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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 -
Devonian Bryozoans of the Holy Cross Mountains, Poland
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. XVIII 1973 No.4 MARIA KIEPURA DEVONIAN BRYOZOANS OF THE HOLY CROSS MOUNTAINS, POLAND. PART II. CYCLOSTOMATA AND CYSTOPORATA Abstract. - Descriptions are given of 33, species of Middle Devonian Bryozoa from the Holy Cross Mts., belonging to the orders Cyclostomata and Cystoporata. Cyclo stomata are represented by 26 species (4 new: Corynotrypa (Corynotrypa) skalensis, C. (C.) basiplata, Stomatopora varigemmata and Diversipora bitubulata n. gen.). Cystoporata are represented by 7 new species: Ceramoporella orbiculata, C. grandi cystica, Favositella integrimuralis, Fistulipora boardmani, F. emphantica, Cyclotrypa nekhoroshevi and Fistuliramus astrovae. The systematic assignment of the genus Hederella Hall, 1881 has been discussed and the "tabulate-like" microstructure of the zooecial walls of this genus examined. In addition, the epifauna and associated assemblages have been characterized as well as the geological and palaeoecological conditions in which the described Bryozoa occurred. INTRODUCTION Among the Middle Devonian Bryozoa of the Holy Cross Mts., the present author has, up to now, described Ctenostomata (Kiepura, 1965). The present paper is a continuation of her investigations on the Middle Devonian Bryozoa of this region and contains descriptions of 33 species belonging to 9 genera of the orders Cyclostomata and Cystoporata occur ring in the Grzegorzowice - Skaly profile. The bryozoan collection of the Palaeozoological Institute of the Polish Academy of Sciences also contains a rich material representing the orders Trepostomata and Cryptostomata from the Middle Devonian of the Holy Cross Mts., which will be described at a future date. The material described in the present paper was collected by the author during several years of fieldwork (1950-1954). -
"Lophophorates" Brachiopoda Echinodermata Asterozoa
Deuterostomes Bryozoa Phoronida "lophophorates" Brachiopoda Echinodermata Asterozoa Stelleroidea Asteroidea Ophiuroidea Echinozoa Holothuroidea Echinoidea Crinozoa Crinoidea Chaetognatha (arrow worms) Hemichordata (acorn worms) Chordata Urochordata (sea squirt) Cephalochordata (amphioxoius) Vertebrata PHYLUM CHAETOGNATHA (70 spp) Arrow worms Fossils from the Cambrium Carnivorous - link between small phytoplankton and larger zooplankton (1-15 cm long) Pharyngeal gill pores No notochord Peculiar origin for mesoderm (not strictly enterocoelous) Uncertain relationship with echinoderms PHYLUM HEMICHORDATA (120 spp) Acorn worms Pharyngeal gill pores No notochord (Stomochord cartilaginous and once thought homologous w/notochord) Tornaria larvae very similar to asteroidea Bipinnaria larvae CLASS ENTEROPNEUSTA (acorn worms) Marine, bottom dwellers CLASS PTEROBRANCHIA Colonial, sessile, filter feeding, tube dwellers Small (1-2 mm), "U" shaped gut, no gill slits PHYLUM CHORDATA Body segmented Axial notochord Dorsal hollow nerve chord Paired gill slits Post anal tail SUBPHYLUM UROCHORDATA Marine, sessile Body covered in a cellulose tunic ("Tunicates") Filter feeder (» 200 L/day) - perforated pharnx adapted for filtering & repiration Pharyngeal basket contractable - squirts water when exposed at low tide Hermaphrodites Tadpole larvae w/chordate characteristics (neoteny) CLASS ASCIDIACEA (sea squirt/tunicate - sessile) No excretory system Open circulatory system (can reverse blood flow) Endostyle - (homologous to thyroid of vertebrates) ciliated groove -
MARINE FAUNA and FLORA of BERMUDA a Systematic Guide to the Identification of Marine Organisms
