The Gynodiastylidae (Crustacea: Cumacea)
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(Crustacea, Malacostraca, Peracarida) from North America
Contributions to Zoology, 72 (I) 1-16 (2003) SPB Academic Publishing hv, The Hague Paleozoic cumaceans (Crustacea, Malacostraca, Peracarida) from North America ² Frederick+R. Schram Cees+H.J. Hof Mapes³ & Snowdon² ¹, Royal+H. Polly 1 Institute for Biodiversity and Ecosystem Dynamics, University ofAmsterdam, Post Box 94766, 1090 GT 2 Amsterdam, Netherlands, [email protected]; Dept. ofEarth Sciences, University of Bristol, Bristol 3 BS8 IRJ, UK; Dept. of Geological Sciences, Ohio University, Athens, Ohio 45701, USA, e-mail: mapes@oak. cats, ohiou.edu Keywords:: Cumacea, North America, Paleozoic, Peracarida Abstract forms inhabit the fine sand and coarse silts perfect for fossilization (Schram, 1986). Bachmayer, (1960) Thiee new species of are described from North malacostracans recorded a poorly preserved cumacean-like speci- America in the UpperMississippian Into Formation ofArkansas, men Palaeocuma hessi from the Callovian, Middle and the Pennsylvanian Eudora Shale of southeastern Kansas. of France’. These Jurassic, Subsequently, Malzahn (1972) appear to be the oldest fossils attributed to the Cumacea and studied two Permian are well-preserved species of the only the third collection of fossil cumaceansanywhere to be described. Permian genus O. and O. Previously depicted forms occur in the Opthalmdiastylis, inflata costata, and Jurassic of Europe. We herein double the numberof described from the marl beds ofZechstein I, Kamp-Lintfort, fossil cumacean species and suggest some adjustments necessary Germany. These latter taxa are noteworthy in that tothe higher ofthe accommodate taxonomy group to apomorphic they exhibit lobed as the features of distinctly eyes, generic the fossil and Recent forms. name implies. This describes paper three new species of Car- Contents boniferous cumaceans from the lino Formation (Up- per Mississippian) of northwestern Arkansas, and the Eudora Shale (Pennsylvanian) of southeastern Introduction 1 Localities and Kansas. -
And Peracarida
Contributions to Zoology, 75 (1/2) 1-21 (2006) The urosome of the Pan- and Peracarida Franziska Knopf1, Stefan Koenemann2, Frederick R. Schram3, Carsten Wolff1 (authors in alphabetical order) 1Institute of Biology, Section Comparative Zoology, Humboldt University, Philippstrasse 13, 10115 Berlin, Germany, e-mail: [email protected]; 2Institute for Animal Ecology and Cell Biology, University of Veterinary Medicine Hannover, Buenteweg 17d, D-30559 Hannover, Germany; 3Dept. of Biology, University of Washington, Seattle WA 98195, USA. Key words: anus, Pancarida, Peracarida, pleomeres, proctodaeum, teloblasts, telson, urosome Abstract Introduction We have examined the caudal regions of diverse peracarid and The variation encountered in the caudal tagma, or pancarid malacostracans using light and scanning electronic posterior-most body region, within crustaceans is microscopy. The traditional view of malacostracan posterior striking such that Makarov (1978), so taken by it, anatomy is not sustainable, viz., that the free telson, when present, bears the anus near the base. The anus either can oc- suggested that this region be given its own descrip- cupy a terminal, sub-terminal, or mid-ventral position on the tor, the urosome. In the classic interpretation, the telson; or can be located on the sixth pleomere – even when a so-called telson of arthropods is homologized with free telson is present. Furthermore, there is information that the last body unit in Annelida, the pygidium (West- might be interpreted to suggest that in some cases a telson can heide and Rieger, 1996; Grüner, 1993; Hennig, 1986). be absent. Embryologic data indicates that the condition of the body terminus in amphipods cannot be easily characterized, Within that view, the telson and pygidium are said though there does appear to be at least a transient seventh seg- to not be true segments because both structures sup- ment that seems to fuse with the sixth segment. -
