Dicyema Japonicum
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												Systema Naturae∗
Systema Naturae∗ c Alexey B. Shipunov v. 5.802 (June 29, 2008) 7 Regnum Monera [ Bacillus ] /Bacteria Subregnum Bacteria [ 6:8Bacillus ]1 Superphylum Posibacteria [ 6:2Bacillus ] stat.m. Phylum 1. Firmicutes [ 6Bacillus ]2 Classis 1(1). Thermotogae [ 5Thermotoga ] i.s. 2(2). Mollicutes [ 5Mycoplasma ] 3(3). Clostridia [ 5Clostridium ]3 4(4). Bacilli [ 5Bacillus ] 5(5). Symbiobacteres [ 5Symbiobacterium ] Phylum 2. Actinobacteria [ 6Actynomyces ] Classis 1(6). Actinobacteres [ 5Actinomyces ] Phylum 3. Hadobacteria [ 6Deinococcus ] sed.m. Classis 1(7). Hadobacteres [ 5Deinococcus ]4 Superphylum Negibacteria [ 6:2Rhodospirillum ] stat.m. Phylum 4. Chlorobacteria [ 6Chloroflexus ]5 Classis 1(8). Ktedonobacteres [ 5Ktedonobacter ] sed.m. 2(9). Thermomicrobia [ 5Thermomicrobium ] 3(10). Chloroflexi [ 5Chloroflexus ] ∗Only recent taxa. Viruses are not included. Abbreviations and signs: sed.m. (sedis mutabilis); stat.m. (status mutabilis): s., aut i. (superior, aut interior); i.s. (incertae sedis); sed.p. (sedis possibilis); s.str. (sensu stricto); s.l. (sensu lato); incl. (inclusum); excl. (exclusum); \quotes" for environmental groups; * (asterisk) for paraphyletic taxa; / (slash) at margins for major clades (\domains"). 1Incl. \Nanobacteria" i.s. et dubitativa, \OP11 group" i.s. 2Incl. \TM7" i.s., \OP9", \OP10". 3Incl. Dictyoglomi sed.m., Fusobacteria, Thermolithobacteria. 4= Deinococcus{Thermus. 5Incl. Thermobaculum i.s. 1 4(11). Dehalococcoidetes [ 5Dehalococcoides ] 5(12). Anaerolineae [ 5Anaerolinea ]6 Phylum 5. Cyanobacteria [ 6Nostoc ] Classis 1(13). Gloeobacteres [ 5Gloeobacter ] 2(14). Chroobacteres [ 5Chroococcus ]7 3(15). Hormogoneae [ 5Nostoc ] Phylum 6. Bacteroidobacteria [ 6Bacteroides ]8 Classis 1(16). Fibrobacteres [ 5Fibrobacter ] 2(17). Chlorobi [ 5Chlorobium ] 3(18). Salinibacteres [ 5Salinibacter ] 4(19). Bacteroidetes [ 5Bacteroides ]9 Phylum 7. Spirobacteria [ 6Spirochaeta ] Classis 1(20). Spirochaetes [ 5Spirochaeta ] s.l.10 Phylum 8. Planctobacteria [ 6Planctomyces ]11 Classis 1(21). - 
												
