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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. -
A New Classification of the Xanthoidea Sensu Lato
Contributions to Zoology, 75 (1/2) 23-73 (2006) A new classifi cation of the Xanthoidea sensu lato (Crustacea: Decapoda: Brachyura) based on phylogenetic analysis and traditional systematics and evaluation of all fossil Xanthoidea sensu lato Hiroaki Karasawa1, Carrie E. Schweitzer2 1Mizunami Fossil Museum, Yamanouchi, Akeyo, Mizunami, Gifu 509-6132, Japan, e-mail: GHA06103@nifty. com; 2Department of Geology, Kent State University Stark Campus, 6000 Frank Ave. NW, North Canton, Ohio 44720, USA, e-mail: [email protected] Key words: Crustacea, Decapoda, Brachyura, Xanthoidea, Portunidae, systematics, phylogeny Abstract Family Pilumnidae ............................................................. 47 Family Pseudorhombilidae ............................................... 49 A phylogenetic analysis was conducted including representatives Family Trapeziidae ............................................................. 49 from all recognized extant and extinct families of the Xanthoidea Family Xanthidae ............................................................... 50 sensu lato, resulting in one new family, Hypothalassiidae. Four Superfamily Xanthoidea incertae sedis ............................... 50 xanthoid families are elevated to superfamily status, resulting in Superfamily Eriphioidea ......................................................... 51 Carpilioidea, Pilumnoidoidea, Eriphioidea, Progeryonoidea, and Family Platyxanthidae ....................................................... 52 Goneplacoidea, and numerous subfamilies are elevated -
The Eocene Decapod Crustacean Fauna of the "Main" Quarry in Arzignano (Vicenza - Ne Italy) with the Description of a New Species of Raninidae
Lavori - Soc. Ven. Sc. Nat. - Vol. 29: 109-117, Venezia, 31 gennaio 2004 THE EOCENE DECAPOD CRUSTACEAN FAUNA OF THE "MAIN" QUARRY IN ARZIGNANO (VICENZA - NE ITALY) WITH THE DESCRIPTION OF A NEW SPECIES OF RANINIDAE CLAUDIO BESCHIN*, ALESSANDRA BUSULINI**, ANTONIO DE ANGELI***, GIULIANO TESSIER** Key words: Crustacea, Decapoda, Raninidae, Eocene, NE Italy. Abstract The Eocene crustacean fauna found in the "Main" quarry of Arzignano (Vicenza - NE Italy) has been studied for twenty years and the number of species is still increasing. Up to now the known species are 53 and belong to 20 families: Callianassidae, Albuneidae, Diogenidae, Dromiidac, Dynomenidae, Raninidae, Calappidae, Hepatidae, Majidae, Dairidae, Parthenopidae, Retroplumidae, Cheiragonidae, Portunidae, Carpiliidae, Goneplacidae, Pilumnidae, Xanthidae, Palicidae and Grapsidae. The new discovery of a very well preserved specimen of great size has allowed the creation of Lophoranina maxima sp. nov. and a better placement of the specimens previously known as L. cf. reussi. The new species is characterized by the number and the distribution of the transverse ridges on the dorsal surface of carapace and the shape and distribution of the little spines on the ridges which vary in the different phases of growth. The genus Lophoranina is widely spread in the Eocene deposits of Veneto. The great size of the studied specimen let us say that L. maxima sp. nov. is the greatest fossil Raninidae that has ever been found. Riassunto La fauna eocenica a crostacei decapodi delta cava "Main" di Arzignano (Vicenza - Italia nordorientale) con la descrizione di una nuova specie di Raninidae. La fauna a crostacei di eta eocenica rinvenuta nella cava "Main" di Arzignano (Vicenza - Italia nordorientale) viene studiata ormai da vent'anni e si arricchisce continuamente di nuove forme. -
Two New Paleogene Species of Mud Shrimp (Crustacea, Decapoda, Upogebiidae) from Europe and North America