MARINE FAUNA AND FLORA OF BERMUDA A Systematic Guide to the Identification of Marine Organisms Edited by WOLFGANG STERRER Bermuda Biological Station St. George's, Bermuda in cooperation with Christiane Schoepfer-Sterrer and 63 text contributors A Wiley-Interscience Publication JOHN WILEY & SONS New York Chichester Brisbane Toronto Singapore ANTHOZOA 159 sucker) on the exumbrella. Color vari many Actiniaria and Ceriantharia can able, mostly greenish gray-blue, the move if exposed to unfavorable condi greenish color due to zooxanthellae tions. Actiniaria can creep along on their embedded in the mesoglea. Polyp pedal discs at 8-10 cm/hr, pull themselves slender; strobilation of the monodisc by their tentacles, move by peristalsis type. Medusae are found, upside through loose sediment, float in currents, down and usually in large congrega and even swim by coordinated tentacular tions, on the muddy bottoms of in motion. shore bays and ponds. Both subclasses are represented in Ber W. STERRER muda. Because the orders are so diverse morphologically, they are often discussed separately. In some classifications the an Class Anthozoa (Corals, anemones) thozoan orders are grouped into 3 (not the 2 considered here) subclasses, splitting off CHARACTERISTICS: Exclusively polypoid, sol the Ceriantharia and Antipatharia into a itary or colonial eNIDARIA. Oral end ex separate subclass, the Ceriantipatharia. panded into oral disc which bears the mouth and Corallimorpharia are sometimes consid one or more rings of hollow tentacles. ered a suborder of Scleractinia. Approxi Stomodeum well developed, often with 1 or 2 mately 6,500 species of Anthozoa are siphonoglyphs. Gastrovascular cavity compart known. Of 93 species reported from Ber mentalized by radially arranged mesenteries. -
End-Permian Mass Extinction in the Oceans: an Ancient Analog for the Twenty-First Century?
EA40CH05-Payne ARI 23 March 2012 10:24 End-Permian Mass Extinction in the Oceans: An Ancient Analog for the Twenty-First Century? Jonathan L. Payne1 and Matthew E. Clapham2 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305; email: [email protected] 2Department of Earth and Planetary Sciences, University of California, Santa Cruz, California 95064; email: [email protected] Annu. Rev. Earth Planet. Sci. 2012. 40:89–111 Keywords First published online as a Review in Advance on ocean acidification, evolution, isotope geochemistry, volcanism, January 3, 2012 biodiversity The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The greatest loss of biodiversity in the history of animal life occurred at the 10.1146/annurev-earth-042711-105329 end of the Permian Period (∼252 million years ago). This biotic catastro- Annu. Rev. Earth Planet. Sci. 2012.40:89-111. Downloaded from www.annualreviews.org Copyright c 2012 by Annual Reviews. phe coincided with an interval of widespread ocean anoxia and the eruption All rights reserved of one of Earth’s largest continental flood basalt provinces, the Siberian by Stanford University - Main Campus Robert Crown Law Library on 06/04/12. For personal use only. 0084-6597/12/0530-0089$20.00 Traps. Volatile release from basaltic magma and sedimentary strata dur- ing emplacement of the Siberian Traps can account for most end-Permian paleontological and geochemical observations. Climate change and, per- haps, destruction of the ozone layer can explain extinctions on land, whereas changes in ocean oxygen levels, CO2, pH, and temperature can account for extinction selectivity across marine animals. -
Animal Origins and the Evolution of Body Plans 621
Animal Origins and the Evolution 32 of Body Plans In 1822, nearly forty years before Darwin wrote The Origin of Species, a French naturalist, Étienne Geoffroy Saint-Hilaire, was examining a lob- ster. He noticed that when he turned the lobster upside down and viewed it with its ventral surface up, its central nervous system was located above its digestive tract, which in turn was located above its heart—the same relative positions these systems have in mammals when viewed dorsally. His observations led Geoffroy to conclude that the differences between arthropods (such as lobsters) and vertebrates (such as mammals) could be explained if the embryos of one of those