												Systematics , Zoogeography , Andecologyofthepriapu
SYSTEMATICS, ZOOGEOGRAPHY, AND ECOLOGY OF THE PRIAPULIDA by J. VAN DER LAND (Rijksmuseum van Natuurlijke Historie, Leiden) With 89 text-figures and five plates CONTENTS Ι Introduction 4 1.1 Plan 4 1.2 Material and methods 5 1.3 Acknowledgements 6 2 Systematics 8 2.1 Historical introduction 8 2.2 Phylum Priapulida 9 2.2.1 Diagnosis 10 2.2.2 Classification 10 2.2.3 Definition of terms 12 2.2.4 Basic adaptive features 13 2.2.5 General features 13 2.2.6 Systematic notes 2 5 2.3 Key to the taxa 20 2.4 Survey of the taxa 29 Priapulidae 2 9 Priapulopsis 30 Priapulus 51 Acanthopriapulus 60 Halicryptus 02 Tubiluchidae 7° Tubiluchus 73 3 Zoogeography and ecology 84 3.1 Distribution 84 3.1.1 Faunistics 90 3.1.2 Expeditions 93 3.2 Ecology 96 3.2.1 Substratum 96 3.2.2 Depth 97 3.2.3 Temperature 97 3.24 Salinity 98 3.2.5 Oxygen 98 3.2.6 Food 99 3.2.7 Predators 100 3.2.8 Communities 102 3.3 Theoretical zoogeography 102 3.3.1 Bipolarity 102 3.3.2 Relict distribution 103 3.3.3 Concluding remarks 104 References 105 4 ZOOLOGISCHE VERHANDELINGEN 112 (1970) 1 INTRODUCTION The phylum Priapulida is only a very small group of marine worms but, since these animals apparently represent the last remnants of a once un- doubtedly much more important animal type, they are certainly of great scientific interest. Therefore, it is to be regretted that a comprehensive review of our present knowledge of the group does not exist, which does not only cause the faulty way in which the Priapulida are treated usually in textbooks and works on phylogeny, but also hampers further studies. - 
												
												New Zealand's Genetic Diversity
1.13 NEW ZEALAND’S GENETIC DIVERSITY NEW ZEALAND’S GENETIC DIVERSITY Dennis P. Gordon National Institute of Water and Atmospheric Research, Private Bag 14901, Kilbirnie, Wellington 6022, New Zealand ABSTRACT: The known genetic diversity represented by the New Zealand biota is reviewed and summarised, largely based on a recently published New Zealand inventory of biodiversity. All kingdoms and eukaryote phyla are covered, updated to refl ect the latest phylogenetic view of Eukaryota. The total known biota comprises a nominal 57 406 species (c. 48 640 described). Subtraction of the 4889 naturalised-alien species gives a biota of 52 517 native species. A minimum (the status of a number of the unnamed species is uncertain) of 27 380 (52%) of these species are endemic (cf. 26% for Fungi, 38% for all marine species, 46% for marine Animalia, 68% for all Animalia, 78% for vascular plants and 91% for terrestrial Animalia). In passing, examples are given both of the roles of the major taxa in providing ecosystem services and of the use of genetic resources in the New Zealand economy. Key words: Animalia, Chromista, freshwater, Fungi, genetic diversity, marine, New Zealand, Prokaryota, Protozoa, terrestrial. INTRODUCTION Article 10b of the CBD calls for signatories to ‘Adopt The original brief for this chapter was to review New Zealand’s measures relating to the use of biological resources [i.e. genetic genetic resources. The OECD defi nition of genetic resources resources] to avoid or minimize adverse impacts on biological is ‘genetic material of plants, animals or micro-organisms of diversity [e.g. genetic diversity]’ (my parentheses). - 
												
												Phylum Nemertea)
THE BIOLOGY AND SYSTEMATICS OF A NEW SPECIES OF RIBBON WORM, GENUS TUBULANUS (PHYLUM NEMERTEA) By Rebecca Kirk Ritger Submitted to the Faculty of the College of Arts and Sciences of American University in Partial Fulfillment of the Requirements for the Degree of Master of Science In Biology Chair: Dr. Qiristopher'Tudge m Dr.David C r. Jon L. Norenburg Dean of the College of Arts and Sciences JuK4£ __________ Date 2004 American University Washington, D.C. 20016 AMERICAN UNIVERSITY LIBRARY 1 1 0 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 1421360 INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. ® UMI UMI Microform 1421360 Copyright 2004 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, Ml 48106-1346 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. THE BIOLOGY AND SYSTEMATICS OF A NEW SPECIES OF RIBBON WORM, GENUS TUBULANUS (PHYLUM NEMERTEA) By Rebecca Kirk Ritger ABSTRACT Most nemerteans are studied from poorly preserved museum specimens. - 
												
