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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. -
Gabaleryon, a New Genus of Widespread Early Toarcian Polychelidan Lobsters Denis Audo, M
Gabaleryon, a new genus of widespread early Toarcian polychelidan lobsters Denis Audo, M. Williams, S. Charbonnier, G Schweigert To cite this version: Denis Audo, M. Williams, S. Charbonnier, G Schweigert. Gabaleryon, a new genus of widespread early Toarcian polychelidan lobsters. Journal of Systematic Palaeontology, Taylor & Francis, 2017, 15 (3), pp.205-222. 10.1080/14772019.2016.1167786. hal-01313737 HAL Id: hal-01313737 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01313737 Submitted on 25 Apr 2017 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. Journal of Systematic Palaeontology, Vol. 000, Issue 000, Month 2015, 000–000 Gabaleryon, a new genus of widespread early Toarcian polychelidan lobsters Denis Audoa,c*, Matt Williamsb, Sylvain Charbonnierc, Günter Schweigertd aUniversité de Rennes 1, EA 7316, 263 Avenue du Général Leclerc CS 74205, 35042 Rennes Cedex, France; bBath Royal Literary and Scientific Institution ; cMuséum national d’Histoire naturelle, Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (CR2P, UMR 7207), Sorbonne Universités-MNHN, CNRS, UPMC-Paris6, 57 rue Cuvier, F- 75005, Paris, France; dStaatliches Museum für Naturkunde, Rosenstein 1, 70191 Stuttgart, Germany. *Corresponding author. Email: [email protected] Polychelidan lobsters are decapod crustaceans with a unique anatomy: a dorsoventrally flattened carapace, four to five pairs of chelate appendages and a completely reduced rostrum. -
Evidence from Fossil Crustaceans in Cold-Water C
Klompmaker et al. BMC Evolutionary Biology (2016) 16:132 DOI 10.1186/s12862-016-0694-0 RESEARCH ARTICLE Open Access Evolution of body size, vision, and biodiversity of coral-associated organisms: evidence from fossil crustaceans in cold- water coral and tropical coral ecosystems Adiël A. Klompmaker1,2,3*, Sten L. Jakobsen4 and Bodil W. Lauridsen5 Abstract Background: Modern cold-water coral and tropical coral environments harbor a highly diverse and ecologically important macrofauna of crustaceans that face elevated extinction risks due to reef decline. The effect of environmental conditions acting on decapod crustaceans comparing these two habitats is poorly understood today and in deep time. Here, we compare the biodiversity, eye socket height as a proxy for eye size, and body size of decapods in fossil cold-water and tropical reefs that formed prior to human disturbance. Results: We show that decapod biodiversity is higher in fossiltropicalreefsfromTheNetherlands,Italy,and Spain compared to that of the exceptionally well-preserved Paleocene (Danian) cold-water reef/mound ecosystem from Faxe (Denmark), where decapod diversity is highest in a more heterogeneous, mixed bryozoan-coral habitat instead of in coral and bryozoan-dominated facies. The relatively low diversity at Faxe was not influenced substantially by the preceding Cretaceous/Paleogene extinction event that is not apparent in the standing diversity of decapods in our analyses, or by sampling, preservation, and/or a latitudinal diversity gradient. Instead, the lower availability of food and fewer hiding places for decapods may explain this low diversity. Furthermore, decapods from Faxe are larger than those from tropical waters for half of the comparisons, which may be caused by a lower number of predators, the delayed maturity, and the increased life span of crustaceans in deeper, colder waters. -
Back Matter (PDF)
INDEX. A. Amies Field,near Broseley, coal-shaft section, 478. Ammonites, vertical range of, in the upper lias Aconcagua, notice of the eruption of, Jan. 18S9, and marlstone of Yorkshire limited, 216. 611. Annagh mine, near Castlemaine, account of, 64. Actinoceras, a genus of Orthocerata, described, Antigua, remarks on a specimen of fossil wood 705. from, 208, 209. Simmsii, observations respecting a Antrim, on the geological structure of the north coral attached to the surface of, 710. eastern part of, 69. Aiken, Arthur, Esq., remarks by, on a piece of physical features and heights of the bog-wood containing small particles of metallic principal mountains, 69. copper, 214. description of the formations :— Aire, notice of the partially petrified wood and mica-slate, hornblende- nuts of the valley of the, 210. slate, granite, &c, 70. Akserai, structure of the country near, 587. — old red sandstone, 71. Alajahscheher, observations on the country near, porphyry, 73. 