Paleontological Contributions

Total Page:16

File Type:pdf, Size:1020Kb

Paleontological Contributions THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS March 1, 1971 Paper 52 CONCEPT OF COMMON BUD AND RELATED PHENOMENA IN BRYOZOA MAXIM K. ELIAS University of Oklahoma, Norman, Oklahoma ABSTRACT The common bud of Stenolaemata (Cyclostomata of authors), as understood by BORG (1926), is analogous to the buds of higher plants in its terminal position on branches of the Bryozoa and in its vital activities. The common bud is truly common to all developing zooecia in a branch of a zoarium in a sense that its coelomic fluid remains undivided distally as long as a branch grows. As soon as a polypide bud originates, subtending to it, an oblique septum begins to rise proxi- mally by fission (BoRc's term) from the cylindrical wall of a branch; thus, a new zooecium with its own polypide is being initiated. All polypide buds originate at the edge of a transverse membrane that seals the coelomic fluid terminally. As the branch continues to grow the developing polypide falls behind the growing edge of the membrane, which BORG named growing zone. Some biologists (including HYMAN) erroneously consider growing zone synonymous with common bud— but the growing zone has the same relationship to the common bud as the meristem of plants has to their bud. The walls and septa of a zoaritnn which possesses a common bud combine their cal- careous layers into a single continuous structure, the colonial plexus (EtaAs' and CONDRA ' S term). The Bryozoa possessing common buds attain a higher level of colonial individualization (sensu BEKLEMISHEV) than those without it, and the greater the transverse expansion and complication of the common bud, the greater the colonial individualization—such as at- tained in more advanced Stenolaemata. Cheilostomata lack common buds, but in Membranipora and related crustose cheilo- stomes, whose colonies are built by contiguous rows of zooecia, each row develops by the means of its terminal linear bud (new term), with its own growing zone. The Ordovician "graptolite" Reticulograptus closely resembles the extant stenolaemate Stegoh ornera violacea (Sars) BORG INTRODUCTION The idea of the common bud, by means of (1926a, p. 254), SMITT believed "that in all Bryo- which the bryozoan colonies are developed, is zoa the developing margin of the zoarium is to be an imaginative concept conceived by F. A. SMITT regarded 'as a colonial bud, a common bud (sam- about a hundred years ago. As BORC briefly stated knopp), which separates [divides] itself by means 2 The University of Kansas Paleontological Contributions—Paper 52 of fission, and develops into separate zoids BORG also clarified biological understanding of [zooidsf " (Smurr, 1865, p. 6, translated by the "developing margin" in the Cyclostomata and BoRc). He erred, however, in his belief that all indicated it to be the growing zone of the com- Bryozoa developed in this manner; and it was mon bud. His most informative statement is NITSCHE (1871, sep. 31 ff.) who explained that quoted: it was not the case with Cheilostomata and Cteno- "At the edge of the terminal membrane the stomata. Accepting this correction, BORG worked ectodermal cells are higher, very closely packed out a revised concept of common bud, and estab- together without any intercellular spaces (pl. 3, lished on the evidence of its presence a "new fig. 12); their cytoplasm is densely granulated. order for the Cyclostomata, co-ordinate with two The mesodermic cells are also placed considerably old orders Gymnolaemata and Ctenostomata . ." closer together. The [ cellular] transition from to "be termed Stenolaemata" (BoRc, 1926a, p. this [marginal zone to the remaining part of 490). This taxonomic connotation ascribes to the the terminal membrane and to the lateral walls common bud foremost significance in a natural of the common bud [ below] is gradually effected. classification of Bryozoa. It is in this zone at the edge of the terminal mem- Whereas BORG described the stages of devel- brane that the growth of the common bud mainly opment of the modern Cyclostomata by the means takes place. Here new cells originate; here new of common bud, he noted that "certain differ- substance is stored in the cuticle, secreted from ences between the various cyclostomatous forms the ectodermal cells; here is also secreted calcare- present themselves even in the earliest develop- ous matter (chapter 4); and, finally, it is here, mental stages," although the common bud itself too, and only here, that the rudiments of the originates and develops in a