Systematics , Zoogeography , Andecologyofthepriapu
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Lesson 4 Plant and Animal Classification and Identification
LESSON 4 PLANT AND ANIMAL CLASSIFICATION AND IDENTIFICATION Aim Become familiar with the basic ways in which plants and animals can be classified and identified CLASSIFICATION OF ORGANISMS Living organisms that are relevant to the ecotourism tour guide are generally divided into two main groups of things: ANIMALS........and..........PLANTS The boundaries between these two groups are not always clear, and there is an increasing tendency to recognise as many as five or six kingdoms. However, for our purposes we will stick with the two kingdoms. Each of these main groups is divided up into a number of smaller groups called 'PHYLA' (or Phylum). Each phylum has certain broad characteristics which distinguish it from other groups of plants or animals. For example, all flowering plants are in the phyla 'Anthophyta' (if a plant has a flower it is a member of the phyla 'Anthophyta'). All animals which have a backbone are members of the phyla 'Vertebrate' (i.e. Vertebrates). Getting to know these major groups of plants and animals is the first step in learning the characteristics of, and learning to identify living things. You should try to gain an understanding of the order of the phyla - from the simplest to the most complex - in both the animal and plant kingdoms. Gaining this type of perspective will provide you with a framework which you can slot plants or animals into when trying to identify them in nature. Understanding the phyla is only the first step, however. Phyla are further divided into groups called 'classes'. Classes are divided and divided again and so on. -
Platyhelminthes, Nemertea, and "Aschelminthes" - A
BIOLOGICAL SCIENCE FUNDAMENTALS AND SYSTEMATICS – Vol. III - Platyhelminthes, Nemertea, and "Aschelminthes" - A. Schmidt-Rhaesa PLATYHELMINTHES, NEMERTEA, AND “ASCHELMINTHES” A. Schmidt-Rhaesa University of Bielefeld, Germany Keywords: Platyhelminthes, Nemertea, Gnathifera, Gnathostomulida, Micrognathozoa, Rotifera, Acanthocephala, Cycliophora, Nemathelminthes, Gastrotricha, Nematoda, Nematomorpha, Priapulida, Kinorhyncha, Loricifera Contents 1. Introduction 2. General Morphology 3. Platyhelminthes, the Flatworms 4. Nemertea (Nemertini), the Ribbon Worms 5. “Aschelminthes” 5.1. Gnathifera 5.1.1. Gnathostomulida 5.1.2. Micrognathozoa (Limnognathia maerski) 5.1.3. Rotifera 5.1.4. Acanthocephala 5.1.5. Cycliophora (Symbion pandora) 5.2. Nemathelminthes 5.2.1. Gastrotricha 5.2.2. Nematoda, the Roundworms 5.2.3. Nematomorpha, the Horsehair Worms 5.2.4. Priapulida 5.2.5. Kinorhyncha 5.2.6. Loricifera Acknowledgements Glossary Bibliography Biographical Sketch Summary UNESCO – EOLSS This chapter provides information on several basal bilaterian groups: flatworms, nemerteans, Gnathifera,SAMPLE and Nemathelminthes. CHAPTERS These include species-rich taxa such as Nematoda and Platyhelminthes, and as taxa with few or even only one species, such as Micrognathozoa (Limnognathia maerski) and Cycliophora (Symbion pandora). All Acanthocephala and subgroups of Platyhelminthes and Nematoda, are parasites that often exhibit complex life cycles. Most of the taxa described are marine, but some have also invaded freshwater or the terrestrial environment. “Aschelminthes” are not a natural group, instead, two taxa have been recognized that were earlier summarized under this name. Gnathifera include taxa with a conspicuous jaw apparatus such as Gnathostomulida, Micrognathozoa, and Rotifera. Although they do not possess a jaw apparatus, Acanthocephala also belong to Gnathifera due to their epidermal structure. ©Encyclopedia of Life Support Systems (EOLSS) BIOLOGICAL SCIENCE FUNDAMENTALS AND SYSTEMATICS – Vol. -
Number of Living Species in Australia and the World