												Comparative Neuroanatomy of Mollusks and Nemerteans in the Context of Deep Metazoan Phylogeny
Comparative Neuroanatomy of Mollusks and Nemerteans in the Context of Deep Metazoan Phylogeny Von der Fakultät für Mathematik, Informatik und Naturwissenschaften der RWTH Aachen University zur Erlangung des akademischen Grades einer Doktorin der Naturwissenschaften genehmigte Dissertation vorgelegt von Diplom-Biologin Simone Faller aus Frankfurt am Main Berichter: Privatdozent Dr. Rudolf Loesel Universitätsprofessor Dr. Peter Bräunig Tag der mündlichen Prüfung: 09. März 2012 Diese Dissertation ist auf den Internetseiten der Hochschulbibliothek online verfügbar. Contents 1 General Introduction 1 Deep Metazoan Phylogeny 1 Neurophylogeny 2 Mollusca 5 Nemertea 6 Aim of the thesis 7 2 Neuroanatomy of Minor Mollusca 9 Introduction 9 Material and Methods 10 Results 12 Caudofoveata 12 Scutopus ventrolineatus 12 Falcidens crossotus 16 Solenogastres 16 Dorymenia sarsii 16 Polyplacophora 20 Lepidochitona cinerea 20 Acanthochitona crinita 20 Scaphopoda 22 Antalis entalis 22 Entalina quinquangularis 24 Discussion 25 Structure of the brain and nerve cords 25 Caudofoveata 25 Solenogastres 26 Polyplacophora 27 Scaphopoda 27 i CONTENTS Evolutionary considerations 28 Relationship among non-conchiferan molluscan taxa 28 Position of the Scaphopoda within Conchifera 29 Position of Mollusca within Protostomia 30 3 Neuroanatomy of Nemertea 33 Introduction 33 Material and Methods 34 Results 35 Brain 35 Cerebral organ 38 Nerve cords and peripheral nervous system 38 Discussion 38 Peripheral nervous system 40 Central nervous system 40 In search for the urbilaterian brain 42 4 General Discussion 45 Evolution of higher brain centers 46 Neuroanatomical glossary and data matrix – Essential steps toward a cladistic analysis of neuroanatomical data 49 5 Summary 53 6 Zusammenfassung 57 7 References 61 Danksagung 75 Lebenslauf 79 ii iii 1 General Introduction Deep Metazoan Phylogeny The concept of phylogeny follows directly from the theory of evolution as published by Charles Darwin in The origin of species (1859). - 
												
												Giant Pacific Octopus (Enteroctopus Dofleini) Care Manual
Giant Pacific Octopus Insert Photo within this space (Enteroctopus dofleini) Care Manual CREATED BY AZA Aquatic Invertebrate Taxonomic Advisory Group IN ASSOCIATION WITH AZA Animal Welfare Committee Giant Pacific Octopus (Enteroctopus dofleini) Care Manual Giant Pacific Octopus (Enteroctopus dofleini) Care Manual Published by the Association of Zoos and Aquariums in association with the AZA Animal Welfare Committee Formal Citation: AZA Aquatic Invertebrate Taxon Advisory Group (AITAG) (2014). Giant Pacific Octopus (Enteroctopus dofleini) Care Manual. Association of Zoos and Aquariums, Silver Spring, MD. Original Completion Date: September 2014 Dedication: This work is dedicated to the memory of Roland C. Anderson, who passed away suddenly before its completion. No one person is more responsible for advancing and elevating the state of husbandry of this species, and we hope his lifelong body of work will inspire the next generation of aquarists towards the same ideals. Authors and Significant Contributors: Barrett L. Christie, The Dallas Zoo and Children’s Aquarium at Fair Park, AITAG Steering Committee Alan Peters, Smithsonian Institution, National Zoological Park, AITAG Steering Committee Gregory J. Barord, City University of New York, AITAG Advisor Mark J. Rehling, Cleveland Metroparks Zoo Roland C. Anderson, PhD Reviewers: Mike Brittsan, Columbus Zoo and Aquarium Paula Carlson, Dallas World Aquarium Marie Collins, Sea Life Aquarium Carlsbad David DeNardo, New York Aquarium Joshua Frey Sr., Downtown Aquarium Houston Jay Hemdal, Toledo - 
												