similar manner from polypides [ polypide buds [ first become visible. the "semispherical primary disc characteristic for This zone in question may conveniently be termed all Cyclostomata" (1926a, p. 255). He also men- the growing zone of the common bud" (BoRc, tioned, in an unobtrusive way, his important 1926a, p. 321 [his underscoring). It is obvious discovery of an optical orientation of the minute that in this statement BORG described the structure particles comprising the calcified layer in the and activities of only a part—even if most essen- Crisiidae, which he examined in polarized light. tial—of the common bud: its growing zone. He found that these particles "are located in a However, because he did not attempt a formal certain direction; namely parallel to the longi- definition of the common bud and limited himself tudinal [along the branches] axis of the [ com- to specific descriptions of its occurrence in various mon} bud"; and, he noted, "the same is true also cyclostomes, he left his concept exposed to mis- of the calcified walls of the zoids [zooids]." No understandings and misinterpretations. observation of similar nature has ever been made elsewhere in the description of other groups of ACKNOWLEDGMENTS In view of the taxonomic the Cyclostomata in this or other books by BORG, connotation of the but greater biological and taxonomical significance concept of common bud, implied in its revision to the optical orientation of the particles in the by BORG (1926a), the present review of the con- calcified layer in Crisiidae was added by the dis- cept became an essential part in biometric research covery of a similar optical orientation of the calcite on fenestrate bryozoans, where an evidence of the in the unit-crystal primary skeleton in fenestrate presence of a common bud was reported by ELIAS bryozoans, hence suggestive of the presence in & CONDRA (1957). The whole research has been them of the common bud.' supported by several grants from the National Science Foundation, the last one in 1967-68, no. I resolutely disagree with the speculative concept of growth GA-817. in fenestellid branches by means of a "conveyor belt" principle, which was adapted for this purpose by TAVENER-SMITH (1969) in Parts of the manuscript have been read by Dr. preference of the natural (for them) growth by means of common HELEN DUNCAN, bud. It seems rather ridiculous to imagine that the same mech- U.S. Geological Survey, and the anism which was imaginatively conceived to explain the growth whole, in its final state, by of certain brachiopod shells by ALWYN WILLIAMS (1966, 1968), Dr. RAYMOND C. would need to be proposed for explanation of the growth of a MOORE, University of Kansas. I am indebted to colonial organism. Even HYMAN (1959), who with the help of her academic redefinition of the well recognized concept of Lophophore, ROGER B. WILLIAMS, of the Paleontological Insti- united into her "Lophophorate Coelomates" (1959, p. 228 ff.) the phyla Phoronida, Ectoprocta, and Brachiopoda, was avoiding any tute, for skillful preparation of new illustrations comparison of growth of the bryozoan colonies to that of brachio- pod shells. after BORG. Elias—Common Bud and Related Phenomena in Bryozoa 3 COMPONENTS OF COMMON BUD The following components are present in the and drag along their sides, as it were, the ecto- common bud of all stenolaemate bryozoan col- derm and mesoderm, which cover the calcareous onies: wall (or septum), from which they originate. ) Terminal membrane which stretches across Thus each septum consists of a central calcareous and covers the bud cavity at the distal margin layer, which is flanked on either side by ectoder- (or margins) in a developing colony. The ter- mal and mesodermal layers. This manner of minal membrane consists (from outside inward) origin "by fission" makes all septa inherently of a very thin cuticle, a one-cell thick layer of possessive of a single primary calcareous layer, ectoderm, and a one-cell thick layer of diffusely directly continuing from the calcareous layer of spaced cells of mesoderm. the zoarial wall, from which they originate. It 2) Coelomic cavity, which is filled with co- is this uniform, one-layered, calcareous structure elomic fluid, sealed by a terminal membrane of all walls and septa which is highly character- above, and contained laterally and proximally by istic of stenolaemates. And because it is a result an outer wall and oblique septa or both. of colonial development through mechanism of bud, the definition of the latter must take 3) Colonial wall and partitions (septa), all of common which (from outside