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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 University of Michigan
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 31, NO. 4, PP. 89-118 July 30, 2004 NEW DECAPODA (CRUSTACEA) FROM THE MIDDLE AND LATE EOCENE OF PAKISTAN AND A REVISION OF LOBONOTUS A. MILNE EDWARDS, 1864 BY CARRIE E. SCHWEITZER, RODNEY M. FELDMANN, AND PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page plus a table of contents will be sent to libraries on the Museum’s mailing list. This will be sent to individuals on request. A list of the separate issues may also be obtained by request. Correspondence should be directed to the Publications Secretary, Museum of Paleontology, The University of Michigan, 1109 Geddes Road, Ann Arbor, Michigan 48109-1079 ([email protected]). VOLS. 1-31: Parts of volumes may be obtained if available. Price lists are available upon inquiry. See also: www.paleontology.lsa.umich.edu/Publications/publicationIntro.html Text and illustrations ©2004 by the Museum of Paleontology, University of Michigan NEW DECAPODA (CRUSTACEA) FROM THE MIDDLE AND LATE EOCENE OF PAKISTAN AND A REVISION OF LOBONOTUS A. MILNE EDWARDS, 1864 BY CARRIE E. SCHWEITZER1, RODNEY M. FELDMANN2, AND PHILIP D. GINGERICH3 Abstract– Recovery of new decapod specimens from middle and late Eocene rocks of Pakistan prompted reevaluation of the known decapod fauna of the region. -
How to Become a Crab: Phenotypic Constraints on a Recurring Body Plan
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 25 December 2020 doi:10.20944/preprints202012.0664.v1 How to become a crab: Phenotypic constraints on a recurring body plan Joanna M. Wolfe1*, Javier Luque1,2,3, Heather D. Bracken-Grissom4 1 Museum of Comparative Zoology and Department of Organismic & Evolutionary Biology, Harvard University, 26 Oxford St, Cambridge, MA 02138, USA 2 Smithsonian Tropical Research Institute, Balboa–Ancon, 0843–03092, Panama, Panama 3 Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA 4 Institute of Environment and Department of Biological Sciences, Florida International University, Biscayne Bay Campus, 3000 NE 151 Street, North Miami, FL 33181, USA * E-mail: [email protected] Summary: A fundamental question in biology is whether phenotypes can be predicted by ecological or genomic rules. For over 140 years, convergent evolution of the crab-like body plan (with a wide and flattened shape, and a bent abdomen) at least five times in decapod crustaceans has been known as ‘carcinization’. The repeated loss of this body plan has been identified as ‘decarcinization’. We offer phylogenetic strategies to include poorly known groups, and direct evidence from fossils, that will resolve the pattern of crab evolution and the degree of phenotypic variation within crabs. Proposed ecological advantages of the crab body are summarized into a hypothesis of phenotypic integration suggesting correlated evolution of the carapace shape and abdomen. Our premise provides fertile ground for future studies of the genomic and developmental basis, and the predictability, of the crab-like body form. Keywords: Crustacea, Anomura, Brachyura, Carcinization, Phylogeny, Convergent evolution, Morphological integration 1 © 2020 by the author(s). -
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). -
Theuniversity Oftexasbulletin 3101 Plate XII 230 the University of Texas Bulletin PLATE XIII Figures— Page 1
TheUniversity of TexasBulletin No. 3101: January 1, 1931 Contributions to Geology, 1931 Bureau of Economic Geology J. A.Udden, Director E. H.Sellards, AssociateDirector PUBLISHED BY THE UNIVERSITY OF TEXAS AUSTIN Publications of The University of Texas Publications Committees GENERAL: Frederic Duncalp Mrs. C. M. Perry J. F.Dobie C. H. Slover J. L.Henderson G. W. Stumberg H. J. Muller A. P.Winston official: E. J. Mathews Killis Campbell C. F. Arrowood C. D.Simmons E. C.H.Bantel Bryant Smith The University publishes bulletins four times a month, so numbered that the first two digits of the number show the year of issue and thelast two the position in the yearly series. (For example, No. 3101 is the first bulletin of the year 1931.) These bulletins comprise the official publica- tions of the University, publications on humanistic and scientific subjects, and bulletins issued from time to time by various divisions of the University. The following bureaus and divisions distribute bulletins issuedby them; communications concerning bulletins in these fields should beaddressed toThe University of Texas,Austin,Texas,care of the bureau or division issuing the bulletin: Bureau of Business Research, Bureau of Economic Geology, Bureau of Engineering Research, Interscholastic League Bureau., andDivision of Extension. Communications concerning all other publications of the University should be addressed toUniversity Publications,TheUniversity of Texas,Austin. Additional copies of this publication may be procured from the Bureau of Economic Geology, The University of Texas, Austin, Texas, at $1.00 per copy The University of Texas Bulletin No. 3101: January 1, 1931 Contributions to Geology, 1931 Bureau of Economic Geology J. -
The Formation of Authigenic Deposits During Paleogene Warm Climatic