Eleven New Species and a New Genus of Diastylidae (Crustacea: Cumacea) from Australia and One New Species from Canada
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Gerken, Sarah, 2013. Eleven new species and a new genus of Diastylidae (Crustacea: Cumacea) from Australia and one new species from Canada. Records of the Australian Museum 66(1): 1–62. [Published 26 February 2014]. http://dx.doi.org/10.3853/j.2201-4349.66.2014.1601 ISSN 0067-1975 (print), ISSN 2201-4349 (online) Published by the Australian Museum, Sydney nature culture discover Australian Museum science is freely accessible online at http://australianmuseum.net.au/Scientific-Publications 6 College Street, Sydney NSW 2010, Australia © The Author, 2014. Journal compilation © Australian Museum, Sydney, 2014 Records of the Australian Museum (2014) Vol. 66, issue number 1, pp. 1–62. ISSN 0067-1975 (print), ISSN 2201-4349 (online) http://dx.doi.org/10.3853/j.2201-4349.66.2014.1601 Eleven New Species and a New Genus of Diastylidae (Crustacea: Cumacea) from Australia and One New Species from Canada Sarah Gerken Department of Biological Sciences, University of Alaska, Anchorage, 3211 Providence Drive, Anchorage, Alaska 99508 United States of America [email protected] Abstract. The shallow water cumacean fauna of Australia is relatively well known, particularly from the southern coasts. However, recent investigations in the collections of the Australian Museum and Museum Victoria have yielded 12 new species and one new genus of diastylid cumaceans, most from continental shelf and slope depths of Australia; one new species in Museum Victoria is from Canadian waters. The new genus Austroleptostylis is described, and the species Leptostylis recalvastra Hale, 1945 is transferred to it, creating the new combination Austroleptostylis recalvastra (Hale, 1945). -
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SCI. MAR., 64 (1): 9-28 SCIENTIA MARINA 2000 Systematics and distribution of cumaceans collected during BENTART-95 cruise around South Shetland Islands (Antarctica)* JORDI CORBERA Carrer Gran 90. Argentona 08310. Spain. E-mail: [email protected] SUMMARY: During the BENTART-95 cruise, 24 stations around the South Shetland Islands and Trinity Island, ranging from 45 to 649 m bottom depth, were sampled using a Macer-GIROQ sledge. Alltogether, 1236 specimens of cumaceans belonging to 25 species were captured. Four of them are new species named Cumella emergens, Procampylaspis halei, Campylaspis heterotuberculata and Leucon (Crymoleucon) costatus. Distribution of cumaceans in this area is depth-depen- dent and the highest diversity was observed at the deeper station. A total of 68 species have been recorded from Antarctic and Subantarctic waters, the greatest part (47 species) were found between 50 and 300 m depth; only 3 species inhabit below 2,500 m depth. Antarctic cumacean fauna shows a high degree of endemism at a specific level (91%), however, only one genus of 19 is endemic. By regions, the Kerguelen Islands have the highest percentage of endemic species (56%). Antarc- tic cumaceans do not seem to have a common origin, some species could have colonized Antarctica through Scotia Arc (as the genus Campylaspis) or emerged from deep-sea while others may be radiated from Antarctica to lower latitudes (as the species of subgenus Crymoleucon). Key words: Cumacea, swimming activity, suprabentos, systematics, distribution, biogeography, Antarctica. INTRODUCTION (Brandt 1993, 1995), to the bioturbation and resus- pension in the benthic ecosystem. Moreover Cumaceans are mainly marine benthic peracarid cumaceans are a food source for fishes (Kurian and crustaceans inhabiting all oceans from the intertidal Radhadevi, 1983) and other macrobenthic inverte- zone to the deepest bottoms (Jones 1969). -
