 8 2.5. Beine 9 2.6. Abdomen 10 2.7. Bereifung 11 2.8. Färbung . 11 download Biodiversity Heritage Library, http://www.biodiversitylibrary.org/ 2 STUTTGARTER BEITRÄGE ZUR NATURKUNDE Ser. A, Nr. 506 2.9. Körpergröße 11 2.10. Abkürzungen 11 3. Schlüssel für die Gattungen 12 4. Schlüssel für die Arten . 42 4.1. Subfamilie Exoristinae 42 4.2. Subfamilie Tachininae 63 4.3. Subfamilie Dexiinae 79 4.4. -
Functional Diversity of Marine Ecosystems After the Late Permian Mass
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Plymouth Electronic Archive and Research Library 1 Title: Functional diversity of marine ecosystems after the Late Permian mass 2 extinction event 3 4 Authors: William J. Foster1*, Richard J. Twitchett1 5 6 Affiliations: 1Plymouth University, School of Geography, Earth and Environmental Sciences, 7 Drake Circus, Plymouth, Devon. PL4 8AA. United Kingdom. 8 9 Keywords: mass extinction; ecospace; reefs; marine invertebrates; Permian; Triassic 10 11 Introductory paragraph: The Late Permian mass extinction event was the most severe such 12 crisis of the past 500 million years and occurred during an episode of global warming. It is 13 assumed to have had significant ecological impact, but its effects on marine ecosystem 14 functioning are unknown and the patterns of marine recovery are debated. We analysed the fossil 15 occurrences of all known Permian-Triassic benthic marine genera and assigned each to a 16 functional group based on their inferred life habit. We show that despite the selective extinction 17 of 62-74% of marine genera there was no significant loss of functional diversity at the global 18 scale, and only one novel mode of life originated in the extinction aftermath. Early Triassic 19 marine ecosystems were not as ecologically depauperate as widely assumed, which explains the 20 absence of a Cambrian-style Triassic radiation in higher taxa. Functional diversity was, however, 21 significantly reduced in particular regions and habitats, such as tropical reefs, and at these scales 22 recovery varied spatially and temporally, probably driven by migration of surviving groups. -
No Slide Title
Tachinidae: The “other” parasitoids Diego Inclán University of Padova Outline • Briefly (re-) introduce parasitoids & the parasitoid lifestyle • Quick survey of dipteran parasitoids • Introduce you to tachinid flies • major groups • oviposition strategies • host associations • host range… • Discuss role of tachinids in biological control Parasite vs. parasitoid Parasite Life cycle of a parasitoid Alien (1979) Life cycle of a parasitoid Parasite vs. parasitoid Parasite Parasitoid does not kill the host kill its host Insects life cycles Life cycle of a parasitoid Some facts about parasitoids • Parasitoids are diverse (15-25% of all insect species) • Hosts of parasitoids = virtually all terrestrial insects • Parasitoids are among the dominant natural enemies of phytophagous insects (e.g., crop pests) • Offer model systems for understanding community structure, coevolution & evolutionary diversification Distribution/frequency of parasitoids among insect orders Primary groups of parasitoids Diptera (flies) ca. 20% of parasitoids Hymenoptera (wasps) ca. 70% of parasitoids Described Family Primary hosts Diptera parasitoid sp Sciomyzidae 200? Gastropods: (snails/slugs) Nemestrinidae 300 Orth.: Acrididae Bombyliidae 5000 primarily Hym., Col., Dip. Pipunculidae 1000 Hom.:Auchenorrycha Conopidae 800 Hym:Aculeata Lep., Orth., Hom., Col., Sarcophagidae 1250? Gastropoda + others Lep., Hym., Col., Hem., Tachinidae > 8500 Dip., + many others Pyrgotidae 350 Col:Scarabaeidae Acroceridae 500 Arach.:Aranea Hym., Dip., Col., Lep., Phoridae 400?? Isop.,Diplopoda -