Bulletin of the Mizunami Fossil Museum, no. 33 (2006), p. 77–85, 2 pls., 1 fig. © 2006, Mizunami Fossil Museum Two new Paleogene species of mud shrimp (Crustacea, Decapoda, Upogebiidae) from Europe and North America Rene H. B. Fraaije1, Barry W. M. van Bakel1, John W. M. Jagt2, and Yvonne Coole3 1Oertijdmuseum De Groene Poort, Bosscheweg 80, NL-5283 WB Boxtel, the Netherlands <[email protected]> 2Natuurhistorisch Museum Maastricht, de Bosquetplein 6-7, NL-6211 KJ Maastricht, the Netherlands <[email protected]> 3St. Maartenslaan 88, NL-6039 BM Stramproy, the Netherlands Abstract Two new species of the mud shrimp genus Upogebia (Callianassoidea, Upogebiidae) are described; U. lambrechtsi sp. nov. from the lower Eocene (Ypresian) of Egem (northwest Belgium), and U. barti sp. nov. from the upper Oligocene (Chattian) of Washington State (USA). Both new species here described have been collected from small, ball-shaped nodules; they are relatively well preserved and add important new data on the palaeobiogeographic distribution of fossil upogebiids. Key words: Crustacea, Decapoda, Upogebiidae, Eocene, Oligocene, Belgium, USA, new species Introduction Jurassic species of Upogebia have been recorded, in stratigraphic order: On modern tidal flats, burrowing upogebiid shrimps constitute the dominant decapod crustacean group. For instance, in the 1 – Upogebia rhacheochir Stenzel, 1945 (p. 432, text-fig. 12; pl. intertidal zone of the northern Adriatic (Mediterranean, southern 42); Britton Formation (Eagle Ford Group), northwest of Dallas Europe) up to 200 individuals per square metre have been recorded (Texas, USA). Stenzel (1945, p. 408) dated the Britton (Dworschak, 1987). Worldwide, several dozens of species of Formation as early Turonian, but a late Cenomanian age is Upogebia and related genera are known, and their number is still more likely (compare Jacobs et al., 2005). -
55819057.Pdf
GEOLOGICA BELGICA MEETING 2006 www.ulg.ac.be/geolsed/geologie www.sciencesnaturelles.be/geology/products/geolbelgica/ 2nd BELGIAN GEOLOGICAL CONGRESS LIEGE, BELGIUM, 7 – 8 September 2006 PROGRAM Thursday September 7th 8H00-9H00: WELCOME OF PARTICIPANTS 9H00-9H10: Opening of the meeting: the word of the president (D. Laduron) CLIMATE AND ENVIRONMENTAL GEOLOGY 9H10-9H30: Yans J., Dupuis C. Dating of the weathering processes in the Ardenne area (Belgium) 9H30-9H50: Quinif Y. U/Th dating of a near water-table speleothem in the cave of Han-sur-Lesse - Implications on geodynamics evolution of Ardenne 9H50-10H10: Petermans T., Rosset P., Foriers E., Camelbeeck T. Evaluation and mapping of local site effects and seismic hazard: case studies in Mons Basin and Brussels region 10H10-10H30: Petit J., Taillez A., Verheyden S., Chou L., Mattielli N. First steps towards Cu and Zn isotope geochemistry in estuarine environments 10H30-10H50: COFFEE BREAK AND POSTER SESSION 10H50-11H10: Missiaen, P., Van Itterbeeck, J., Folie, A.,. Markevich, V.S., Van Damme,D., Dian-Yong, G., Smith, Th. The Subeng mammal site (Late Paleocene, China): evidence for a unique woodland on the dry Mongolian Plateau 11H10-11H30: De Vleeschouwer F., Van Vliët-Lanoé B., Fagel N., Richter T., Boës X., Gehrels M. High resolution petrography of impregnated peat columns containing tephras. Principle, applications and perspectives 11H30-11H50: Renson V., De Vleeschouwer F., Fagel N., Mattielli N., Nekrassoff S., Streel, M. Contribution of elemental and lead isotopes geochemistry to archeology in a Belgian peat bog (Hautes Fagnes) 11H50-12H10: De Batist M., Artemov Y., Beaubien S., Greinert J., Holzner C., Kipfer R., Lombardi S., McGinnis D., Naudts L., Schmale O., Schubert C., Van Rensbergen P., Zuppi G.M. -
Geologic Map of Alaska
Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey Front cover. Color shaded relief map of Alaska and surroundings. Sources: 100-meter-resolution natural image of Alaska, http://nationalmap.gov/small_scale/mld/nate100.html; rivers and lakes dataset, http://www.asgdc.state.ak.us/; bathymetry and topography of Russia and Canada, https://www.ngdc.noaa.gov/mgg/global/global.html. Back cover. Previous geologic maps of Alaska: 1906—Brooks, A.H., Abbe, Cleveland, Jr., and Goode, R.U., 1906, The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof: U.S. Geological Survey Professional Paper 45, 327 p., 1 sheet. 1939—Smith, P.S., 1939, Areal geology of Alaska: U.S. Geological Survey Professional Paper 192, 100 p., 18 plates. 1957—Dutro, J.T., Jr., and Payne, T.G., 1957, Geologic map of Alaska: U.S. Geological Survey, scale 1:2,500,000. 1980—Beikman, H.M., 1980, Geologic map of Alaska: U.S. Geological Survey Special Map, scale 1:2,500,000, 2 sheets. Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. -
(Malacostraca: Decapoda) Z Územia Západných Karpát: Súţasný Stav
Spoloþný kongres Slovenskej a ýeskej geologickej spoloþnosti Fosílne desaĢnožce (Malacostraca: Decapoda) z územia Západných Karpát: súþasný stav poznania M. Hyžný Katedra geológie a paleontológie, Prírodoved. fakulta Univerzity Komenského v Bratislave, [email protected] esaĢnožce (Malacostraca: Decapoda) patria Ružomberka uvádzajú Lörenthey & Beurlen (1929) Dmedzi najdiverzifikovanejšie skupiny pankru- taxóny Laeviranina fabianii, Harpactoxanthopsis staceí a v rámci kôrovcov (Crustacea) tvoria druho- quadrilobata a Harpactocarcinus punctulatus. vo najpoþetnejší rad. V zbierkovom fonde Liptovského múzea v Ružom- Ich systematickému výskumu sa na území Zá- berku sa nachádzajú aj zvyšky krabov urþené do padných Karpát venovala v minulosti iba malá po- druhov Ranina reussi a Ranina bittneri; ich syste- zornosĢ. Prvou a vlastne aj poslednou monografiou matické zaradenie þaká na potvrdenie bližším štú- venovanou fosílnym desaĢnožcom, spracovávajú- diom. cou materiál aj z územia dnešného Slovenska, je Z tomášovských vrstiev lokality Ćurkovec uvá- monografická práca Lörentheya & Beurlena (1929). dza Hyžný (2007, 2008a) zvyšky taxónov Ranina Príspevok sumarizuje doterajšie poznatky o tejto nov. sp. (v Hyžný 2007 uvedený ako Ranina specio- skupine zo súvrství slovenskej þasti Západných sa a Ranina sp.), Calappilia tridentata (v Hyžný Karpát. 2008a uvedený ako Calappilia nov. sp.), Coeloma vigil a ?Portunites sp.; ako aj ichnofosílie prisudzo- Mezozoikum vané þinnosti desaĢnožcov Thalassinoides igen. Zvyšky desaĢnožcov v mezozoických fáciách a Ophiomorpha igen. Z rovnakých vrstiev okolia nášho územia sú veĐmi sporadické. Za dosiaĐ naj- súþasnej obce Radatice bol Reussom (1859) opísaný významnejší možno považovaĢ nález dorzálneho taxón Ranina hazslinszkyi. Na typovom materiáli karapaxu homolodromioidného kraba druhu Tanid- však nie sú dostatoþne zachované znaky dôležité pre romites insignis vo vápencoch bohunického súvrs- spoĐahlivé odlíšenie od ostatných druhov rodu Ra- tvia stredno-oxfordského veku lokality Štepnická nina; taxón teda þaká na revíziu. -
Mary Jane Rathbun Papers, 1886-1938 and Undated
Mary Jane Rathbun Papers, 1886-1938 and undated Finding aid prepared by Smithsonian Institution Archives Smithsonian Institution Archives Washington, D.C. Contact us at [email protected] Table of Contents Collection Overview ........................................................................................................ 1 Administrative Information .............................................................................................. 1 Historical Note.................................................................................................................. 1 Descriptive Entry.............................................................................................................. 1 Names and Subjects ...................................................................................................... 2 Container Listing ............................................................................................................. 3 Series 1: GENERAL CORRESPONDENCE, 1894-1938. ARRANGED ALPHABETICALLY................................................................................................... 3 Series 2: MANUSCRIPTS, 1923-1937. ARRANGED CHRONOLOGICALLY.......... 6 Series 3: FOSSIL CRUSTACEA RESEARCH FILE. ARRANGED ALPHABETICALLY................................................................................................... 9 Series 4: PHOTOGRAPHS, 1886, AND UNDATED.............................................. 19 Series 5: AUTOBIOGRAPHICAL MEMOIR, UNDATED......................................... 20 Series -