University of Cape Coast Assessment of Aquatic
UNIVERSITY OF CAPE COAST ASSESSMENT OF AQUATIC ECOSYSTEMS, THE FISHERY AND SOCIO-ECONOMICS OF A COASTAL AREA IN THE SHAMA DISTRICT, GHANA BY ISAAC OKYERE THESIS SUBMITTED TO THE DEPARTMENT OF FISHERIES AND AQUATIC SCIENCES, SCHOOL OF BIOLOGICAL SCIENCES, UNIVERSITY OF CAPE COAST IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR AWARD OF DOCTOR OF PHILOSOPHY DEGREE IN FISHERIES AND AQUATIC SCIENCES MARCH 2015 DECLARATION Candidate’s Declaration I hereby declare that this thesis is the result of my own original work and that no part of it has been presented for another degree in this university or elsewhere. Candidate’s Signature...................................... Date...................................... Name: Isaac Okyere Supervisors’ declaration We hereby declare that the preparation and presentation of the thesis were supervised in accordance with the guidelines on supervision of thesis laid down by the University of Cape Coast. Principal Supervisor’s Signature............................... Date............................. Name: Prof. John Blay Co – Supervisor’s Signature....................................... Date................................ Name: Dr. Patrick Agbesinyale ii ABSTRACT The study provides requisite scientific and socio-economic data for sustainable management of the fishery and aquatic ecosystems at Anlo Beach in the Shama District, Ghana. Physico-chemical conditions, macrozoobenthic fauna, and the fish and fishery characteristics of River Pra Estuary, the associated wetlands and marine waters were studied from February 2012 to December 2013. Economics of the fishery, governance and other livelihood activities were also investigated. Data were partly analyzed with quantitative (FiSAT and Ecopath with Ecosim) and qualitative (loop analysis) fishery modeling tools. High turbidities (> 500 ppm), low dissolved oxygen (< 5 mg/l) and high nitrate and phosphate concentrations were recorded in the estuary especially in 2012 possibly emanating from illegal mining activities upstream. -
Cumacea of the NEP: Equator to Aleutians and Intertidal to the Abyss Part 1
Cumacea of the NEP: equator to Aleutians and intertidal to the abyss Part 1. Introduction and General Comments dbcadien 15 October 2006 (revised 21 November 2011) Introduction The Order Cumacea is a relatively small one, much smaller than either the Order Amphipoda, or the Order Isopoda. Even so, over 1032 described species were listed in the order up to 1992 (Bacescu 1988, 1992), and that number has continued to swell. Most areas of the globe probably contain many undescribed species. If we use a multiplier based on the percentage of undescribed taxa known from the NEP, the world cumacean fauna would be expected to reach well above 1800 eventually. It's members are relatively uniform in size and external form, all looking like small balls or tubes on a stick. This structure results from the presence of a more or less globose carapace (which can become considerably flattened) combined with a tapering thoracic region, and a long narrow abdomen terminating in the two uropods. The flavor of the group is well presented by Stebbing (1893), which while rich in detail, is very readable. Cumaceans are relatively important members of the benthic community, being the second most abundant group of crustaceans retained on a 1mm screen (Barnard and Given 1961). Definition The definition of the order from Schram (1986) is: "Carapace short, fused to at least first three thoracomeres, can fuse with up to six, laterally enclosing a branchial cavity, with lateral lappets that extend anteriad and mediad to form a pseudorostrum; eyes generally fused, located -