Numbers of Living Species in Australia and the World 2nd edition Arthur D. Chapman Australian Biodiversity Information Services australia’s nature Toowoomba, Australia there is more still to be discovered… Report for the Australian Biological Resources Study Canberra, Australia September 2009 CONTENTS Foreword 1 Insecta (insects) 23 Plants 43 Viruses 59 Arachnida Magnoliophyta (flowering plants) 43 Protoctista (mainly Introduction 2 (spiders, scorpions, etc) 26 Gymnosperms (Coniferophyta, Protozoa—others included Executive Summary 6 Pycnogonida (sea spiders) 28 Cycadophyta, Gnetophyta under fungi, algae, Myriapoda and Ginkgophyta) 45 Chromista, etc) 60 Detailed discussion by Group 12 (millipedes, centipedes) 29 Ferns and Allies 46 Chordates 13 Acknowledgements 63 Crustacea (crabs, lobsters, etc) 31 Bryophyta Mammalia (mammals) 13 Onychophora (velvet worms) 32 (mosses, liverworts, hornworts) 47 References 66 Aves (birds) 14 Hexapoda (proturans, springtails) 33 Plant Algae (including green Reptilia (reptiles) 15 Mollusca (molluscs, shellfish) 34 algae, red algae, glaucophytes) 49 Amphibia (frogs, etc) 16 Annelida (segmented worms) 35 Fungi 51 Pisces (fishes including Nematoda Fungi (excluding taxa Chondrichthyes and (nematodes, roundworms) 36 treated under Chromista Osteichthyes) 17 and Protoctista) 51 Acanthocephala Agnatha (hagfish, (thorny-headed worms) 37 Lichen-forming fungi 53 lampreys, slime eels) 18 Platyhelminthes (flat worms) 38 Others 54 Cephalochordata (lancelets) 19 Cnidaria (jellyfish, Prokaryota (Bacteria Tunicata or Urochordata sea anenomes, corals) 39 [Monera] of previous report) 54 (sea squirts, doliolids, salps) 20 Porifera (sponges) 40 Cyanophyta (Cyanobacteria) 55 Invertebrates 21 Other Invertebrates 41 Chromista (including some Hemichordata (hemichordates) 21 species previously included Echinodermata (starfish, under either algae or fungi) 56 sea cucumbers, etc) 22 FOREWORD In Australia and around the world, biodiversity is under huge Harnessing core science and knowledge bases, like and growing pressure. -
Autor: T-I Ij Ii 11 Iil U Li U Titel: H I] Il !J Band: I~ Ii Fj Ii [I S
;; ij Il 1I U it li ii H 13 u Autor: t-i ij ii 11 iil u li U Titel: H I] Il !J Band: I~ Ii fj iI [i s. 181 - 201. li 13 U li U It ii I,i Ii U t-i il il ii 11 il 11 li Il il lil U Ii il 1I l~ li Ii vörhanuen 1I 1,1 ti U n u 1I ii It 11 u I1 U li 1.1 it jj u ii u n 11 ii 11 H.l l,I II n il ii li ii ii U Ii U li 11 I] II !l !:! 1'1 I1 6 ?e> O$-15k~w'rl~1i. 180 T.A. Platonova& L. V. Kulangieva: Marine £noplido- ZOOSYST. ROSSICA Val. 3 @ Zoological Institute, Sl.Peter~ 1995 pharynx aod proposal of two new families. Zool. Tchesunov, A. V. 1991. On the slruclure of thc cephaJic Zhurn., 69(8): 5-17. (In Russian), culiclc in frcc-living ncmatodcsof thc famHy Linho- - Tchesunov, A.V. 1990b. Long-hairy Xyalida (Ncma- mocidae (Nemaloda. Chromadoria, Siphonolaimo- loda, Chromadoria, Monhystcrida) in thc Whitc ideaL Zoo!. Zhurn., 70(5): 21-27. (In RussianL The phylogeny and classification ofthe phylum Sca: ncw spccics, new combinations arid s~atusof Ih~ genus Trichotheristus. Zoo!. Zhurn., 69(10): 5-19. Reeei."ed 27 Mo)! /99J (In R!JssianL Cephalorhyncha A.V. Adrianov & V.V. Malakhov Adrianov, A.V. & Malakhoy, V. V. 1995. Thc phylogcny and c1assification of thc phylum Cephalorhyncha. Zoosystematica Rossica, 3(2),' 1994: 181-201. The phylum Ccphalorhyncha is a laxon including headproboscis worms: Priapulida, Loricifera, Kinorhyncha, Nematomorpha. -
Multi-Gene Analyses of the Phylogenetic Relationships Among the Mollusca, Annelida, and Arthropoda Donald J
Zoological Studies 47(3): 338-351 (2008) Multi-Gene Analyses of the Phylogenetic Relationships among the Mollusca, Annelida, and Arthropoda Donald J. Colgan1,*, Patricia A. Hutchings2, and Emma Beacham1 1Evolutionary Biology Unit, The Australian Museum, 6 College St. Sydney, NSW 2010, Australia 2Marine Invertebrates, The Australian Museum, 6 College St., Sydney, NSW 2010, Australia (Accepted October 29, 2007) Donald J. Colgan, Patricia A. Hutchings, and Emma Beacham (2008) Multi-gene analyses of the phylogenetic relationships among the Mollusca, Annelida, and Arthropoda. Zoological Studies 47(3): 338-351. The current understanding of metazoan relationships is largely based on analyses of 18S ribosomal RNA ('18S rRNA'). In this paper, DNA sequence data from 2 segments of 28S rRNA, cytochrome c oxidase subunit I, histone H3, and U2 small nuclear (sn)RNA were compiled and used to test phylogenetic relationships among the Mollusca, Annelida, and Arthropoda. The 18S rRNA data were included in the compilations for comparison. The analyses were especially directed at testing the implication of the Eutrochozoan hypothesis that the Annelida and Mollusca are more closely related than are the Annelida and Arthropoda and at determining whether, in contrast to analyses using only 18S rRNA, the addition of data from other genes would reveal these phyla to be monophyletic. New data and available sequences were compiled for up to 49 molluscs, 33 annelids, 22 arthropods, and 27 taxa from 15 other metazoan phyla. The Porifera, Ctenophora, and Cnidaria were used as the outgroup. The Annelida, Mollusca, Entoprocta, Phoronida, Nemertea, Brachiopoda, and Sipuncula (i.e., all studied Lophotrochozoa except for the Bryozoa) formed a monophyletic clade with maximum likelihood bootstrap support of 81% and a Bayesian posterior probability of 0.66 when all data were analyzed. -
