Symmetry of Echinoderms: from Initial Bilaterally-Asymmetric Metamerism to Pentaradiality
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Conservation and Diversification of Appendage Identity Specification Mechanisms Along the Anteroposterior and Proximodistal Axes in Panarthropoda Frank W
University of Connecticut OpenCommons@UConn Doctoral Dissertations University of Connecticut Graduate School 8-23-2013 Conservation and Diversification of Appendage Identity Specification Mechanisms Along the Anteroposterior and Proximodistal Axes in Panarthropoda Frank W. Smith III University of Connecticut, [email protected] Follow this and additional works at: https://opencommons.uconn.edu/dissertations Recommended Citation Smith, Frank W. III, "Conservation and Diversification of Appendage Identity Specification Mechanisms Along the Anteroposterior and Proximodistal Axes in Panarthropoda" (2013). Doctoral Dissertations. 161. https://opencommons.uconn.edu/dissertations/161 Conservation and Diversification of Appendage Identity Specification Mechanisms Along the Anteroposterior and Proximodistal Axes in Panarthropoda Frank Wesley Smith III, PhD University of Connecticut, 2013 A key characteristic of arthropods is their diverse serially homologous segmented appendages. This dissertation explores diversification of these appendages, and the developmental mechanisms producing them. In Chapter 1, the roles of genes that specify antennal identity in Drosophila melanogaster were investigated in the flour beetle Tribolium castaneum. Antenna-to-leg transformations occurred in response to RNA interference (RNAi) against homothorax, extradenticle, spineless and Distal-less. However, for homothorax/extradenticle RNAi, the extent of transformation along the proximodistal axis differed between embryogenesis and metamorphosis. This suggests that distinct mechanisms specify antennal identity during flour beetle embryogenesis and metamorphosis and leads to a model for the evolution of the Drosophila antennal identity mechanism. Homothorax/Extradenticle acquire many of their identity specification roles by acting as Hox cofactors. In chapter 2, the metamorphic roles of the Hox genes, extradenticle, and homothorax were compared in T. castaneum. homothorax/extradenticle RNAi and Hox RNAi produced similar body wall phenotypes but different appendage phenotypes. -
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). -
Stages of Embryonic Development of the Zebrafish
DEVELOPMENTAL DYNAMICS 2032553’10 (1995) Stages of Embryonic Development of the Zebrafish CHARLES B. KIMMEL, WILLIAM W. BALLARD, SETH R. KIMMEL, BONNIE ULLMANN, AND THOMAS F. SCHILLING Institute of Neuroscience, University of Oregon, Eugene, Oregon 97403-1254 (C.B.K., S.R.K., B.U., T.F.S.); Department of Biology, Dartmouth College, Hanover, NH 03755 (W.W.B.) ABSTRACT We describe a series of stages for Segmentation Period (10-24 h) 274 development of the embryo of the zebrafish, Danio (Brachydanio) rerio. We define seven broad peri- Pharyngula Period (24-48 h) 285 ods of embryogenesis-the zygote, cleavage, blas- Hatching Period (48-72 h) 298 tula, gastrula, segmentation, pharyngula, and hatching periods. These divisions highlight the Early Larval Period 303 changing spectrum of major developmental pro- Acknowledgments 303 cesses that occur during the first 3 days after fer- tilization, and we review some of what is known Glossary 303 about morphogenesis and other significant events that occur during each of the periods. Stages sub- References 309 divide the periods. Stages are named, not num- INTRODUCTION bered as in most other series, providing for flexi- A staging series is a tool that provides accuracy in bility and continued evolution of the staging series developmental studies. This is because different em- as we learn more about development in this spe- bryos, even together within a single clutch, develop at cies. The stages, and their names, are based on slightly different rates. We have seen asynchrony ap- morphological features, generally readily identi- pearing in the development of zebrafish, Danio fied by examination of the live embryo with the (Brachydanio) rerio, embryos fertilized simultaneously dissecting stereomicroscope. -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Reinterpretation of the Enigmatic Ordovician Genus Bolboporites (Echinodermata)