inward) consist of a very thin this into account. cuticle comprising a calcareous layer (precipitated 6) Otherwise oriented calcareous septa, which by ectodermal epithelium), ectoderm, and meso- originate from the oblique septa, such as "median derm (Fig. 1). vertical" (BoRG, 1926a, p. 270) septa rising along the two opposite oblique 4) Growing zone, a ringlike area along the the linear coalescence of septa in Acamptostega (Stomatopora, Tubuli- contact of the terminal membrane and the colonial pora), as explained below. wall, where new cells of ectoderm and mesoderm originate and polypi& buds make their "first appearance." SPECIAL TERMS PERTAINING TO 5) Oblique calcareous septa, which arise in STENOLAEMATA (CYCLOSTO- part of the coelomic cavity by send- the proximal MATA) AND FENESTRATA ing out from the colonial wall, as if by fission, oblique ingrowths (internal outgrowths) which Proper understanding of special terms which ascend subparallel to the wall toward the terminal indicate the peculiar processes in growth by means membrane.
Recommended publications
  • Bryozoan Studies 2019
    BRYOZOAN STUDIES 2019 Edited by Patrick Wyse Jackson & Kamil Zágoršek Czech Geological Survey 1 BRYOZOAN STUDIES 2019 2 Dedication This volume is dedicated with deep gratitude to Paul Taylor. Throughout his career Paul has worked at the Natural History Museum, London which he joined soon after completing post-doctoral studies in Swansea which in turn followed his completion of a PhD in Durham. Paul’s research interests are polymatic within the sphere of bryozoology – he has studied fossil bryozoans from all of the geological periods, and modern bryozoans from all oceanic basins. His interests include taxonomy, biodiversity, skeletal structure, ecology, evolution, history to name a few subject areas; in fact there are probably none in bryozoology that have not been the subject of his many publications. His office in the Natural History Museum quickly became a magnet for visiting bryozoological colleagues whom he always welcomed: he has always been highly encouraging of the research efforts of others, quick to collaborate, and generous with advice and information. A long-standing member of the International Bryozoology Association, Paul presided over the conference held in Boone in 2007. 3 BRYOZOAN STUDIES 2019 Contents Kamil Zágoršek and Patrick N. Wyse Jackson Foreword ...................................................................................................................................................... 6 Caroline J. Buttler and Paul D. Taylor Review of symbioses between bryozoans and primary and secondary occupants of gastropod
    [Show full text]
  • Smithsonian Miscellaneous Collections
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 67, NUMBER 6 CAMBRIAN GEOLOGY AND PALEONTOLOGY IV No. 6.—MIDDLE CAMBRIAN SPONGIAE (With Plates 60 to 90) BY CHARLES D. WALCOTT (Publication 2580) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION 1920 Z$t Bovb Qgattimote (press BALTIMORE, MD., U. S. A. CAMBRIAN GEOLOGY AND PALEONTOLOGY IV No. 6.—MIDDLE CAMBRIAN SPONGIAE By CHARLES D. WALCOTT (With Plates 60 to 90) CONTENTS PAGE Introduction 263 Habitat = 265 Genera and species 265 Comparison with recent sponges 267 Comparison with Metis shale sponge fauna 267 Description of species 269 Sub-Class Silicispongiae 269 Order Monactinellida Zittel (Monaxonidae Sollas) 269 Sub-Order Halichondrina Vosmaer 269 Halichondrites Dawson 269 Halichondrites elissa, new species 270 Tuponia, new genus 271 Tuponia lineata, new species 272 Tuponia bellilineata, new species 274 Tuponia flexilis, new species 275 Tuponia flexilis var. intermedia, new variety 276 Takakkawia, new genus 277 Takakkawia lineata, new species 277 Wapkia, new genus 279 Wapkia grandis, new species 279 Hazelia, new genus 281 Hazelia palmata, new species 282 Hazelia conf erta, new species 283 Hazelia delicatula, new species 284 Hazelia ? grandis, new species 285. Hazelia mammillata, new species 286' Hazelia nodulifera, new species 287 Hazelia obscura, new species 287 Corralia, new genus 288 Corralia undulata, new species 288 Sentinelia, new genus 289 Sentinelia draco, new species 290 Smithsonian Miscellaneous Collections, Vol. 67, No. 6 261 262 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 6j Family Suberitidae 291 Choia, new genus 291 Choia carteri, new species 292 Choia ridleyi, new species 294 Choia utahensis, new species 295 Choia hindei (Dawson) 295 Hamptonia, new genus 296 Hamptonia bowerbanki, new species 297 Pirania, new genus 298 Pirania muricata, new species 298 Order Hexactinellida O.
