A Field Guide to the Silurian Echinodermata of the British Isles
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Systematic Comparison of Sea Urchin and Sea Star Developmental Gene Regulatory Networks Explains How Novelty Is Incorporated in Early Development
ARTICLE https://doi.org/10.1038/s41467-020-20023-4 OPEN Systematic comparison of sea urchin and sea star developmental gene regulatory networks explains how novelty is incorporated in early development Gregory A. Cary 1,3,5, Brenna S. McCauley1,4,5, Olga Zueva1, Joseph Pattinato1, William Longabaugh2 & ✉ Veronica F. Hinman 1 1234567890():,; The extensive array of morphological diversity among animal taxa represents the product of millions of years of evolution. Morphology is the output of development, therefore phenotypic evolution arises from changes to the topology of the gene regulatory networks (GRNs) that control the highly coordinated process of embryogenesis. A particular challenge in under- standing the origins of animal diversity lies in determining how GRNs incorporate novelty while preserving the overall stability of the network, and hence, embryonic viability. Here we assemble a comprehensive GRN for endomesoderm specification in the sea star from zygote through gastrulation that corresponds to the GRN for sea urchin development of equivalent territories and stages. Comparison of the GRNs identifies how novelty is incorporated in early development. We show how the GRN is resilient to the introduction of a transcription factor, pmar1, the inclusion of which leads to a switch between two stable modes of Delta-Notch signaling. Signaling pathways can function in multiple modes and we propose that GRN changes that lead to switches between modes may be a common evolutionary mechanism for changes in embryogenesis. Our data additionally proposes a model in which evolutionarily conserved network motifs, or kernels, may function throughout development to stabilize these signaling transitions. 1 Department of Biological Sciences, Carnegie Mellon University, Pittsburgh, PA 15213, USA. -
(Echinodermata: Holothuroidea) from the Latest Cretaceous Of
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universität München: Elektronischen Publikationen 285 Zitteliana 89 Short Communication First report of sea cucumbers (Echinodermata: Holothuroidea) from the latest Cretaceous of Paläontologie Bayerische Bavaria,GeoBio- Germany & Geobiologie Center Staatssammlung 1,2,3 LMU München für Paläontologie und Geologie LMUMike MünchenReich 1 n München, 01.07.2017 SNSB - Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, 80333 Munich, Germany 2 n Manuscript received Ludwig-Maximilians-Universität München, Department für Geo- und Umweltwissenschaften, 30.12.2016; revision ac- Paläontologie und Geobiologie, Richard-Wagner-Straße 10, 80333 Munich, Germany 3 cepted 21.01.2017 GeoBio-Center der Ludwig-Maximilians-Universität München, Richard-Wagner-Straße 10, 80333 Munich, Germany n ISSN 0373-9627 E-mail: [email protected] n ISBN 978-3-946705-00-0 Zitteliana 89, 285–289. Key words: fossil Holothuroidea; Cretaceous; Maastrichtian; Bavaria; Germany Schüsselwörter: fossile Holothuroidea; Kreide; Maastrichtium; Bayern; Deutschland The Bavarian Gerhardtsreit Formation (‶Gerhardts- 1993; Smith 2004) due to different reasons (Reich reiter Mergel″ / ‶Gerhardtsreiter Schichten″; cf. 2013). There are nearly 1,700 valid extant sea cucum- Böhm 1891; Hagn 1960; Wagreich et al. 2004), also ber species (Smiley 1994; Kerr 2003; Paulay pers. known as Gerhartsreit Formation (‶Gerhartsreiter comm.) known worldwide. The fossil record (since Schichten″; Hagn et al. 1981, 1992; Schwarzhans the Middle Ordovician; Reich 1999, 2010), by con- 2010; Pollerspöck & Beaury 2014) or ‶Gerhards- trast, is discontinuous in time and recorded ranges reuter Schichten″ (Egger 1899; Hagn & Hölzl 1952; of species with around 1,000 reported forms (Reich de Klasz 1956; Herm 1979, 2000) is exposed in Up- 2013, 2014, 2015b) since the early 19th century. -