Comments on Cumacea for LH - Part 3
Comments on Cumacea for LH - Part 3. The Family Diastylidae dbcadien 5 November 2006 The Diastylidae is a relatively large family (17 genera and over two hundred species, Bacescu 1992; now grown to 21 genera, Milhlenhardt-Siegel 2003) which is quite common in the NEP, especially in its Arctic and Boreal areas. Eight of these genera occur in the NEP, and are discussed below.. A key to the genera in the family is provided by Jones (1969), but genera from couplet 16 on in that key are now considered to belong in the family Gynodiastylidae (see Day 1980). As one of three families bearing articulated telsons, its members are most often confused with members of the other two, Gynodiastylidae and Lampropidae. This confusion extends to even knowledgeable workers, with some describing lampropids as diastylids (see Gladfelter 1975). The family key provided in the first part of this series should allow appropriate allocation of specimens to families. More of NEP diastylid species are described than was the case with the last family, the bodotriids. Of the 38 diastylids reported from the NEP, only 7 belong to provisional taxa. This is perhaps due to the relatively shallow distribution of bodotriids, into habitats frequently unsampled, while diastylids are commonly found further offshore where they can be easily taken by dredge, core, and trawl. The family also has more affinity for cold waters than does the Bodotriidae, with many of the NEP forms of only Arctic or boreal distribution. Lastly, diastylids tend to be larger than bodotriids, with some of the largest species of cumaceans in the family. -
Campylaspis Rufa Hart, 1930 Figure 2.25
Campylaspis rufa Hart, 1930 Figure 2.25 Material Examined. Santa Maria Basin region, Phase II. Cruise 1-1 (November, 1986), Sta. R-3 (2); Cruise 1-2 (January, 1987), R-7 (4). Description. Female, 3.5 mm. Carapace large, smooth, comprising more than half total length of body, extending dorsally over pereonites 1 -3; antennal notch obsolescent; eyelobe broadened, without lenses. Pereopod 2 articles 5 and 7 subequal in length. Uropod peduncles twice length of endopod and approximately equal in length to last 2 pleonites combined; medial margin of peduncle armed with large scales giving coarsely serrate appearance; endopod with about 7 medial setae. Color dark reddish-brown to orange, with large dark red chromatophores scattered over body. Remarks. The very small adult body size and smooth, reddish brown carapace serves to distinguish this species from all others in the Santa Maria Basin region. Campylaspis rufa has never been found in even moderate abundance; its occurrence here extends its range throughout the Oregonian Province. Type Locality and Type Specimens. Mitlenatch, Vancouver Island, British Columbia, 200 m.; type in British Columbia Provincial Museum. Distribution. Vancouver Island to Point Conception, 200 - 565 m. Figure 2.25. Campylaspis rufa Hart, 1930. Female: A, carapace and pereonites, lateral view; B, body, lateral view; C, carapace, dorsal view; D, uropods. Scale A-C = 1mm, D = 0.1 mm. 163 Campylaspis rubromaculata Lie, 1971 Figure 2.26 Campylaspis nodulosa Lie, 1969 (non Sars, 1887) Material Examined. Santa Maria Basin, Phase II, Cruise 1-1 (November, 1986), Sta. R-4 (1), R-5 (14), R-7 (8), PJ-1 (15); Cruise 1-2 (January, 1987), R-l (3), R-2 (1), R-4 (1), R-5 (4), PJ-1 (10); Cruise 1-3 (May, 1987), R-l (3), R-8 (3), PJ-1 (9); Cruise 2-3 (October, 1987), R-5 (3), PJ-1 (6); Cruise 2-4 (January, 1988), R-l (2), R-8 (2), PJ-1 (16); Cruise 2-5 (May, 1988), R-l (1), PJ-1 (2); Cruise 3-1 (October, 1988), PJ- 1 (1); Cruise 3-4 (May, 1989), R-l (3), R-8 (1), PJ-1 (9). -