Reinterpretation of the enigmatic Ordovician genus Bolboporites (Echinodermata). Emeric Gillet, Bertrand Lefebvre, Véronique Gardien, Emilie Steimetz, Christophe Durlet, Frédéric Marin To cite this version: Emeric Gillet, Bertrand Lefebvre, Véronique Gardien, Emilie Steimetz, Christophe Durlet, et al.. Reinterpretation of the enigmatic Ordovician genus Bolboporites (Echinodermata).. Zoosymposia, Magnolia Press, 2019, 15 (1), pp.44-70. 10.11646/zoosymposia.15.1.7. hal-02333918 HAL Id: hal-02333918 https://hal.archives-ouvertes.fr/hal-02333918 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Reinterpretation of the Enigmatic Ordovician Genus Bolboporites 2 (Echinodermata) 3 4 EMERIC GILLET1, BERTRAND LEFEBVRE1,3, VERONIQUE GARDIEN1, EMILIE 5 STEIMETZ2, CHRISTOPHE DURLET2 & FREDERIC MARIN2 6 7 1 Université de Lyon, UCBL, ENSL, CNRS, UMR 5276 LGL-TPE, 2 rue Raphaël Dubois, F- 8 69622 Villeurbanne, France 9 2 Université de Bourgogne - Franche Comté, CNRS, UMR 6282 Biogéosciences, 6 boulevard 10 Gabriel, F-2100 Dijon, France 11 3 Corresponding author, E-mail: [email protected] 12 13 Abstract 14 Bolboporites is an enigmatic Ordovician cone-shaped fossil, the precise nature and systematic affinities of 15 which have been controversial over almost two centuries. -
First Record of the Colonial Ascidian Didemnum Vexillum Kott, 2002 in the Mediterranean: Lagoon of Venice (Italy)
BioInvasions Records (2012) Volume 1, Issue 4: 247–254 Open Access doi: http://dx.doi.org/10.3391/bir.2012.1.4.02 © 2012 The Author(s). Journal compilation © 2012 REABIC Research Article First record of the colonial ascidian Didemnum vexillum Kott, 2002 in the Mediterranean: Lagoon of Venice (Italy) Davide Tagliapietra1*, Erica Keppel1, Marco Sigovini1 and Gretchen Lambert2 1 CNR - National Research Council of Italy, ISMAR - Marine Sciences Institute, Arsenale - Tesa 104, Castello 2737/F, I-30122 Venice, Italy 2 University of Washington Friday Harbor Laboratories, Friday Harbor, WA 98250. Mailing address: 12001 11th Ave. NW, Seattle, WA 98177, USA E-mail: [email protected] (DT), [email protected] (EK), [email protected] (MS), [email protected] (GL) *Corresponding author Received: 30 July 2012 / Accepted: 16 October 2012 / Published online: 23 October 2012 Abstract Numerous colonies of the invasive colonial ascidian Didemnum vexillum Kott, 2002 have been found in the Lagoon of Venice (Italy) in 2012, overgrowing fouling organisms on maritime structures such as docks, pilings, and pontoons. This is the first record for the Mediterranean Sea. A survey conducted in July 2012 revealed that D. vexillum is present in the euhaline and tidally well flushed zones of the lagoon, whereas it was absent at the examined estuarine tracts and at the zones surrounding the saltmarshes. Suitable climatic, physiographic and saline features together with a high volume of international maritime traffic make the Lagoon of Venice a perfect hub for the successful introduction of temperate non-native species. Key words: Didemnum vexillum, Mediterranean, Lagoon of Venice, ascidian, fouling, marinas, invasive species Introduction cold coasts of North America and Europe as well as from Japan where it is probably native Didemnum vexillum Kott, 2002 (Ascidiacea: (Bullard et al. -
Metamerism in Cephalochordates and the Problem of the Vertebrate Head TAKAYUKI ONAI*,1,2, NORITAKA ADACHI1 and SHIGERU KURATANI1
Int. J. Dev. Biol. 61: 621-632 (2017) doi: 10.1387/ijdb.170121to www.intjdevbiol.com Metamerism in cephalochordates and the problem of the vertebrate head TAKAYUKI ONAI*,1,2, NORITAKA ADACHI1 and SHIGERU KURATANI1 1Evolutionary Morphology Laboratory, RIKEN center for Developmental Biology, Chuo-ku, Kobe, Japan and 2Department of Anatomy, School of Medical Sciences, University of Fukui, Matsuokashimoaizuki, Japan ABSTRACT The vertebrate head characteristically exhibits a complex pattern with sense organs, brain, paired eyes and jaw muscles, and the brain case is not found in other chordates. How the extant vertebrate head has evolved remains enigmatic. Historically, there have been two conflicting views on the origin of the vertebrate head, segmental and non-segmental views. According to the segmentalists, the vertebrate head is organized as a metameric structure composed of segments equivalent to those in the trunk; a metamere in the vertebrate head was assumed to consist of a somite, a branchial arch and a set of cranial nerves, considering that the head evolved from rostral segments of amphioxus-like ancestral vertebrates. Non-segmentalists, however, considered that the vertebrate head was not segmental. In that case, the ancestral state of the vertebrate head may be non-segmented, and rostral segments in amphioxus might have been secondarily gained, or extant vertebrates might have evolved through radical modifications of amphioxus-like ancestral vertebrate head. Comparative studies of mesodermal development in amphioxus and vertebrate gastrula embryos have revealed that mesodermal gene expressions become segregated into two domains anteroposteriorly to specify the head mesoderm and trunk mesoderm only in vertebrates; in this segregation, key genes such as delta and hairy, involved in segment formation, are expressed in the trunk mesoderm, but not in the head mesoderm, strongly suggesting that the head meso- derm of extant vertebrates is not segmented. -