Geologie Und Paläontologie
LWL-Museum für Naturkunde Westfälisches Landesmuseum mit Planetarium Geologie und Paläontologie Liste aller lieferbaren Hefte | Stand 16.12.2020 Geologie und Paläontologie in Westfalen Heft 53 Schallreuter, Roger: Ostrakoden aus silurischen Geschieben IV. (69 Heft 62 Skupin, Klaus; Stritzke, Rüdiger: Frühdrenthezeitliche S., 14 Taf.) Januar 2000, 978-3-924590-65-9 257 g - 14,57 € Ablagerungen im östlichen und südöstlichen Münsterland. Wiese, Frank; Kaplan, Ulrich: Der Mittel-/Ober-Turon Grenzbereich im Raum Lengerich. Heft 54 Mutterlose, Jörg; Klein, Christian; Kessels, Kai: Die Floren- und Kaplan, Ulrich: Neue Beobachtungen zu den Stromberg-Schichten, Faunenführung des Ober-Valangin (Unter-Kreide) in NW Deutschland. (95 Untercampan, Oberkreide, südöstliches Münsterland. S., 29 Abb., 23 Taf.) Januar 2000, 978-3-924590-66-6 342g - 17,90 € Schöllmann, Lothar: Archaeostomatopodea (Malacostraca, Hoplocarida) aus dem Namur B (höheres Marsdenium, Karbon) von Hagen-Vorhalle (NRW, Heft 55 Schallreuter, Roger: Ostrakoden a. silurischen Geschieben V. Deutschland) und eine Neudefinition einiger Arten der Familie Rödder, Gerhard; Ziegler, Fred-Karsten: Kloedenia saalensis n. sp., eine neue Tyrannophontidae. (141 S., 46 Abb., 2 Tab., 10 Taf.) obersilurische Ostrakodenart aus einem Beyrichienkalk-Geschiebe des November 2004, 978-3-924590-81-9 468 g - 19,90 € Münsterländer Hauptkiessandzuges. Braun, Andreas; Gosny, Olaf: Strukturbietend erhaltene Achsen von Bilignea Heft 63 Grzegorczyk, Detlef; Gumprecht, Almuth; Hendricks, Alfred; Lanser, aus Kieselschiefern des Unter-Karbons bei Wuppertal (Bergisches Land, Klaus-Peter; Schöllmann, Lothar: Anwendung des Denkmalschutzgesetzes Deutschland). (117 S., 1 Abb., 2 Tab., 23 Taf. ) von Nordrhein-Westfalen im Bereich der Paläontologie. November 2000, 978-3-924590-68-0 394 g - 18,41 € Grzegorczyk, Detlef: In die Denkmallisten eingetragene Bodendenkmäler in Westfalen-Lippe (Stand 2004). -
Crustacea : Decapoda : Erymidae) Dans Le Jurassique
Première occurrence d’Enoploclytia M’Coy, 1849 (Crustacea : Decapoda : Erymidae) dans le Jurassique First occurence of Enoploclytia M’Coy, 1849 (Crustacea: Decapoda: Erymidae) in the Jurassic Julien Devillez Muséum national d’Histoire naturelle, Paris Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (CR2P, UMR 7207), Sorbonne Universités, MNHN, UPMC, CNRS, 57 rue Cuvier F-75005 Paris (France) [email protected] Sylvain Charbonnier Muséum national d’Histoire naturelle, Paris Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (CR2P, UMR 7207), Sorbonne Universités, MNHN, UPMC, CNRS, 57 rue Cuvier F-75005 Paris (France) [email protected] Jean-Philippe Pezy Normandie Univ, UNICAEN, CNRS, M2C, 14000 CAEN, France [email protected] RÉSUMÉ Parmi les Erymidae Van Straelen, 1925, connus dès le Permien supérieur (Changhsingien) et répandus au Jurassique, le genre Enoploclytia M’Coy, 1849 passe pour être apparu tardivement en raison de son absence avant le Crétacé. Jusqu’à présent, le plus ancien représentant était E. augustobonae Devillez, Charbonnier, Hyžný & Leroy, 2016 du Crétacé inférieur (Barrémien) de l’est du bassin de Paris (France). Cependant, un nouveau fossile récolté en Normandie (France), présentant une architecture des sillons de la carapace typique d’Enoploclytia, atteste de la présence du genre dès le Jurassique supérieur (Oxfordien). MOTS CLÉS Crustacé, Erymidae, France, homard, Jurassique, Mésozoïque, Normandie. ABSTRACT Among the Erymidae Van Straelen, 1925, known as early as the Late Permian (Changhsingian) and widespread in the Jurassic, the genus Enoploclytia M’Coy, 1849 seems to have a late appearance because of its lack before the Cretaceous. Until now, the oldest representative was E. -
