Ocular Pores Are Part of the Water—Vascular System
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Echinoidea Clypeasteroidea
Biodiversity Journal, 2014, 5 (2): 291–358 Analysis of some astriclypeids (Echinoidea Clypeast- eroida) Paolo Stara1* & Luigi Sanciu2 1Centro Studi di Storia Naturale del Mediterraneo - Museo di Storia Naturale Aquilegia, Via Italia 63, Pirri-Cagliari and Geomuseo Monte Arci, Masullas, Oristano, Sardinia, Italy; e-mail: [email protected] *Corresponding author The systematic position of some astriclypeid species assigned through times to the genera Amphiope L. Agassiz, 1840 and Echinodiscus Leske, 1778 is reviewed based on the plating ABSTRACT pattern characteristics of these two genera universally accepted, and on the results of new studies. A partial re-arrangement of the family Astriclypeidae Stefanini, 1912 is herein pro- posed, with the institution of Sculpsitechinus n. g. and Paraamphiope n. g., both of them char- acterized by a peculiar plating-structure of the interambulacrum 5 and of the ambulacra I and V. Some species previously attributed to Amphiope and Echinodiscus are transferred into these two new genera. Two new species of Astriclypeidae are established: Echinodiscus andamanensis n. sp. and Paraamphiope raimondii n. sp. Neotypes are proposed for Echin- odiscus tenuissimus L. Agassiz, 1840 and E. auritus Leske, 1778, since these species were still poorly defined, due to the loss of the holotypes and, for E. auritus, also to the unclear geographical/stratigraphical information about the type-locality. A number of additional nom- inal fossil and extant species of "Echinodiscus" needs revision based on the same method. KEY WORDS Astriclypeidae; Amphiope; Paraamphiope; Echinodiscus; Sculpsitechinus; Oligo-Miocene. Received 28.02.2014; accepted 14.03.2014; printed 30.06.2014 Paolo Stara (ed.). Studies on some astriclypeids (Echinoidea Clypeasteroida), pp. -
Taxonomía Y Biogeografía Ecológica De Los Equinoideos Irregulares (Echinoidea: Irregularia) De México
Taxonomía y biogeografía ecológica de los equinoideos irregulares (Echinoidea: Irregularia) de México Alejandra Martínez-Melo1, 2, Francisco Alonso Solís-Marín2, Blanca Estela Buitrón-Sánchez3 & Alfredo Laguarda-Figueras2 1. Posgrado de Ciencias del Mar y Limnología (PCML), Universidad Nacional Autónoma de México (UNAM). México, D. F. 04510, México; [email protected] 2. Laboratorio de Sistemática y Ecología de Equinodermos, Instituto de Ciencias del Mar y Limnología (ICML), UNAM. Apdo. Post. 70-305, México, D. F. 04510, México; [email protected] 3. Departamento de Paleontología, Instituto de Geología (IG), UNAM, Cd. Universitaria, Delegación Coyoacán, México, D. F. 04510, México; [email protected] Recibido 04-VI-2014. Corregido 09-X-2014. Aceptado 04-XI-2014. Abstract: Taxonomy and ecologic biogeography of the irregular Echinoids (Echinoidea: Irregularia) from Mexico. Mexico owns 643 species of echinoderms, almost 10% of the known echinoderm species in the planet. Its geographic location -between the oceanic influences of the Western Central Atlantic and the Eastern Central Pacific- largely explains its enormous biological and ecological diversity. Research on echinoderms in Mexico began in the late nineteenth century; however, there are no reviews on its irregular echinoids. This work reviews the taxonomic and geographic information of irregular echinoids from Mexico, housed in four collections: 1) Colección Nacional de Equinodermos “Ma. Elena Caso Muñoz” from the Instituto de Ciencias del Mar y Limnología (ICML), Universidad Nacional Autónoma de México (UNAM); 2) Invertebrate Zoology Collection, Smithsonian Museum of Natural History, Washington, D.C., United States of America (USA); 3) Invertebrate Collection, Museum of Comparative Zoology, University of Harvard, Boston, Massachusetts, USA and 4) Invertebrate Zoology, Peabody Museum, Yale University, New Haven, Connecticut, USA. -