Aspects of Life Mode Among Ordovician Asteroids: Implications of New Specimens from Baltica
Aspects of life mode among Ordovician asteroids: Implications of new specimens from Baltica DANIEL B. BLAKE and SERGEI ROZHNOV Blake, D.B. and Rozhnov, S. 2007. Aspects of life mode among Ordovician asteroids: Implications of new specimens from Baltica. Acta Palaeontologica Polonica 52 (3): 519–533. A new genus and species of Asteroidea (Echinodermata), Estoniaster maennili, is described from the Upper Ordovician (Caradocian) of Estonia; it is similar to the western European genus Platanaster and the North American Lanthanaster and an as yet unpublished new genus. Specimens of Urasterella? sp. and Cnemidactis sp. are recognized from the Middle Ordovician of northwest Russia; although similar to known species, incomplete preservation precludes more precise tax− onomic assessment. Asteroids are important in many existing marine communities, and in spite of a meager fossil record, diversity suggests they were important in the early Paleozoic as well. Some debate has centered on arm flexibility in early asteroids, which bears on their roles in their communities. Parallels in ambulacral series arrangement between Ordovician and extant species and presence of an ambulacral furrow indicate similar broad ranges of motion and therefore potentially parallel ecologic roles. Many factors might have contributed to the differences between ancient and extant ambulacral ar− ticulation, including changes in positioning of a part of the water vascular system, changes in predation and bioturbation pressures, and taphonomic events that obscure skeletal details. Key words: Echinodermata, Asteroidea, functional morphology, Ordovician, Baltica. Daniel B. Blake [[email protected]], Department of Geology, University of Illinois, 1301 W. Green St., Urbana 61801, IL, USA; Sergei Rozhnov [[email protected]], Paleontological Institute, Russian Academy of Sciences, Profsoyusnaya 123, Mos− cow, 117647, Russia. -
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. -
Cretaceous Fossils from the Chesapeake and Delaware Canal
Cretaceous S;cial Publication No. 18 Fossils from the Chesapeake and Delaware Canal A Guide for Students and Collectors Edward M. Lauginiger / /~ / CRETACEOUS FOSSILS FROM THE CHESAPEAKE AND DELAWARE CANAL: A GUIDE FOR STUDENTS AND COLLECTORS By Edward M. Lauginiger Biology Teacher Academy Park High School Sharon Hill, Pennsylvania September 1988 Reprinted 1997 CONTENTS Page INTRODUCTION. • 1 ACKNOWLEDGMENTS 2 PREVIOUS STUDIES. 3 FOSSILS AND FOSSILIZATION 5 Requirements for Fossilization 6 Types of Fossilization 7 GEOLOGY •• 10 CLASSIFICATON OF FOSSILS. 12 Kingdom Monera • 13 Kindgom Protista 1 3 Kingdom Plantae. 1 4 Kingdom Animalia 15 Phylum Porifera 15 Phylum Cnidaria (Coelenterata). 16 Phylum Bryozoa. 16 Phylum Brachiopoda. 17 Phylum Mollusca • 18 Phylum Annelida •. 22 Phylum Arthropoda • 23 Phylum Echinodermata. 24 Phylum Chordata 24 COLLECTING LOCALITIES 28 FOSSIL CHECK LIST 30 BIBLIOGRAPHY. 33 PLATES. ••• 39 iii FIGURES Page Figure 1 • Index map of the Chesapeake and Delaware Canal Area. .. .. 2 Figure 2. Generalized stratigraphic column of the formations exposed at the C & D Canal. 11 Figure 3. Foraminifera 14 Figure 4. Porifera 16 Figure 5. Cnidaria 16 Figure 6. Bryozoa. 17 Figure 7. Brachiopoda. 18 Figure 8. Mollusca-Gastropoda. 19 Figure 9. Mollusca-Pelecypoda. 21 Figure 10. Mollusca-Cephalopoda 22 Figure 11. Annelida . 22 Figure 12. Arthropoda 23 Figure 13. Echinodermata. 25 Figure 1 4. Chordata . 27 Figure 1 5. Collecting localities at the Chesapeake and Delaware Canal . ... .. 29 v CRETACEOUS FOSSILS FROM THE CHESAPEAKE AND DELAWARE CANAL: A GUIDE FOR STUDENTS AND COLLECTORS Edward M. Lauginiger INTRODUCTION Fossil collectors have been attracted to Delaware since the late 1820s when the excavation of the Chesapeake and Delaware (C&D) Canal first exposed marine fossils of Cretaceous age (Fig. -
