GY 112L: Earth History Lab

Total Page:16

File Type:pdf, Size:1020Kb

GY 112L: Earth History Lab UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Week 11 Paleozoic Part 2 Instructor: Dr. Douglas W. Haywick Today’s Agenda The Paleozoic Part 2 (Lab 8 exercises) 1) Sponges & Stromatoporoids 2) Stromatolites 3) Corals 4) Bryozoans 5) Stratigraphy Sponges Sponge Facts: Taxonomy: Phylum: Porifera Sponges Sponge Facts: Taxonomy: Phylum: Porifera Range: Cambrian-Recent Sponges excurrent pore Sponge Facts: incurrent pore Taxonomy: Phylum: Porifera Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder excurrent pore Sponges Sponge Facts: Taxonomy: Phylum: Porifera Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Mineral composition: spongin with spicules or calcite (calcisponges) Sponges Sponge Facts: Taxonomy: Phylum: Porifera Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Mineral composition: spongin with spicules or calcite (calcisponges) Fossil Pres.: mineral replacement or pristine Stromatoporoids Now known to be a type of sponge. They were important paleozoic reef builders Stromatoporoids Stromatoporoid Facts: Taxonomy: Phylum: Porifera Range: Ordovician-Mississippian Cretaceous? Mode of Life: Marine, benthic, filter feeder Mineral composition: calcite Fossil Pres.: pristine Stromatolites The first “visible” fossils Stromatolites Stromatolite Facts: Taxonomy: Kingdom: Cyanobacteria Range: Archean-Recent Mode of Life: Marine, benthic, colonial, photosynthesis Mineral composition: calcite Fossil Pres.: pristine Corals One of the most important animals as far as geology is concerned. They evolved early and showed amazing diversity Corals Coral Facts: Taxonomy: Phylum: Cnidaria Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Mode of Life: Marine, benthic, filter feeder, colonial or solitary (stinging cells) Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Mode of Life: Marine, benthic, filter feeder, colonial or solitary (stinging cells) Mineral composition: calcite or aragonite Corals Coral Facts: Taxonomy: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Mode of Life: Marine, benthic, filter feeder, colonial or solitary (stinging cells) Mineral composition: calcite or aragonite Fossil Pres.: pristine, molds/chalky/replaced Bryozoans (Moss Animals) Bryozoan Facts: Taxonomy: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Bryozoans Bryozoan Facts: Taxonomy: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Bryozoans Bryozoan Facts: Taxonomy: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Mode of Life: Marine, benthic, filter feeder, colonial Bryozoans Bryozoan Facts: Taxonomy: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Mode of Life: Marine, benthic, filter feeder, colonial Mineral composition: calcite and aragonite Bryozoans Bryozoan Facts: Taxonomy: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Mode of Life: Marine, benthic, filter feeder, colonial Mineral composition: calcite and aragonite Fossil Pres.: pristine Bryozoan Forms Digitate Lacy Bryozoan Anatomy The living chambers are called zooecia The animals are called zooids Stratigraphy and Rock Suites Collections of rocks from a specific region that cover a specific time frame 1) Niagara Falls (limestone and dolostone) Stratigraphy and Rock Suites Why a waterfall and not a set of rapids? Consider the stratigraphy. 1) Niagara Falls Stratigraphy and Rock Suites Rate of retreat Lab Time GY 112L: Earth History Lab 8: Paleozoic Rocks and Fossils 2 Instructor: Dr. Doug Haywick [email protected] This is a free open access lecture, but not for commercial purposes. For personal use only. .
Recommended publications
  • "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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Corals (Anthozoa, Tabulata and Rugosa)
    Bulletin de l’Institut Scientifique, Rabat, section Sciences de la Terre, 2008, n°30, 1-12. Corals (Anthozoa, Tabulata and Rugosa) and chaetetids (Porifera) from the Devonian of the Semara area (Morocco) at the Museo Geominero (Madrid, Spain), and their biogeographic significance Andreas MAY Saint Louis University - Madrid campus, Avenida del Valle 34, E-28003 Madrid, Spain e-mail: [email protected] Abstract. The paper describes the three tabulate coral species Caliapora robusta (Pradáčová, 1938), Pachyfavosites tumulosus Janet, 1965 and Thamnopora major (Radugin, 1938), the rugose coral Phillipsastrea ex gr. irregularis (Webster & Fenton in Fenton & Fenton, 1924) and the chaetetid Rhaphidopora crinalis (Schlüter, 1880). The specimens are described for the first time from Givetian and probably Frasnian strata of Semara area (Morocco, former Spanish Sahara). The material is stored in the Museo Geominero in Madrid. The tabulate corals and the chaetetid demonstrate close biogeographic relationships to Central and Eastern Europe as well as to Western Siberia. The fauna does not show any special influence of the Eastern Americas Realm. Key words: Anthozoa, biogeography, Devonian, tabulate corals, Morocco, West Sahara palaeogeographic province Coraux (Anthozoa, Tabulata et Rugosa) et chaetétides (Porifera) du Dévonien de la région de Smara (Maroc) déposés au Museo Geominero (Madrid) et leur signification biogéographique. Résumé. L´article décrit trois espèces de coraux tabulés : Caliapora robusta (Pradáčová, 1938), Pachyfavosites tumulosus Janet, 1965, et Thamnopora major (Radugin, 1938), le corail rugueux Phillipsastrea ex gr. irregularis (Webster & Fenton in Fenton & Fenton, 1924) ainsi que le chaetétide Rhaphidopora crinalis (Schlüter, 1880). Les spécimens, entreposés au Museo Geominero de Madrid, proviennent des couches givétiennes et probablement frasniennes de différents gisements de la région de Smara (Maroc, ancien Sahara espagnol), d’où elles sont décrites pour la première fois.
