The Origin and Homology of the Jointed Appendages of Carpoid and Pelmatozoan Echinoderms
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Zamora, S., Rahman, IA, & Smith, AB (2012). Plated Cambrian
Zamora, S., Rahman, I. A., & Smith, A. B. (2012). Plated Cambrian bilaterians reveal the earliest stages of echinoderm evolution. PLoS ONE, 7(6), [e38296]. https://doi.org/10.1371/journal.pone.0038296 Publisher's PDF, also known as Version of record Link to published version (if available): 10.1371/journal.pone.0038296 Link to publication record in Explore Bristol Research PDF-document University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Plated Cambrian Bilaterians Reveal the Earliest Stages of Echinoderm Evolution Samuel Zamora1, Imran A. Rahman2, Andrew B. Smith1* 1 Department of Palaeontology, The Natural History Museum, London, United Kingdom, 2 School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, United Kingdom Abstract Echinoderms are unique in being pentaradiate, having diverged from the ancestral bilaterian body plan more radically than any other animal phylum. This transformation arises during ontogeny, as echinoderm larvae are initially bilateral, then pass through an asymmetric phase, before giving rise to the pentaradiate adult. Many fossil echinoderms are radial and a few are asymmetric, but until now none have been described that show the original bilaterian stage in echinoderm evolution. Here we report new fossils from the early middle Cambrian of southern Europe that are the first echinoderms with a fully bilaterian body plan as adults. Morphologically they are intermediate between two of the most basal classes, the Ctenocystoidea and Cincta. -
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. -
Progress in Echinoderm Paleobiology
Journal of Paleontology, 91(4), 2017, p. 579–581 Copyright © 2017, The Paleontological Society 0022-3360/17/0088-0906 doi: 10.1017/jpa.2017.20 Progress in echinoderm paleobiology Samuel Zamora1,2 and Imran A. Rahman3 1Instituto Geológico y Minero de España (IGME), C/Manuel Lasala, 44, 9ºB, 50006, Zaragoza, Spain 〈[email protected]〉 2Unidad Asociada en Ciencias de la Tierra, Universidad de Zaragoza-IGME, Zaragoza, Spain 3Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, United Kingdom 〈[email protected]〉 Echinoderms are a diverse and successful phylum of exclusively Universal elemental homology (UEH) has proven to be one marine invertebrates that have an extensive fossil record dating of the most powerful approaches for understanding homology back to Cambrian Stage 3 (Zamora and Rahman, 2014). There in early pentaradial echinoderms (Sumrall, 2008, 2010; Sumrall are five extant classes of echinoderms (asteroids, crinoids, and Waters, 2012; Kammer et al., 2013). This hypothesis echinoids, holothurians, and ophiuroids), but more than 20 focuses on the elements associated with the oral region, extinct groups, all of which are restricted to the Paleozoic identifying possible homologies at the level of specific plates. (Sumrall and Wray, 2007). As a result, to fully appreciate the Two papers, Paul (2017) and Sumrall (2017), deal with the modern diversity of echinoderms, it is necessary to study their homology of plates associated with the oral area in early rich fossil record. pentaradial echinoderms. The former contribution describes and Throughout their existence, echinoderms have been an identifies homology in various ‘cystoid’ groups and represents a important component of marine ecosystems. -
PROGRAMME ABSTRACTS AGM Papers
The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important. -
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). -
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. -
Reply to €˜Re-Evaluating the Phylogenetic Position
MATTERS ARISING https://doi.org/10.1038/s41467-020-14922-9 OPEN Reply to ‘Re-evaluating the phylogenetic position of the enigmatic early Cambrian deuterostome Yanjiahella’ ✉ Timothy P. Topper1,2 , Junfeng Guo3, Sébastien Clausen 4, Christian B. Skovsted2 & Zhifei Zhang 1 REPLYING TO Zamora, et al. Nature Communications https://doi.org/10.1038/s41467-020-14920-x (2020) ecently we documented a bilaterally symmetrical, solitary not detectable using light photography and SEM, as predicted. The 2 1234567890():,; organism, Yanjiahella biscarpa from the early Cambrian statement from Zamora et al. that latex casting could have R 1 (Fortunian) of China . We interpreted that Y. biscarpa resolved many of the uncertainties surrounding the composition, possessed an echinoderm-like plated theca, a muscular stalk shape and arrangement of the plates and the morphology of the similar to hemichordates and a pair of long, feeding appendages. stalk is an overstatement and ambitiously delivered without direct Our interpretation and our phylogenetic analysis suggest that examination of the fossil specimens. Y. biscarpa is a stem-echinoderm, which would confirm that The stereom microstructure of Cambrian echinoderms is poorly echinoderms acquired plates before pentaradial symmetry and known5, as the majority of specimens are preserved as moulds, or that their history is firmly rooted in bilateral forms. Zamora et al.2 recrystallized skeletons and the primary three-dimensional mor- however, have criticized our interpretation, arguing against an phology of their stereom has been obscured4–6. Generally, only echinoderm affinity, instead suggesting that the phylogenetic superficial pitting is preserved and it is this pitting that is inter- placement of Y. -
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). -
The Genetic Factors of Bilaterian Evolution Peter Heger1*, Wen Zheng1†, Anna Rottmann1, Kristen a Panfilio2,3, Thomas Wiehe1
RESEARCH ARTICLE The genetic factors of bilaterian evolution Peter Heger1*, Wen Zheng1†, Anna Rottmann1, Kristen A Panfilio2,3, Thomas Wiehe1 1Institute for Genetics, Cologne Biocenter, University of Cologne, Cologne, Germany; 2Institute for Zoology: Developmental Biology, Cologne Biocenter, University of Cologne, Cologne, Germany; 3School of Life Sciences, University of Warwick, Gibbet Hill Campus, Coventry, United Kingdom Abstract The Cambrian explosion was a unique animal radiation ~540 million years ago that produced the full range of body plans across bilaterians. The genetic mechanisms underlying these events are unknown, leaving a fundamental question in evolutionary biology unanswered. Using large-scale comparative genomics and advanced orthology evaluation techniques, we identified 157 bilaterian-specific genes. They include the entire Nodal pathway, a key regulator of mesoderm development and left-right axis specification; components for nervous system development, including a suite of G-protein-coupled receptors that control physiology and behaviour, the Robo- Slit midline repulsion system, and the neurotrophin signalling system; a high number of zinc finger transcription factors; and novel factors that previously escaped attention. Contradicting the current view, our study reveals that genes with bilaterian origin are robustly associated with key features in extant bilaterians, suggesting a causal relationship. *For correspondence: [email protected] Introduction The taxon Bilateria consists of multicellular animals