GY 112L Earth History
GY 112L Earth History Lab 11 The Mesozoic: Part Two GY 112L Instructors: Douglas Haywick, James Connors, Mary Anne Connors Department of Earth Sciences, University of South Alabama Fifth Edition: August 2009© The Fine Print Contents of these lab exercises are the intellectual property of the authors, particularly Dr. Doug Haywick. Contents cannot be reproduced outside of the University of South Alabama “family” (faculty and students) without the permission of D. Haywick. Internet users can seek this permission by contacting Dr. Haywick through the web address provided below. This manual is constantly being updated and occasionally, even improved. Typos, grammatical errors and sections that make no sense whatsoever may, or may not, be intentional. If you find an error, show it to your instructor. You may get bonus points. More likely you will be told to go away The recipes that are included in some sections are intended to prove that you can eat anything as long as you serve it with plenty of ketchup. Neither Haywick, nor the Connors are responsible for any food poisoning that might occur if you actually try them. http:/www.southalabama.edu/geology/haywick 1 Week Eleven The Mesozoic, Part Two: Molluscs (Cephalopods), Echinoderms and Alabama Stratigraphy Background: Well the good news is that we are rapidly approaching the end of this course. The bad news is that we are rapidly approaching the end of this course and we still have several important animal groups to consider. When we last visited the molluscs two weeks ago, we only had time to consider the gastropods and bivalves. -
Th TRILO the Back to the Past Museum Guide to TRILO BITES
With regard to human interest in fossils, trilobites may rank second only to dinosaurs. Having studied trilobites most of my life, the English version of The Back to the Past Museum Guide to TRILOBITES by Enrico Bonino and Carlo Kier is a pleasant treat. I am captivated by the abundant color images of more than 600 diverse species of trilobites, mostly from the authors’ own collections. Carlo Kier The Back to the Past Museum Guide to Specimens amply represent famous trilobite localities around the world and typify forms from most of the Enrico Bonino Enrico 250-million-year history of trilobites. Numerous specimens are masterpieces of modern professional preparation. Richard A. Robison Professor Emeritus University of Kansas TRILOBITES Enrico Bonino was born in the Province of Bergamo in 1966 and received his degree in Geology from the Depart- ment of Earth Sciences at the University of Genoa. He currently lives in Belgium where he works as a cartographer specialized in the use of satellite imaging and geographic information systems (GIS). His proficiency in the use of digital-image processing, a healthy dose of artistic talent, and a good knowledge of desktop publishing software have provided him with the skills he needed to create graphics, including dozens of posters and illustrations, for all of the displays at the Back to the Past Museum in Cancún. In addition to his passion for trilobites, Enrico is particularly inter- TRILOBITES ested in the life forms that developed during the Precambrian. Carlo Kier was born in Milan in 1961. He holds a degree in law and is currently the director of the Azul Hotel chain. -
Glossary for the Echinodermata
