10 Echinoderm Webquest

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Name: __________________________ Echinoderm Webquest #10 Period: ______ Incredible Echinoderms Link 1: http://www.earthlife.net/inverts/echinodermata.html Scroll down to the “Record Holders” section of the webpage. 1. What is the largest species of starfish? What is its arm reach? (Insert a picture of this animal) 2. What is the heaviest species of starfish? What is its weight in pounds? (Insert a picture of this animal) 3. What is the largest species of sea cucumber? What is its length and diameter? (Insert a picture of this animal) 4. Where will you find the smallest species of starfish and sea urchins? 5. What is the deepest living echinoderm? At what depth is it found? Where is it located? 6. Select and research one of the record holder species from above. Write a short paragraph about his species which includes other interesting facts and unique information. Virtual Echinoderm Link 2: http://bio.rutgers.edu/~gb102/lab_3/401bm-asteroidea.html 7. Describe the pathway of the water vascular system. 8. Click continue. What can you find among the spines of a sea urchin? 9. What is Aristotle’s Lantern? (Insert a picture of it) Name: __________________________ Echinoderm Webquest #10 Period: ______ 10. Click on the words “sand dollar.” The flattened body of the sand dollar is an adaptation for what lifestyle? 11. Click continue. In what ways are sea cucumbers different from other echinoderms? Starfish Outbreak Link 3: http://www.biologynews.net/archives/2008/01/14/starfish_outbreak_threatens_corals.html 12. Read the article. This article is about which species of starfish? (Include a picture) 13. What is thought to be causing the outbreak? 14. Why is this outbreak such a concern? Everlasting Knives Link 4: http://www.telegraph.co.uk/news/earth/earthnews/8224831/Sea-urchin-could-lead-to- knives-that-never-need-sharpening.html 15. Read and write a short summary of this article. Sea Urchins and Humans Link 5: http://news.nationalgeographic.com/news/2006/11/061109-sea-urchins.html 16. Why are sea urchins such an important part of the kelp forest ecosystem? 17. Click “Continue on Next Page.” Describe the genetic evidence which supports the claim that humans and sea urchins are closely related. .

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The A/P Axis in Echinoderm Ontogeny and Evolution: Evidence from Fossils and Molecules
EVOLUTION & DEVELOPMENT 2:2, 93–101 (2000) The A/P axis in echinoderm ontogeny and evolution: evidence from fossils and molecules Kevin J. Peterson,a,b César Arenas-Mena,a,c and Eric H. Davidsona,* aDivision of Biology, California Institute of Technology, Pasadena, CA 91125, USA; bDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA; cStowers Institute for Medical Research, Kansas City, MO 64110, USA *Author for correspondence (email: [email protected]) SUMMARY Even though echinoderms are members of the such that there is but a single plane of symmetry dividing the Bilateria, the location of their anterior/posterior axis has re- animal into left and right halves. We tentatively hypothesize mained enigmatic. Here we propose a novel solution to the that this plane of symmetry is positioned along the dorsal/ven- problem employing three lines of evidence: the expression of tral axis. These axis identifications lead to the conclusion that a posterior class Hox gene in the coeloms of the nascent the five ambulacra are not primary body axes, but instead are adult body plan within the larva; the anatomy of certain early outgrowths from the central anterior/posterior axis. These fossil echinoderms; and finally the relation between endo- identifications also shed insight into several other evolutionary skeletal plate morphology and the associated coelomic tis- mysteries of various echinoderm clades such as the indepen- sues. All three lines of evidence converge on the same answer, dent evolution of bilateral symmetry in irregular echinoids, but namely that the location of the adult mouth is anterior, and the do not elucidate the underlying mechanisms of the adult co- anterior/posterior axis runs from the mouth through the adult elomic architecture.