Paleozoic Cumaceans (Crustacea, Malacostraca, Peracarida) from North America
Contributions to Zoology, 72 (I) 1-16 (2003) SPB Academic Publishing hv, The Hague Paleozoic cumaceans (Crustacea, Malacostraca, Peracarida) from North America ² Frederick+R. Schram Cees+H.J. Hof Mapes³ & Snowdon² ¹, Royal+H. Polly 1 Institute for Biodiversity and Ecosystem Dynamics, University ofAmsterdam, Post Box 94766, 1090 GT 2 Amsterdam, Netherlands, [email protected]; Dept. ofEarth Sciences, University of Bristol, Bristol 3 BS8 IRJ, UK; Dept. of Geological Sciences, Ohio University, Athens, Ohio 45701, USA, e-mail: mapes@oak. cats, ohiou.edu Keywords:: Cumacea, North America, Paleozoic, Peracarida Abstract forms inhabit the fine sand and coarse silts perfect for fossilization (Schram, 1986). Bachmayer, (1960) Thiee new species of are described from North malacostracans recorded a poorly preserved cumacean-like speci- America in the UpperMississippian Into Formation ofArkansas, men Palaeocuma hessi from the Callovian, Middle and the Pennsylvanian Eudora Shale of southeastern Kansas. of France’. These Jurassic, Subsequently, Malzahn (1972) appear to be the oldest fossils attributed to the Cumacea and studied two Permian are well-preserved species of the only the third collection of fossil cumaceansanywhere to be described. Permian genus O. and O. Previously depicted forms occur in the Opthalmdiastylis, inflata costata, and Jurassic of Europe. We herein double the numberof described from the marl beds ofZechstein I, Kamp-Lintfort, fossil cumacean species and suggest some adjustments necessary Germany. These latter taxa are noteworthy in that tothe higher ofthe accommodate taxonomy group to apomorphic they exhibit lobed as the features of distinctly eyes, generic the fossil and Recent forms. name implies. This describes paper three new species of Car- Contents boniferous cumaceans from the lino Formation (Up- per Mississippian) of northwestern Arkansas, and the Eudora Shale (Pennsylvanian) of southeastern Introduction 1 Localities and Kansas. -
On the Biogeography of Cumacea (Crustacea, Malacostraca). a Comparison Between South America, the Subantarctic Islands and Antarctica: Present State of the Art*
SCI. MAR., 63 (Supl. 1): 295-302 SCIENTIA MARINA 1999 MAGELLAN-ANTARCTIC: ECOSYSTEMS THAT DRIFTED APART. W.E. ARNTZ and C. RÍOS (eds.) On the biogeography of Cumacea (Crustacea, Malacostraca). A comparison between South America, the Subantarctic Islands and Antarctica: present state of the art* UTE MÜHLENHARDT-SIEGEL Zoologisches Institut und Zoologisches Museum, Universität Hamburg, Martin-Luther-King-Platz 3, 20146 Hamburg, Germany SUMMARY: Cumacea (Crustacea) were collected during the “Joint Magellan” expedition in November 1994, by means of an epibenthic sledge from RV “Victor Hensen”. The cumaceans were well represented, the second abundant order after the amphipods, among the other Peracarida in depth ranges between 25 and 665 m. Twenty-five species were found in the sam- ples mainly from the Beagle Channel, nine of them were already known for this region. 14 species were recorded for the first time for this region, 2 of them were known from the northern Argentinian coast and one from Antarctica. The most important in terms of species richness and abundance were the families Diastylidae, Nannastacidae and Leuconidae. In the Beagle Channel an almost completely different cumacean fauna was found compared to the Subantarctic Islands, the Antarc- tic Peninsula and eastern Antarctic (Prydz Bay) regions. Comparison of published data and the present results show mod- erate overlap in the cumacean fauna at the species level between the periantarctic South Georgian shelf / Antarctic Penin- sula (48%). Little correspondence at the species level was found between Antarctica / Subantarctic Kerguelen (14 %), South Georgia / Kerguelen (13 %) and Magellan / Antarctica (11 %). Interestingly, the Magellan region and South Georgia show very little species overlap (5 %). -
