Stereom Morphogenesis and Differentiation During Regeneration of Adambulacral Spines of Asterias Rubens (Echinodermata, Asteroida)

Total Page:16

File Type:pdf, Size:1020Kb

Stereom Morphogenesis and Differentiation During Regeneration of Adambulacral Spines of Asterias Rubens (Echinodermata, Asteroida) Zoomorphology (1990) 109:263-272 Zoomorphology © Springer-Verlag 1990 Stereom morphogenesis and differentiation during regeneration of adambulacral spines of Asterias rubens (Echinodermata, Asteroida) Ph. Dubois 1'* and M. Jangoux ~'z 1 Laboratoire de Biologic marine (CP 160), Universit~ Libre de Bruxelles, 50, av F.D. Roosevelt, B-1050 Bruxelles, Belgium 2 Laboratoire de Biologic marine, Universit~ de Mons-Hainaut, 19, av Maistriau, B-7000 Mons, Belgium Received July 15, 1989 Summary. The very first mineral deposits appearing in viz. the development of long linear processes, of short regenerating fractured adambulacral spines of Asterias unbranched processes and of short branched processes. rubens are minute polyhedrons that cover the surface A survey of the literature allows the suggestion that the of fractured trabeculae. Polyhedrons fuse together form- implementation of these elementary events is sufficient ing a fold from which a microspine differentiates. Micro- to describe most types of stereom morphogenesis. spines develop into long linear trabeculae which send out lateral processes at regular length intervals. Lateral processes from adjacent trabeculae fuse together, bridg- ing the trabeculae and giving the regenerate the typical meshwork structure of stereom. Most of the regenerate A. Introduction is built up according to this growth pattern which en- sures its longitudinal growth. Simultaneously, the initial The skeleton of postmetamorphic echinoderms is com- fascicular stereom of the stub sends out short radial pro- posed of discrete dermic elements, the ossicles, bound cesses which branch into upward and downward di- together by collagenous and muscular fibres. Each ossi- rected subprocesses. The latter fuse with their equiva- cle is typically made of a tridimensional network of high- lents located above or below, building up longitudinal magnesium calcite trabeculae, the stereom. The stereom rows of stereom meshes. These rows then bridge together morphology has been rather intensively investigated by additional branched or unbranched lateral processes, over the past 15 years (e.g. Macurda and Meyer 1975; so forming a new stereom layer which progressively Smith 1980a, b; Blake 1984; Hendler and Byrne 1987) covers the whole stub. Up to three new layers of stereom and the different architectural organizations of the tra- are formed in this way at the stub periphery. These be- beculae - viz. the so-called stereom fabrics - have been come continuous with the stereom layers of the regener- codified by Smith (1980a). On the contrary, whereas ate by fusion of reciprocal subprocesses, so ensuring the numerous works were devoted to skeleton development, continuity between the stub and the regenerate. In both few studies have dealt specifically with stereom morpho- structures the first stage of mineralization results in an genesis. These concern chiefly echinoid outer append- open stereom. Stereom thickening occurs in a second ages during either their early formation (Ludwig 1882; stage of mineralization (that is chronologically separated Th~el 1892; Gordon 1926a, b, 1929) or their regenera- from the formation of the open stereom) and results tion (Heatfield 1971 ; Mischor 1975; Hilgers and Splecht- in the differentiation of the original stereom fabrics (i.e. na 1979). fascicular stereom). Regeneration of removed spines The present paper considers both stereom growth starts with the formation of a new spine base made of and stereom differentiation in regenerating adambulac- labyrinthic stereom. The development of the latter most- ral spines of the asteroid Asterias rubens. Its goals are ly relies on short branched and unbranched processes to describe stereom morphogenesis in an asteroid echin- which fuse with each other or with predifferentiated oderm and to provide a first approach to the calcifying meshes. After completion of its base, the regenerating mechanisms operating in a well-defined asteroid skeleto- spine lengthens and thickens similarly to the regenerat- genic site. ing fractured spines. The diversity of the stereom growth processes observed in the present work may be reduced to the combination of one to three elementary events, B. Materials and methods * Senior research assistant NFSR (Belgium) Individuals of A. rubens Linnaeus, 1758, were collected by SCUBA