    [Show full text]
  • Palaeontologia Electronica DISCRIMINATION OF
    Palaeontologia Electronica http://palaeo-electronica.org DISCRIMINATION OF FENESTRATE BRYOZOAN GENERA IN MORPHOSPACE Steven J. Hageman and Frank K. McKinney ABSTRACT Concepts for generic diagnoses and discrimination of biserial fenestrate Bryozoa (Fenestellidae) have varied historically, but have largely been based on specialized colony forms (e.g., Archimedes), the shape and budding arrangement of chambers and other internal skeletal features such as hemisepta, and occasionally on the pres- ence or absence of discrete characters, such as placement of nodes on the frontal sur- face (e.g., Minilya). The question remains as to whether biserial fenestrate genera represent real biological clades, or whether they are convenient groupings of morpho- types based on untested characters. This study evaluates the distribution of 1075 operational taxonomic units (OTUs) from 15 fenestrate genera with measurements for nine morphometric characters – external features are not emphasized in most generic diagnoses. Here, each OTU represents a composite or idealized individual from a col- ony. Results show that OTUs plotted in principal component space do largely form coherent clusters based on a priori generic assignments. Thus the groupings based on characters other than the ones used to originally define them, add support to the notion of biological significance for recognized genera. The exceptions actually highlight and help resolve known issues. Therefore, we recognize Alternifenestella as a junior syn- onym of the genus Spinofenestella, and propose reassignment of Laxifenestella serrat- ula in Snyder (1991) to Fenestella serratula, and Fenestella sp. 1 in Ernst and Schroeder (2007) as Rectifenestella. We do not advocate that biserial fenestrate generic concepts should be based on the nine external characters used in this study, but rather that they can be used independently to evaluate the coherence of genera based on other discrete characters.
    [Show full text]
  • A New Mississippian Hexactinellid Sponge from the Western Gondwana: Taxonomic and Paleobiogeographic Implications
    A new Mississippian hexactinellid sponge from the western Gondwana: Taxonomic and paleobiogeographic implications MARCELO G. CARRERA, JUAN JOSE RUSTÁN, N. EMILIO VACCARI, and MIGUEL EZPELETA Carrera, M.G., Rustán, J.J., Vaccari N.E., and Ezpeleta, M. 2018. A new Mississippian hexactinellid sponge from the western Gondwana: Taxonomic and paleobiogeographic implications. Acta Palaeontologica Polonica 63 (1): 63–70. A Mississippian hexactinellid sponge from the western Argentina improves the extremely poor late Paleozoic sponge records from Gondwana. The sponge is included in the subfamily Thysanodictyinae of family Dictyospongiidae. The new genus and species Minitaspongia parvis is erected, and its well-preserved spicular structure is described in detail repre- senting the first approximation of the spicule assemblage in Thysanodictyinae. The skeleton is clathrate, three-dimensional with at least two ranks of rectangular openings. This first report of this subfamily outside North America represents the best-known hexactinellid and the first dictyosponge record from the Carboniferous of Gondwana. Unlike the occurrences of Thysanodictyinae in North America, with thick skeletons linked to high-energy shallow water settings, Minitaspongia occurs in low-energy water siliciclastic settings related to a cold climate and glacimarine deposits. Accordingly, the complex wall structure of this sponge should not be invoked as a necessary adaptation to high energy and shallow water settings. Key words: Porifera, Hexactinellida, Reticulosa, Carboniferous, Mississippian, Argentina. Marcelo G. Carrera [[email protected]], CICTERRA-CONICET Universidad Nacional de Córdoba, Facultad de Ciencias Exactas Físicas y Naturales, Av. Vélez Sarfield 1611, Ciudad Universitaria, 5016, Córdoba, Argentina. Juan José Rustan [[email protected]], N. Emilio Vaccari [[email protected]], and Miguel Ezpeleta [[email protected]], CICTERRA-CONICET Universidad Nacional de Córdoba and Universidad Nacional de La Rioja, Av.
