Decapod Crustacea : Raninidae
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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. -
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Contributions to Zoology, 72 (2-3) 83-84 (2003) SPB Academic Publishing bv, The Hague An interesting case of homonymy: Notopus de Haan, 1841 (Crustacea, Raninidae; Recent) and Notopus Leonardi, 1983 (ichnofossil; Devonian) ³ Barry+W.M. van Bakel¹, John+W.M. Jagt² & René+H.B. Fraaije 1 2 Schepenhoek 235, NL-5403 GB Uden, the Netherlands; Natuurhistorisch Museum Maastricht, de 3 Bosquetplein 6-7, P.O. Box 882, NL-6200 AW Maastricht, the Netherlands; Oertijdmuseum de Groene Poort, Bosscheweg 80, NL-5283 WB Boxtel, the Netherlands Keywords: Homonymy, Crustacea, ichnofossils, Notopus Abstract N. petri, involves an ichnofossil from the Devonian of Paran-, Brazil (Leeonardi, 1983: 236). Leonard! Upper Cretaceous strata in the type area of the Maastrichtian interpreted this as the imprint of the left front limb Stage Netherlands, NE have yielded (SE Belgium) compara- of an amphibian. Roek & Rage (1994), who restudied tively abundant and diverse raninid assemblages (Collins et al., Leonardos .original material, were of the opinion 1995; Fraaye & van Bakel, 1998). To date, seven species are that this ichnofossil taxon did not represent part of known: Eumorphocorystes sculptus, Pseudoraninella muelleri, but rather similar to Lyreidinapyriformis, Raninoides? quadrispinosus,Raniliformis an amphibian trackway, was asteroid chevrona, Raniliformis prebaltica and Raniliformis occlusa. traces of an or ophiuroid, comparable to These Maastricht occur mainly from the portion of the Asteriacites upper the ichnofossil genus von Schlotheim. Formation[Emael, Nekum andMeerssen members, Belemnitella Irrespective of the correct assignment of this junior and Belemnella (Neobelemnella) kazimiroviensis bio- ichnotaxon, Notopus Leonard!, 1983 (non de Haan, zones]. is in need of substitute the 1841) a name, more so with since ichnotaxon names compete (palaeo)zoo- taxa June Introduction logical (A.K. -
Notopus Dorsipes (Linnaeus) in Singapore: First Record of the Brachyuran Superfamily Raninoidea (Crustacea: Decapoda) on the Sunda Shelf
NATURE IN SINGAPORE 2012 5: 19–25 Date of Publication: 27 January 2012 © National University of Singapore NOTOPUS DORSIPES (LINNAEUS) IN SINGAPORE: FIRST RECORD OF THE BRACHYURAN SUPERFAMILY RANINOIDEA (CRUSTACEA: DECAPODA) ON THE SUNDA SHELF Martyn E. Y. Low1* and S. K. Tan2 1Department of Marine and Environmental Sciences, Graduate School of Engineering and Science University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa 903-0213, Japan 2Raffles Museum of Biodiversity Research, National University of Singapore 6 Science Drive 2, Singapore 117546, Republic of Singapore (*Corresponding author: [email protected]) INTRODUCTION Recently, a brachyuran crab identified as Notopus dorsipes (Linnaeus, 1758), was found at Changi (north-east Singapore). This represents the first record of the superfamily Raninoidea de Haan, 1839, in Singapore and on the Sunda Shelf (Figs. 1, 2). The superfamily Raninoidea has a worldwide distribution and its members inhabit marine habitats from the intertidal zone to over 300 m deep (reviewed in Ahyong et al., 2009; see also Dawson & Yaldwyn, 1994). Fifty species of raninoids are currently assigned to 12 genera in six subfamilies (Ng et al., 2008). Notopus dorsipes belongs to a monotypic genus currently assigned to the subfamily Notopodinae Serène & Umali, 1972 (see Ng et al., 2008). Originally described as Cancer dorsipes by Linnaeus (1758), this species has had a confused nomenclatural history (see Holthuis, 1962). In order to stabilise the name Cancer dorsipes Linnaeus, Holthuis (1962: 55) designated a figure in Rumphius (1705: pl. 10: Fig. 3) as the lectotype of Notopus dorsipes (reproduced as Fig. 3). De Haan (1841) established the genus Notopus for Cancer dorsipes Linnaeus, the type species by monotypy. -
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). -