    [Show full text]
  • Comprehensive Phylogenomic Analyses Resolve Cnidarian Relationships and the Origins of Key Organismal Traits
    Comprehensive phylogenomic analyses resolve cnidarian relationships and the origins of key organismal traits Ehsan Kayal1,2, Bastian Bentlage1,3, M. Sabrina Pankey5, Aki H. Ohdera4, Monica Medina4, David C. Plachetzki5*, Allen G. Collins1,6, Joseph F. Ryan7,8* Authors Institutions: 1. Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution 2. UPMC, CNRS, FR2424, ABiMS, Station Biologique, 29680 Roscoff, France 3. Marine Laboratory, university of Guam, UOG Station, Mangilao, GU 96923, USA 4. Department of Biology, Pennsylvania State University, University Park, PA, USA 5. Department of Molecular, Cellular and Biomedical Sciences, University of New Hampshire, Durham, NH, USA 6. National Systematics Laboratory, NOAA Fisheries, National Museum of Natural History, Smithsonian Institution 7. Whitney Laboratory for Marine Bioscience, University of Florida, St Augustine, FL, USA 8. Department of Biology, University of Florida, Gainesville, FL, USA PeerJ Preprints | https://doi.org/10.7287/peerj.preprints.3172v1 | CC BY 4.0 Open Access | rec: 21 Aug 2017, publ: 21 Aug 20171 Abstract Background: The phylogeny of Cnidaria has been a source of debate for decades, during which nearly all-possible relationships among the major lineages have been proposed. The ecological success of Cnidaria is predicated on several fascinating organismal innovations including symbiosis, colonial body plans and elaborate life histories, however, understanding the origins and subsequent diversification of these traits remains difficult due to persistent uncertainty surrounding the evolutionary relationships within Cnidaria. While recent phylogenomic studies have advanced our knowledge of the cnidarian tree of life, no analysis to date has included genome scale data for each major cnidarian lineage. Results: Here we describe a well-supported hypothesis for cnidarian phylogeny based on phylogenomic analyses of new and existing genome scale data that includes representatives of all cnidarian classes.
    [Show full text]
  • Guide to the Identification of Precious and Semi-Precious Corals in Commercial Trade
    'l'llA FFIC YvALE ,.._,..---...- guide to the identification of precious and semi-precious corals in commercial trade Ernest W.T. Cooper, Susan J. Torntore, Angela S.M. Leung, Tanya Shadbolt and Carolyn Dawe September 2011 © 2011 World Wildlife Fund and TRAFFIC. All rights reserved. ISBN 978-0-9693730-3-2 Reproduction and distribution for resale by any means photographic or mechanical, including photocopying, recording, taping or information storage and retrieval systems of any parts of this book, illustrations or texts is prohibited without prior written consent from World Wildlife Fund (WWF). Reproduction for CITES enforcement or educational and other non-commercial purposes by CITES Authorities and the CITES Secretariat is authorized without prior written permission, provided the source is fully acknowledged. Any reproduction, in full or in part, of this publication must credit WWF and TRAFFIC North America. The views of the authors expressed in this publication do not necessarily reflect those of the TRAFFIC network, WWF, or the International Union for Conservation of Nature (IUCN). The designation of geographical entities in this publication and the presentation of the material do not imply the expression of any opinion whatsoever on the part of WWF, TRAFFIC, or IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The TRAFFIC symbol copyright and Registered Trademark ownership are held by WWF. TRAFFIC is a joint program of WWF and IUCN. Suggested citation: Cooper, E.W.T., Torntore, S.J., Leung, A.S.M, Shadbolt, T. and Dawe, C.