groups were inverted during development. Geoffroy’s suggestion was regarded as preposterous at the time and was largely dismissed until recently. However, the discovery of two genes that influence a sys- tem of extracellular signals involved in development has lent new support to Geof- froy’s seemingly outrageous hypothesis. Genes that Control Development A A vertebrate gene called chordin helps to establish cells on one side of the embryo human and a lobster carry similar genes that control the development of the body as dorsal and on the other as ventral. A probably homologous gene in fruit flies, called axis, but these genes position their body sog, acts in a similar manner, but has the opposite effect. Fly cells where sog is active systems inversely. A lobster’s nervous sys- become ventral, whereas vertebrate cells where chordin is active become dorsal. How- tem runs up its ventral (belly) surface, whereas a vertebrate’s runs down its dorsal ever, when sog mRNA is injected into an embryo (back) surface. -
Ponasterone a and F, Ecdysteroids from the Arctic Bryozoan Alcyonidium Gelatinosum
molecules Article Ponasterone A and F, Ecdysteroids from the Arctic Bryozoan Alcyonidium gelatinosum Kine Østnes Hansen 1,* ID , Johan Isaksson 2, Eirin Glomsaker 1, Jeanette Hammer Andersen 1 ID and Espen Hansen 1 ID 1 Marbio, UiT—The Arctic University of Norway, Breivika, N-9037 Tromsø, Norway; [email protected] (E.G.); [email protected] (J.H.A.); [email protected] (E.H.) 2 Department of Chemistry, UiT—The Arctic University of Norway, Breivika, N-9037 Tromsø, Norway; [email protected] * Correspondence: [email protected]; Tel.: +47-77649272 Received: 18 May 2018; Accepted: 12 June 2018; Published: 19 June 2018 Abstract: A new ecdysteroid, ponasterone F (1) and the previously reported compound ponasterone A(2) were isolated from specimens of the Arctic marine bryozoan Alcyonidium gelatinosum collected at Hopenbanken, off the coast of Edgeøya, Svalbard. The structure of 1 was elucidated, and the structure of 2 confirmed by spectroscopic methods including 1D and 2D NMR and analysis of HR-MS data. The compounds were evaluated for their ability to affect bacterial survival and cell viability, as well as their agonistic activities towards the estrogen receptors α and β. The compounds were not active in these assays. Compound 2 is an arthropod hormone controlling molting and are known to act as an allelochemical when produced by plants. Even though its structure has been previously reported, this is the first time a ponasterone has been isolated from a bryozoan. A. gelatinosum produced 1 and 2 in concentrations surpassing those expected of hormonal molecules, indicating their function as defence molecules against molting predators. -
Cribrilina Mutabilisn. Sp., an Eelgrass-Associated Bryozoan (Gymnolaemata: Cheilostomata) with Large Variationin Title Zooid Morphology Related to Life History
Cribrilina mutabilisn. sp., an Eelgrass-Associated Bryozoan (Gymnolaemata: Cheilostomata) with Large Variationin Title Zooid Morphology Related to Life History Author(s) Ito, Minako; Onishi, Takumi; Dick, Matthew H. Zoological Science, 32(5), 485-497 Citation https://doi.org/10.2108/zs150079 Issue Date 2015-10 Doc URL http://hdl.handle.net/2115/62926 Type article File Information ZS32-5 485-497.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP ZOOLOGICAL SCIENCE 32: 485–497 (2015) © 2015 Zoological Society of Japan Cribrilina mutabilis n. sp., an Eelgrass-Associated Bryozoan (Gymnolaemata: Cheilostomata) with Large Variation in Zooid Morphology Related to Life History Minako Ito1, Takumi Onishi2, and Matthew H. Dick2* 1Graduate School of Environmental Science, Hokkaido University, Aikappu 1, Akkeshi-cho, Akkeshi-gun 088-1113, Japan 2Department of Natural History Sciences, Faculty of Science, Hokkaido University, N10 W8, Sapporo 060-0810, Japan We describe the cribrimorph cheilostome bryozoan Cribrilina mutabilis n. sp., which we detected as an epibiont