Crustacea: Decapoda: Erymidae): New Synonyms, Systematic and Stratigraphic Implications
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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. -
Decapode.Pdf
We are pleased and honored to welcome at the Paléospace Museum of Villers-sur-Mer the “6th Symposium on Mesozoic and Cenozoic Decapod Crustaceans”. Villers-sur-Mer is a place universally known by specialists and amateurs of palaeontology due to its famous Vaches Noires cliffs. Villers-sur-Mer has also the distinction of being the only French seaside resort located on the Greenwich Meridian line. The Paléospace is a Museum funded in 2011 with the label Musée de France. Three main animations linked to the Time are presented: palaeontology, astronomy and nature with the neighbouring marsh. The museum is in a constant evolution. For instance, an exhibition specially dedicated to dinosaurs was opened two years ago and a planetarium will open next summer. Every year a very high quality temporary exhibition takes place during the summer period with very numerous animations during all the year. The Paléospace does not stop progressing in term of visitors (56 868 in 2015) and its notoriety is universally recognized both by the other museums as by the scientific community. We are very proud of these unexpected results. We thank the dynamism and the professionalism of the Paléospace team which is at the origin of this very great success. We wish you a very good stay at Villers-sur-Mer, a beautiful visit of the Paléospace and especially an excellent congress. Jean-Paul Durand, Mayor and President of Paléospace MOT DU MAIRE DE VILLERS-SUR-MER Nous sommes très heureux et très honorés d’accueillir à Villers-sur-Mer, le « 6e Symposium on Mesozoic and Cenozoic Decapod Crustaceans » dans le cadre du Paléospace. -
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. -
New Studies of Decapod Crustaceans from the Upper Jurassic Lithographic Limestones of Southern Germany
Contributions to Zoology, 72 (2-3) 173-179 (2003) SPB Academic Publishing bv, The Hague New studies of decapod crustaceans from the Upper Jurassic lithographic limestones of southern Germany Günter Schweigert¹ & Alessandro Garassino² 2 1 Staatliches Museum fiir Naturkunde, Rosenstein I, D-70I91 Stuttgart, Germany; Museo civico di Storia naturale, Corso Venezia 55, 1-20121 Milano, Italy Keywords:: Crustacea, Decapoda, lithographic limestones, Upper Jurassic, Solnhofen, fossil record, diversity Abstract Introduction The Upper Jurassic lithographic limestones ofsouthern Germany TheUpper Jurassic lithographic limestones in south- have long been known for their exceptional preservation of ern Germany outcrop at numerous localities are of decapod crustaceans (Glaessner, 1965), similar to the Upper and differentage setting and span an area of sev- Cretaceous of Lebanon (Hakel, Hadjoula) and the still poorly eral hundreds of kilometers (Fig. 1, Table 1) with known Callovian strataat La Voulte-sur-Rhône (France). In these localities in the Frankische Alb often summarized non-bioturbatedlimestones, the decay of decapod skeletons is that mineralized and reduced, so besides the heavily chelae as ‘Solnhofen Lithographic Limestones’. Many fos- often even delicate structures such as pleopods and carapace sils, both in old and new collections (fossil traders), antennae are preserved. Recently, new decapod material has which is are labeled ‘Solnhofen’, highly mislead- been obtained from both scientific and commercial excavations, ing and precludes recognition of evolutionary trends in part in reopened lithographic limestone quarries. I. Fossiliferous lithographic limestones in southern Germany. Downloaded from Brill.com09/24/2021 08:25:23AM via free access 174 G. Schweigert & A. Garassino - New studies of Jurassic limestones from Germany Table I. -
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. -
On Unreported Historical Specimens of Marine Arthropods from The