The Weeks Formation Konservat-Lagerstätte and the Evolutionary Transition of Cambrian Marine Life
Downloaded from http://jgs.lyellcollection.org/ by guest on October 1, 2021 Review focus Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2018-042 The Weeks Formation Konservat-Lagerstätte and the evolutionary transition of Cambrian marine life Rudy Lerosey-Aubril1*, Robert R. Gaines2, Thomas A. Hegna3, Javier Ortega-Hernández4,5, Peter Van Roy6, Carlo Kier7 & Enrico Bonino7 1 Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, NSW 2351, Australia 2 Geology Department, Pomona College, Claremont, CA 91711, USA 3 Department of Geology, Western Illinois University, 113 Tillman Hall, 1 University Circle, Macomb, IL 61455, USA 4 Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 6 Department of Geology, Ghent University, Krijgslaan 281/S8, B-9000 Ghent, Belgium 7 Back to the Past Museum, Carretera Cancún, Puerto Morelos, Quintana Roo 77580, Mexico R.L.-A., 0000-0003-2256-1872; R.R.G., 0000-0002-3713-5764; T.A.H., 0000-0001-9067-8787; J.O.-H., 0000-0002- 6801-7373 * Correspondence: [email protected] Abstract: The Weeks Formation in Utah is the youngest (c. 499 Ma) and least studied Cambrian Lagerstätte of the western USA. It preserves a diverse, exceptionally preserved fauna that inhabited a relatively deep water environment at the offshore margin of a carbonate platform, resembling the setting of the underlying Wheeler and Marjum formations. However, the Weeks fauna differs significantly in composition from the other remarkable biotas of the Cambrian Series 3 of Utah, suggesting a significant Guzhangian faunal restructuring. -
Filogranula Cincta (Goldfuss, 1831), a Serpulid Worm (Polychaeta, Sedentaria, Serpulidae) from the Bohemian Cretaceous Basin
SBORNÍK NÁRODNÍHO MUZEA V PRAZE ACTA MUSEI NATIONALIS PRAGAE Řada B – Přírodní vědy • sv. 71 • 2015 • čís. 3–4 • s. 293–300 Series B – Historia Naturalis • vol. 71 • 2015 • no. 3–4 • pp. 293–300 FILOGRANULA CINCTA (GOLDFUSS, 1831), A SERPULID WORM (POLYCHAETA, SEDENTARIA, SERPULIDAE) FROM THE BOHEMIAN CRETACEOUS BASIN TOMÁŠ KOČÍ Department of Palaeontology, Natural History Museum, National Museum, Václavské náměstí 68, 115 79 Praha 1, the Czech Republic; Ivančická 581, Praha 9 – Letňany 199 00, the Czech Republic; e-mail: [email protected] MANFRED JÄGER Lindenstrasse 53, D-72348 Rosenfeld, Germany; e-mail: [email protected] Kočí, T., Jäger, M. (2015): Filogranula cincta (GOLDFUSS, 1831), a serpulid worm (Polychaeta, Sedentaria, Serpulidae) from the Bohemian Cretaceous Basin. – Acta Mus. Nat. Pragae, Ser. B Hist. Nat., 71(3-4): 293–300, Praha. ISSN 1804-6479. Abstract. Tubes of the serpulid worm Filogranula cincta (GOLDFUSS, 1831) were found in several rocky coast facies and other nearshore / shallow water localities in the Bohemian Cretaceous Basin ranging in geological age from the Late Cenomanian to the Late Turonian. A mor - phological description, discussion regarding systematics and taxonomy and notes on palaeoecology and stratigraphy are presented. ■ Late Cretaceous, Polychaeta, Filogranula, Serpulidae, Palaeoecology Received April 24, 2015 Issued December, 2015 Introduction any Filogranula cincta specimen. It seems that, apart from the vague mention from Strehlen by Wegner (1913), for more Filogranula cincta (GOLDFUSS, 1831) is a small and than a hundred years no additional finds of Filogranula inconspicuous but nevertheless common serpulid species in cincta from the BCB had been published until the present the Bohemian Cretaceous Basin (BCB). -
Lifestyle of the Octoradiate Eoandromeda in the Ediacaran