												Centimeter-Wide Worm-Like Fossils from the Lowest Cambrian of South
www.nature.com/scientificreports OPEN Centimeter-wide worm-like fossils from the lowest Cambrian of South China Received: 15 May 2017 Xingliang Zhang1, Wei Liu1, Yukio Isozaki2 & Tomohiko Sato2 Accepted: 20 October 2017 The trace fossil record implies that large worm-like animals were in place along with the skeletonizing Published: xx xx xxxx organisms during the initial stage of the Cambrian explosion. Body fossils of large worms, however, have so far not been found. Here, we describe a large, soft-bodied, worm-like organism, Vittatusivermis annularius gen. et sp. nov. from the lowest Cambrian of South China, which is constrained to the Fortunian Age (541–529 Ma) of the Cambrian Period. The elongate body of Vittatusivermis was large enough to have supported organ systems and a fuid skeleton that facilitated peristaltic locomotion, thus allowing for more complex patterns of movement than those of fatworms. Its occurrence on the same bedding surface as trace fossils suggests that Vittatusivermis might have produced epichnial trails and shallow burrows on and within sediments. Therefore, Vittatusivermis is likely to have been one of the long expected producers of trace fossils in the earliest Cambrian. Te Cambrian explosion was an evolutionary event of great magnitude, as evidenced by the abrupt appearances of diverse animal lineages in the fossil record during the early Cambrian (~541–509 Ma)1–4. Tubes, shells, and sclerites of small shelly faunas are characteristic fossils of the Terreneuvian Epoch (~541–521 Ma)5,6. Exceptionally preserved sof-bodied faunas in subsequent Cambrian Epoch 2 (~521–509 Ma) reveal a more complete faunal composition of the Cambrian explosion7,8. - 
												
												CAPÍTULO 7 Phylum Dicyemida Francisco Brusa Y Lisandro Negrete
CAPÍTULO 7 Phylum Dicyemida Francisco Brusa y Lisandro Negrete "Desde su descubrimiento han constituido un rompecabezas taxonómico". LIBBIE H. HYMAN, THE INVERTEBRATES (1940) El phylum Dicyemida tradicionalmente se asociaba a los ortonéctidos, que parasitan varios grupos de in- vertebrados marinos (“turbelarios”, nemertinos, poliquetos, moluscos gasterópodos y bivalvos, ofiuros y ascidias), y se los incluía en el phylum Mesozoa, por su grado de organización intermedio entre los proto- zoos y metazoos. Actualmente, debido a diferencias en su anatomía y en el ciclo de vida se los reconoce como pertenecientes a dos phyla, Dicyemida y Orthonectida. Los diciémidos son un grupo de pequeños animales vermiformes que parasitan los apéndices renales de moluscos cefalópodos. Presentan especificidad parasitaria y generalmente un individuo hospedador puede albergar más de una especie parásita. Se reconocen 112 especies válidas distribuidas en nueve géneros, cinco de los cuales son monoespecíficos (Catalano, 2012). Los diciémidos están mejor representados en el hemisferio norte, mientras que se conocen pocos registros en el hemisferio sur; este sesgo podría deberse a los escasos estudios en esta región. Son animales muy sencillos con el cuerpo constituido por pocas células (menos de 40), sin tejidos ni órganos. No obstante se ha reportado la presencia de uniones intercelulares entre distintas células en los individuos de los diferentes estadios del ciclo de vida. Se ha observado la pre- sencia de zónula adherens, mácula adherens y uniones gap. Si bien no se han encontrado componentes extracelulares formando una lámina basal o fibras de colágeno, sí se ha reportado la presencia de fibronec- tina y colágeno tipo IV con patrones de distribución similares a los de la lámina basal (Czaker y Janssen, 1998; Czaker, 2000). - 
												
