Structural Arrangement and Properties of Spicules in Glass Sponges
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(1104L) Animal Kingdom Part I
(1104L) Animal Kingdom Part I By: Jeffrey Mahr (1104L) Animal Kingdom Part I By: Jeffrey Mahr Online: < http://cnx.org/content/col12086/1.1/ > OpenStax-CNX This selection and arrangement of content as a collection is copyrighted by Jerey Mahr. It is licensed under the Creative Commons Attribution License 4.0 (http://creativecommons.org/licenses/by/4.0/). Collection structure revised: October 17, 2016 PDF generated: October 17, 2016 For copyright and attribution information for the modules contained in this collection, see p. 58. Table of Contents 1 (1104L) Animals introduction ....................................................................1 2 (1104L) Characteristics of Animals ..............................................................3 3 (1104L)The Evolutionary History of the Animal Kingdom ..................................11 4 (1104L) Phylum Porifera ........................................................................23 5 (1104L) Phylum Cnidaria .......................................................................31 6 (1104L) Phylum Rotifera & Phylum Platyhelminthes ........................................45 Glossary .............................................................................................53 Index ................................................................................................56 Attributions .........................................................................................58 iv Available for free at Connexions <http://cnx.org/content/col12086/1.1> Chapter 1 (1104L) Animals introduction1 -
Review of the Mineralogy of Calcifying Sponges
Dickinson College Dickinson Scholar Faculty and Staff Publications By Year Faculty and Staff Publications 12-2013 Not All Sponges Will Thrive in a High-CO2 Ocean: Review of the Mineralogy of Calcifying Sponges Abigail M. Smith Jade Berman Marcus M. Key, Jr. Dickinson College David J. Winter Follow this and additional works at: https://scholar.dickinson.edu/faculty_publications Part of the Paleontology Commons Recommended Citation Smith, Abigail M.; Berman, Jade; Key,, Marcus M. Jr.; and Winter, David J., "Not All Sponges Will Thrive in a High-CO2 Ocean: Review of the Mineralogy of Calcifying Sponges" (2013). Dickinson College Faculty Publications. Paper 338. https://scholar.dickinson.edu/faculty_publications/338 This article is brought to you for free and open access by Dickinson Scholar. It has been accepted for inclusion by an authorized administrator. For more information, please contact [email protected]. © 2013. Licensed under the Creative Commons http://creativecommons.org/licenses/by- nc-nd/4.0/ Elsevier Editorial System(tm) for Palaeogeography, Palaeoclimatology, Palaeoecology Manuscript Draft Manuscript Number: PALAEO7348R1 Title: Not all sponges will thrive in a high-CO2 ocean: Review of the mineralogy of calcifying sponges Article Type: Research Paper Keywords: sponges; Porifera; ocean acidification; calcite; aragonite; skeletal biomineralogy Corresponding Author: Dr. Abigail M Smith, PhD Corresponding Author's Institution: University of Otago First Author: Abigail M Smith, PhD Order of Authors: Abigail M Smith, PhD; Jade Berman, PhD; Marcus M Key Jr, PhD; David J Winter, PhD Abstract: Most marine sponges precipitate silicate skeletal elements, and it has been predicted that they would be among the few "winners" in an acidifying, high-CO2 ocean. -
Tabachnickia Nom. Nov., a New Name for the Preoccupied Sponge Genus Platella Tabachnick, 1988 (Porifera: Hexactenellida)
