Part I—New American Wutinoceratidae with Review of Actinoceroid Occurrences in Eastern Hemisphere and Part II—Some Whiterock and Chazy Endoceroids
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CEPHALOPODS 688 Cephalopods
click for previous page CEPHALOPODS 688 Cephalopods Introduction and GeneralINTRODUCTION Remarks AND GENERAL REMARKS by M.C. Dunning, M.D. Norman, and A.L. Reid iving cephalopods include nautiluses, bobtail and bottle squids, pygmy cuttlefishes, cuttlefishes, Lsquids, and octopuses. While they may not be as diverse a group as other molluscs or as the bony fishes in terms of number of species (about 600 cephalopod species described worldwide), they are very abundant and some reach large sizes. Hence they are of considerable ecological and commercial fisheries importance globally and in the Western Central Pacific. Remarks on MajorREMARKS Groups of CommercialON MAJOR Importance GROUPS OF COMMERCIAL IMPORTANCE Nautiluses (Family Nautilidae) Nautiluses are the only living cephalopods with an external shell throughout their life cycle. This shell is divided into chambers by a large number of septae and provides buoyancy to the animal. The animal is housed in the newest chamber. A muscular hood on the dorsal side helps close the aperture when the animal is withdrawn into the shell. Nautiluses have primitive eyes filled with seawater and without lenses. They have arms that are whip-like tentacles arranged in a double crown surrounding the mouth. Although they have no suckers on these arms, mucus associated with them is adherent. Nautiluses are restricted to deeper continental shelf and slope waters of the Indo-West Pacific and are caught by artisanal fishers using baited traps set on the bottom. The flesh is used for food and the shell for the souvenir trade. Specimens are also caught for live export for use in home aquaria and for research purposes. -
Nautiloid Shell Morphology
MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOWER STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOIVER 1964 STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EXOFFICIO THEHONORABLEJACKM.CAMPBELL ................................ Governor of New Mexico LEONARDDELAY() ................................................... Superintendent of Public Instruction APPOINTEDMEMBERS WILLIAM G. ABBOTT ................................ ................................ ............................... Hobbs EUGENE L. COULSON, M.D ................................................................. Socorro THOMASM.CRAMER ................................ ................................ ................... Carlsbad EVA M. LARRAZOLO (Mrs. Paul F.) ................................................. Albuquerque RICHARDM.ZIMMERLY ................................ ................................ ....... Socorro Published February 1 o, 1964 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.50 Contents Page ABSTRACT ....................................................................................................................................................... 1 INTRODUCTION -
New Fossil Finds from the Cambro-Silurian Meta-Sediments on Hardangervidda
New Fossil Finds from the Cambro-Silurian Meta-sediments on Hardangervidda ARILD ANDRESEN Andresen, A. 1974: New fossil finds from the Cambro-Silurian meta-sedi ments on Hardangervidda. Norges geol. Unders. 304, 55-60. The occurrence of Actinoceroid cephalopods {Ormoceras (?) sp.), brachiopods {Orthis ss.), and trilobites {Ptycbopyge sp.) in a crystalline limestone over lying bluish quartzite on Hardangervidda indicates that Orthoceras Limestone of the Lower Ordovician Asaphus Series (Etage 3c) is present. The underlying quartzites are correlated with stage 3a-3b in the Oslo Region. A. Andresen, Mineralogisk-Geologisk Museum, Sarsgt. 1, Oslo 5, Norway Introduction Hardangervidda (Fig. 1) is, outside the Oslo Region, one of the largest areas in Norway where Cambro-Silurian sediments of eastern facies (foreland fac ies) are exposed. The stratigraphy and structure of these rocks are not very well known, partly because of the inaccessibility of the area, and partly due to the intense deformation and lack of fossiliferous beds. Even though the fossils described in this paper are badly preserved, making identification of species in some cases uncertain and in other cases impossible, they give some information about the Cambro-Silurian stratigraphy. The earliest contribution to the geology of Hardangervidda was made by Dahll (1861), who reported fossiliferous beds with Dictyonema flabelliforme (2e in the stratigraphic sequence of the Oslo Region) from Holberget (Fig. 1). Later, Brøgger (1893), after more detailed mapping, established a strati graphic sequence for the rocks overlying the Precambrian basement. In this sequence all the rocks above the Precambrian basement were assumed to be in a normal succession. The subdivision he established was, from the base upwards: 1, Alum shale; 2, Quartizite; 3, Crystalline limestone (marble); 4, Phyllites; 5, Various crystalline rocks. -