Offprint requests to: Ph. Dubois diving at Seharendijk (Zealand, The Netherlands). The asteroids 264 were kept in a closed-circuit marine aquarium (30%0, 10-14 ° C) fixed with 1% OsO4 in the same buffer. Decalcification was per- and fed to satiety with mussels (Mytilus edulis Linnaeus, 1758). formed using the double embedding method of Holland and Grim- Regeneration of fractured or removed adambulacral spines mer (1981). Pieces were dehydrated in ethanol and embedded in was initiated either by cutting off the upper two-thirds of the spines Spurr's medium. Semithin sections were stained using the method or by removing the spines. Investigated spines were of similar size of Humphrey and Pittman (1974). (2.68 +0.12 mm; n= 10). At variable time intervals, samples of six regenerating spines were taken from each investigated asteroid (by severing the tissues which bind the spines to the adambulacral plates) and processed for microscopy (see below). A detailed experi- mental schedule is presented in Table 1. In order to prevent the C. Results contraction of the ambulacral groove, spines were sampled on an- aesthetized asteroids. Anaesthesia was performed by immersing L Spine morphology whole asteroids for 30 min in a 0.1% (v/v) filtered sea water solu- tion of propylene phenoxetol (Nipa Laboratories) (Hildeman and Dix 1972). The asteroids resumed their activity 15-60 min after One or two (rarely three) adambulacral spines are being returned to normal sea water. Assessment of the possible jointed to each adambulacral plate of A. rubens. As is effect of anaesthesia on skeletogenesis was achieved using a control usual in echinoderm calcified appendages, the spines are group whose individuals were submitted to a restricted number covered by a prismatic epidermis that is separated from of samplings and anaesthesias (see Table l). the stereom by a layer of periossicular connective tissue Removed spines were preserved in 70% ethanol. The stereom was cleaned of its associated soft tissues (viz., epidermis, dermis which is itself continuous with the stroma that fills the and stroma) in two different ways according to the samples: (1) stereom pore space. Adambulacral spines are attached intact spines were incubated for 24 h at 50° C in a neutral solution to adambulacral plates by both collagen and muscular of 0.1% (w/v) proteinase N (Serva) (Dubois and Jangoux 1985) fibres. Adradial muscle fibres are segregated in a thick and (2) regenerating spines were incubated for 15-60 min in 10% bundle, the so-called depressor muscle (Hyman 1955), (v/v) common bleach (" Eau de Javel") supersaturated with CaCO3 while abradial fibres are scattered among collagen fibres under dissecting microscope control. (This last method was used because proteinase incubation deeply etches the regenerate al- (Fig. 2). though it perfectly cleans the stereom of intact spines without any The spine skeleton is made of a single stereom unit trace of etching. After stereom cleaning, the spines were washed in which two parts can be recognized: the base and the in distilled water and air-dried. For light microscopy, cleaned spines shaft (Fig. 1). The base core is formed of labyrinthic were embedded either in Spurr's or in Petropoxy 154 (Palouse, stereom while the base lower face - viz. the area which Washington) resins and ground longitudinally using either abrasive papers of increasing gradation (250-1200) or carborundum. forms the spine/plate joint - consists of either labyrinthic Mounting was carried out using Canada balsam. For scanning stereom (insertion dimple of the depressor muscle) or electron microscopy (SEM), cleaned spines were mounted on alu- irregular perforate stereom (joint surface) (nomenclature minium stubs, coated with gold in a sputter coater and observed of stereom fabrics according to Smith 1980a). The spine with an ISI-DS 130 SEM. stereom differs sharply from the base to the shaft, chang- Histological observations were performed on spines fixed with ing abruptly from labyrinthic to fascicular (Figs. 1, 3). 3% glutaraldehyde in cacodylate buffer (0.1 M, pH 7.3) and post- The structure of the shaft stereom differs according to the considered face of the spine. On the adradial face, most thick trabeculae run parallel to the long axis of Table 1. Experimental schedule for the study of regeneration of the spine; the stereom pores are narrow and elongated, adambulacral spines in Asterias rubens Experiment Regeneration Regeneration Regeneration of fractured of fractured of removed spines spines spines (control) Figs. 1-7. Morphology of whole adambulacral spines and first Number 4 3 2 stage of regeneration of fractured spines (SEM micrographs except of asteroids 2). Abbreviations: b, base; c, concentric mineral layers; d, insertion dimple of the depressor muscle; dm, depressor muscle; e, epider- Arm size (cm) 7.8-9.0 7.6-10.0 8.3 8.7 mis; fo, fold; pc, periossicular connective tissue; po, polyhedrons; Number 125 50 125 m microspine; s, shaft; st, stroma of spines (25/arm) (10/arm) (25/arm) fractured Fig. 1. Adradial face of the skeleton (arrows, cenical thans) or removed/ Fig. 2. Semithin section of a decalcified spine jointed to its adambu- asteroid lacral plate (Ordinary microscope-OM-micrography)