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Contributions to Zoology, 72 (2-3) 119-130 (2003) SPB Academic Publishing bv, The Hague Evolution of reef-associated decapod crustaceans through time, with particular reference to the Maastrichtian type area René+H.B. Fraaije Oertijdmuseum de Groene Poort, Bosscheweg 80, NL-5283 WB Boxtel, the Netherlands Keywords: Decapod crustacean evolution, K/T boundary, biostratigraphy Abstract prior to 1987 by various authors (Bosquet, 1854; van Binkhorst, 1857; Binkhorst van den Binkhorst, The result of of some twenty years intensive collecting from 1861; Noetling, 1881; Pelseneer, 1886;Forir, 1887a- in the strata Maastrichtian type area is a collection ofmore than c, 1889; Mulder, 1981) suffer from a lack of strati- 1,200 generally small-sized anomuranand brachyuran remains. graphic control. A taxonomic revision of most of The of the stratigraphical ranges thirty-one species known to these was carried out Collins al. date species by et (1995). from the Maastricht Formation (Late Maastrichtian) are shown Since 1987, new from the Maastrichtian and five successive decapod assemblages are discussed. species For the first time, crustacean to decapod remains now turn out type area were described and discussed by Fraaye be useful biostratigraphic tools on a local to regional scale. & Collins (1987), Feldmann et al. (1990), Jagt et al. (1991, 1993), Collins et al. (1995), Fraaye (1996 a-c, 2002), Fraaye & van Bakel (1998) and Jagt et Introduction al. (2000). Rigid collecting from six key sections (see Collins Brachyurans utilize a broad of feeding types, array et al. 1995, p. 168, fig. 1) during the past two de- including deposit feeding, filter feeding, seaweed cades has resulted in an extensive, stratigraphically grazing, and have been scavenging predation. -
Phylogenetics of the Brachyuran Crabs (Crustacea: Decapoda): the Status of Podotremata Based on Small Subunit Nuclear Ribosomal RNA
Available online at www.sciencedirect.com Molecular Phylogenetics and Evolution 45 (2007) 576–586 www.elsevier.com/locate/ympev Phylogenetics of the brachyuran crabs (Crustacea: Decapoda): The status of Podotremata based on small subunit nuclear ribosomal RNA Shane T. Ahyong a,*, Joelle C.Y. Lai b, Deirdre Sharkey c, Donald J. Colgan c, Peter K.L. Ng b a Biodiversity and Biosecurity, National Institute of Water and Atmospheric Research, Private Bag 14901 Kilbirnie, Wellington, New Zealand b School of Biological Sciences, National University of Singapore, Kent Ridge, Singapore c Australian Museum, 6 College Street, Sydney, NSW 2010, Australia Received 26 January 2007; revised 13 March 2007; accepted 23 March 2007 Available online 13 April 2007 Abstract The true crabs, the Brachyura, are generally divided into two major groups: Eubrachyura or ‘advanced’ crabs, and Podotremata or ‘primitive’ crabs. The status of Podotremata is one of the most controversial issues in brachyuran systematics. The podotreme crabs, best recognised by the possession of gonopores on the coxae of the pereopods, have variously been regarded as mono-, para- or polyphyletic, or even as non-brachyuran. For the first time, the phylogenetic positions of the podotreme crabs were studied by cladistic analysis of small subunit nuclear ribosomal RNA sequences. Eight of 10 podotreme families were represented along with representatives of 17 eubr- achyuran families. Under both maximum parsimony and Bayesian Inference, Podotremata was found to be significantly paraphyletic, comprising three major clades: Dromiacea, Raninoida, and Cyclodorippoida. The most ‘basal’ is Dromiacea, followed by Raninoida and Cylodorippoida. Notably, Cyclodorippoida was identified as the sister group of the Eubrachyura. -
Crustacean Research 49: 237-262 (2020)
Crustacean Research 2020 Vol.49: 237–262 ©Carcinological Society of Japan. doi: 10.18353/crustacea.49.0_237 Description of a new genus for Cyrtorhina balabacensis Serène, 1971, with notes on the Cyrtorhininae (Decapoda, Brachyura, Raninidae) Peter K. L. Ng, Danièle Guinot Abstract.̶ The raninid genus Cyrtorhina Monod, 1956, is revised and restricted to Cyrtorhina granulosa Monod, 1956, from West Africa. A new genus, Flaberhina, is established for C. balabacensis Serène, 1971 from the Philippines and New Caledonia. Despite their superficial similarities, the two genera can easily be separated by the structures of the carapace, eye, antenna, pterygostome, thoracic sternum, pleon and penis. The taxonomy of the subfamily Cyrtorhininae Guinot & Ng, 2020, which con- tains both fossil and extant taxa, is also reviewed. LSID urn:lsid:zoobank.org:pub:D9C27598-A52F-4207-8C22-CDDF9E8E8FFD Key words: Raninoidea, Cyrtorhina, Flaberhina, new genus, Cyrtorhininae, systematics, review ■ Introduction until the present study. Serène & Umali (1972: 49) subsequently redescribed and figured the The raninid genus Cyrtorhina Monod, 1956, species and type specimen in greater detail. was established for one new species, Cyrtorhina balabacensis was known only from C. granulosa Monod, 1956. The holotype was the single type female of Serène (1971). a dry specimen in the Muséum national Between 2001 and 2002, however, the authors d'Histoire naturelle (MNHN), Paris, labelled as obtained three specimens of C. balabacensis “Cyrtorhina granulosa nov. sp. (A. Milne Ed- from fishermen in Balicasag Island in the cen- wards in sched.)” but the name was never pub- tral Philippines, all collected by tangle nets. lished by A. Milne Edwards. -