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). -
Cryptic Speciation Among Meiofaunal Flatworms Henry J
Winthrop University Digital Commons @ Winthrop University Graduate Theses The Graduate School 8-2018 Cryptic Speciation Among Meiofaunal Flatworms Henry J. Horacek Winthrop University, [email protected] Follow this and additional works at: https://digitalcommons.winthrop.edu/graduatetheses Part of the Biology Commons Recommended Citation Horacek, Henry J., "Cryptic Speciation Among Meiofaunal Flatworms" (2018). Graduate Theses. 94. https://digitalcommons.winthrop.edu/graduatetheses/94 This Thesis is brought to you for free and open access by the The Graduate School at Digital Commons @ Winthrop University. It has been accepted for inclusion in Graduate Theses by an authorized administrator of Digital Commons @ Winthrop University. For more information, please contact [email protected]. CRYPTIC SPECIATION AMONG MEIOFAUNAL FLATWORMS A thesis Presented to the Faculty Of the College of Arts and Sciences In Partial Fulfillment Of the Requirements for the Degree Of Master of Science In Biology Winthrop University August, 2018 By Henry Joseph Horacek August 2018 To the Dean of the Graduate School: We are submitting a thesis written by Henry Joseph Horacek entitled Cryptic Speciation among Meiofaunal Flatworms. We recommend acceptance in partial fulfillment of the requirements for the degree of Master of Science in Biology __________________________ Dr. Julian Smith, Thesis Advisor __________________________ Dr. Cynthia Tant, Committee Member _________________________ Dr. Dwight Dimaculangan, Committee Member ___________________________ Dr. Adrienne McCormick, Dean of the College of Arts & Sciences __________________________ Jack E. DeRochi, Dean, Graduate School Table of Contents List of Figures p. iii List of Tables p. iv Abstract p. 1 Acknowledgements p. 2 Introduction p. 3 Materials and Methods p. 18 Results p. 28 Discussion p. -
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. -
(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 Anatomy, Affinity, and Phylogenetic Significance of Markuelia
EVOLUTION & DEVELOPMENT 7:5, 468–482 (2005) The anatomy, affinity, and phylogenetic significance of Markuelia Xi-ping Dong,a,Ã Philip C. J. Donoghue,b,Ã John A. Cunningham,b,1 Jian-bo Liu,a andHongChengc aDepartment of Earth and Space Sciences, Peking University, Beijing 100871, China bDepartment of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK cCollege of Life Sciences, Peking University, Beijing 100871, China ÃAuthors for correspondence (email: [email protected], [email protected]) 1Present address: Department of Earth and Ocean Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, UK. SUMMARY The fossil record provides a paucity of data on analyses have hitherto suggested assignment to stem- the development of extinct organisms, particularly for their Scalidophora (phyla Kinorhyncha, Loricifera, Priapulida). We embryology. The recovery of fossilized embryos heralds new test this assumption with additional data and through the insight into the evolution of development but advances are inclusion of additional taxa. The available evidence supports limited by an almost complete absence of phylogenetic stem-Scalidophora affinity, leading to the conclusion that sca- constraint. Markuelia is an exception to this, known from lidophorans, cyclonerualians, and ecdysozoans are primitive cleavage and pre-hatchling stages as a vermiform and direct developers, and the likelihood that scalidophorans are profusely annulated direct-developing bilaterian with terminal primitively metameric. circumoral and posterior radial arrays of spines. Phylogenetic INTRODUCTION et al. 2004b). Very early cleavage-stage embryos of presumed metazoans and, possibly, bilaterian metazoans, have been re- The fossil record is largely a record of adult life and, thus, covered from the late Neoproterozoic (Xiao et al.