												(Drumian, Miaolingian) Marjum Formation of Western Utah, USA
First palaeoscolecid from the Cambrian (Drumian, Miaolingian) Marjum Formation of western Utah, USA WADE W. LEIBACH, RUDY LEROSEY-AUBRIL, ANNA F. WHITAKER, JAMES D. SCHIFFBAUER, and JULIEN KIMMIG Leibach, W.W., Lerosey-Aubril, R., Whitaker, A.F., Schiffbauer, J.D., and Kimmig, J. 2021. First palaeoscolecid from the Cambrian (Drumian, Miaolingian) Marjum Formation of western Utah, USA. Acta Palaeontologica Polonica 66 (X): xxx–xxx. The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It preserves a diverse non-biomineralized fossil assemblage, which is dominated by panarthropods and sponges. Infaunal components are particularly rare, and are best exemplified by the poorly diverse scalidophoran fauna and the uncertain presence of palaeoscolecids amongst it. To date, only a single Marjum Formation fossil has been tentatively assigned to the palaeoscolecid taxon Scathascolex minor. This specimen and two recently collected worm fragments were analysed in this study using scanning electron microscopy and energy dispersive X-ray spectrometry. The previous occurrence of a Marjum Formation palaeoscolecid is refuted based on the absence of sclerites in the specimen, which we tentatively assign to an unidentified species of Ottoia. The two new fossils, however, are identified as a new palaeoscolecid taxon, Arrakiscolex aasei gen. et sp. nov., characterized by the presence of hundreds of size-constrained (20–30 µm), smooth- rimmed, discoid plates on each annulus. This is the first indisputable evidence for the presence of palaeoscolecids in the Marjum biota, and a rare occurrence of the group in the Cambrian of Laurentia. Palaeoscolecids are now known from nine Cambrian Stage 3–Guzhangian localities in Laurentia, but they typically represent rare components of the biotas. - 
												
												A Probable Oligochaete from an Early Triassic Lagerstätte of the Southern Cis-Urals and Its Evolutionary Implications
Editors' choice A probable oligochaete from an Early Triassic Lagerstätte of the southern Cis-Urals and its evolutionary implications DMITRY E. SHCHERBAKOV, TARMO TIMM, ALEXANDER B. TZETLIN, OLEV VINN, and ANDREY Y. ZHURAVLEV Shcherbakov, D.E., Timm, T., Tzetlin, A.B., Vinn, O., and Zhuravlev, A.Y. 2020. A probable oligochaete from an Early Triassic Lagerstätte of the southern Cis-Urals and its evolutionary implications. Acta Palaeontologica Polonica 65 (2): 219–233. Oligochaetes, despite their important role in terrestrial ecosystems and a tremendous biomass, are extremely rare fossils. The palaeontological record of these worms is restricted to some cocoons, presumable trace fossils and a few body fossils the most convincing of which are discovered in Mesozoic and Cenozoic strata. The Olenekian (Lower Triassic) siliciclastic lacustrine Petropavlovka Lagerstätte of the southern Cis-Urals yields a number of extraordinary freshwater fossils including an annelid. The segmented body with a secondary annulation of this fossil, a subtriangular prostomium, a relatively thick layered body wall and, possibly, the presence of a genital region point to its oligochaete affinities. Other fossil worms which have been ascribed to clitellates are reviewed and, with a tentative exception of two Pennsylvanian finds, affinities of any pre-Mesozoic forms to clitellate annelids are rejected. The new fossil worm allows tracing of a persuasive oligochaete record to the lowermost Mesozoic and confirms a plausibility of the origin of this annelid group in freshwater conditions. Key words: Annelida, Clitellata, Oligochaeta, Mesozoic, Lagerstätte, Russia. Dmitry E. Shcherbakov [[email protected]], Borissiak Palaeontological Institute, Russian Academy of Sciences, Profso- yuz naya St 123, Moscow 117647, Russia. - 
												