Westfalens Jurassic Park – Tetrapoden Aus Dem Ornatenton
plan and a highly specialised mode of locomo- en bevestigd het vermoeden dat de diversica- tion using four ippers. The discovery of the tie van de Plesiosauria in het late Trias plaats- skeleton of a Plesiosaurus at Warburg-Bonen- vond. Ze overleefden de nog slecht begrepen burg is the rst ever skeletal and thus con- massa-uitsterving aan het eind van het Trias rmed evidence dating from the Triassic peri- door hun gespecialiseerde marine levenswijze. od. Rhaeticosaurus is a basal Pliosaurus, which conrms the assumption that the diversica- Literatur tion of Plesiosauria occurred during the late Roger Benson/Mark Evans/Patrick S. Druckenmiller, Triassic. Thanks to their high-marine life form, High Diversity, Low Disparity and Small Body Size in Plesiosaurs (Reptilia, Sauropterygia) from the Triassic– Plesiosauria survived the extinction event that Jurassic Boundary. PLoS ONE 7(3), 2012, e31838. – Detlef occurred at the end of the Triassic, which is not Grzegorczyk, Ein Meeresreptil aus Warburg-Bonenburg. yet fully understood. Archäologie in Westfalen-Lippe 2014, 2015, 26–28. – Paul Martin Sander u. a., Die paläontologische Grabung AUSGRABUNGEN UND FUNDE UND FUNDE AUSGRABUNGEN Samenvatting in der Rhät-Lias-Tongrube der Fa. Lücking bei Warburg- Bonenburg (Kr. Höxter) im Frühjahr 2015. Geologie und Plesiosauria waren de meest gedifferentieerde Paläontologie in Westfalen 88, 2016, 11–37. – Tanja en succesvolste marine reptielen uit de Jura en Wintrich u. a., A Triassic Plesiosaurian Skeleton and Bone het Krijt, met een uniek ontwerp en een sterk Histology inform on Evolution of a unique Body Plan. gespecialiseerde, viervinnige wijze van voort- Sciences Advances 3, 2017, e1701144. bewegen. -
Documentation and Revision of the Index Ostracods from the Lower and Middle Jurassic in SW Germany According to BUCK (1954)
Palaeodiversity 2: 119–167; Stuttgart, 30.12.2009. 119 Documentation and revision of the index ostracods from the Lower and Middle Jurassic in SW Germany according to BUCK (1954) MATTHIAS FRANZ, EKATERINA TESAKOVA & ELKE BEHER Abstract The ostracods from the unpublished table by BUCK (1954) are revised and figured by SEM photographs. Two new species, Aphelocythere? asymmetrica n. sp. and Palaeocytheridea blaszykina n. sp., are described. Three manuscript names are formally established here: Neurocythere cingata n. sp. BRAUN in FRANZ et al., N. tricostata n. sp. BRAUN in FRANZ et al. and Bairdia pumicosa n. sp. SHEPPARD in FRANZ et al. The stratigraphical distribution of all species in the BUCK table in SW Germany has been modified according to literature data. K e y w o r d s : Ostracods, Lower Jurassic, Middle Jurassic, SW Germany. Kurzfassung Die Ostrakoden der unveröffentlichten Tabelle von BUCK (1954) werden revidiert und mittels REM-Aufnahmen abgebildet. Zwei neue Arten, Aphelocythere? asymmetrica n. sp. und Palaeocytheridea blaszykina n. sp., werden aufgestellt; darüberhinaus werden drei Arten, Neurocythere cingata n. sp. BRAUN in FRANZ et al. und N. tricostata n. sp. BRAUN in FRANZ et al. sowie Bairdia pumicosa n. sp. SHEPPARD in FRANZ et al. hiermit veröffentlicht. Die stratigraphischen Reichweiten der Arten der BUCK-Tabelle in SW-Deutschland wurden anhand von Literaturdaten modifiziert. Contents 1. Introduction ............................................................................ 119 2. Stratigraphy ............................................................................121 -
