Re-Evaluating the Phylogenetic Position of the Enigmatic Early Cambrian Deuterostome Yanjiahella

Total Page:16

File Type:pdf, Size:1020Kb

Re-Evaluating the Phylogenetic Position of the Enigmatic Early Cambrian Deuterostome Yanjiahella Re-evaluating the phylogenetic position of the enigmatic early Cambrian deuterostome Yanjiahella. Samuel Zamora, David F. Wright, Rich Mooi, Bertrand Lefebvre, Thomas E. Guensburg, Przemyslaw Gorzelak, Bruno David, Colin D. Sumrall, Selina R. Cole, Aaron W. Hunter, et al. To cite this version: Samuel Zamora, David F. Wright, Rich Mooi, Bertrand Lefebvre, Thomas E. Guensburg, et al.. Re-evaluating the phylogenetic position of the enigmatic early Cambrian deuterostome Yanjiahella.. Nature Communications, Nature Publishing Group, 2020, 11 (1), pp.1286. 10.1038/s41467-019-09059- 3. hal-02520490 HAL Id: hal-02520490 https://hal.archives-ouvertes.fr/hal-02520490 Submitted on 21 Jan 2021 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. Distributed under a Creative Commons Attribution - NonCommercial| 4.0 International License 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. 5 Univ. Lille, CNRS, UMR 8198 – Evo-Eco-Paleo, 59000 Lille, France. Correspondence and requests for materials should be addressed to T.P.T. (email: [email protected]) NATURE COMMUNICATIONS | (2019) 10:1366 | https://doi.org/10.1038/s41467-019-09059-3 | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | https://doi.org/10.1038/s41467-019-09059-3 chinoderms (pentaradially symmetrical forms) are one of known as Bed III14 and is Fortunian in age14–16 having been Ethe most familiar and ubiquitous of all animal groups. correlated with the Purella antiqua shelly fossil zone14 (Sup- Because of their sturdy calcitic skeletons, they have a rich plementary Figure 1). Carbon isotope chemostratigraphic fossil record, first appearing during Cambrian Stage 3 (about 520 studies support this age15,16. Ma ago)1. However, it was not until the advent of molecular analyses that there was a general agreement as to how echino- Description. Small (20–50 mm in height) bilateral animal having derms were related to other deuterostomes2–11. Molecular data a globular to conical multi-plated theca, two long organic walled consistently resolves echinoderms and hemichordates as sister feeding appendages, and a stalk divided into two morphologically taxa within the clade Ambulacraria, a sister group to the Chor- distinct zones (proximal and distal). The theca is covered with data2–5. Yet, the origins and early evolution of the group has been numerous irregular, ovoid to polygonal plates (Figs. 1a–c, 2a, c a source of considerable conjecture, not least because the radial and Supplementary Figs. 2a, 3a, d, g). Plates are up to 2.5 mm in body plan of echinoderms is quite different from the bilaterally length and width with an unknown original composition. In some symmetrical organization of hemichordates and chordates12.A specimens, partial recovery between adjacent plates suggests that pre-radial history of the echinoderms has been suggested, a the theca might have been imbricately plated (Fig. 2a and Sup- possibility supported by recent anatomical development ana- plementary Fig. 3a, c). However, plates seem to be grossly abutted lyses13. The fossil record has yet to resolve this debate, as the early in other specimens or areas, so that definite assumption over history of the clade remains poorly documented and the first plating type would be overstated (Fig. 1a and Supplementary echinoderms to emerge in Cambrian Stage 3 already appear Figs. 2a, 4b, d, h, 5a). Thecal plating is often preserved as slightly relatively derived1,2,12. Interpretation of characters at the base of dislocated (a possible alternative explanation for apparent the Ambulacraria is further complicated by the apparent diver- imbrication of plates) with juxtaposition of internal and external gent morphology of the two hemichordate groups2 and the body molds. Due to the variation in outer shape and size of individual plan of the ancestral ambulacrarian remains idealized. plates, plating was most probably irregularly arranged during life, Here we analyze the systematic affinity and phylogenetic with plates loosely embedded within tegument. The variable relationships of Yanjiahella biscarpa14 from the Yanjiahe For- shape of the theca (Figs. 1a–c, 2a and Supplementary Figs. 2a, 3a, mation in Hubei, China. Our analysis illustrates that Y. biscarpa is d, 4a–d, g–h, 5a, e, i) also supports this