"Lophophorates" Brachiopoda Echinodermata Asterozoa
Deuterostomes Bryozoa Phoronida "lophophorates" Brachiopoda Echinodermata Asterozoa Stelleroidea Asteroidea Ophiuroidea Echinozoa Holothuroidea Echinoidea Crinozoa Crinoidea Chaetognatha (arrow worms) Hemichordata (acorn worms) Chordata Urochordata (sea squirt) Cephalochordata (amphioxoius) Vertebrata PHYLUM CHAETOGNATHA (70 spp) Arrow worms Fossils from the Cambrium Carnivorous - link between small phytoplankton and larger zooplankton (1-15 cm long) Pharyngeal gill pores No notochord Peculiar origin for mesoderm (not strictly enterocoelous) Uncertain relationship with echinoderms PHYLUM HEMICHORDATA (120 spp) Acorn worms Pharyngeal gill pores No notochord (Stomochord cartilaginous and once thought homologous w/notochord) Tornaria larvae very similar to asteroidea Bipinnaria larvae CLASS ENTEROPNEUSTA (acorn worms) Marine, bottom dwellers CLASS PTEROBRANCHIA Colonial, sessile, filter feeding, tube dwellers Small (1-2 mm), "U" shaped gut, no gill slits PHYLUM CHORDATA Body segmented Axial notochord Dorsal hollow nerve chord Paired gill slits Post anal tail SUBPHYLUM UROCHORDATA Marine, sessile Body covered in a cellulose tunic ("Tunicates") Filter feeder (» 200 L/day) - perforated pharnx adapted for filtering & repiration Pharyngeal basket contractable - squirts water when exposed at low tide Hermaphrodites Tadpole larvae w/chordate characteristics (neoteny) CLASS ASCIDIACEA (sea squirt/tunicate - sessile) No excretory system Open circulatory system (can reverse blood flow) Endostyle - (homologous to thyroid of vertebrates) ciliated groove -
The Paleoecology and Biogeography of Ordovician Edrioasteroids
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 8-2011 The Paleoecology and Biogeography of Ordovician Edrioasteroids Rene Anne Lewis University of Tennessee - Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Paleontology Commons Recommended Citation Lewis, Rene Anne, "The Paleoecology and Biogeography of Ordovician Edrioasteroids. " PhD diss., University of Tennessee, 2011. https://trace.tennessee.edu/utk_graddiss/1094 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Rene Anne Lewis entitled "The Paleoecology and Biogeography of Ordovician Edrioasteroids." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Doctor of Philosophy, with a major in Geology. Michael L. McKinney, Major Professor We have read this dissertation and recommend its acceptance: Colin D. Sumrall, Linda C. Kah, Arthur C. Echternacht Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) THE PALEOECOLOGY AND BIOGEOGRAPHY OF ORDOVICIAN EDRIOASTEROIDS A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville René Anne Lewis August 2011 Copyright © 2011 by René Anne Lewis All rights reserved. -
Ecophenotypic Variation and Developmental Instability in the Late Cretaceous Echinoid Micraster Brevis (Irregularia; Spatangoida)
RESEARCH ARTICLE Ecophenotypic Variation and Developmental Instability in the Late Cretaceous Echinoid Micraster brevis (Irregularia; Spatangoida) Nils Schlüter* Georg-August University of Göttingen, Geoscience Centre, Department of Geobiology, Goldschmidtstr. 