    [Show full text]
  • Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park
    Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park By Linda Sue Lassiter1, Justin S. Tweet2, Frederick A. Sundberg3, John R. Foster4, and P. J. Bergman5 1Northern Arizona University Department of Biological Sciences Flagstaff, Arizona 2National Park Service 9149 79th Street S. Cottage Grove, Minnesota 55016 3Museum of Northern Arizona Research Associate Flagstaff, Arizona 4Utah Field House of Natural History State Park Museum Vernal, Utah 5Northern Arizona University Flagstaff, Arizona Introduction As impressive as the Grand Canyon is to any observer from the rim, the river, or even from space, these cliffs and slopes are much more than an array of colors above the serpentine majesty of the Colorado River. The erosive forces of the Colorado River and feeder streams took millions of years to carve more than 290 million years of Paleozoic Era rocks. These exposures of Paleozoic Era sediments constitute 85% of the almost 5,000 km2 (1,903 mi2) of the Grand Canyon National Park (GRCA) and reveal important chronologic information on marine paleoecologies of the past. This expanse of both spatial and temporal coverage is unrivaled anywhere else on our planet. While many visitors stand on the rim and peer down into the abyss of the carved canyon depths, few realize that they are also staring at the history of life from almost 520 million years ago (Ma) where the Paleozoic rocks cover the great unconformity (Karlstrom et al. 2018) to 270 Ma at the top (Sorauf and Billingsley 1991). The Paleozoic rocks visible from the South Rim Visitors Center, are mostly from marine and some fluvial sediment deposits (Figure 5-1).
    [Show full text]
  • (Use Bookmarks to Browse) News from the Membership New
    BBuulllleettiinn Volume 7 Number 2 July 2011 (Use bookmarks to browse) News from the Membership New Members Frank Kenneth (Ken) McKinney, 1943-2011 Ken McKinney: How I Discovered Bryozoans Sea Drift – Remembering Ken McKinney European Journal of Taxonomy Report from the 10th Larwood Meeting Announcement: 11th Larwood Meeting Award for the Bryozoa Home Page New from the IBA: Annals of Bryozoology 3 Bryozoan Bookstall In Memoriam: Karen Emilie Bille Hansen In Memoriam: Rory Milne Featured Journal Covers Meetings and Conferences Recent Publications Copyright © 2011 by the International Bryozoology Association. Eckart Håkansson, President Timothy S. Wood, Secretary Abigail Smith, Treasurer ISSN 1941-7918 Comments regarding this Bulletin should be addressed to the IBA Secretary: [email protected] Further information at www.bryozoa.net/iba News from the Membership Priska Schäfer, Andrej Ernst, and Joachim Scholz. We would like to inform the IBA community, that the conference volume of "Bryozoan studies 2010" is in good progress. We intend to have the volume published in spring 2012. Best wishes from Kiel! Alex Gruhl. I am very pleased to have received an EU Marie Curie post-doctoral fellowship to work for two more years with Beth Okamura at the NHM in London. In this project we will continue research on myxozoan parasites, with a specific focus on development and evolution of major body plan features in this group. And of course I will also not neglect their hosts - bryozoans! More soon on one of the next meetings! Masato Hirose. Recently, I have got postdoctoral fellow in the National Museum of Nature and Sciences Tokyo.