Shrimps, Lobsters, and Crabs of the Atlantic Coast of the Eastern United States, Maine to Florida
SHRIMPS, LOBSTERS, AND CRABS OF THE ATLANTIC COAST OF THE EASTERN UNITED STATES, MAINE TO FLORIDA AUSTIN B.WILLIAMS SMITHSONIAN INSTITUTION PRESS Washington, D.C. 1984 © 1984 Smithsonian Institution. All rights reserved. Printed in the United States Library of Congress Cataloging in Publication Data Williams, Austin B. Shrimps, lobsters, and crabs of the Atlantic coast of the Eastern United States, Maine to Florida. Rev. ed. of: Marine decapod crustaceans of the Carolinas. 1965. Bibliography: p. Includes index. Supt. of Docs, no.: SI 18:2:SL8 1. Decapoda (Crustacea)—Atlantic Coast (U.S.) 2. Crustacea—Atlantic Coast (U.S.) I. Title. QL444.M33W54 1984 595.3'840974 83-600095 ISBN 0-87474-960-3 Editor: Donald C. Fisher Contents Introduction 1 History 1 Classification 2 Zoogeographic Considerations 3 Species Accounts 5 Materials Studied 8 Measurements 8 Glossary 8 Systematic and Ecological Discussion 12 Order Decapoda , 12 Key to Suborders, Infraorders, Sections, Superfamilies and Families 13 Suborder Dendrobranchiata 17 Infraorder Penaeidea 17 Superfamily Penaeoidea 17 Family Solenoceridae 17 Genus Mesopenaeiis 18 Solenocera 19 Family Penaeidae 22 Genus Penaeus 22 Metapenaeopsis 36 Parapenaeus 37 Trachypenaeus 38 Xiphopenaeus 41 Family Sicyoniidae 42 Genus Sicyonia 43 Superfamily Sergestoidea 50 Family Sergestidae 50 Genus Acetes 50 Family Luciferidae 52 Genus Lucifer 52 Suborder Pleocyemata 54 Infraorder Stenopodidea 54 Family Stenopodidae 54 Genus Stenopus 54 Infraorder Caridea 57 Superfamily Pasiphaeoidea 57 Family Pasiphaeidae 57 Genus -
On a Rare Species of Spanner Crab Ranina Ranina (Crustacea: Brachyura: Raninidae) from Gulf of Mannar, India
On a rare speciesJ. Mar. ofBiol. Spanner Ass. India, Crab 49 Ranina (1) : 89 ranina - 90, Januaryfrom Gulf - June of 2007Mannar, India 89 Note On a rare species of Spanner crab Ranina ranina (Crustacea: Brachyura: Raninidae) from Gulf of Mannar, India C.Kasinathan, Sandhya Sukumaran, A.Gandhi, N.Boominathan and M.Rajamani Regional Centre of Central Marine Fisheries Research Institute, Marine Fisheries P.O., Mandapam Camp - 623 520, Tamil Nadu, India Abstract A rare species of the Spanner crab Ranina ranina (Linnaeus, 1758) is reported from Gulf of Mannar, in India. The description of the morphological features of the species is given. Spanner crabs inhabit coastal waters of several coun- tries in the Indian and Pacific oceans, from the east coasts of southern Africa to Hawaii and the Great Barrier Reef. They prefer bare sandy areas and inhabit intertidal waters to depths more than 100m. They aggregate to spawn during the warmer months and mate at any stage in the moult cycle (Brown, 1986) and females store the sperm until the eggs are extruded.During spawning the females often bury themselves to incubate and protect the eggs. Large females produce at least 2 batches of eggs, each season with an average number of 1,20,000 per batch. The eggs remain attached to the female for 4 – 5 weeks before hatching (Brown, 1986). They pass through 8 larval stages during the following 5 to 8 (longest in higher latitudes) weeks of their life, and then they settle before metamorphosis to the recognizable spanner crab form Fig. 1. Ranina ranina landed at Pamban (Brown, 1986). -
Late Cretaceous and Paleocene Decapod Crustaceans from James Ross Basin, Antarctic Peninsula Author(S): Rodney M