on eelgrass (Zostera marina) at Akkeshi, Hokkaido, northern Japan. This species shows three distinct zooid types during summer: the R (rib), I (intermediate), and S (shield) types. Evidence indicates that zooids commit to development as a given type, rather than transform from one type to another with age. Differences in the frontal spinocyst among the types appear to be mediated by a simple developmental mechanism, acceleration or retardation in the production of lateral costal fusions as the costae elongate during ontogeny. Colonies of all three types were identical, or nearly so, in partial nucleotide sequences of the mitochondrial COI gene (555–631 bp), suggesting that they represent a single species. -
Growth Geometry and Measurement of Growth Rates in Marine Bryozoans: a Review
BRYOZOAN STUDIES 2019 Growth geometry and measurement of growth rates in marine bryozoans: a review Abigail M. Smith1* and Marcus M. Key, Jr.2 1 Department of Marine Science, University of Otago, P.O. Box 56, Dunedin 9054, New Zealand [*corresponding author: email: [email protected]] 2 Department of Earth Sciences, Dickinson College, P.O. Box 1773, Carlisle, PA 17013-2896, USA ABSTRACT measuring and reporting growth rate in bryozoans The relationship between age and size in colonial will ensure they are robust and comparable. marine organisms is problematic. While growth of individual units may be measured fairly easily, the growth of colonies can be variable, complex, and INTRODUCTION difficult to measure. We need this information in Bryozoans are lophophorate aquatic invertebrates order to manage and protect ecosystems, acquire which typically form colonies by iterative addition bioactive compounds, and understand the history of of modular clones (zooids). Freshwater species environmental change. Bryozoan colonial growth are uncalcified; the majority of marine species are forms, determined by the pattern of sequential calcified, so that there is an extensive fossil record of addition of zooids or modules, enhance feeding, marine bryozoan colonies. When calcified colonies colony integration, strength, and/or gamete/larval grow large, they can provide benthic structures dispersal. Colony age varies from three months to which enhance biodiversity by provision of sheltered 86 years. Growth and development, including both habitat. Agencies who wish to manage or protect addition of zooids and extrazooidal calcification, these productive habitats need to understand the can be linear, two-dimensional across an area, or longevity and stability of these structures. -
Ctenostomatous Bryozoa from São Paulo, Brazil, with Descriptions of Twelve New Species
Zootaxa 3889 (4): 485–524 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2014 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3889.4.2 http://zoobank.org/urn:lsid:zoobank.org:pub:0256CD93-AE8A-475F-8EB7-2418DF510AC2 Ctenostomatous Bryozoa from São Paulo, Brazil, with descriptions of twelve new species LEANDRO M. VIEIRA1,2, ALVARO E. MIGOTTO2 & JUDITH E. WINSTON3 1Departamento de Zoologia, Centro de Ciências Biológicas, Universidade Federal de Pernambuco, Recife, PE 50670-901, Brazil. E-mail: [email protected] 2Centro de Biologia Marinha, Universidade de São Paulo, São Sebastião, SP 11600–000, Brazil. E-mail: [email protected] 3Smithsonian Marine Station, 701 Seaway Drive, Fort Pierce, FL 34949, USA. E-mail: [email protected] Abstract This paper describes 21 ctenostomatous bryozoans from the state of São Paulo, Brazil, based on specimens observed in vivo. A new family, Jebramellidae n. fam., is erected for a newly described genus and species, Jebramella angusta n. gen. et sp. Eleven other species are described as new: Alcyonidium exiguum n. sp., Alcyonidium pulvinatum n. sp., Alcyonidium torquatum n. sp., Alcyonidium vitreum n. sp., Bowerbankia ernsti n. sp., Bowerbankia evelinae n. sp., Bow- erbankia mobilis n. sp., Nolella elizae n. sp., Panolicella brasiliensis n. sp., Sundanella rosea n. sp., Victorella araceae n. sp. Taxonomic and ecological notes are also included for nine previously described species: Aeverrillia setigera (Hincks, 1887), Alcyonidium hauffi Marcus, 1939, Alcyonidium polypylum Marcus, 1941, Anguinella palmata van Beneden, 1845, Arachnoidella evelinae (Marcus, 1937), Bantariella firmata (Marcus, 1938) n. comb., Nolella sawayai Marcus, 1938, Nolella stipata Gosse, 1855 and Zoobotryon verticillatum (delle Chiaje, 1822). -