Taxonomic Atlas
r r r TAXONOMIC ATLAS OF THE BENTHIC FAUNA OF THE SANTA MARIA BASES AND WESTERN SANTA BARBARA CHANNEL - - Volume 11 — The Crustacea Part 2 The Isopoda, Cumacea and Tanaidacea " ^ V* SANTA BARBARA MUSEUM OF NATURAL HISTORY Santa Barbara, California " Research Published in this Volume was Supported by U.S. Department of the Interior Minerals Management Service Pacific OCS Region 770 Paseo Camarillo Camarillo, California 93010 Under Contract No. 14-35-0001-30484 TAXONOMIC ATLAS OF THE BENTHIC FAUNA OF THE SANTA MARIA BASIN AND WESTERN SANTA BARBARA CHANNEL VOLUME 11 The Crustacea Part 2 The Isopoda, Cumacea and Tanaidacea Edited by James A. Blake and Paul H. Scott SANTA BARBARA MUSEUM OF NATURAL HISTORY Santa Barbara, California <jQ \_ NATURAL HISTORY | IGM § libsary § , fs ~2_ gANGF.U=-R BOUNTY 3 V.I I TAXONOMIC ATLAS OF THE BENTHIC FAUNA OF THE SANTA MARIA BASIN AND WESTERN SANTA BARBARA CHANNEL Volume 11 The Crustacea Part 2 - The Isopoda, Cumacea and Tanaidacea ©1997 Santa Barbara Museum of Natural History 2559 Puesta del Sol Road Santa Barbara, California 93105-2936 Original Date of Publication: 20 May 1997 All rights reserved. This book may not be reproduced in whole or in part for any purpose whatever, without written permission from the publisher (Santa Barbara Museum of Natural History). Printed and bound by Alternative Graphics, Goleta, California Production editor, Adele Smith Layout by Marie Murphy Cover photograph by Ron McPeak: An undescribed species of Idoteidae from central California. Photograph digitally enhanced by Marie -
Impact of Climate-Induced Dynamics on a Coastal Benthic Ecosystem from the West Antarctic Peninsula
Impact of Climate-induced dynamics on a Coastal Benthic Ecosystem from the West Antarctic Peninsula Francesca Pasotti 2015 Impact of Climate-induced dynamics on a Coastal Benthic Ecosystem from the West Antarctic Peninsula By Francesca Pasotti Promotor: Prof. Dr. Ann Vanreusel Academic year 2014-2015 This thesis is submitted in partial fulfillment of the requirements for the degree of Doctor in Science (Marine Sciences) Committee members Reading Committee Prof. Bruno Danis (Marine Biology Laboratory, Université Libre de Bruxelles, Belgium) Prof. Wim Vyverman (Phycology and Aquatic Ecology Laboratory, Ghent University, Belgium) Dr. Marleen De Troch (Marine Biology Laboratory, Ghent University, Belgium) Examination Comittee Dr. Elie Verleyen (Phycology and Aquatic Ecology Laboratory, Ghent University, Belgium) Dr. Ulrike Braeckman (Marine Biology Laboratory, Ghent University, Belgium) Prof. Dr. Tom Moens (Marine Biology Laboratory, Ghent University, Belgium) Prof. Dr. Magda Vincx (Marine Biology Laboratory, Ghent University, Belgium) Prof. Dr. Doris Abele (Dept. of Functional Ecology, Alfred Wegener Institute, Germany) Prof. Wim Vyverman (Phycology and Aquatic Ecology Laboratory, Ghent University Belgium) Dr. Marleen De Troch (Marine Biology Laboratory, Ghent University, Belgium) Prof. Dr. Ann Vanreusel (promoter, Marine Biology Laboratory, Ghent University, Belgium) Prof. Dr. Dominique Adriaens (chairman, Dept. of Evolutionary Morphology of Vertebrates, Ghent University, Belgium) Aknowledgments The last lines I find myself writing are actually the first in importance for my heart. This PhD thesis would have never been possible without many and several causes and conditions (hence, wonderful people) which shaped my life. First of all, I need to thank my parents and family, who gave me this life, nurtured me when I was little and transmitted me those basic human values which made me go through life in a lighter, yet stronger way.