Cambrian Cephalopods
BULLETIN 40 Cambrian Cephalopods BY ROUSSEAU H. FLOWER 1954 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ...................... Governor of New Mexico Tom Wiley ......................................... Superintendent of Public Instruction APPOINTED MEMBERS Robert W. Botts ...................................................................... Albuquerque Holm 0. Bursum, Jr. ....................................................................... Socorro Thomas M. Cramer ........................................................................ Carlsbad Frank C. DiLuzio ..................................................................... Los Alamos A. A. Kemnitz ................................................................................... Hobbs Contents Page ABSTRACT ...................................................................................................... 1 FOREWORD ................................................................................................... 2 ACKNOWLEDGMENTS ............................................................................. 3 PREVIOUS REPORTS OF CAMBRIAN CEPHALOPODS ................ 4 ADEQUATELY KNOWN CAMBRIAN CEPHALOPODS, with a revision of the Plectronoceratidae ..........................................................7 -
Part I. Revision of Buttsoceras. Part II. Notes on the Michelinoceratida
MEMOIR 10 PART I Revision of Buttsoceras PART II Notes on the Michelinoceratida By ROUSSEAU H. FLOWER 1 9 6 2 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ........................................ Governor of New Mexico Tom Wiley .......................................................... Superintendent of Public Instruction APPOINTED MEMBERS William G. Abbott ............................................................................................... Hobbs Holm 0. Bursum, Jr. ......................................................................................... Socorro Thomas M. Cramer ......................................................................................... Carlsbad Frank C. DiLuzio ...................................................................................... Albuquerque Eva M. Larrazolo (Mrs. Paul F.) ............................................................... Albuquerque Published October I2, 1962 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.00 Contents PART I REVISION OF BUTTSOCERAS Page ABSTRACT ....................................................................................................................... INTRODUCTION ............................................................................................................................. -
Xiphias Gladius Stomach Content Analysis Is an in Zones a and B, Fish Were Stored Linnaeus, 1758, Is a Mesopelagic Important Tool in Ecological and in Ice
The diet of the swordfish tained from a longline vessel between 1 and 15th March 1991 by using Xiphias gbdius Linnaeus, mackerel, Scomber spp., as bait. 1 758, in the central east Atlantic, Zone C Gulf of Guinea (3O09'- 0°36'N and 26O27'-4O17'W). Fifteen with emphasis on the role of swordfish (standard length [SL] between 140-209 cm) were selected cephalopods on the basis of the presence of cephalopods in their stomachs. Vicente Hernández-García These were taken from catches Dpto de Biología, Facultad de Ciencias del Mar made by a longliner between May Univ. de Las Palmas de G. Canaria and July of 1991 by using mackerel C P 350 1 7, Canary Islands, Spain and squid, Illex sp., as bait. Stomach preservation and analysis The swordfish Xiphias gladius Stomach content analysis is an In zones A and B, fish were stored Linnaeus, 1758, is a mesopelagic important tool in ecological and in ice. After landing, fish were mea- teleost with a cosmopolitan distri- fisheries biology studies. Oceanic sured from the tip of the lower jaw bution between 45"N anci 45"s iati- vertebrates are often more efficient to the fork of the taii (S¿). During tude. It is an opportunistic preda- collectors of cephalopods than any commercial operations the internal tor feeding mainly on pelagic ver- available sampling gear (Bouxin organs were removed before the tebrates and invertebrates (Palko and Legendre, 1936; Clarke, 1966). fish were weighed. The stomach et al., 1981). The diet. of the sword- The p'irpose nf thir st11dy was to rnntents nf earh fish, incli~dingal1 fish has been studied mainly in the expand knowledge of the diet of the hard parts found in the stomach western Atlantic Ocean (Tibbo et swordfish from the central east At- wall folds (otoliths, very small al., 1961; Scott and Tibbo, 1968, lantic Ocean, with special emphasis beaks, and lenses), were weighed 1974; Toll and Hess, 1981; Stillwell on the role of cephalopod species. -