Animal Phylum Poster Porifera
Phylum PORIFERA CNIDARIA PLATYHELMINTHES ANNELIDA MOLLUSCA ECHINODERMATA ARTHROPODA CHORDATA Hexactinellida -- glass (siliceous) Anthozoa -- corals and sea Turbellaria -- free-living or symbiotic Polychaetes -- segmented Gastopods -- snails and slugs Asteroidea -- starfish Trilobitomorpha -- tribolites (extinct) Urochordata -- tunicates Groups sponges anemones flatworms (Dugusia) bristleworms Bivalves -- clams, scallops, mussels Echinoidea -- sea urchins, sand Chelicerata Cephalochordata -- lancelets (organisms studied in detail in Demospongia -- spongin or Hydrazoa -- hydras, some corals Trematoda -- flukes (parasitic) Oligochaetes -- earthworms (Lumbricus) Cephalopods -- squid, octopus, dollars Arachnida -- spiders, scorpions Mixini -- hagfish siliceous sponges Xiphosura -- horseshoe crabs Bio1AL are underlined) Cubozoa -- box jellyfish, sea wasps Cestoda -- tapeworms (parasitic) Hirudinea -- leeches nautilus Holothuroidea -- sea cucumbers Petromyzontida -- lamprey Mandibulata Calcarea -- calcareous sponges Scyphozoa -- jellyfish, sea nettles Monogenea -- parasitic flatworms Polyplacophora -- chitons Ophiuroidea -- brittle stars Chondrichtyes -- sharks, skates Crustacea -- crustaceans (shrimp, crayfish Scleropongiae -- coralline or Crinoidea -- sea lily, feather stars Actinipterygia -- ray-finned fish tropical reef sponges Hexapoda -- insects (cockroach, fruit fly) Sarcopterygia -- lobed-finned fish Myriapoda Amphibia (frog, newt) Chilopoda -- centipedes Diplopoda -- millipedes Reptilia (snake, turtle) Aves (chicken, hummingbird) Mammalia -
(Anthozoa) from the Lower Oligocene (Rupelian) of the Eastern Alps, Austria
TO L O N O G E I L C A A P I ' T A A T L E I I A Bollettino della Società Paleontologica Italiana, 59 (3), 2020, 319-336. Modena C N O A S S. P. I. Scleractinian corals (Anthozoa) from the lower Oligocene (Rupelian) of the Eastern Alps, Austria Rosemarie Christine Baron-Szabo* & Diethard Sanders R.C. Baron-Szabo, Department of Invertebrate Zoology, Smithsonian Institution, NMNH, W-205, MRC 163, P.O. Box 37012, Washington DC, 20013- 7012 USA; Forschungsinstitut Senckenberg, Senckenberganlage 25, D-60325 Frankfurt/Main, Germany; [email protected]; Rosemarie.Baron- [email protected] *corresponding author D. Sanders, Institut für Geologie, Universität of Innsbruck, Innrain 52, A-6020 Innsbruck, Austria; [email protected] KEY WORDS - Scleractinia, taxonomy, paleoecology, paleobiogeography. ABSTRACT - In the Werlberg Member (Rupelian pro parte) of the Paisslberg Formation (Eastern Alps), an assemblage of colonial corals of eleven species pertaining to eleven genera and eleven families was identified:Stylocoenia carryensis, Acropora lavandulina, ?Colpophyllia sp., Dendrogyra intermedia, Caulastraea pseudoflabellum, Hydnophyllia costata, Pindosmilia cf. brunni, Actinacis rollei, Pavona profunda, Agathiphyllia gregaria, and Faksephyllia faxoensis. This is the first Oligocene coral assemblage reported from the Paisslberg Formation (Werlberg Member) of the Eastern Alps, consisting exclusively of colonial forms. The assemblage represents the northernmost fauna of reefal corals reported to date for Rupelian time. The Werlberg Member accumulated during marine transgression onto a truncated succession of older carbonate rocks. The corals grew as isolated colonies and in carpets in a protected shoreface setting punctuated by high-energy events. Coral growth forms comprise massive to sublamellar forms, and branched (dendroid, ramose) forms.