deduction. Some speci- a stem-group echinoderm, confirming that plating was acquired mens show an almost continuous transition between stalk and by echinoderms prior to pentaradial symmetry and that the early theca (Fig. 2f, g and Supplementary Figs. 4a–d, 5a, e, i), so only the members of the clade were bilaterally symmetrical. Yanjiahella change in plating marks that boundary between these areas, with biscarpa exhibits morphological characters that are shared with plates being absent in the stalk. Thecal plates have differentiated both enteropneusts and echinoderms, demonstrating that the smooth (inner) surface and an outer (external) surface ornament enteropneust body plan is ancestral within the Hemichordata. of parallel ribs (Fig. 1c, 2a and Supplementary Figs. 3a, c). The The mosaic of morphologies that this taxon displays may proximal stalk is cylindrical (Figs. 1a, d, 2a, f, g and Supple- illustrate the deepest roots of the Ambulacraria and is therefore mentary Figs. 2b–c, h, 3a, e, 4f, i, 5e, i) and tapers distally (Fig. 1a, crucial for interpreting the early history of the deuterostome e and Supplementary Figs. 2c, h, 4g, 5a, e, i). The proximal stalk is clade. transversely ridged (distance between two successive ridges about 100 µm); the ridges are usually very fine, but can be locally Results and discussion thickened (Fig. 1c, d, Supplementary Fig. 2b). The distal stalk is Systematic paleontology. not transversely ridged but finely, longitudinally striated (Fig. 1e, g and Supplementary Figs. 2e–h, 5h) and is otherwise in perfect Total-group Echinodermata continuity with the proximal stalk. The relative rigidity of the Class, Order, Family indet. stalk seems to decrease distally as the proximal part is generally Yanjiahella biscarpa Guo, Li, Han, Ou, Zhou and Zheng almost straight with accentuated folds (Figs. 1, 2 and Supple- (2012). mentary Figs. 2, 3, 5a, e, i), although it is sometimes gently curved distally (Fig. 1 and Supplementary Fig. 2), while the striated distal Yanjiahella biscarpa;Guoetal.(2012),p.793,Figs.2k–m, 3c. zone of the stalk is invariably curved and looped (Figs. 1a, 2a and – Yanjiahella ancarpa;Guoetal.(2012),p.793,Figs.2a c, 3a. Supplementary Figs. 2a, 3a, 4g, 5a, e, i). A median, internal Yanjiahella monocarpa; Guo et al. (2012), p. 795, structure, visible from the posterior margin of the theca extends Figs. 2d–j, 3b. through the muscular stalk (Fig. 2a, d, f and Supplementary Figs. 5a–d). This structure is interpreted as the digestive tract and 14 Holotype. ELI-HS722 (see Guo et al. , Fig. 2k). Originally it continues through the proximal stalk region into the distal zone three species were nominally described in the same publica- of the stalk (Fig. 2d and Supplementary Figs. 4g, 5a–d). However, 14 “ ” tion , based on the number of preserved arms (here termed the digestive tract always disappears before the posterior extre- feeding appendages).
Recommended publications
  • 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.
    [Show full text]
  • 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]
  • 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.
    [Show full text]
  • Early Cambrian (Stage 4) Brachiopods from the Shipai Formation in the Three Gorges Area of South China
    Journal of Paleontology, page 1 of 30 Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/21/1937-2337 doi: 10.1017/jpa.2020.117 Early Cambrian (Stage 4) brachiopods from the Shipai Formation in the Three Gorges area of South China Xiaolin Duan,1 Marissa J. Betts,1,2 Lars E. Holmer,1,3 Yanlong Chen,1 Fan Liu,1 Yue Liang,1 and Zhifei Zhang1* 1State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an, 710069, China <[email protected]>, <[email protected]> 2Division of Earth Sciences, School of Environmental and Rural Science, University of New England, Armidale, NSW 2351, Australia <[email protected]> 3Department of Earth Sciences, Paleobiology, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden <[email protected]> Abstract.—Diverse and abundant fossil taxa have been described in the lower Cambrian Shipai Formation in the Three Gorges area of Hubei Province, South China, but the taxonomy and diversity of the co-occurring brachiopod fauna are still far from clear. Here we describe the brachiopod fauna recovered from the Shipai Formation in the Three Gorges area of South China, including representatives of the subphylum Linguliformea: linguloids (Lingulellotreta ergalievi, Eoobolus malongensis, and Neobolidae gen.