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Amphipholis Squamata MICHAEL P
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Biology of Echinoderms
Echinoderms Branches on the Tree of Life Programs ECHINODERMS Written and photographed by David Denning and Bruce Russell Produced by BioMEDIA ASSOCIATES ©2005 - Running time 16 minutes. Order Toll Free (877) 661-5355 Order by FAX (843) 470-0237 The Phylum Echinodermata consists of about 6,000 living species, all of which are marine. This video program compares the five major classes of living echinoderms in terms of basic functional biology, evolution and ecology using living examples, animations and a few fossil species. Detailed micro- and macro- photography reveal special adaptations of echinoderms and their larval biology. (THUMBNAIL IMAGES IN THIS GUIDE ARE FROM THE VIDEO PROGRAM) Summary of the Program: Introduction - Characteristics of the Class Echinoidea phylum. spine adaptations, pedicellaria, Aristotle‘s lantern, sand dollars, urchin development, Class Asteroidea gastrulation, settlement skeleton, water vascular system, tube feet function, feeding, digestion, Class Holuthuroidea spawning, larval development, diversity symmetry, water vascular system, ossicles, defensive mechanisms, diversity, ecology Class Ophiuroidea regeneration, feeding, diversity Class Crinoidea – Topics ecology, diversity, fossil echinoderms © BioMEDIA ASSOCIATES (1 of 7) Echinoderms ... ... The characteristics that distinguish Phylum Echinodermata are: radial symmetry, internal skeleton, and water-vascular system. Echinoderms appear to be quite different than other ‘advanced’ animal phyla, having radial (spokes of a wheel) symmetry as adults, rather than bilateral (worm-like) symmetry as in other triploblastic (three cell-layer) animals. Viewers of this program will observe that echinoderm radial symmetry is secondary; echinoderms begin as bilateral free-swimming larvae and become radial at the time of metamorphosis. Also, in one echinoderm group, the sea cucumbers, partial bilateral symmetry is retained in the adult stages -- sea cucumbers are somewhat worm–like.
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An Invertebrate Is an Animal Without a Backbone. They Have No Internal Skeleton and Normally Have Soft, Flexible Bodies
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Upper Ordovician) at Wequiock Creek, Eastern Wisconsin
~rnooij~~~mij~rnoo~ ~oorn~rn~rn~~ rnoo~~rnrn~rn~~ Number 35 September, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois REVIEW COMMITTEE FOR THIS CONTRIBUTION: T.N. Bayer, Winona State College University, Winona Minnesota M.E. Ostrom, Wisconsin Geological Survey, Madison, Wisconsin Peter Sheehan, Milwaukee Public Museum· ISBN :0-89326-016-4 Milwaukee Public Museum Press Published by the Order of the Board of Trustees Milwaukee Public Museum Accepted for publication July, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois Abstract: The Maquoketa Group (Upper Ordovician) is poorly exposed in eastern Wisconsin. The most extensive exposure is found along Wequiock Creek, about 10 kilometers north of Green Bay. There the selection includes a small part of the upper Scales Shale and good exposures of the Fort Atkinson Limestone and Brainard Shale. The exposed Scales Shale is 2.4 m of clay, uniform in appearance and containing no apparent fossils. Limestone and dolomite dominate the 3.9 m thick Fort Atkinson Limestone. The carbonate beds alternate with layers of dolomitic shale that contain little to no fauna. The shales represent times of peak terrigenous clastic deposition in a quiet water environment. The car- bonates are predominantly biogenic dolomite and biomicrite. Biotic succession within single carbonate beds includes replacement of a strophomenid-Lepidocyclus dominated bottom community by a trep- ostome bryozoan-Plaesiomys-Lepidocyclus dominated community. Transported echinoderm and cryptostome bryozoan biocalcarenites are common.
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•...~ ..~ THE ECHINODERM NEWSLETTER Number 22. 1997 Editor: Cynthia Ahearn Smithsonian Institution National Museum of Natural History Room W-31S, Mail Stop 163 Washington D.C. 20560, U.S.A. NEW E-MAIL: [email protected] Distributed by: David Pawson Smithsonian Institution National Museum of Natural History Room W-321, Mail Stop 163 Washington D.C. 20560, U.S.A. The newsletter contains information concerning meetings and conferences, publications of interest to echinoderm biologists, titles of theses on echinoderms, and research interests, and addresses of echinoderm biologists. Individuals who desire to receive the newsletter should send their name, address and research interests to the editor. The newsletter is not intended to be a part of the scientific literature and should not be cited, abstracted, or reprinted as a published document. A. Agassiz, 1872-73 ., TABLE OF CONTENTS Echinoderm Specialists Addresses Phone (p-) ; Fax (f-) ; e-mail numbers . ........................ .1 Current Research ........•... .34 Information Requests .. .55 Announcements, Suggestions .. • .56 Items of Interest 'Creeping Comatulid' by William Allison .. .57 Obituary - Franklin Boone Hartsock .. • .58 Echinoderms in Literature. 59 Theses and Dissertations ... 60 Recent Echinoderm Publications and Papers in Press. ...................... • .66 New Book Announcements Life and Death of Coral Reefs ......•....... .84 Before the Backbone . ........................ .84 Illustrated Encyclopedia of Fauna & Flora of Korea . • •• 84 Echinoderms: San Francisco. Proceedings of the Ninth IEC. • .85 Papers Presented at Meetings (by country or region) Africa. • .96 Asia . ....96 Austral ia .. ...96 Canada..... • .97 Caribbean •. .97 Europe. .... .97 Guam ••• .98 Israel. 99 Japan .. • •.••. 99 Mexico. .99 Philippines .• . .•.•.• 99 South America .. .99 united States .•. .100 Papers Presented at Meetings (by conference) Fourth Temperate Reef Symposium................................•......