NARG Newsletter, July 2006 Radiocarbon Dating
ISSUE VII JULY 2006 NARG Newsletter North America Research Group The Bone Wars he Bone Wars were an infamous period Tin the history of paleontology when the INSIDE THIS ISSUE two pre-eminent paleontologists of the time, Edward Drinker Cope and Othniel Charles The Bone Wars 1 Marsh, were competing to see who could find Radiocarbon Dating 2 the most, and most sensational, new species of dinosaur. This competition was marred by Trip Reports bribery, politics, violations of American Oligocene Shoreline 3 Woodburn Dig 10 Indian territories, and virulent personal attacks. Northwest Fossil Fest 4 Edward Drinker Othniel Charles Fossil Gallery 8 The Bone Wars were triggered by the 1858 Cope Marsh Featured Fossil 10 discovery of the holotype specimen of fossilized bones were unearthed. Cope moved Hadrosaurus foulkii by William Parker Foulke to Haddonfield to be near the discoveries, and Happy Birthday NARG 12 in the marl pits of Haddonfield, New Jersey. soon rivaled his mentor in fame. Trilobites It was the first nearly-complete skeleton of a Ecology & Environments 15 dinosaur ever found, and sparked great At the time, Marsh was a professor at Yale interest in the new field of paleontology. The University (which was still called Yale College), skeleton was sent to the Academy of Natural in New Haven, Connecticut, studying Sciences in Philadelphia, where it was named fossilized dinosaur tracks in the Connecticut and described in 1858 by Joseph Leidy, who Valley. As the first American professor of was perhaps the leading paleontologist of the paleontology, the discoveries in New Jersey time. were of intense interest. -
Cephalopods from the Late Eocene Hoko River Formation, Northwestern Washington Richard L
Oi<~e2> K A.. Natural History Museum ifiCl^i Of Los Angeles County IVooCL Invertebrate Paleontology J. Vakom.. 62(1). 1988. pp. 76-82 Copyright 1488. The- Paleontologual Society 0022-3360,88/0062-0076S03.00 CEPHALOPODS FROM THE LATE EOCENE HOKO RIVER FORMATION, NORTHWESTERN WASHINGTON RICHARD L. SQUIRES Department of Geological Sciences, California State University, Northridge 91330 ABSTRACT—Rare specimens of the nautiloids Nautilus and Aturia and extremely rare specimens of a sepiamorph sepiid are described from the late Eocene Hoko River Formation, northern Olympic Peninsula, Washington. The well-preserved partial phragmocones are from channel-fill clastics deposited on the inner and middle slopes of a submarine-fan system. The Nautilus specimen is allied to N. cookanum Whitfield from middle Eocene strata, New Jersey, and is probably conspecific with Nautilus sp. (Miller) from late Eocene strata, northwestern Oregon, both of which were previously assigned to Eutrephoceras. This is the first record of Nautilus in the northeastern Pacific. The Aturia specimen is tentatively identified as A. cf. A. alabamensis (Morton), a species previously only known from late Eocene strata in the Atlantic-Gulf Coastal area and northeastern Mexico. Aturia alabamensis may be the same as numerous Eocene North American aturiid species. The two sepiamorph sepiid specimens resemble Belosepia Voltz but are probably generically distinct. They are only the second record of sepiids in the Eocene of the northeastern Pacific. INTRODUCTION rizian Stage (late Eocene). He also inferred, based on the benthic ATE EOCENE cephalopods are rare in the northeastern Pacific. foraminifers, that the formation was deposited in relatively cool, L moderately shallow ocean waters between lower neritic and up- The occurrence of three genera at a locality in northwestern permost bathyal depths. -