Paleontological Society Late Cretaceous and Paleocene Decapod Crustaceans from James Ross Basin, Antarctic Peninsula Author(s): Rodney M. Feldmann, Dale M. Tshudy, Michael R. A. Thomson Source: Memoir (The Paleontological Society), Vol. 28, Supplement to Vol. 67, no. 1 of the Journal of Paleontology (Jan., 1993), pp. 1-41 Published by: Paleontological Society Stable URL: http://www.jstor.org/stable/1315582 Accessed: 16/01/2009 20:00 Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/page/info/about/policies/terms.jsp. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/action/showPublisher?publisherCode=paleo. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. JSTOR is a not-for-profit organization founded in 1995 to build trusted digital archives for scholarship. We work with the scholarly community to preserve their work and the materials they rely upon, and to build a common research platform that promotes the discovery and use of these resources. For more information about JSTOR, please contact [email protected]. Paleontological Society is collaborating with JSTOR to digitize, preserve and extend access to Memoir (The Paleontological Society). -
Systematic Evaluation of Raninid Cuticle Microstructure
Bulletin of the Mizunami Fossil Museum, no. 35 (2009), p. 15–41, 13 figs., 2 tables. 5 © 2009, Mizunami Fossil Museum Systematic evaluation of raninid cuticle microstructure David A. Waugh1, Rodney M. Feldmann1, and Carrie E. Schweitzer2 1Department of Geology, Kent State University, Kent, Ohio 44242 USA<[email protected]><[email protected]> 2Department of Geology, Kent State University Stark Campus, 6000 Frank Ave. NW, North Canton Ohio 44720 USA<[email protected]> Abstract Studies of decapod cuticle microstructure in both the paleontologic and neontologic literature generally focus on understanding cuticular construction and recognizing these features in fossil material. We examine the cuticle of 57 species in 26 genera within the Raninoidea. Within each genus cuticle microstructure of raninids is generally similar, but in successively higher taxonomic groups, greater variance is seen within and between groups. The subfamily Lyreidinae contains microstructures limited to pits and upright nodes. The Paleocorystinae contains species with predominantly upright nodes and cuticle that generally differs from the other subfamilies. The remaining subfamilies, including the Ranininae, Raninoidinae, Cyrtorhininae, and Notopodinae, are generally similar in their cuticle microstructure; they exhibit inclined nodes, and various combinations of pits, setal pits, depressions, and perforations. The Symethidae contains fungiform nodes, similar to those seen in Cretacoranina, a genus within the Paleocorystinae. Traditional taxonomic characters clearly separate the subfamilies of the Raninidae as well as separating the Raninidae from the Symethidae. Similar cuticle microstructures may appear in different subfamilies. Based upon cuticle microstructure alone, the Raninidae can be divided into three, morphotypes; the Paleocorystinae with upright and fungiform nodes, the Lyreidinae with pits and upright nodes, and the Ranininae, Raninoidinae, Cyrtorhininae, and Notopodinae with inclined nodes. -
Southeastern Regional Taxonomic Center South Carolina Department of Natural Resources
Southeastern Regional Taxonomic Center South Carolina Department of Natural Resources http://www.dnr.sc.gov/marine/sertc/ Southeastern Regional Taxonomic Center Invertebrate Literature Library (updated 9 May 2012, 4056 entries) (1958-1959). Proceedings of the salt marsh conference held at the Marine Institute of the University of Georgia, Apollo Island, Georgia March 25-28, 1958. Salt Marsh Conference, The Marine Institute, University of Georgia, Sapelo Island, Georgia, Marine Institute of the University of Georgia. (1975). Phylum Arthropoda: Crustacea, Amphipoda: Caprellidea. Light's Manual: Intertidal Invertebrates of the Central California Coast. R. I. Smith and J. T. Carlton, University of California Press. (1975). Phylum Arthropoda: Crustacea, Amphipoda: Gammaridea. Light's Manual: Intertidal Invertebrates of the Central California Coast. R. I. Smith and J. T. Carlton, University of California Press. (1981). Stomatopods. FAO species identification sheets for fishery purposes. Eastern Central Atlantic; fishing areas 34,47 (in part).Canada Funds-in Trust. Ottawa, Department of Fisheries and Oceans Canada, by arrangement with the Food and Agriculture Organization of the United Nations, vols. 1-7. W. Fischer, G. Bianchi and W. B. Scott. (1984). Taxonomic guide to the polychaetes of the northern Gulf of Mexico. Volume II. Final report to the Minerals Management Service. J. M. Uebelacker and P. G. Johnson. Mobile, AL, Barry A. Vittor & Associates, Inc. (1984). Taxonomic guide to the polychaetes of the northern Gulf of Mexico. Volume III. Final report to the Minerals Management Service. J. M. Uebelacker and P. G. Johnson. Mobile, AL, Barry A. Vittor & Associates, Inc. (1984). Taxonomic guide to the polychaetes of the northern Gulf of Mexico.