Pseudosonninia, a New Genus of Oppeliid Ammonite (Haploceratoidea) from the Callovian (Middle Jurassic) of the Neuquén Basin, Argentina
VOLUMINA JURASSICA, 2019, XVII: 39–48 DOI: 10.7306/VJ.17.3 Pseudosonninia, a new genus of oppeliid ammonite (Haploceratoidea) from the Callovian (Middle Jurassic) of the Neuquén Basin, Argentina Horacio PARENT1, Alberto C. GARRIDO2, Günter SCHWEIGERT3, Luciano BRAMBILLA4 Key words: ammonites, Callovian, Los Molles Fm., Chacay Melehué, Argentina. Abstract. From the uppermost part of the Los Molles Formation (upper Lower and lower Middle Callovian) in Chacay Melehué (Neu- quén Province, Argentina), a group of hecticoceratine ammonites with a conspicuous morphology not assimilable to any known genus of this subfamily has been recently discovered. These forms are inflated oxycones with a prominent, sharp keel developed from the juvenile phragmocone up to the adult peristome. The new genus Pseudosonninia is established on the basis of these ammonites, with Pseudoson- ninia chacaymelehuensis n. gen. n. sp. as its type species. The new genus seems to be endemic to the Neuquén Basin and is recorded here from the upper Lower and lower Middle Callovian of Chacay Melehué and Río de Los Patos. INTRODUCTION zons of the Lower Callovian Bodenbenderi and Proximum zones, as well as from the highest levels of the Los Molles The Lower-Middle Callovian oppeliids from the upper Fm., a few meters below the Tábanos Fm., which are situated part of the Los Molles Fm. are poorly known throughout the above the Proximum Zone. Among these ammonites there Neuquén Basin (Fig. 1A). Besides several papers mention- are hecticoceratine morphotypes mostly belonging to Hecti- ing different species (e.g. Keidel, 1910; Groeber, 1918, coceras Bonarelli, 1893, but others correspond to an unde- Groeber et al., 1953; Stipanicic, 1965; Westermann, 1967; scribed genus. -
Annual Meeting 2014
The Palaeontological Association 58th Annual Meeting 16th–19th December 2014 University of Leeds PROGRAMME abstracts and AGM papers Public transport to the University of Leeds BY TRAIN: FROM TRAIN STATION ON FOOT: Leeds Train Station links regularly to all major UK cities. You The University campus is a 20 minute walk from the train can get from the station to the campus on foot, by taxi or by station. The map below will help you find your way. bus. A taxi ride will take about 10 minutes and it will cost Leave the station through the exit facing the main concourse. approximately £5. Turn left past the bus stops and walk down towards City Square. Keeping City Square on your left, walk straight up FROM TRAIN STATION BY BUS: Park Row. At the top of the road turn right onto The Headrow, We advise you to take bus number 1 which departs from passing The Light shopping centre on your left. After The Light Infirmary Street. The bus runs approximately every 10 minutes turn left onto Woodhouse Lane to continue uphill. Keep going, and the journey takes 10 minutes. passing Morrisons, Leeds Metropolitan and the Dry Dock You should get off the bus just outside the Parkinson Building. boat pub heading for the large white clock tower. This is the (There is also the £1 Leeds City Bus which takes you from the Parkinson building. train station to the lower end of campus but the journey time is much longer). BY COACH: If you arrive by coach you can catch bus numbers 6,28 or 97 to the University (Parkinson Building).