    [Show full text]
  • Lower Silurian, Aeronian) of New York, USA
    Journal of Paleontology, 93(4), 2019, p. 628–657 Copyright © The Author(s), 2019. 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. 0022-3360/19/1937-2337 doi: 10.1017/jpa.2018.101 Bryozoan fauna from the Reynales Formation (lower Silurian, Aeronian) of New York, USA Andrej Ernst,1 Carlton E. Brett,2 and Mark A. Wilson3 1Institut für Geologie, Universität Hamburg, Bundesstr. 55, D-20146 Hamburg, Germany <[email protected]> 2Department of Geology, University of Cincinnati, Cincinnati, Ohio 45221-0013, USA <[email protected]> 3Department of Earth Sciences, The College of Wooster, Wooster, Ohio 44691, USA <[email protected]> Abstract.—Thirteen bryozoan species are described from the Brewer Dock (Hickory Corners) Member of the Reynales Formation (lower Silurian, Aeronian) at the locality Hickory Corners in western New York, USA. Three species are new: trepostomes Homotrypa niagarensis n. sp. and Leioclema adsuetum n. sp. and the rhabdomesine cryptostome Moyerella parva n. sp. Only one species, Hennigopora apta Perry and Hattin, 1960, developed obligatory encrusting colonies whereas the others produced erect ramose colonies of various thicknesses and shapes: cylindrical, branched, and lenticular. Bryozoans display high abundance and richness within the rock. This fauna is characteristic of a moderately agitated environment with a stable substrate. The identified species reveal paleobiogeographic connections to other Silurian localities of New York as well as Ohio and Indiana (USA) and Anticosti (Canada).
    [Show full text]
  • Bryozoan Fauna of the Upper Clays Ferry, Kope, and Lower Fairview Formations (Edenian, Upper Ordovician) at Moffett Road, Northe
    Bryozoan fauna of the upper Clays Ferry, Kope, and lower Fairview Formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky By Olgerts L. Karklins U.S. Geological Survey Open-File Report 83-31 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Contents Page Abstract 1 Introduction 2 Description of locality 5 Previous work 5 Materials and methods 6 Moffett Road section 7 Composition 8 Abundance and distribution 10 Biostratigraphy 10 Bryozoans of the Edenian Stage in the Moffett Road section 14 Systematic Paleontology 15 Order Trepostomata 17 Family Monticuliporidae 17 Heterotrypidae 20 Batostomellidae 24 Amplexoporidae 26 Trematoporidae 28 Caloporidae 30 Family unknown 33 Order Cystoporata 34 Family Ceramoporidae 34 Constellariidae 37 Order Cryptostomata 38 Suborder Fenestelloidea 38 Family Phylloporinidae 38 ii (contents, cont.) Page Suborder Ptilodictyoidea ' 39 Family Ptilodictyidae 39 Stictoporellidae 41 Ehinidictyidae 41 References cited 43 Illustrations Table 1. Ranges of species in feet, relative abundance in percent and the number of prepared specimens of each species in stratigraphic order above the base of the Moffett Road section. Figure 1. Index maps of location of Moffett Road section (A) and the De Mossville 1:24000 quadrangle (B) in northern Kentucky. Figure 2. Pie diagram of relative abundance of species in the Moffett Road section. Plate 1. Occurrence of species and stratigraphic positions of collections in the Moffett Road section. Plate 2. Stratigraphic ranges and relative abundances of species in the Moffett Road section. iii Bryozoan fauna of the upper Clays Ferry, Kope, and lower Fairview Formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky Abstract Bryozoans are abundant and highly diversified in the Kope Formation (Upper Ordovician) of the proposed stratotype section for the Edenian Stage in Kentucky.