February 2011 Christina Ball ©RBCM Phil Lambert GLOSSARY FOR THE ECHINODERMATA OVERVIEW The echinoderms are a globally distributed and morphologically diverse group of invertebrates whose history dates back 500 million years (Lambert 1997; Lambert 2000; Lambert and Austin 2007; Pearse et al. 2007). The group includes the sea stars (Asteroidea), sea cucumbers (Holothuroidea), sea lilies and feather stars (Crinoidea), the sea urchins, heart urchins and sand dollars (Echinoidea) and the brittle stars (Ophiuroidea). In some areas the group comprises up to 95% of the megafaunal biomass (Miller and Pawson 1990). Today some 13,000 species occur around the world (Pearse et al. 2007). Of those 13,000 species 194 are known to occur in British Columbia (Lambert and Boutillier, in press). The echinoderms are a group of almost exclusively marine organisms with the few exceptions living in brackish water (Brusca and Brusca 1990). Almost all of the echinoderms are benthic, meaning that they live on or in the substrate. There are a few exceptions to this rule. For example several holothuroids (sea cucumbers) are capable of swimming, sometimes hundreds of meters above the sea floor (Miller and Pawson 1990). One species of holothuroid, Rynkatorpa pawsoni, lives as a commensal with a deep-sea angler fish (Gigantactis macronema) (Martin 1969). While the echinoderms are a diverse group, they do share four unique features that define the group. These are pentaradial symmetry, an endoskeleton made up of ossicles, a water vascular system and mutable collagenous tissue. While larval echinoderms are bilaterally symmetrical the adults are pentaradially symmetrical (Brusca and Brusca 1990). All echinoderms have an endoskeleton made of calcareous ossicles (figure 1). -
An Upper Mississippian Echinoderm Microfauna from the Genicera Formation of Northern León (Carboniferous, Cantabrian Mountains, N Spain)
SPANISH JOURNAL OF PALAEONTOLOGY An Upper Mississippian echinoderm microfauna from the Genicera Formation of northern León (Carboniferous, Cantabrian Mountains, N Spain) Joachim PABST* & Hans-Georg HERBIG Institut für Geologie und Mineralogie, Universität zu Köln. Zülpicher Str. 49a, D-50674 Köln. [email protected]; [email protected] * Corresponding author Pabst, J. & Herbig, H. 2020. An Upper Mississippian echinoderm microfauna from the Genicera Formation of northern León (Carboniferous, Cantabrian Mountains, N Spain). [Microfauna de equinodermos del Misisipiense Superior de la Formación Genicera del norte de León (Carbonífero, Cordillera Cantábrica, N de España)]. Spanish Journal of Palaeontology, 35 (1), 47-76. Manuscript received 30 January 2019 https://doi.org/10.7203/sjp.35.1.17116 Manuscript accepted 12 November 2019 © Sociedad Española de Paleontología ISSN 2255-0550 ABSTRACT RESUMEN For the fi rst time an echinoderm microfauna is recorded from Por primera vez se describe una microfauna de equinodermos the cephalopod limestone facies (‘griotte facies’) of the lower de las calizas nodulosas con cefalópodos (“griotte facies”) Carboniferous (Mississippian) Genicera Fm. (Alba Fm.). de la Formación Genicera (Formación Alba) del Carbonífero The formation is widespread in the Cantabrian Mountains inferior (Misisipiense). Si bien esta formación es de in NW Spain, but the ossicles are from some sections in considerable extensión en la Cordillera Cantábrica en el the surroundings of the Bernesga valley in northern León. norte de España, los oscículos descritos solo proceden de They have been derived from insoluble acetic acid residues unas secciones de los alrededores del valle de Bernesga al from samples of the upper and especially of the uppermost norte de León. -
Beche-De-Mer
ISSN 1025-4943 Secretariat of the Pacific Community BECHE-DE-MER Number 13 — July 2000 INFORMATION BULLETIN Editor and group coordinator: Chantal Conand, Université de La Réunion, Laboratoire de biologie marine, 97715 Saint-Denis Cedex, La Réunion, France. [Fax: +262 938166; E-mail: [email protected]]. Production: Information Section, Marine Resources Division, SPC, B.P. D5, 98848 Noumea Cedex, New Caledonia. [Fax: +687 263818; E-mail: [email protected]; Website: http://www.spc.int/coastfish]. Produced with financial assistance from France and Australia. Editorial Dear Readers, Inside this issue This is the 13th issue of the Bulletin. I would like to take this op- portunity to thank all those who have contributed to it and ask Aspects of sea cucumber that you take an active role in its improvement, as many of you broodstock