Morphological Study on Radula of Nine Cephalopods in the Coastal Waters of China
第 26 卷第 5 期 水 产 学 报 Vol .26, No.5 2002 年 10 月 JOURNAL OF FISHERIES OF CHINA Oct ., 2002 文章编号 :1000 -0615(2002)05 -0417 -06 Morphological study on radula of nine cephalopods in the coastal waters of China ZHENG Xiao-dong , WANG Ru-cai (The Key Lab of Mariculture Certificated by the Ministry of Education , Ocean University of Qingdao , Qingdao 266003 , China) Abstract :The radula of nine cephalopods are compared on the basis of scanning electron microscopic observation and morphological measurements .Results indicate that all of them consist of 7 longitudinal rows of teeth :a median tooth and the 1st , 2nd , and 3rd lateral or lateral , inner marginal , and outer marginal teeth .The formula of radula is 3·1·3 .Sepioidea (Sepia robsoni , S .esculenta , S .pharaonis , S .latimanus , S .aculeata , Sepiella maindroni , Euprymna berryi)has only one cusp in the median tooth , and a marginal plate is absent .The median tooth has 3 and/or 5 cusps and marginal plates are found in the two species of Octopus ocellatus and O .variabilis .Other differences in the radula structure among the nine species are illustrated in detail .The relationships of radula of the cuttlefishes , octopuses and squids are discussed .It is suggested that radula should be thought in the cuttlefish taxonomy . Key words:cephalopods ;cuttlefish ;radula ;morphology ;scanning electron microscope(SEM) CLC number :S917 ;Q954 Document code :A 1 Introduction Anatomical characters have traditionally been used in fisheries biology to describe geographic variation in some exploited species of cephalopods[ 1-4] .Unlike molecular genetic markers , it is obvious that phenotypic variation is influenced by environmental factors , and the genetic component of such variance is uncertain[ 5] . -
A New Genus and Three New Species of Decapodiform Cephalopods (Mollusca: Cephalopoda)
Rev Fish Biol Fisheries (2007) 17:353-365 DOI 10.1007/S11160-007-9044-Z .ORIGINAL PAPER A new genus and three new species of decapodiform cephalopods (Mollusca: Cephalopoda) R. E. Young • M. Vecchione • C. F, E, Roper Received: 10 February 2006 / Accepted: 19 December 2006 / Pubhshed online: 30 March 2007 © Springer Science+Business Media B.V. 2007 Abstract We describe here two new species of Introduction oegopsid squids. The first is an Asperoteuthis (Chiroteuthidae), and it is based on 18 specimens. We describe three new species of cephalopods This new species has sucker dentition and a from three different families in two different funnel-mantle locking apparatus that are unique orders that have little in common except they are within the genus. The second new species is a from unusual and poorly known groups. The Promachoteuthis (Promachoteuthidae), and is unique nature of these cephalopods has been based on a unique specimen. This new species known for over 30 years but they were not has tentacle ornamentation which is unique within described because (1) with two species we waited the genus. We also describe a new genus and a new for the collection of more or better material species of sepioid squid in the subfamily Hetero- which never materialized and (2) with one species teuthinae (Sepiolidae) and it is based on four the type material was misplaced, virtually forgot- specimens. This new genus and species exhibits ten and only recently rediscovered. The 2006 unique modifications of the arms in males. CIAC symposium was the stimulus to finally publish these species which should have been Keywords Amphorateuthis alveatus • published in the first CIAC symposium in 1985. -
Defensive Behaviors of Deep-Sea Squids: Ink Release, Body Patterning, and Arm Autotomy
Defensive Behaviors of Deep-sea Squids: Ink Release, Body Patterning, and Arm Autotomy by Stephanie Lynn Bush A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Integrative Biology in the Graduate Division of the University of California, Berkeley Committee in Charge: Professor Roy L. Caldwell, Chair Professor David R. Lindberg Professor George K. Roderick Dr. Bruce H. Robison Fall, 2009 Defensive Behaviors of Deep-sea Squids: Ink Release, Body Patterning, and Arm Autotomy © 2009 by Stephanie Lynn Bush ABSTRACT Defensive Behaviors of Deep-sea Squids: Ink Release, Body Patterning, and Arm Autotomy by Stephanie Lynn Bush Doctor of Philosophy in Integrative Biology University of California, Berkeley Professor Roy L. Caldwell, Chair The deep sea is the largest habitat