Recommended publications
  • Skeletonized Microfossils from the Lower–Middle Cambrian Transition of the Cantabrian Mountains, Northern Spain
    Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain SÉBASTIEN CLAUSEN and J. JAVIER ÁLVARO Clausen, S. and Álvaro, J.J. 2006. Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain. Acta Palaeontologica Polonica 51 (2): 223–238. Two different assemblages of skeletonized microfossils are recorded in bioclastic shoals that cross the Lower–Middle Cambrian boundary in the Esla nappe, Cantabrian Mountains. The uppermost Lower Cambrian sedimentary rocks repre− sent a ramp with ooid−bioclastic shoals that allowed development of protected archaeocyathan−microbial reefs. The shoals yield abundant debris of tube−shelled microfossils, such as hyoliths and hyolithelminths (Torellella), and trilobites. The overlying erosive unconformity marks the disappearance of archaeocyaths and the Iberian Lower–Middle Cambrian boundary. A different assemblage occurs in the overlying glauconitic limestone associated with development of widespread low−relief bioclastic shoals. Their lowermost part is rich in hyoliths, hexactinellid, and heteractinid sponge spicules (Eiffelia), chancelloriid sclerites (at least six form species of Allonnia, Archiasterella, and Chancelloria), cambroclaves (Parazhijinites), probable eoconchariids (Cantabria labyrinthica gen. et sp. nov.), sclerites of uncertain af− finity (Holoplicatella margarita gen. et sp. nov.), echinoderm ossicles and trilobites. Although both bioclastic shoal com− plexes represent similar high−energy conditions, the unconformity at the Lower–Middle Cambrian boundary marks a drastic replacement of microfossil assemblages. This change may represent a real community replacement from hyolithelminth−phosphatic tubular shells to CES (chancelloriid−echinoderm−sponge) meadows. This replacement coin− cides with the immigration event based on trilobites previously reported across the boundary, although the partial infor− mation available from originally carbonate skeletons is also affected by taphonomic bias.
    [Show full text]
  • A Stem Group Echinoderm from the Basal Cambrian of China and the Origins of Ambulacraria
    ARTICLE https://doi.org/10.1038/s41467-019-09059-3 OPEN A stem group echinoderm from the basal Cambrian of China and the origins of Ambulacraria Timothy P. Topper 1,2,3, Junfeng Guo4, Sébastien Clausen 5, Christian B. Skovsted2 & Zhifei Zhang1 Deuterostomes are a morphologically disparate clade, encompassing the chordates (including vertebrates), the hemichordates (the vermiform enteropneusts and the colonial tube-dwelling pterobranchs) and the echinoderms (including starfish). Although deuter- 1234567890():,; ostomes are considered monophyletic, the inter-relationships between the three clades remain highly contentious. Here we report, Yanjiahella biscarpa, a bilaterally symmetrical, solitary metazoan from the early Cambrian (Fortunian) of China with a characteristic echinoderm-like plated theca, a muscular stalk reminiscent of the hemichordates and a pair of feeding appendages. Our phylogenetic analysis indicates that Y. biscarpa is a stem- echinoderm and not only is this species the oldest and most basal echinoderm, but it also predates all known hemichordates, and is among the earliest deuterostomes. This taxon confirms that echinoderms acquired plating before pentaradial symmetry and that their history is rooted in bilateral forms. Yanjiahella biscarpa shares morphological similarities with both enteropneusts and echinoderms, indicating that the enteropneust body plan is ancestral within hemichordates. 1 Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, 710069 Xi’an, China. 2 Department of Palaeobiology, Swedish Museum of Natural History, Box 50007104 05, Stockholm, Sweden. 3 Department of Earth Sciences, Durham University, Durham DH1 3LE, UK. 4 School of Earth Science and Resources, Key Laboratory for the study of Focused Magmatism and Giant Ore Deposits, MLR, Chang’an University, 710054 Xi’an, China.