												The Palaeoscolecida and the Evolution of the Ecdysozoa Andrey Yu
The Palaeoscolecida and the evolution of the Ecdysozoa Andrey Yu. Zhuravlev1, José Antonio Gámez Vintaned2 and Eladio Liñán1 1Área y Museo de Paleontología, Departamento de Ciencias de la Tierra, Facultad de Ciencias, Universidad de Zaragoza, C/ Pedro Cerbuna, 12, E-50009 Zaragoza, Spain 2Área de Paleontología, Departamento de Geologica, Facultad de Ciencias Biológicas, Univeristat de València, C/ Doctor Moliner, 50, E-46100 Burjassot, Spain Email: [email protected] AbstrAct rÉsUMÉ Palaeoscolecidans are a key group for understanding the ear- Les Paléoscolécides sont un groupe clé pour la compréhen- ly evolution of the Ecdysozoa. The Palaeoscolecida possess sion des débuts de l’évolution des Ecdysozoa. Les Pal- a terminal mouth and an anus, an invertible proboscis with aeoscolecida possèdent une bouche terminale et un anus, pointed scalids, a thick integument of diverse plates, sensory un proboscis inversible aux scalides pointues, un tégument papillae and caudal hooks. These are features that draw a épais de plaques diverses, des papilles sensorielles et des secret out of these worms, indicating palaeoscolecidan af- crochets caudaux. Ceux-ci sont des traits qui tirent un secret finities with the phylum Cephalorhyncha, which embraces de ces vers, ce qui indique des affinités paléoscolecides avec priapulids, kinorhynchs, loriciferans and nematomorphs. At le phylum des Cephalorhyncha qui inclut les priapulides, les the same time, the Palaeoscolecida share a number of char- kinorhynches, les loricifères et les nématomorphes. Cepen- acters with the lobopod-bearing Cambrian ecdysozoans, the dant, les Palaeoscolecida ont aussi quelques-uns des mêmes Xenusia. Xenusians commonly possess a terminal mouth, caractères que les Xenusia, ces écdysozaires cambriens qui a proboscis (although not retractable), and a thick integu- portaient des lobopodes. - 
												
												A New Dicyemid from Octopus Hubbsorum (Mollusca: Cephalopoda: Octopoda) Author(S) :Sheila Castellanos-Martinez, M
A New Dicyemid from Octopus hubbsorum (Mollusca: Cephalopoda: Octopoda) Author(s) :Sheila Castellanos-Martinez, M. Carmen Góómez, F. G. Hochberg, Camino Gestal, and Hidetaka Furuya Source: The Journal of Parasitology, 97(2):265-269. 2011. Published By: American Society of Parasitologists DOI: 10.1645/GE-2577.1 URL: http://www.bioone.org/doi/full/10.1645/GE-2577.1 BioOne (www.bioone.org) is a a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. J. Parasitol., 97(2), 2011, pp. 265–269 F American Society of Parasitologists 2011 A NEW DICYEMID FROM OCTOPUS HUBBSORUM (MOLLUSCA: CEPHALOPODA: OCTOPODA) Sheila Castellanos-Martinez, M. Carmen Go´ mez*, F. G. HochbergÀ, Camino Gestal, and Hidetaka Furuya` Instituto de Investigaciones Marinas (CSIC), Eduardo Cabello 6, 36208 Vigo, Spain. e-mail: [email protected] ABSTRACT: A new species of dicyemid mesozoan is described from Octopus hubbsorum Berry, 1953, collected in the south of Bahia de La Paz, Baja California Sur, Me´xico.