    [Show full text]
  • Well-Preserved Fenestrate Bryozoans in Mississippian Building Stones, Utrecht, the Netherlands
    Swiss J Palaeontol (2018) 137:99–102 https://doi.org/10.1007/s13358-017-0141-x SHORT CONTRIBUTION Well-preserved fenestrate bryozoans in Mississippian building stones, Utrecht, The Netherlands 1,2 3 Stephen K. Donovan • Patrick N. Wyse Jackson Received: 11 July 2017 / Accepted: 25 October 2017 / Published online: 15 November 2017 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2017 Abstract Unusually well-preserved fenestrate bryozoans lying, unlithified Quaternary sediments (Meijer 1985). In have been identified in Mississippian (Lower Carbonifer- such a setting, building stones take on an additional sig- ous) building stones in Utrecht, the Netherlands. Speci- nificance for the geologist. That is, where there are no mens in adjacent properties presumably came from the rocks in situ, specimens transported and accumulated by same horizon, presumably from Belgium. Although scant mankind provide both aesthetic pleasure, and, potentially, internal morphological detail can be discerned, the general opportunities for fieldwork and research (e.g., Donovan arrangement of the meshwork, together with the disposition 2015). Common building stones in Dutch cities include of autozooecia, show affinities with Rectifenestella Moro- various grey Upper Palaeozoic limestones, mostly Missis- zova, which has straight-sided fenestrules into which lat- sippian (Lower Carboniferous), and which were imported eral autozooecial apertures do not extend. This may be the from Belgium and elsewhere. Palaeontological field guides first detailed record of bryozoans from the Mississippian to these limestones, such as Reumer (2016) and Van building stones of the Netherlands. Roekel (2007), illustrate and document the prominent Mississippian taxa including tabulate and rugose corals, Keywords Urban geology Á Lower Carboniferous Á crinoids, brachiopods and molluscs (Donovan and Madern Taphonomy Á Konservat-Lagersta¨tten Á Belgium 2016; Donovan et al.
    [Show full text]
  • Epizoan and Endoskeletozoan Distribution Across Reassembled Ramose Stenolaemate Bryozoan Zoaria from the Upper Ordovician (Katian) of the Cincinnati Arch Region, USA
    Epizoan and endoskeletozoan distribution across reassembled ramose stenolaemate bryozoan zoaria from the Upper Ordovician (Katian) of the Cincinnati Arch region, USA PATRICK N. WYSE JACKSON & MARCUS M. KEY, JR WYSE JACKSON, P.N. & KEY, M.M., JR, 2019:11:15. Epizoan and endoskeletozoan distribution across reassembled ramose stenolaemate bryozoan zoaria from the Upper Ordovician (Katian) of the Cincinnati Arch region, USA. Australasian Palaeontological Memoirs 52, 169–178. ISSN 2205–8877. The Upper Ordovician (Katian) of the Cincinnati, Ohio, USA region has yielded bedding-plane assemblages of ramose stenolaemate bryozoans. Sixteen colonies were reassembled which provide valuable data on the settlement patterns of epizoans and endoskeletozoans, information on the timing of infestation and encrustation, and on environmental and taphonomic conditions affecting the bryozoan colonies. Various parameters were assessed: the size, incidence and position of borings; whether or not they show a regeneration rim that would indicate an in-vivo relationship between host and boring organism; and the position on branches of epizoans, measured on proximal and distal colony portions, and on the upper-facing or lower- facing sides of colonies as they lay on the substrate. Epizoans include thin adnate colonies of Crepipora and other unidentified cystoporate bryozoans, cornulitids, the problematicum Hederella and the cnidarian Sphenothallus. Encrustation was generally slight and in all but one colony was evenly distributed on all sides of branches indicating probable in-vivo infestation. The one exception suggests that the colony acted as a hardground once it had toppled over and was lying on the substrate. Boring into the zoarial skeleton took place both before and after death of colonies.