    [Show full text]
  • Lee-Riding-2018.Pdf
    Earth-Science Reviews 181 (2018) 98–121 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Marine oxygenation, lithistid sponges, and the early history of Paleozoic T skeletal reefs ⁎ Jeong-Hyun Leea, , Robert Ridingb a Department of Geology and Earth Environmental Sciences, Chungnam National University, Daejeon 34134, Republic of Korea b Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996, USA ARTICLE INFO ABSTRACT Keywords: Microbial carbonates were major components of early Paleozoic reefs until coral-stromatoporoid-bryozoan reefs Cambrian appeared in the mid-Ordovician. Microbial reefs were augmented by archaeocyath sponges for ~15 Myr in the Reef gap early Cambrian, by lithistid sponges for the remaining ~25 Myr of the Cambrian, and then by lithistid, calathiid Dysoxia and pulchrilaminid sponges for the first ~25 Myr of the Ordovician. The factors responsible for mid–late Hypoxia Cambrian microbial-lithistid sponge reef dominance remain unclear. Although oxygen increase appears to have Lithistid sponge-microbial reef significantly contributed to the early Cambrian ‘Explosion’ of marine animal life, it was followed by a prolonged period dominated by ‘greenhouse’ conditions, as sea-level rose and CO2 increased. The mid–late Cambrian was unusually warm, and these elevated temperatures can be expected to have lowered oxygen solubility, and to have promoted widespread thermal stratification resulting in marine dysoxia and hypoxia. Greenhouse condi- tions would also have stimulated carbonate platform development, locally further limiting shallow-water cir- culation. Low marine oxygenation has been linked to episodic extinctions of phytoplankton, trilobites and other metazoans during the mid–late Cambrian.
    [Show full text]
  • (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.
    [Show full text]
  • Sponges) and Phylum Cnidaria (Jellyfish, Sea Anemones and Corals
    4/14/2014 Kingdom Animalia: Phylum Porifera (sponges) and Phylum Cnidaria (jellyfish, sea anemones and corals) 1 4/14/2014 Animals have different types of symmetry AsymmetricalÆ Radial Æ Bilateral Æ Embryo development provides information about how animal groups are related Blastula: hallow with a single layer of cells Gastrula: results in two layers of cells and cavity (gut) with one opening (blastopore) Cavity reaches the other side and the gut is like a tube Some cells from a third layer of cells A second cavityyg forms between the gut and the outside of the animal 2 4/14/2014 Animals have different number of true tissue layers and different type of gut No true tissuesÆ Two tissue layers Æ Three tissue layersÆ No gutÆ Sac like gutÆ Tube like gutÆ Phylum Porifera: Simplest of Animals Sponges: No tissues, no symmetry Intracellular digestion, no digestive system or cavity Collar cells or choanocytes Support by spicules or spongin fibers 3 4/14/2014 Procedure 1 • Grantia sponge Locate osculum • Sponge spicules Bell Labs Research on Deep-Sea Sponge Yields Substantial Mechanical Engineering Insights 4 4/14/2014 Medications from Sponges Thirty percent of all potential new natural medicine has been isolated in sponges. About 75% of the recently registered and patented material to fight cancer comes from sponges. Furthermore, it appears that medicine from sponges helps, for example, asthma and psoriasis; therefore it offers enormous possibilities for research. Eribulin, a novel chemotherapy drug derived from a sea sponge, improves survival in heavily-pretreated metastatic breast cancer. Phylum Cnidaria Coral Sea Anemone Man-of-war Hydra Jellyfish 5 4/14/2014 Phylum Cnidaria Tissues: Endoderm Ectoderm Type of gut: Symmetry: Radial Cnidocytes or Stinging cells Polyp or Medusa form Importance Some jellyfish are considered a delicacy Corals: Medicines cabinets for the 21st century cancer cell inhibitor Sunscreen 6 4/14/2014 Procedure 2 2.