A Taxonomic Review of British Decapod Crustacea
Bulletin of the Mizunami Fossil Museum, no. 29 (2002), p. 81-92. A taxonomic review of British decapod Crustacea Joe S. H. Collins 8 Shaw's Cottages, Perry Rise, London, SE23 2QN, U. K. & Department of Palaeontology, The Natural History Museum, Cromwell Road, London, SW7 5BD, U. K. Abstract Recent changes in the taxonomic position of a number of British decapod crustaceans are brought together from their respective publications. A new crab genus, Stintonius, is described to contain Portunites subovata Quayle & Collins, 1981, Panopeus kempi Ouayle & Collins, 1981, is also transferred to a new genus, Sereneopeus, and a subspecies, Dromilites lamarckii humerosus Quayle & Collins, 1981, is raised to specific status. Key words: Crustacea, Decapoda, Mesozoic, Cenozoic, England Introduction Coeloma sp., from Boxstones, in Suffolk requires verification, while A. Bell (1921) himself, cast doubt on Accounts of the fossil crabs of the British succession are the identification of Calappa sp. that he first recorded in widely distributed in the scientific literature and there is 1897. Cancer deshayesii is considered herein; Maja no recent review that considers their taxonomic diversity. veruccosa, recorded from an almost entire carapace from Continuing research and refinement of diagnoses, often as the Coralline Crag of Butley, presently occurs in the not reflecting the constant differences of opinion between Mediterranean (Zariquiey Alvarez, 1946). The Monograph the 'splitters' and the 'lumpers', latterly largely attendant of the Crustacea of the London Clay by Thomas Bell upon the revision of the Treatise on Invertebrate (1858) remains the only collective work concerning the Palaeontology (Decapoda, Part R) (Feldmann, R. M. & Eocene species. -
A Review of the Decapod Crustaceans from the Tertiary of the Isle of Wight, Hampshire, U
Bulletin of the Mizunami Fossil Museum, no. 38 (2012), p. 33–51, 4 pls., 2 figs., 2 tables. 33 © 202, Mizunami Fossil Museum A review of the decapod crustaceans from the Tertiary of the Isle of Wight, Hampshire, U. K, with description of three new species W. J. Quayle* and J. S. H. Collins** * 4, Argyll Street, Ryde, Isle of Wight, Hampsire, England<[email protected]> ** 8, Shaws Cottages, Perry Rise, London, SE23 2QN, and The Natural History Museum, London, SW7 5BD, England Abstract To the known decapod crustaceans of the Tertiary deposits of the Isle of Wight, Hampshire, the Early Eocene species, Basinotopus lamarkii (Desmarest) and Dromilites bucklandi Bell are introduced from the mainland, as are Glyphithyreus wetherelli (Bell), Rhachiosoma bispinosum Woodward, Coeloma (Litoricola) dentate (Woodward), Xanthilites bowerbanki Bell, and Xanthopsis unispinosa (M'Coy), the stratigrahic range of which has been extended to the London Clay on the Island. The development of an anomaly concerning Zanthopsis unispinosa, also present, if not peculiar to the island, is well established. A carapace of Harpactocarcinus sp. from this horizon is the first British record for the genus. Late Eocene species new to the island are Goniocypoda quaylei Crane, Orthakrolophus depressus? (Quayle and Collins) and Typilobus belli Quayle and Collins. Three new genera and species are described from the Late Eocene Headon Hill Formation; a callianassid, Vecticallichirus abditus; a goneplacid, Gonioplacoides minuta, and a hexapodid, Headonipus tuberculosus. New, superior material of the Late Eocene species, Typilobus obscurus Quayle and Collins, from the type locality, Colwell Bay necessitates a new description. A table of all known Tertiary species of decapod crustaceans from the Isle of Wight is appended.