592. • carboniferous series, Allen Bank, remarks on a specimen of calcareous 74. fossil wood from, 208,209. —• new red sandstone, 75. Allesley, near Coventry, observations on the lias, 77. beds containing silicified stems of trees, 347. • green sand or mulatto, n • remarks on specimens of fossil woods 78. from, 214. chalk, 79. Allihies, notice of the copper mines of, 27. —— trap, 81. Alluvial accumulations, notices of, in the St. •' •• syenite veins which Lawrence, 90, 96,100. traverse mica-slate and chalk to the south of —— comparison of, with the Fair Head, 179. tertiary accumulations, 96. Ardleigh, section of London clay near, 369. , notices of, in Cutch, Argillaceous limestone and schist, description of, 304. -
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. -
Departement De La Haute-Saone
DEPARTEMENT DE LA HAUTE-SAONE Actualisation Avril 2011 S O M M A I R E 1. Présentation du document et de son utilisation 1.1 - Note introductive 1.2 - Fiche modèle 2. Informations générales sur le risque sismique 2.1 - Le phénomène sismique 2.2 - L’aléa sismique 2.3 - La vulnérabilité 2.4 - L’évaluation du risque sismique 2.5 - Les outils de gestion du risque sismique 2.6 - Les responsabilités des acteurs en matière de prévention du risque sismique 3. Cadre réglementaire et technique de la prévention du risque sismique 3.1 - L’architecture générale des textes législatifs, réglementaires et techniques 3.2 - Le zonage réglementaire sismique de la France 3.3 - Les règles de construction parasismique 3.4 - Le scénario de risque sismique 3.5 - Le PPRN-sismique 3.6 - La gestion de crise 3.7 - Le « plan séisme » Références Glossaire Liens utiles 1.Note introductive 1.1 Note introductive au classeur de communication sur la prévention du risque sismique Dans le cadre du programme national de prévention du risque sismique dit Le classeur de communication est constitué de fiches synthétiques pré - « Plan Séisme » lancé en 2005 et de l’évolution réglementaire en cours en sentant les principes nationaux et permettant une adaptation au contexte matière de prévention de ce risque, le Ministère de l'Ecologie, du Dévelop - local ainsi que d’un CD-Rom comportant notamment la version électro - pement durable, des Transports et du Logement a souhaité lancer une nique du classeur. action de communication à destination des préfectures par le biais du présent classeur et de documents associés. -
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Fiche Horaire Ligne : 11_0509 - RP MOLLANS - ARPENANS + Pomoy Validité à partir du 04/09/2017 Itinéraire : Ligne scolaire Itinéraires 11-0509A1 11-0509A1 Commune Point d'arrêt lm-jv--- lm-jv--- POMOY Village 08:10 13:10 Salle Polyvalente 08:11 13:11 MOLLANS Ecole Primaire 08:16 13:16 ARPENANS Ecole maternelle 08:23 13:23 MOLLANS Ecole Primaire 08:30 13:30 Transporteur : SARL TARD Michel et Fils 33 places sous-traité à SARL DU GARAGE BOSCHUNG Horaires ARPENANS et MOLLANS : LM JV : 08 h 30 - 11 h 30 * 13 h 30 - 16 h 30 Direction des Mobilités du Quotidien | Unité Territoriale de la Haute-Saône | Espace 70 - 4A Rue de l'industrie 70000 Vesoul | Tél: 03.84.95.78.80 | Mél: [email protected] Fiche Horaire Ligne : 11_0509 - RP MOLLANS - ARPENANS + Pomoy Validité à partir du 04/09/2017 Itinéraire : Ligne scolaire Itinéraires 11-0509R1 11-0509R1 Commune Point d'arrêt lm-jv--- lm-jv--- MOLLANS Ecole Primaire 11:35 16:35 ARPENANS Ecole maternelle 11:42 16:42 MOLLANS Ecole Primaire 11:49 16:49 POMOY Salle Polyvalente 11:54 16:53 Village 11:55 16:54 Transporteur : SARL TARD Michel et Fils 33 places sous-traité à SARL DU GARAGE BOSCHUNG Horaires ARPENANS et MOLLANS : LM JV : 08 h 30 - 11 h 30 * 13 h 30 - 16 h 30 Direction des Mobilités du Quotidien | Unité Territoriale de la Haute-Saône | Espace 70 - 4A Rue de l'industrie 70000 Vesoul | Tél: 03.84.95.78.80 | Mél: [email protected] Fiche Horaire Ligne : 11_23 - MOLLANS - LURE Validité à partir du 04/09/2017 Itinéraire : Ligne scolaire Nota : A Itinéraires 11-23A1 Commune Point d'arrêt -
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. -
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).