    [Show full text]
  • Ambulacraria - Andrew B
    PHYLOGENETIC TREE OF LIFE – Ambulacraria - Andrew B. Smith AMBULACRARIA Andrew B. Smith Department of Palaeontology, The Natural History Museum, London SW7 5BD, UK Keywords: Echinoderms, crinoids, ophiuroids, asteroids, echinoids, holothurians, hemichordates, enteropneustes, pterobranchs, Xenoturbella, phylogeny, evolution, mode of life, developmental biology, fossil record, biodiversity Contents 1. General Introduction 2. The Echinodermata 2.1. General features 2.2. Crinoidea (sea lillies and feather stars) 2.3. Asteroidea (starfishes and cushion stars) 2.4. Ophiuroidea (brittlestars and basket stars) 2.5. Holothuroidea (sea cucumbers) 2.6. Echinoidea (sea urchins) 2.7. Stem group echinoderms 3. The Hemichordata 3.1. General features 3.2. Pterobranchs 3.3. Enteropneusts. 4. Plactosphaeroidea (Xenoturbella) Bibliography Bibliographical sketch Summary The Ambulacraria is a major clade of invertebrates that are the immediate sister group to the chordates. It comprises the phyla Echinodermata and Hemichordata and the puzzling genus Xenoturbella, the latter being included on the basis of its molecular similarity. The morphological characters uniting Echinodermata and Hemichordata are listed, as are those that characterize each phylum separately. The five classes of echinoderm and two classes of hemichordate are brief described, and information is provided about their mode of life, development, geological history and current views on their phylogenetic relationships. 1. General Introduction Ambulacraria is the formal name applied to a group of invertebrate animals that includes the echinoderms and hemichordates. They are exclusively marine and their origins extend back some 525 Ma to the Cambrian radiation when the earliest examples appear in the fossil record, although their actual origins probably lie slightly earlier, based on molecular clock studies.
    [Show full text]
  • Ultrastructural and Microanalytical Results from Echinoderm Calcite: Implications for Biomineralization and Diagenesis of Skeletal Material
    Micron and Microscopica Acta, Vol. 15, No. 2, pp. 85-90, 1984. 0739-6260/84 83.00+0.00 Printed in Great Britain. C) 1984 Pergamon Press Ltd. ULTRASTRUCTURAL AND MICROANALYTICAL RESULTS FROM ECHINODERM CALCITE: IMPLICATIONS FOR BIOMINERALIZATION AND DIAGENESIS OF SKELETAL MATERIAL DAVID F. BLAKE, DONALD R. PEACOR Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. and LAWRENCE F. ALLARD Department of Materials and Metallurgical Engineering, University of Michigan, Ann Arbor, MI 48109, U.S.A. (Received 9 January 1984) Abstract—Magnesian calcite skeletal elements ofthe modern crinoid echinoderm Neocrinus blakei were studied using high resolution TEM, high voltage TEM and STEM microanalysis. Unlike inorganic magnesian calcites which are compositionally heterogeneous, magnesium in these skeletal calcites is homogeneous to at least the 0.1 jim level. While a mosaic structure exists in echinoderm calcite, high voltage TEM reveals the absence of defects or dislocation features which should exist as a consequence ofthe structure. By comparison, inorganic magnesian calcites show a plethora of defects and dislocation features. High resolution lattice fringe images of the echinoderm calcite exhibit a kinking of fringes between mosaic domains, the boundaries ofwhich are largely coherent. Large scale dislocation structures are not observed. Such a ‘stressed’ lattice structure, if pervasive, explains conflicting observations concerning the ‘single crystal’ or ‘polycrystalline aggregate’ nature of echinoderm calcite. The microstructural and microchemical data demonstrate strong organismal control of skeletal deposition in Echinodermata. Both ultrastructural and compositional heterogeneity/homogeneity should be assessed when determining the susceptibility of skeletal material to diagenetic change. Index key words: Echinoderm calcite, biomineralization, analytical electron microscopy, skeletal diagenesis, magnesian calcite.