On unreported historical specimens of marine arthropods from the Solnhofen and Nusplingen Lithographic Limestones (Late Jurassic, Germany) housed at the Muséum national d’Histoire naturelle, Paris Giliane P. Odin, Sylvain Charbonnier, Julien Devillez, Günter Schweigert To cite this version: Giliane P. Odin, Sylvain Charbonnier, Julien Devillez, Günter Schweigert. On unreported historical specimens of marine arthropods from the Solnhofen and Nusplingen Lithographic Limestones (Late Jurassic, Germany) housed at the Muséum national d’Histoire naturelle, Paris. Geodiversitas, Museum National d’Histoire Naturelle Paris, 2019, 41 (1), pp.643. 10.5252/geodiversitas2019v41a17. hal- 02332523 HAL Id: hal-02332523 https://hal.archives-ouvertes.fr/hal-02332523 Submitted on 24 Oct 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. On unreported historical specimens of marine arthropods from the Solnhofen and Nusplingen Lithographic Limestones (Late Jurassic, Germany) housed at the Muséum national d’Histoire naturelle, Paris Sur des spécimens historiques inédits d’arthropodes marins des Calcaires Lithographiques de Solnhofen et Nusplingen (Jurassique supérieur, Allemagne) conservés au Muséum national d’Histoire naturelle, Paris Unreported specimens of marine arthropods from Solnhofen Giliane P. ODIN Centre de Recherche en Paléontologie – Paris (CR2P, UMR 7207), Sorbonne Université, MNHN, CNRS, Muséum national d'Histoire naturelle, Département Origines & Evolution (CP38), 8 rue Buffon, 75005 Paris (France). -
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. -
A Widely Distributed Species During Aptian Times
Aptian Crustacea from Colombia 1 BOLETÍN DE LA SOCIEDAD GEOLÓGICA MEXICANA D GEOL DA Ó VOLUMEN 60, NÚM. 1, 2008, P. 1-10 E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s Occurrence of Meyeria magna M’Coy, 1849 in Colombia: a widely distributed species during Aptian times Francisco J. Vega1,*, Rodney M. Feldmann2, Fernando Etayo-Serna3, Hermann D. Bermúdez-Aguirre4 and Jorge Gómez3 1 Instituto de Geología, Universidad Nacional Autónoma de México. Ciudad Universitaria. México, D.F., Mexico. 2 Department of Geology, Kent State University, Kent, Ohio, 44242, USA. 3 INGEOMINAS-Museo Geológico José Royo y Gómez, Dg 5334-53, Bogota DC, Colombia. 4 Geostratos Lta. Cra. 40, no. 22C-60, Bloque B3, Apto. 1201, Bogotá DC, Colombia. * [email protected] Abstract Occurrence of the mecochirid decapod Meyeria magna M’Coy 1849 is documented based on numerous articulated specimens collected from upper Aptian strata of Colombia. This report represents the fi rst record in America for the species, previously reported from Aptian deposits of Europe. The numerous specimens of a relatively uniform size found in a single stratigraphic level suggests a mass mortality event, favorable conditions for the development of the community, or both. The stratigraphic range for the genus Meyeria is confi rmed to be Lower to Upper Cretaceous. Key words: Crustacea, Mecochiridae, Meyeria, Aptian, Colombia. Resumen La presencia del decápodo mecoquírido Meyeria magna M’Coy 1849, es documentada con base en numerosos ejemplares articulados, recolectados en estratos del Aptiano superior de Colombia. -
Crustáceos Decápodos (Arthropoda: Crustacea: Decapoda) De Aguas Profundas Del Pacífico Mexicano: Lista De Especies Y Material Recolectado Durante El Proyecto TALUD
Crustáceos decápodos (Arthropoda: Crustacea: Decapoda) de aguas profundas del Pacífico mexicano: lista de especies y material recolectado durante el proyecto TALUD Michel E. Hendrickx1 INTRODUCCIÓN Los crustáceos decápodos son organismos omnipresentes en los mares y océanos de la Tierra y han sido encontrados desde la zona intermareal hasta las profundida- des abisales. Contienen los muy conocidos cangrejos, los camarones, los langosti- nos y las langostas. Algunas especies son particularmente llamativas por su forma y sus colores. El grupo de los crustáceos decápodos corresponde a una orden dentro del filo de los Arthropoda (Subfilo Crustacea: Orden Decapoda). Se caracteriza por tener un caparazón generalmente bien calcificado y (salvo algunas excepciones) 10 pares de “patas” (o pereiópodos) que sirven como apéndices prensiles o para desplazarse. Contiene unas 18000 especies y está formado por dos subórdenes y 10 infraordenes. El primer suborden, los Dendrobranchiata, corresponde, entre otras especies, a los camarones clásicos (e.g., los Penaeidae que se pescan en las costas de México). Los Pleocyemata, el segundo suborden de decápodos, contiene todas las demás especies de camarones, langostinos, langostas y cangrejos reparti- das entre 10 infraordenes (Stenopodidea, Caridea, Astacidea, Glypheidea, Axiidea, 1 Laboratorio de Invertebrados Bentónicos, Instituto de Ciencias del Mar y Limnología, Uni- dad Académica Mazatlán, Universidad Nacional Autónoma de México, Joel Montes Cama- rena s/n, Mazatlán 82040, Sinaloa, México. Correo-e: [email protected]. 283 Gebiidea, Achelata, Polychelida, Anomura y Brachyura) (De Grave et al. 2009). De estos, ocho tienen representantes en aguas profundas (Martin y Davis 2001, Brusca y Brusca 2002). Los Glypheidae, con solamente dos especies vivas, no tienen representantes en aguas profundas. -