    [Show full text]
  • Abstract Volume
    https://doi.org/10.3301/ABSGI.2019.04 Milano, 2-5 July 2019 ABSTRACT BOOK a cura della Società Geologica Italiana 3rd International Congress on Stratigraphy GENERAL CHAIRS Marco Balini, Università di Milano, Italy Elisabetta Erba, Università di Milano, Italy - past President Società Geologica Italiana 2015-2017 SCIENTIFIC COMMITTEE Adele Bertini, Peter Brack, William Cavazza, Mauro Coltorti, Piero Di Stefano, Annalisa Ferretti, Stanley C. Finney, Fabio Florindo, Fabrizio Galluzzo, Piero Gianolla, David A.T. Harper, Martin J. Head, Thijs van Kolfschoten, Maria Marino, Simonetta Monechi, Giovanni Monegato, Maria Rose Petrizzo, Claudia Principe, Isabella Raffi, Lorenzo Rook ORGANIZING COMMITTEE The Organizing Committee is composed by members of the Department of Earth Sciences “Ardito Desio” and of the Società Geologica Italiana Lucia Angiolini, Cinzia Bottini, Bernardo Carmina, Domenico Cosentino, Fabrizio Felletti, Daniela Germani, Fabio M. Petti, Alessandro Zuccari FIELD TRIP COMMITTEE Fabrizio Berra, Mattia Marini, Maria Letizia Pampaloni, Marcello Tropeano ABSTRACT BOOK EDITORS Fabio M. Petti, Giulia Innamorati, Bernardo Carmina, Daniela Germani Papers, data, figures, maps and any other material published are covered by the copyright own by the Società Geologica Italiana. DISCLAIMER: The Società Geologica Italiana, the Editors are not responsible for the ideas, opinions, and contents of the papers published; the authors of each paper are responsible for the ideas opinions and con- tents published. La Società Geologica Italiana, i curatori scientifici non sono responsabili delle opinioni espresse e delle affermazioni pubblicate negli articoli: l’autore/i è/sono il/i solo/i responsabile/i. ST3.2 Cambrian stratigraphy, events and geochronology Conveners and Chairpersons Per Ahlberg (Lund University, Sweden) Loren E.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Grand Patrons RICHARD K. BAMBACH ARTHUR J. BOUCOT
    OGic OGic L al L al O S O S T O T O N N C C O O I I E E E E T L T L Y Y A A P P OFFICERS AND EDITORS OF THE PALEONTOLOGICAL SOCIETY Grand Patrons ANDREW H. KNOLL RICHARD K. BAMBACH CHARLES LANE ARTHUR J. BOUCOT ALLAN R. LARSON President PETER J. HARRIES, SIMON SCHNEIDER, Editor, Special Publications RODNEY M. FELDMAN AND CARRIE SCHWEITZER CECILIA LENK AND PAUL K. STROTHER BRUCE MacFADDEN, North Carolina State CASP COLIN SUMRALL, ROBERT AND ELVIRA GASTALDO JERE H. LIPPS Florida Museum of Natural History CRAIG SCOTT, Univ. of Tennessee, Knoxville THE FAMILY OF N. GARY LANE ALAN R. LORD MICHAEL HAUTMANN, bmacfadd@fl mnh.ufl .edu Royal Tyrrell Museum of Paleontology [email protected] A. R. (PETE) PALMER CHRIS MAPLES AND SARA MARCUS Univ. of Zurich J. WILLIAM SCHOPF President-Elect MARY SILCOX, Education/Outreach Coordinator JANET WOOD McGREGOR RAMAN J. SINGH WILLIAM DiMICHELE, MARTIN J. HEAD, Univ. of Toronto Scarborough ROWAN LOCKWOOD, CHERYL L. METZ STEVEN M. STANLEY Smithsonian Institution Brock Univ. College of William & Mary MOLLY F. AND CALVIN MILLER EDUARDO LEORRI SORIANO, [email protected] [email protected] RONALD W. MORIN THOMAS HEGNA, East Carolina Univ., Greenville Patrons OSBORNE B. NYE, JR. Past President Western Illinois Univ. Diversity and Inclusion Coordinator EDWARD J. ANDREW, JR. DAVID VARRICCHIO, TERESA O’NEILL ARNOLD I. MILLER, DENA SMITH, WILLIAM I. AUSICH Montana State Univ. RONALD L. PARSLEY Univ. of Cincinnati SAMANTHA HOPKINS, Univ. of Colorado BRUCE M. BELL MARK E. PATZKOWSKY [email protected] Univ.