    [Show full text]
  • Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea
    animals Article Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea 1, , 1, , 2 3 Anastasios Varkoulis * y, Konstantinos Voulgaris * y, Stefanos Zaoutsos , Antonios Stratakis and Dimitrios Vafidis 1 1 Department of Ichthyology and Aquatic Environment, Nea Ionia, University of Thessaly, 38445 Volos, Greece; dvafi[email protected] 2 Department of Energy Systems, University of Thessaly, 41334 Larisa, Greece; [email protected] 3 School of Mineral Resources Engineering, Crete Technical University of Crete, 73100 Chania, Greece; [email protected] * Correspondence: [email protected] (A.V.); [email protected] (K.V.) These authors contributed equally to this work. y Received: 19 June 2020; Accepted: 2 August 2020; Published: 4 August 2020 Simple Summary: Arbacia lixula, Paracentrotus lividus and Sphaerechinus granularis play a key role in many sublittoral biocommunities of the Mediterranean Sea. However, their skeletons seem to differ, both morphologically and in chemical composition. Thus, the skeletal elements display different properties, which are affected not only by the environment, but also by the vital effect of each species. We studied the microstructural morphology and crystalline phase of the test and spines, while also examining the effect of time on their elemental composition. Results showed morphologic differences among the three species both in spines and tests. They also seem to respond differently to possible time-related changes. The mineralogical composition of P.lividus appears to be quite different compare to the other two species. The results of the present study may contribute to a better understanding of the skeletal properties of these species, this being especially useful in predicting the effects of ocean acidification.
    [Show full text]
  • Middle Ordovician) of Västergötland, Sweden - Faunal Composition and Applicability As Environmental Proxies
    Microscopic echinoderm remains from the Darriwilian (Middle Ordovician) of Västergötland, Sweden - faunal composition and applicability as environmental proxies Christoffer Kall Dissertations in Geology at Lund University, Bachelor’s thesis, no 403 (15 hp/ECTS credits) Department of Geology Lund University 2014 Microscopic echinoderm remains from the Darriwilian (Middle Ordovician) of Västergötland, Sweden - faunal composition and applicability as environmental proxies Bachelor’s thesis Christoffer Kall Department of Geology Lund University 2014 Contents 1 Introduction ......................................................................................................................................................... 7 1.1 The Ordovician world and faunas 8 1.2 Phylum Echinodermata 8 1.3 Ordovician echinoderms 9 1.3.1 Asterozoans, 1.3.2 Blastozoans 9 1.3.3 Crinoids 10 1.3.4 Echinozoans 10 1.3.4.1 Echinoidea, 1.3.4.2 Holothuroidea, 1.3.4.3 Ophiocistoidea,…., 1.3.4.6 Stylophorans 10 1.4 Pelmatozoan morphology 10 2 Geologocal setting ............................................................................................................................................. 11 3 Materials and methods ..................................................................................................................................... 13 4 Results ................................................................................................................................................................ 14 4.1 Morphotypes 15 4.1.1 Morphotype
    [Show full text]
  • Antarctic Urchin Ctenocidaris Speciosa Spines: Lessons from the Deep
    Cali. Biol. Mar. (2013) 54 : 649-655 Antarctic urchin Ctenocidaris speciosa spines: lessons from the deep Ana I. CATARINO1, Virginie GUIBOURT1, Claire MOUREAUX1, Chantai DE RIDDER1, Philippe COMPERE2 and Philippe DUBOIS1 H) Laboratoire de Biologie Marine, Université Libre de Bruxelles, CP 160/10; av FD Roosevelt 50; 1050 Brussels, Belgium. Telephone: +32-2-650.29.70, fax: +32-2-650.27.96, E-mail:[email protected] O) Département des Sciences et Gestion de IEnvironnement, Université de Liège, Bât. B6c, allée du 6 Août 10; 4000 Liège, Belgium Abstract: Ocean acidification is leading to changes in the oceanic carbonate system. As a result, calcium carbonate saturation horizon is shallowing, especially at high latitudes. Biogenic high magnesium-calcites could be particularly vulnerable, since their solubility is either similar or greater than that of aragonite. Cidaroid urchins have magnesium-calcite spines covered by a polycrystalline cortex which becomes exposed to seawater when mature (not covered by an epidermis). However, deep species live at low calcium carbonate saturation states, especially at high latitudes. We describe here the morphology and the magnesium content of Ctenocidaris speciosa spines collected at different depths from the Weddell Sea (Antarctica) and relate the features with seawater calcium carbonate saturation. We observed that the spines cortex of C. speciosa presented a thicker inner cortex layer and a lower [Mg2+] below the aragonite saturation horizon. We suggest that the cortex of cidaroid spines is able to resist to low calcium carbonate saturation state. Résumé : Les épines de l ’oursin antarctique Ctenocidaris speciosa : leçons venues des profondeurs. L’acidification des océans apporte des changements dans le système des carbonates de l’eau de mer.