    [Show full text]
  • Systematics 071718
    Invertebrate Paleontology Systematics Classification of Invertebrate Taxa for the Laboratory Fall 2018 The following is an annotated list of the taxa you will be identifying in the Invertebrate Paleontology lab. It is correlated with the groups we are covering in lecture, so you will also find this useful during class. Some taxa are not included because they are rare as specimens or relatively unimportant for paleontological fieldwork. When asked to “identify” a specimen on a lab test or in the field, please give the most specific taxonomic rank and name (e.g., “Class Hexactinellida”). This listing is revised every year – it is not the same as last year’s compilation. I’ve inserted spaces below the specific taxa so you can add notes and drawings. I’ve also left the backs of the pages blank so that you can use them for notes as well. Please let me know how you would improve this listing so that it is more helpful. You may use this entire book, the text as well as any notes and diagrams you add in your own handwriting, on the lab tests and the final lab- lecture examination. Table of Contents Phylum Haptophyta 2 Phylum Bacillariophyta 2 Phylum Foraminiferida 3 Phylum Radiolaria 4 Phylum Porifera 5 Phylum Cnidaria 7 Phylum Brachiopoda 11 Phylum Bryozoa 17 Phylum Hyolitha 19 Phylum Mollusca 20 Phylum Arthropoda 27 Phylum Echinodermata 32 Phylum Hemichordata 36 Phylum Annelida 37 Incertae sedis 37 Trace Fossils 39 Full Taxonomic List (Name and Age Ranges Only) 42 1 Nomina si nescis, perit et cognitio rerum If you do not know the names, the knowledge of these things vanishes (Linnaeus) Kingdom PROTISTA: Prepaleozoic – Recent A polyphyletic group used for convenience until the higher taxonomy is sorted out.
    [Show full text]
  • Bryozoans and Corals from Indiana and Learn the Basics of Their Classification and Anatomy
    Geol G308 Paleontology and Geology of Indiana Name: ____________________________________ Lab 5 Corals and Bryozoa Corals (Phylum Cnidaria) and bryozoans (Phylum Bryozoa) are two common Paleozoic groups. Skeletons of the two groups are superficially similar, but the animals are very different and unrelated to each other. In this lab you will look at bryozoans and corals from Indiana and learn the basics of their classification and anatomy. The groups are diverse with many, many species, often requiring a specialist to identify them correctly. Nevertheless, it is possible to learn some of the major features that make up their diversity. Corals Many cnidarians lack skeletons, but corals (Anthozoa) are a major exception. Coral polyps produce a calcium carbonate skeleton that serves as a supporting, cup-like base around them. Some corals are solitary, usually forming a horn-like base, while others are colonial, forming a tile-like mosaic of supporting structures that are fused in a single colony. Anatomically corals are one of the simplest metazoan phyla. Only sponges have simpler tissue structures. Ecologically corals are predators, most of them using stinging cells on the polyp’s tentacles to immobilize prey before it is ingested. Coral anatomy (from Boardman, Cheetham and Powell, 1987. Fossil Invertebrates. Blackwell Scientific: Palo Alto). Department of Geological Sciences | P. David Polly 1 Classification Class Anthozoa (Precambrian to recent) Order Rugosa (Middle Ordovician through Permian) Have septa and tabulae in skeleton Often solitary, but sometimes colonial Have calcite skeletons Order Tabulata (Lower Ordovician through Permian) Have tabulae in skeleton, but septa are often reduced or absent Always colonial Have calcite skeletons Order Scleractina (Triassic to recent) Includes most living corals Have septa, but usually no tabulae Have aragonitic skeletons Coral growth forms Colonial Rugosa Tabulata Scleractinia S T T S Solitary T S S R S R (from Boardman, Cheetham and Powell, 1987.
    [Show full text]