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Paleontological Resource Inventory at Chickasaw National Recreation Area, Oklahoma
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Field Trip: Palaeozoic Echinoderms from Northern Spain
FIELD TRIP: PALAEOZOIC ECHINODERMS FROM NORTHERN SPAIN S. Zamora & I. Rábano (eds.), Progress in Echinoderm Palaeobiology. Cuadernos del Museo Geominero, 19. Instituto Geológico y Minero de España, Madrid. ISBN: 978-84-7840-961-7 © Instituto Geológico y Minero de España 2015 FIELD TRIP: PALAEOZOIC ECHINODERMS FROM NORTHERN SPAIN Samuel Zamora 1 (coord.) José Javier Álvaro 2, Miguel Arbizu 3, Jorge Colmenar 4, Jorge Esteve 2, Esperanza Fernández-Martínez 5, Luis Pedro Fernández 3, Juan Carlos Gutiérrez-Marco 2, Juan Luis Suárez Andrés 6, Enrique Villas 4 and Johnny Waters 7 1 Instituto Geológico y Minero de España, Manuel Lasala 44 9ºB, 50006 Zaragoza, Spain. [email protected] 2 Instituto de Geociencias (CSIC-UCM), José Antonio Novais 12, 28040 Madrid, Spain. [email protected], jcgrapto@ ucm.es, [email protected] 3 Departamento de Geología, Universidad de Oviedo, Jesús Arias de Velasco s/n, 33005 Oviedo, Spain. [email protected], [email protected] 4Área de Paleontología, Departamento de Ciencias de la Tierra, Universidad de Zaragoza, Pedro Cerbuna 12, 50009 Zaragoza, Spain. [email protected], [email protected] 5 Facultad de Biología y Ciencias Ambientales, Universidad de León, Campus of Vegazana, 24071 León, Spain. [email protected] 6 Soningeo, S.L. PCTCAN, Isabel Torres, 9 P20. 39011 Santander, Cantabria, Spain. [email protected] 7 Department of Geology, Appalachian State University, ASU Box 32067, Boone, NC 28608-2067, USA. [email protected] Keywords: Cambrian, Ordovician, Silurian, Devonian, echinoderms, environments, evolution. INTRODUCTION Samuel Zamora Spain contains some of the most extensive and fossiliferous Palaeozoic outcrops in Europe , including echinoderm faunas that are internationally significant in terms of systematics, palaeoecology and palaeobiogeography.
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Echinoderm Synopsis
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Development of a Lecithotrophic Pilidium Larva Illustrates Convergent Evolution of Trochophore-Like Morphology Marie K
Hunt and Maslakova Frontiers in Zoology (2017) 14:7 DOI 10.1186/s12983-017-0189-x RESEARCH Open Access Development of a lecithotrophic pilidium larva illustrates convergent evolution of trochophore-like morphology Marie K. Hunt and Svetlana A. Maslakova* Abstract Background: The pilidium larva is an idiosyncrasy defining one clade of marine invertebrates, the Pilidiophora (Nemertea, Spiralia). Uniquely, in pilidial development, the juvenile worm forms from a series of isolated rudiments called imaginal discs, then erupts through and devours the larval body during catastrophic metamorphosis. A typical pilidium is planktotrophic and looks like a hat with earflaps, but pilidial diversity is much broader and includes several types of non-feeding pilidia. One of the most intriguing recently discovered types is the lecithotrophic pilidium nielseni of an undescribed species, Micrura sp. “dark” (Lineidae, Heteronemertea, Pilidiophora). The egg-shaped pilidium nielseni bears two transverse circumferential ciliary bands evoking the prototroch and telotroch of the trochophore larva found in some other spiralian phyla (e.g. annelids), but undergoes catastrophic metamorphosis similar to that of other pilidia. While it is clear that the resemblance to the trochophore is convergent, it is not clear how pilidium nielseni acquired this striking morphological similarity. Results: Here, using light and confocal microscopy, we describe the development of pilidium nielseni from fertilization to metamorphosis, and demonstrate that fundamental aspects of pilidial development are conserved. The juvenile forms via three pairs of imaginal discs and two unpaired rudiments inside a distinct larval epidermis, which is devoured by the juvenile during rapid metamorphosis. Pilidium nielseni even develops transient, reduced lobes and lappets in early stages, re-creating the hat-like appearance of a typical pilidium.
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