3, 37077, Göttingen, Germany * [email protected] Abstract The Late Cretaceous echinoid genus Micraster (irregular echinoids, Spatangoida) is one of the most famous examples of a continuous evolutionary lineage in invertebrate palaeontol- ogy. The influence of the environment on the phenotype, however, was not tested so far. OPEN ACCESS This study analyses differences in phenotypical variations within three populations of Micra- Citation: Schlüter N (2016) Ecophenotypic Variation ster (Gibbaster) brevis from the early Coniacian, two from the Münsterland Cretaceous and Developmental Instability in the Late Cretaceous Basin (Germany) and one from the North Cantabrian Basin (Spain). The environments of Echinoid Micraster brevis (Irregularia; Spatangoida). the Spanish and the German sites differed by their sedimentary characteristics, which are PLoS ONE 11(2): e0148341. doi:10.1371/journal. pone.0148341 generally a crucial factor for morphological adaptations in echinoids. Most of the major phe- notypical variations (position of the ambitus, periproct and development of the subanal fas- Editor: Steffen Kiel, Naturhistoriska riksmuseet, SWEDEN ciole) among the populations can be linked to differences in their host sediments. These phenotypic variations are presumed to be an expression of phenotpic plasticiy, which has Received: November 11, 2015 not been considered in Micraster in previous studies. Two populations (Erwitte area, Ger- Accepted: January 15, 2016 many; Liencres area, Spain) were tested for stochastic variation (fluctuating asymmetry) Published: February 5, 2016 due to developmental instability, which was present in all studied traits. -
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. -
International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution"
International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013 Lindskog, Anders; Mehlqvist, Kristina 2013 Link to publication Citation for published version (APA): Lindskog, A., & Mehlqvist, K. (Eds.) (2013). International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013. (International Geological Correlation Programme, UNESCO; Vol. 3). Department of Geology, Lund University. Total number of authors: 2 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 ANDERS LINDSKOG | KRISTINA MEHLQVIST Printed by Media-Tryck, Lund 2013 Proceedings of the 3rd IGCP 591 Annual Meeting Proceedings of the 3 Lund, Sweden, 9–19 June 2013 EDITED BY ANDERS LINDSKOG | KRISTINA MEHLQVIST DEPARTMENT OF GEOLOGY | LUND UNIVERSITY The abstracts within this volume were presented at the 3rd IGCP 591 Annual rd Meeting, which was held in Lund, Sweden, in June 2013. -
(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. -
Phylum Echinodermata Phylum Echinodermata
Phylum Echinodermata Phylum Echinodermata About 7,000 species Strictly marine, mostly benthic. Typical deuterostomes. Phylum Echinodermata Class Crinoidea (sea lilies) Phylum Echinodermata Class Crinoidea Class Asteroidea (sea stars) Phylum Echinodermata Class Crinoidea Class Asteroidea Class Ophiuroidea (brittle stars and basket stars) Phylum Echinodermata Class Crinoidea Class Asteroidea Class Ophiuroidea Class Echinoidea (sea urchins and sand dollars) Phylum Echinodermata Class Crinoidea Class Asteroidea Class Ophiuroidea Class Echinoidea Class Holothuroidea (sea cucumbers) What do Echinoderms look like? Pentamerous radial symmetry. Oral and aboral surfaces. Oral surface has ambulacral grooves associated with tubefeet called podia. What do Echinoderms look like? Oral and aboral surfaces. What do Echinoderms look like? Arms (ambulacra) numbered with reference to the madreporite. Ambulacrum opposite is A then proceed couterclockwise. Ambulara C and D are the bivium, A B and E are the trivium. What do Echinoderms look like? Body wall Epidermis covers entire body. Endoskeleton of ossicles with tubefeet and dermal branchia protruding through and spines and pedicellaria on outside. What do Echinoderms look like? Body wall Ossicles can be fused into a test (urchins and sand dollars). Ossicles spread apart in cucumbers. Ossicles intermediate and variable in seastars. Muscle fibers beneath ossicles. What do Echinoderms look like? Body wall Tubercles and moveable spines on skeletal plates of echinoids. Small muscles attach spines to test. What do Echinoderms look like? Water vascular system Fluid-filled canals for internal transport and locomotion. Fluid similar to sewater but has coelomcytes and organic molecules. Moved through system with cilia. What do Echinoderms look like? Water vascular system Asteroidea: Madreporite on aboral surface. -