    [Show full text]
  • Strength and Toughness of Bio-Fusion Materials
    Polymer Journal (2015) 47, 99–105 & 2015 The Society of Polymer Science, Japan (SPSJ) All rights reserved 0032-3896/15 www.nature.com/pj FOCUS REVIEW Strength and toughness of bio-fusion materials Ko Okumura In nature, there are many strong and tough biomaterials that result from the fusion of soft and hard elements. These materials include nacre, crustacean exoskeletons and spider webs. Here, we review previous studies on such bio-fusion materials, emphasizing the importance of simple models to gain a physical understanding of the emergence of strength and toughness from these structures. Thus, a simple understanding obtained through biologically inspired models provides useful guiding principles for the development of artificial tough composites by mimicking biomaterials. Polymer Journal (2015) 47, 99–105; doi:10.1038/pj.2014.97; published online 5 November 2014 INTRODUCTION of a monolith of the hard element.6 In recent years, more detailed Various animals and plants in nature have developed strong and tough substructures have been found.24–26 materials, often with magnificent hierarchical structures.1–4 Nacre, a There has been a controversy regarding the elastic behavior of glittering layer found on the surface of pearls or inside certain nacre’s soft element. The estimation of the modulus ranges from seashells, is one such example: hard layers are glued together by thin 4GPa6 to 100 Pa.27 However, the soft protein-based elements have soft adhesive sheets,5 which results in remarkable strength and been observed to behave like gels.5
    [Show full text]
  • Biological Control of Skeleton Properties in Echinoderms
    Echinoderm Research, De Ridder. Dubois, Lahaye & Jangoux (eds) 0 1990 Balkema, Rotterdam. ISBN 90 6191 141 9 Biological control of skeleton properties in echinoderms Ph. Dubois* Laboratoire de Biologie marine (CP 160), Universitd Libre de Bnucelles, Bnucelles, Belgique ABSTRACT: Echinoderms have a high-magnesium calcite skeleton whose cristallographic, chemical, and morphological properties make it different from abiotic calcites. The available data show that the single crystal behaviour, the conchoidal fracture properties, the high-magnesium content, and the stereom structure could be partly explained by the properties of the organic nacromolecules associated with the mineral phase. Data suzest that these compounds could produce the stereom properties through stereochemical interactions with calcite. of CaC03 and MgC03 in a calcite lattice. i.e. a high-magnesium calcite (Chave Echinoderms have a calcitic skeleton of 1952). The RgC03 content ranges from 3.0 mesodermal origin. This skeleton is to 43.5 mole?/, (Schroeder et al. 1969) developed by most postmetamorphic and averages 13.5-16.2 mole% according individuals as well as by larvae of to the class considered (V!eber 1969). echinoids and ophiuroids. The growing Such a concentration would make evidence indicates that the echinoderm skeleton metastable in postmetamorphic and larval skeletons are standard inorganic temperature/ pressure homologous structures (see Emlet 1985, conditions (Lerman 1965). Parks et al. 1987, Drager et al. 1989, Most single ossicles show properties Dubois 6r Chen 1989, Richardson et al. of light polarization and X-ray 1989). The echinoderm skeleton may be diffraction as though they were carved considered as a paradigm of biologically out of a single crystal of calcite even controlled mineralized structures (I.:ann when they are several centimetres in et al.
    [Show full text]
  • Potential Effects of Ocean Acidification on Cold-Water Marine Invertebrates
    Potential Effects of Ocean Acidification on Cold-Water Marine Invertebrates by © Katie Helena Verkaik A thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the degree of Master of Science in Marine Biology Department of Ocean Sciences Memorial University August 2015 St. John’s, Newfoundland and Labrador Abstract Anthropogenic emissions of carbon dioxide are causing an overall decrease of ocean pH, now termed ocean acidification (OA). This change in water chemistry has potentially dire implications for organisms living in marine environments, especially at high latitudes where carbonate saturation states are already low. OA has been shown to affect processes such as calcification, physiology, reproduction and development, with species-specific differences being observed. The goal of the present study was to better understand the effects of OA on weakly calcifying, cold-water species with lecitotrophic larvae, using the sea cucumber Cucumaria frondosa. In addition, it aimed to gain information on how OA might affect deep-sea organisms, using the hermaphroditic polychaete Ophryotrocha sp. Focal species were exposed to a ~0.4 unit decrease in pH for 19-26 weeks using a realistic flow-through system. I then investigated the reproductive output of each species, as well as its behaviour, spawning, larval development and calcification. Lipid and fatty acid profiles were also examined in C. frondosa. Findings varied between the two species. Gamete synthesis was disrupted by low pH in C. frondosa. Consequently, mature oocytes exhibited morphological discrepancies and negative buoyancy, leading to high embryonic mortality. Skeletal ossicles were affected in terms of abundance, microstructural appearance and chemical composition.