Banerjee et al. Journal of Palaeogeography (2020) 9:27 https://doi.org/10.1186/s42501-020-00076-8 Journal of Palaeogeography REVIEW Open Access The formation of authigenic deposits during Paleogene warm climatic intervals: a review Santanu Banerjee1* , Tathagata Roy Choudhury1, Pratul Kumar Saraswati1 and Sonal Khanolkar2 Abstract Although Paleogene warm climatic intervals have received considerable attention for atmospheric and oceanographic changes, the authigenic mineralization associated with these time spans remains overlooked. An extensive review of the literature reveals a close correspondence between the high abundance of glauconite and warm climatic intervals during the Paleogene period. The abundance of phosphorite, ironstone, lignite and black shale deposits reveals similar trends. Although investigated thoroughly, the origin of these authigenic deposits is never understood in the background of Paleogene warming climatic intervals. A combination of factors like warm seawater, hypoxic shelf, low rate of sedimentation, and enhanced rate of continental weathering facilitated the glauconitization. The last factor caused the excess supply of nutrients, including Fe, Si, K, Mg and Al through the rivers, the cations needed for the formation of glauconite. The excessive inflow of nutrient-rich freshwater into the shallow seas further ensured high organic productivity and stratification in shallow shelves, causing hypoxia. The consequent rapid rise in sea-level during the warm periods created extensive low-relief shallow marine shelves starved in sediments. Oxygen-deficiency in the shallow marine environment facilitated the fixation of Fe into the glauconite structure. The inflow of nutrient-rich water during the warm climatic intervals facilitated the formation of phosphorite, ironstone, and organic-matter-rich sedimentary deposits as well. -
(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 -
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. -
Early Eocene Evolution of Carbonate Depositional Environments
2017 | 70/1 | 11–25 | 5 Figs. | 2 Pls. | www.geologia-croatica.hr Journal of the Croatian Geological Survey and the Croatian Geological Society Early Eocene evolution of carbonate depositional environments recorded in the Čikola Canyon (North Dalmatian Foreland Basin, Croatia) Jelena Španiček1, Vlasta Ćosović1, Ervin Mrinjek1 and Igor Vlahović2 1 University of Zagreb, Faculty of Science, Department of Geology, Horvatovac 102a, HR-10000 Zagreb, Croatia; (corresponding author: [email protected]) 2 University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Department of Geology and Geological Engineering, Pierottijeva 6, HR-10000 Zagreb, Croatia doi: 10.4154/gc.2017.05 Abstract Article history: The stratigraphic succession in the Čikola Canyon (part of the North Dalmatian Foreland Basin) Manuscript received November 08, 2016 was studied in detail to describe both the sedimentological characteristics and fossil assem- Revised manuscript accepted February 25, 2017 blages of the Lower Eocene deposits during the initial stage of the foreland basin formation. Available online February 28, 2017 The North Dalmatian Basin now represents a part of the Outer Dinarides, and was developed in front of the evolving Dinaric structures by tectonic deformation and marine transgression of an emerged and denuded Mesozoic Adriatic Carbonate Platform (AdCP). During the initial phase, a distal ramp of a foreland basin was formed, characterised by carbonate sedimenta- tion, lasting until the Middle Eocene. In a studied section more than 300 m thick, porcelaneous foraminifera, Alveolina, Orbitolites and complex miliolids (Idalina, Periloculina) prevail, associated with conical agglutinated forms, nummulitids and red algae. These samples belong to the SBZ 11–12 (Ypresian), according to occurrences of Alveolina decastroi, Alveolina cremae, Alveolina multicanalifera and Coskino- lina liburnica. -
ESCONI Library March 2015
Title Author Year Type American Indian Ways of Life, Illinois State Museum,No. 9 Deuel, Thorne 1958 ARCHAEOLOGY-pamphlet Ancient North America, 4th ed. Fagan, Brian M. 2005 ARCHAEOLOGY Archaeology: A Brief Introduction, 9th Ed. Fagan, Brian M. 2006 ARCHAEOLOGY Asiatic Echoes: The Identification of Chinese Pictograms in North American Rock Writing Ruskamp, John A., Jr. 2011 ARCHAEOLOGY Asiatic Echoes: The Identification of Ancient Chinese Pictograms in pre- Columbian North American Rock Writing, 2nd Ed. Ruskamp, John A., Jr. 2013 ARCHAEOLOGY Atlas of the North American Indian Waldman, Carl 1985 ARCHAEOLOGY Bulletin #1 - Illinois Archaeology Illinois Archaeological Surv. 1959 ARCHAEOLOGY-pamphlet Bulletin #2 - Indian Mounds & Villages in Illinois Illinois Archaeological Surv. 1960 ARCHAEOLOGY Bulletin #3 - Chicago Area Archaeology Illinois Archaeological Surv. 1961 ARCHAEOLOGY Bulletin #4 - Reports on Illinois Prehistory Illinois Archaeological Surv. 1963 ARCHAEOLOGY Bulletin #5 - Middle Woodland Sites in Illinois Illinois Archaeological Surv. 1965 ARCHAEOLOGY Bulletin #6 - Hopewell & Woodland Site Archaeology in Illinois Illinois Archaeological Surv. 1968 ARCHAEOLOGY Bulletin #7 - Explorations Into Cahokia Archaeology Illinois Archaeological Surv. 1969 ARCHAEOLOGY Bulletin #8 - Mississippian Site Archaeology in Illinois Illinois Archaeological Surv. 1971 ARCHAEOLOGY Bulletin #9 - Late Woodland Site Archaeology in Illinois Illinois Archaeological Surv. 1973 ARCHAEOLOGY Central States Archaeological Journal, Vol. 28 No. 1-4 1981 ARCHAEOLOGY-pamphlet