    [Show full text]
  • On Some Hydroids (Cnidaria) from the Coast of Pakistan
    Pakistan J. Zool., vol. 38(3), pp. 225-232, 2006. On Some Hydroids (Cnidaria) from the Coast of Pakistan NASEEM MOAZZAM AND MOHAMMAD MOAZZAM Institute of Marine Sciences, University of Karachi, Karachi 75270, Pakistan (NM) and Marine Fisheries Department, Government of Pakistan, Fish Harbour, West Wharf, Karachi 74900, Pakistan (MM) Abstract .- The paper deals with the occurrence of eleven species of the hydroids from the coast of Pakistan. All the species are reported for the first time from Pakistan. These species are Hydractinia epidocleensis, Pennaria disticha, Eudendrium capillare, Orthopyxis cf. crenata, Clytia noliformis, C. hummelincki, Dynamena crisioides, D. quadridentata, Sertularia distans, Pycnotheca mirabilis and Macrorhynchia philippina. Key words: Hydroids, Coelenterata, Pakistan, Hydractinia, Pennaria, Eudendrium, Orthopyxis, Clytia, Dynamena, Sertularia, Pycnotheca, Macrorhynchia. INTRODUCTION used in the paper are derived from Millard (1975), Gibbons and Ryland (1989), Ryland and Gibbons (1991). In comparison to other invertebrates, TAXONOMIC ENUMERATION hydroids are one of the least known groups of marine animals from the coast of Pakistan Haque Family BOUGAINVILLIIDAE (1977) reported a few Cnidaria from the Pakistani Genus HYDRACTINIA Van Beneden, 1841 coast including two hydroids i.e. Plumularia flabellum Allman, 1883 (= P. insignis Allman, 1. Hydractinia epidocleensis Leloup, 1931 1883) and Campanularia juncea Allman, 1874 (= (Fig. 1) Thyroscyphus junceus (Allman, 1876) from Keamari and Bhit Island, Karachi, respectively. Ahmed and Hameed (1999), Ahmed et al. (1978) and Haq et al. (1978) have mentioned the presence of hydroids in various habitats along the coast of Pakistan. Javed and Mustaquim (1995) reported Sertularia turbinata (Lamouroux, 1816) from Manora Channel, Karachi. The present paper describes eleven species of Cnidaria collected from the Pakistani coast all of which are new records for Pakistan.
    [Show full text]
  • Sponges and Bryozoans of Sandusky Bay
    Ohio Naturalist. [Vol. 1, No. SPONGES AND BRYOZOANS OF SANDUSKY BAY. F. L. LANDACRE. The two small groups of fresh water sponges and Bryozoa re- ceived some attention at the Lake laboratory during the summer of 1900 All our fresh water sponges belong to one family, the SpongiUidae, which has about seven genera. They differ from the marine sponges- in two particulars. They form skeletons of silicon only, while marine sponges may form silicious or limy or spongin skeletons. The spongin skeleton-is the-one that gives the bath sponge its value.. They also form winter buds or statoblasts which carry the sponge over the winter and reproduce it again in the spring. This peculiar process was probably acquired on account of the changes in temperature and in amount of moisture to which animals living in fresh water streams are subjected. The sponge dies in the fall of the year and its skeleton of silicious spines or spicules can be found with no protoplasm. The character of the spines in the body of the sponge and those surrounding the statoblast differ greatly, and those around the statoblast are the main reliance in identifying sponges. So that if a statoblast is found the sponge from which it came can be determined, and on the other hand it is frequently very difficult to determine the species of a sponge if it has not yet formed its stato- blast. The statoblast is a globular or disc-shaped, nitroginous cell with a chimney-like opening where the protoplasm escapes in the spring. The adult sponge is non-sexual but the statoblasts give rise to ova and spermatozoa which unite and produce a new sponge.
    [Show full text]
  • Note on the Fine Skeletal Structures in Scleractinia and in Tabulata
    Title Note on the Fine Skeletal Structures in Scleractinia and in Tabulata Author(s) Kato, Makoto Citation Journal of the Faculty of Science, Hokkaido University. Series 4, Geology and mineralogy, 14(1), 51-56 Issue Date 1968-02 Doc URL http://hdl.handle.net/2115/35982 Type bulletin (article) File Information 14(1)_51-56.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP NOTE ON THE FINE SKELETAL STRUCTURES IN SCLERACTINIA AND IN TABULATA by Makoto KATo (with 1 Text-figure) (Contribution from the Department of Geology and Mineralogy, Faculty of Science, Hokl<aido University. No. 1069) On the fine sketetal structures in Scleractinia Scleractinia is a vast group including reef corals of recent time. Much knowl- edge on the ecology, physiology and so on of the recent Scleractinians has been accumulated up to the present by a number of research worlcers. By deduction, biological aspects of fossil Scleractinians may be readily sought in these data on recent corals. Being an extinct group, however, nothing definite has been ascertained as to the true biological aspects of Palaeozoic Rugosa, though many functional features or conditions of Scleractinia can be also attributed to Rugosa, since the former is the nearest ally to the latter. Hence, one must study in every detail the biology of the recent Scleractinia, for the thorough understanding of Palaeozoic Rugosa, It is well known that in Scleractinia microstructure of coral skeleton has been taken as a clue to major divisions of the group. (VAuGHAN 8c WELLs, 1943 : WEms, 1956) Recent comprehensive work on Scleractinia by ALLoiTEAu (1957) also gave importance to the microstructure in the classification of the said group, For the sake of comparison with Palaeozoic corals, the writer also examined many thin sections of Scleractinians kept at the British Museum of Natural History.
    [Show full text]