    [Show full text]
  • 2540 Organic Matrix-Related Mineralization of Sea Urchin
    [Frontiers in Bioscience 16, 2540-2560, June 1, 2011] Organic Matrix-related mineralization of sea urchin spicules, spines, test and teeth Arthur Veis Feinberg School of Medicine, Northwestern University, Department of Cell and Molecular Biology, 303 E. Chicago Avenue, Chicago Illinois, USA TABLE OF CONTENTS 1. Abstract 2. Introduction 3. Body plan and skeletal elements of the mature echinoid, Lytechinus variegatus (Lv) 3.1. Teeth and masticatory structure 3.2. Spines and body wall 3.3. Pluteus and embryonic spicule formation 4. Protein components of the sea urchin skeletal elements and biomineralization 5. Biochemical and immunological identification of mineralization related proteins 6. Categorizing the mineralization-related genomic sequences 7. The potential role of phosphopeptides in calcite mineralization processes 8. Prospects for the future 9. Acknowledgements 10. References 1. ABSTRACT 2. INTRODUCTION The camarodont echinoderms have five distinct Echinoderms have long been a subject of study of mineralized skeletal elements: embryonic spicules, mature special interest to students of genetics and developmental test, spines, lantern stereom and teeth. The spicules are biology and an extensive literature has been developed. In transient structural elements whereas the spines, and test 2006 the Sea Urchin Sequencing Consortium (1) published plates are permanent. The teeth grow continuously. The the complete genome of the Strongylocentrotus purpuratus. mineral is a high magnesium calcite, but the magnesium While most of the genes were involved with the content is different in each type of skeletal element, varying developmental, metabolic and immunological aspects of from 5 to 40 mole% Mg. The organic matrix creates the functions of the urchins, several hundred genes were spaces and environments for crystal initiation and growth.
    [Show full text]
  • Stereom Microstructures of Cambrian Echinoderms Revealed by Cathodoluminescence (CL)
    Palaeontologia Electronica palaeo-electronica.org Stereom microstructures of Cambrian echinoderms revealed by cathodoluminescence (CL) Przemysław Gorzelak and Samuel Zamora ABSTRACT Echinoderms possess a skeleton with a unique and distinctive meshlike micro- structure called stereom that is underpinned by a specific family of genes. Stereom is thus considered the major echinoderm synapomorphy and is recognized already in some Cambrian echinoderm clades. However, data on the skeletal microstructures of early echinoderms are still sparse and come only from isolated ossicles of limited taxo- nomic value in which the primary calcium carbonate has been replaced or thinly coated by phosphates, silica or iron oxides. Here, we applied cathodoluminescence (CL) to reveal stereom microstructures of the diagenetically altered calcitic skeletons of some Cambrian echinoderms (in particu- lar Protocinctus, Stromatocystites and Dibrachicystidae). CL not only provides insights into the diagenesis of their skeletons but also reveals primary microstructural details that are not visible under transmitted light or SEM. Different stereom types (resembling labyrinthic, fascicular, galleried, microperforate and imperforate microfabrics) compara- ble to those observed in extant echinoderms have been recognized for the first time in these Cambrian taxa. Our results show that the stereom microstructures widely occur in various Cambrian echinoderm clades which suggest that they likely evolved the same genetically controlled biomineralization mechanisms as those observed in mod- ern echinoderms. These results underline that the CL technique can be a powerful tool in the detec- tion of the microstructural organization in even severely recrystallized echinoderm specimens. Given the close association between the skeletal microstructure and the investing soft tissues, the method presented here opens new possibilites for revealing skeletal growth and soft tissue palaeoanatomy of fossil echinoderms.
    [Show full text]