management have already indicated that the Bulletin is useful to you. by A.D. Morgan p. 2 Is the current presentation by section, i.e. 1) New Information, Athyonidium chilensis 2) Correspondence, 3) Publications, satisfactory?: by C. Ravest Presa p. 9 • Which section should be given more space? Sea cucumber fishery in • In the ‘New Information’ section, would you have new infor- the Philippines mation for the columns on ‘In situ spawning observations’ by S. Schoppe p. 10 and ‘Asexual reproduction through fission observations’? Are these columns suitable? Conservation of • The ‘Aquaculture’ column has been continued thanks to the aspidochirotid holothurians in collaboration of S. Battaglene from ICLARM. We regret the the littoral waters of Kenya closure of the Coastal Aquaculture Centre (CAC) Solomon by Y. -
Origin and Significance of Lovén's Law in Echinoderms
Journal of Paleontology, 94(6), 2020, p. 1089–1102 Copyright © 2020, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2020.31 Origin and significance of Lovén’s Law in echinoderms Christopher R. C. Paul1 and Frederick H. C. Hotchkiss2 1School of Earth Sciences, University of Bristol, Bristol, UK <[email protected]> 2Marine and Paleobiological Research Institute, P.O. Box 1016, Vineyard Haven, Massachusetts, USA 02568 <hotchkiss@MPRInstitute. org> Abstract.—Lovén’s Law described the position of larger basicoronal ambulacral plates in echinoids. The smaller basi- coronal plates form first in ontogeny. We restate Lovén’s Law to describe the position of first ambulacral plates using Carpenter’s ambulacra and left (L) or right (R) as: AR, BL, CR, DL, ER, with EA the pair of ambulacra both identical and adjacent. First ambulacral plates of the Cambrian edrioasteroid, Walcottidiscus, code identically. The transition from a tri-radiate 1-1-1 pattern to the 2-1-2 ambulacral pattern of Walcottidiscus and other pentaradiate Paleozoic echinoderms results in Lovén’s Law. This provides an hypothesis for the origin of Lovén’s Law and predicts its widespread occurrence among echinoderm classes. The ‘BD different’ pattern of primary brachioles in pentaradiate glyptocystitoid Rhombifera results from subterminal branching of the ambulacra. The ontogenetic sequence was triradiate, then lateral ambulacra bifurcated, and finally second brachioles developed. -
Glossary of Terms for Echinoderms
Southeastern Regional Taxonomic Center South Carolina Department of Natural Resources http://www.dnr.sc.gov/marine/sertc/ GLOSSARY OF TERMS FOR ECHINODERMS (taken from the SERTC Echinoderm Taxonomy Workshop manual) ABACTINAL. The area of the body opposite the mouth. ABORAL. In a direction away from the mouth; the part of the body opposite the mouth. ACCESSORY DORSAL ARM PLATE. In some ophiuroids, one or several small, symmetrically arranged plates that are inserted between the dorsal arm plate and the lateral arm plate. ACTINAL. The surface of the body that contains the mouth. ADAMBULACRAL. Towards, or immediately adjacent to, an ambulacrum. ADAPICAL. In echinoids, towards the highest part of the test. ADORAL SHIELDS. In ophiuroids, a pair of plates, one of which is found at each side of the oral shield. ADPRESSED. Squeezed against. The adpressed arm spines of ophiuroids are flattened against the sides of the arm. AMBULACRAL GROOVE. In asteroids, the groove on the oral (ventral) surface of the arm, in which the tube feet are carried. Its sides are formed by the adambulacral plates, and it is roofed by the ambulacral plates. In crinoids, a furrow on the oral (dorsal) surface of the pinnules, arms, and central body, which is lined with cilia and bordered by the tube feet. AMBULACRUM. A zone of the body that carries tube feet (pl. ambulacra). Echinoderms generally have 5 ambulacra. The midline of an ambulacrum is a radius. ANAL CONE (or TUBE). In crinoids and echinoids, a fleshy projection bearing the anus at its apex. ANCHOR. See OSSICLE TYPES. ANCHOR PLATE. See OSSICLE TYPES.