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. -
Tropical Marine Invertebrates CAS BI 569 Phylum Echinodermata by J
Tropical Marine Invertebrates CAS BI 569 Phylum Echinodermata by J. R. Finnerty Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata *Nematoda *Platyhelminthes Acoelomorpha Calcispongia Silicispongiae PROTOSTOMIA Phylum Phylum Phylum CHORDATA ECHINODERMATA HEMICHORDATA Blastopore -> anus Radial / equal cleavage Coelom forms by enterocoely ! Protostome = blastopore contributes to the mouth blastopore mouth anus ! Deuterostome = blastopore becomes anus blastopore anus mouth Halocynthia, a tunicate (Urochordata) Coelom Formation Protostomes: Schizocoely Deuterostomes: Enterocoely Enterocoely in a sea star Axocoel (protocoel) Gives rise to small portion of water vascular system. Hydrocoel (mesocoel) Gives rise to water vascular system. Somatocoel (metacoel) Gives rise to lining of adult body cavity. Echinoderm Metamorphosis ECHINODERM FEATURES Water vascular system and tube feet Pentaradial symmetry Coelom formation by enterocoely Water Vascular System Tube Foot Tube Foot Locomotion ECHINODERM DIVERSITY Crinoidea Asteroidea Ophiuroidea Holothuroidea Echinoidea “sea lilies” “sea stars” “brittle stars” “sea cucumbers” “urchins, sand dollars” Group Form & Habit Habitat Ossicles Feeding Special Characteristics Crinoids 5-200 arms, stalked epifaunal Internal skeleton suspension mouth upward; mucous & Of each arm feeders secreting glands on sessile podia Ophiuroids usually 5 thin arms, epifaunal ossicles in arms deposit feeders act and appear like vertebrae -
A Probable Case of Heterochrony in the Solutan
A probable case of heterochrony in the solutan Dendrocystites Barrande, 1887 (Echinodermata: Blastozoa) from the Upper Ordovician of the Prague Basin (Czech Republic) and a revision of the family Dendrocystitidae Bassler, 1938 FLEUR NOAILLES, BERTRAND LEFEBVRE & LIBOR KAIÈKA The morphology of the Late Ordovician solutan Dendrocystites is reevaluated based on more than 300 specimens from the Letná and Zahořany formations (Prague Basin, Czech Republic). This genus is reported for the first time from the Bohdalec Formation, and its presence is confirmed in the Vinice Formation. The morphology of all specimens of the stratigraphically older species D. barrandei (Sandbian) is identical to that of small to medium-size individuals of D. sedgwicki (Katian). Distinctive characters of D. sedgwicki occur only in the largest specimens, and are all size-related (more asymmetrical thecal outlines, stronger ornamentation, rosetting pattern of thecal plates, proliferation of platelets in the proxistele). Consequently, the transition from D. barrandei to D. sedgwicki is interpreted as the result of heterochronic processes, with the largest individuals of D. sedgwicki displaying hyperadult morphologies (hyper- morphosis). Dendrocystites is locally abundant in both the Letná and Zahořany formations, but extremely rare in the deeper deposits of the Vinice and Bohdalec formations. This pattern coincides closely with first order fluctuations of the sea-level in the Prague Basin. The life orientation and implied feeding strategy of Dendrocystites and other solutans are both critically discussed. Several independent lines of evidence suggest that solutans were more likely detritus-feeders. Finally, it is proposed that two morphologically distinct patterns of dististele organization were elaborated independently from the polyplated, undifferentiated stalk-like appendage of Coleicarpus (plesiomorphic condition).