on Earth and holds the majority of its’ animal biomass. Due to the limitations of observing, capturing and studying these diverse and numerous organisms, little is known about them. The majority of deep-sea species are known only from net-caught specimens, therefore behavioral ecology and functional morphology were assumed. The advent of human operated vehicles (HOVs) and remotely operated vehicles (ROVs) have allowed scientists to make one-of-a-kind observations and test hypotheses about deep-sea organismal biology. Cephalopods are large, soft-bodied molluscs whose defenses center on crypsis. Individuals can rapidly change coloration (for background matching, mimicry, and disruptive coloration), skin texture, body postures, locomotion, and release ink to avoid recognition as prey or escape when camouflage fails. Squids, octopuses, and cuttlefishes rely on these visual defenses in shallow-water environments, but deep-sea cephalopods were thought to perform only a limited number of these behaviors because of their extremely low light surroundings. -
Holochoanites Are Endoceroids Rousseau H
HOLOCHOANITES ARE ENDOCEROIDS ROUSSEAU H. FLOWER, New York State Museum Albany 1, N. Y. INTRODUCTION The Holochoanites may be defined as those cephalopods in which the septal necks are so elongated that they extend from the septum of which they are a part and a prolongation, apicad to the next septum, or even farther. Hyatt (1884) first regarded the Holochoanoidea as one of two major divisions of the Nautiloidea. Later (1900) he replaced his other division, the Ellipochoanoidea, by four divisions the Orthochaonites, Cyrtochoanites, Schistochoanites and Mixochoanites, and changed the name Holochoanoidea to Holochoanites for uniformity. In the mean- time, further study caused him to modify the contents of the holochoanitic division materially. Some genera originally placed in this group, such as Trocholites, proved upon further study to possess ellipochoanitic septal necks. The genus Aturia, while properly holochoanitic, was removed, because it was recognized that it represented a development of elongated septal necks in Tertiary time, which was obviously quite unrelated to that of other holochoanitic cephalopods, few of which survived the close of the Ordovician. Miller and Thompson (1937) showed that the elongation of the septal necks in Aturia was a secondary feature and the ellipochoanitic ancestry was indicated by the retention of connecting rings. It was believed that the Holochaonites proper contain cephalopods in which the long necks were primitive, and no connecting rings were developed. Unfortunately Hyatt does not seem to have committed himself on his ideas concerning the relationship of the Holochoanites with other cephalopods. It is not clear whether this was because of his preoccupation with the phyletic sig- nificance of early stages and the controversy that developed about the origin of the Ammonoidea and their relationship to the Nautiloidea, or whether he was as much perplexed by the problem as have been those of us who have come after him in the study of cephalopods. -
Geology and Fossils Craigleith Area Ontario
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Upper Peninsula
GEOLOGICAL SURVEY OF MICHIGAN. For this object I have zealously worked. How far I have succeeded in the effort the reader may judge; and I shall feel well satisfied if he finds the picture I give worth UPPER PENINSULA attentive study, without having it surrounded by a 1869-1873 borrowed glistening frame, composed of a collection of ACCOMPANIED BY AN items from almost every branch of human knowledge. ATLAS OF MAPS. Very respectfully yours, C. ROMINGER. VOL. I. PART III. PALÆOZOIC ROCKS. INTRODUCTION. BY DR. C. ROMINGER BY the Legislative Assembly of 1871, the continuation of a geological survey of the State of Michigan was determined upon, in such a manner as to divide the work PUBLISHED BY AUTHORITY OF THE LEGISLATURE OF into three districts, each of which was to be investigated MICHIGAN. independently by different parties. UNDER THE DIRECTION OF THE BOARD OF GEOLOGICAL SURVEY. The third district, intrusted to me, comprises the Lower Peninsula, and the eastern half of the Upper Peninsula, NEW YORK or that portion which Is not included in the iron and JULIUS BIEN copper regions. Its surface rock is exclusively 1873 composed of members of the palæozoic series; while In Entered according to Act of Congress, in the year 1873, by the other two, older crystalline and metamorphic rocks GOVERNOR J. J. BAGLEY, prevail. for the State of Michigan, in the Office of the Librarian of Congress, at Washington. On the Lower Peninsula only a partial reconnoissance TO THE HONORABLE BOARD OF GEOLOGICAL SURVEY OF tour has been made through Little Traverse Bay region.