    [Show full text]
  • 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
    [Show full text]
  • Plated Cambrian Bilaterians Reveal the Earliest Stages of Echinoderm Evolution
    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.
    [Show full text]
  • Paleontological Contributions
    THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS July 14, 1988 Paper 120 HOMALOZOAN ECHINODERMS OF THE WHEELER FORMATION (MIDDLE CAMBRIAN) OF WESTERN UTAH' Georges Ubaghs and R. A. Robison Laboratoire de Paléontologie Animale, Université de Liége, B-4000, Liége, Belgium Department of Geology, The University of Kansas, Lawrence, Kansas 66045 Abstract. —Three new species, representing three of the four homalozoan classes, are described from the upper Wheeler Formation of middle Middle Cambrian age in west- central Utah. Ctenocystis colodon n. sp. is only the fifth species of Ctenocystoidea to be described. The new order Ctenocystida is defined. The solutan Castericystis? sprinklei n. sp. is the fifth species of Homoiostelea to be reported from Cambrian strata. The cornute Cothurnocystis? bifida n. sp. is the fifth species of Stylophora to be reported from Middle Cambrian strata worldwide and only the second from North America. This homalozoan fauna is among the most diverse known from any Cambrian formation. AMONG ECHINODERMS, homalozoans are un House Range, and the stylophoran Cothur- usual in their complete lack of radial symmetry. nocystis? bifida from the House Range. Representatives are relatively rare, especially in Each homalozoan species in the Wheeler Cambrian strata. Three new Cambrian spe- Formation is from a different locality. Such low cies, which represent three of the four homa- diversity is typical of most Cambrian echi- lozoan classes, are described here. All are noderm faunas, although locally each species from the upper Wheeler Formation of west- may be represented by numerous individuals. central Utah and include the ctenocystoid For several years, knowledge of the class Ctenocystis colodon from the Drum Mountains, Ctenocystoidea was limited to the single species the homoiostelean Castericystis? sprinklei from the Ctenocystis utahensis Robison and Sprinkle, 1969, which is locally abundant in the Spence Shale of Manuscript received 15 November 1987.
    [Show full text]
  • Stylophoran Supertrees Revisited
    Stylophoran supertrees revisited BERTRAND LEFEBVRE Lefebvre, B. 2005. Stylophoran supertrees revisited. Acta Palaeontologica Polonica 50 (3): 477–486. Supertree analysis is a recent exploratory method that involves the simultaneous combination of two or more charac− ter−based source trees into a single consensus supertree. This method was recently applied by Ruta to a fossil group of enigmatic Palaeozoic forms, the stylophoran echinoderms. Ruta’s supertree suggested that mitrates are polyphyletic and originated from paraphyletic cornutes. Re−examination of Ruta’s data matrix strongly suggests that most source trees were based on dubious homologies resulting from theory−laden assumptions (calcichordate model) or superficial similar− ities (ankyroid scenario). A new supertree analysis was performed using a slightly corrected version of Ruta’s original combined matrix; the 70% majority−rule consensus of 24,168 most parsimonious supertrees suggests that mitrates are monophyletic and derived from paraphyletic cornutes. A second new supertree analysis was generated to test the influ− ence of the pruning of three taxa in some calcichordate source trees; the 70% majority−rule consensus of 3,720 shortest supertrees indicates that both cornutes and mitrates are monophyletic and derived from a Ceratocystis−like ancestor. The two new supertree analyses demonstrate the dramatic influence of the relative contributions of each initial assumption of plate homologies (and underlying anatomical interpretations), in original source trees, on the final topology of supertrees. Key words: Echinodermata, Stylophora, Cornuta, Mitrata, Ankyroida, Calcichordata, supertree, Palaeozoic. Bertrand Lefebvre [bertrand.lefebvre@u−bourgogne.fr], Biogéosciences, Université de Bourgogne, 6 boulevard Ga− briel, F−21000 Dijon, France. Introduction disparate, character−derived trees (Purvis 1995; Bininda− Emonds et al.
    [Show full text]