Late Jurassic) Fossils from Owadów–Brzezinki Quarry, Central Poland: a Review and Perspectives
VOLUMINA JURASSICA, 2016, XIV: 123–132 DOI: 10.5604/17313708 .1222641 New finds of well-preserved Tithonian (Late Jurassic) fossils from Owadów–Brzezinki Quarry, Central Poland: a review and perspectives Błażej BŁAŻEJOWSKI1, Piotr GIESZCZ2, Daniel TYBOROWSKI1, 3 Key words: Late Jurassic, Tithonian, marine and terrestrial fossils, palaeontology, palaeobiogeography. Abstract. Here we briefly report the discovery of new, exceptionally well-preserved Late Jurassic (Tithonian) fossils from Owadów– Brzezinki quarry – one of the most important palaeontological sites in Poland. These finds which comprise organisms living originally in different environments indicate that the Owadów–Brzezinki site represents a link �������������������������������������������������������–������������������������������������������������������ most probably in a form of open marine passages �����–���� be- tweeen distinct palaeobiogeographical provinces. This creates an unprecedented opportunity for better recognition of the regional palaeo- biogeography of adjacent European areas during the Late Jurassic. INTRODUCTION 2012; Kin et al., 2012). These sites, only slightly older than Owadów–Brzezinki (placed near the Early/Late Tithonian The palaeontological site located in Owadów–Brzezinki boundary after Matyja et al., 2016) share many features, quarry (Fig. 1) is one of the most important palaeontological such as a coastal-lagoonal setting, and a great abundance of discoveries described in recent years from Poland (Kin et al., well-preserved fossils. These Bavarian -
The Massive Death of Lobsters Smothered Within Their Thalassinoides Burrows: the Example of the Lower Barremian from Lusitanian Basin (Portugal)
Versão online: http://www.lneg.pt/iedt/unidades/16/paginas/26/30/209 Comunicações Geológicas (2016) 103, Especial I, 143-152 ISSN: 0873-948X; e-ISSN: 1647-581X The massive death of lobsters smothered within their Thalassinoides burrows: the example of the lower Barremian from Lusitanian Basin (Portugal) A morte em massa de lagostas sepultadas no interior das suas galerias do tipo Thalassinoides: o exemplo do Barremiano inferior da Bacia Lusitânica (Portugal) C. Neto de Carvalho 1,* Artigo original © 2014 LNEG – Laboratório Nacional de Geologia e Energia IP Original Article Abstract: Some years ago an exceptional site with the preservation of the evolutiva demonstrada pela ocorrência de Thalassinoides associados a lagostas mecochirid lobster Meyeria rapax (Harbort) within their burrows was glyphoídeos desde o Jurássico Superior ao Aptiano, e à sua progressiva described in the Early Cretaceous of Cabo Espichel sector, Lusitanian Basin, substituição pelos thalassinídeos, com algumas excepções registadas para as Portugal. The large number of articulated specimens preserved at the bottom lagostas queladas, a partir do Cretácico Superior. Esta tendência para a of Thalassinoides burrow systems in, at least, four different beds of the Boca convergência evolutiva no hábito fossorial é comparável com os padrões do Chapim Formation (lower Barremian) suggests that a sudden cyclic event evolutivos de diversificação das lagostas e dos thalassinídeos reconhecidos was responsible for the collective killing below the bottom of a confined recentemente. lagoon, and led to the very rare preservation of both burrows and producers. Palavras-chave: Meyeria rapax ; Thalassinoides suevicus ; morte colectiva; The explanation may be found in the highly heterogranular, coarse-grained convergência comportamental; Barremiano inferior; Bacia Lusitânica clastic filling of the burrow systems which represent influxes of freshwater and large volumes of siliciclastics that may had suddenly drop the salinity 1 Geopark Naturtejo da Meseta Meridional – UNESCO Global Geopark. -
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).