Lifestyle of the Octoradiate Eoandromeda in the Ediacaran Authors: Wang, Ye, Wang, Yue, Tang, Feng, Zhao, Mingsheng, and Liu, Pei Source: Paleontological Research, 24(1) : 1-13 Published By: The Palaeontological Society of Japan URL: https://doi.org/10.2517/2019PR001 BioOne Complete (complete.BioOne.org) is a full-text database of 200 subscribed and open-access titles in the biological, ecological, and environmental sciences published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Complete website, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/terms-of-use. Usage of BioOne Complete content is strictly limited to personal, educational, and non - commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Downloaded From: https://bioone.org/journals/Paleontological-Research on 15 Feb 2020 Terms of Use: https://bioone.org/terms-of-use Access provided by Bing Search Engine Paleontological Research, vol. 24, no. 1, pp. 1–13, JanuaryEoandromeda 1, 2020 ’s Lifestyle 1 © by the Palaeontological Society of Japan doi:10.2517/2019PR001 Lifestyle of the Octoradiate Eoandromeda in the Ediacaran YE WANG1, YUE WANG1, FENG TANG2, MINGSHENG ZHAO3 and PEI LIU1 1Resource and Environmental Engineering College, Guizhou University, Huanx 550025, Guiyang, Guizhou, China (e-mail: [email protected]) 2Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Street 100037, Beijing, China 3College of Paleontology, Shenyang Normal Univeristy, 253 Huanhe N Street 110034, Shengyang, Liaoning, China Received May 14, 2018; Revised manuscript accepted January 26, 2019 Abstract. -
Quantitative Study of Developmental Biology Confirms Dickinsonia As a Metazoan
1 Quantitative study of developmental biology confirms Dickinsonia 2 as a metazoan 3 4 Renee S. Hoekzema a,b,1, Martin D. Brasier b,†, Frances S. Dunn c,d, and Alexander G. Liuc,e,1 5 6 a Department of Mathematics, University of Oxford, Radcliffe Observatory Quarter, 7 Woodstock Road, Oxford, OX2 6GG, UK. 8 b Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, 9 UK. 10 c School of Earth Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, 11 Bristol, BS8 1TQ, UK. 12 d British Geological Survey, Nicker Hill, Keyworth, NG12 5GG, UK. 13 e Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 14 3EQ, UK. 15 1To whom correspondence may be addressed. Email: [email protected] or 16 [email protected] 17 † Deceased. 18 19 Keywords. Metazoan evolution, bilaterian, Ediacaran, development, ontogeny 20 The late Ediacaran soft-bodied macro-organism Dickinsonia (age range ~560–550Ma) 21 has often been interpreted as an early animal, and is increasingly invoked in debate on 22 the evolutionary assembly of eumetazoan bodyplans. However, conclusive positive 23 evidence in support of such a phylogenetic affinity has not been forthcoming. Here we 24 subject a collection of Dickinsonia specimens interpreted to represent multiple 25 ontogenetic stages to a novel, quantitative method for studying growth and development 26 in organisms with an iterative bodyplan. Our study demonstrates that Dickinsonia grew 27 via pre-terminal ‘deltoidal’ insertion and inflation of constructional units, followed by a 28 later inflation-dominated phase of growth. -
The Cambrian Substrate Revolution and the Early Evolution of Attachment in MARK Suspension-Feeding Echinoderms
Earth-Science Reviews 171 (2017) 478–491 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev The Cambrian Substrate Revolution and the early evolution of attachment in MARK suspension-feeding echinoderms ⁎ Samuel Zamoraa,b, , Bradley Delinec, J. Javier Álvarod, Imran A. Rahmane a Instituto Geológico y Minero de España, C/Manuel Lasala, 44, 9B, Zaragoza 50006, Spain b Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington DC 20013-7012, USA c University of West Georgia, Carrollton, GA, USA d Instituto de Geociencias (CSIC-UCM), c/José Antonio Novais 12, 28040 Madrid, Spain e Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, UK ARTICLE INFO ABSTRACT Keywords: The Cambrian, characterized by the global appearance of diverse biomineralized metazoans in the fossil record Palaeoecology for the first time, represents a pivotal point in the history of life. This period also documents a major change in Evolution the nature of the sea floor: Neoproterozoic-type substrates stabilized by microbial mats were replaced by un- fl Sea oor consolidated soft substrates with a well-developed mixed layer. The effect of this transition on the ecology and Attachment evolution of benthic metazoans is termed the Cambrian Substrate Revolution (CSR), and this is thought to have impacted greatly on early suspension-feeding echinoderms in particular. According to this paradigm, most echinoderms rested directly on non-bioturbated soft substrates as sediment attachers and stickers during the Cambrian Epoch 2. As the substrates became increasingly disturbed by burrowing, forming a progressively thickening mixed layer, echinoderms developed new strategies for attaching to firm and hard substrates.