_____________Mun. Ent. Zool. Vol. 5, No. 1, January 2010__________ 297 SCIENTIFIC NOTE TABACHNICKIA NOM. NOV., A NEW NAME FOR THE PREOCCUPIED SPONGE GENUS PLATELLA TABACHNICK, 1988 (PORIFERA: HEXACTENELLIDA) Hüseyin Özdikmen* * Gazi Üniversitesi, Fen-Edebiyat Fakültesi, Biyoloji Bölümü, 06500 Ankara / TÜRKİYE. E- mail: [email protected] [Özdikmen, H. 2010. Tabachnickia nom. nov., a new name for the preoccupied sponge genus Platella Tabachnick, 1988 (Porifera: Hexactenellida). Munis Entomology & Zoology, 5 (1): 297-298] Family HYALONEMATIDAE Genus TABACHNICKIA nom. nov. Platella Tabachnick, 1988. In Academy of Sciences of the USSR. Structural and functional researches of the marine benthos. Academy of Sciences of the USSR, Moscow: 52. (Porifera: Hexactenellida: Amphidiscophora: Amphidiscosida: Hyalonematidae). Preoccupied by Platella Coryell & Fields, 1937. Amer. Mus. Novit., no. 956, 3. (Crustaceae: Ostracoda: Podocopa: Platycopida: Platycopina: Cytherelloidea: Cytherellidae). Remarks on nomenclatural change: Tabachnick (1988) described a monotypic genus Platella for a sponge with the type species Platella polybasalia Tabachnick, 1988 by the original designation from Central Pacific. It is stil used as a valid genus name (e.g. Tabachnick & Menshenina, 2002). Unfortunately, the generic name was already preoccupied by Coryell & Fields (1937), who had described the genus Platella for a fossil ostracod with the type species Platella gatunensis Coryell & Fields, 1937 from Panama. Then Puri (1960) described a new species in the genus as Platella mulleri Puri, 1960. It was assigned to Cytherellidae by Benson et al. (1961); and to Platycopida by Sepkoski (2002). Thus, the genus name Platella Tabachnick, 1988 is a junior homonym of the genus name Platella Coryell & Fields, 1937. So I propose a new replacement name Tabachnickia nom. -
The Lower Bathyal and Abyssal Seafloor Fauna of Eastern Australia T
O’Hara et al. Marine Biodiversity Records (2020) 13:11 https://doi.org/10.1186/s41200-020-00194-1 RESEARCH Open Access The lower bathyal and abyssal seafloor fauna of eastern Australia T. D. O’Hara1* , A. Williams2, S. T. Ahyong3, P. Alderslade2, T. Alvestad4, D. Bray1, I. Burghardt3, N. Budaeva4, F. Criscione3, A. L. Crowther5, M. Ekins6, M. Eléaume7, C. A. Farrelly1, J. K. Finn1, M. N. Georgieva8, A. Graham9, M. Gomon1, K. Gowlett-Holmes2, L. M. Gunton3, A. Hallan3, A. M. Hosie10, P. Hutchings3,11, H. Kise12, F. Köhler3, J. A. Konsgrud4, E. Kupriyanova3,11,C.C.Lu1, M. Mackenzie1, C. Mah13, H. MacIntosh1, K. L. Merrin1, A. Miskelly3, M. L. Mitchell1, K. Moore14, A. Murray3,P.M.O’Loughlin1, H. Paxton3,11, J. J. Pogonoski9, D. Staples1, J. E. Watson1, R. S. Wilson1, J. Zhang3,15 and N. J. Bax2,16 Abstract Background: Our knowledge of the benthic fauna at lower bathyal to abyssal (LBA, > 2000 m) depths off Eastern Australia was very limited with only a few samples having been collected from these habitats over the last 150 years. In May–June 2017, the IN2017_V03 expedition of the RV Investigator sampled LBA benthic communities along the lower slope and abyss of Australia’s eastern margin from off mid-Tasmania (42°S) to the Coral Sea (23°S), with particular emphasis on describing and analysing patterns of biodiversity that occur within a newly declared network of offshore marine parks. Methods: The study design was to deploy a 4 m (metal) beam trawl and Brenke sled to collect samples on soft sediment substrata at the target seafloor depths of 2500 and 4000 m at every 1.5 degrees of latitude along the western boundary of the Tasman Sea from 42° to 23°S, traversing seven Australian Marine Parks. -
The Unique Skeleton of Siliceous Sponges (Porifera; Hexactinellida and Demospongiae) That Evolved first from the Urmetazoa During the Proterozoic: a Review” by W
Biogeosciences Discuss., 4, S262–S276, 2007 Biogeosciences www.biogeosciences-discuss.net/4/S262/2007/ BGD Discussions c Author(s) 2007. This work is licensed 4, S262–S276, 2007 under a Creative Commons License. Interactive Comment Interactive comment on “The unique skeleton of siliceous sponges (Porifera; Hexactinellida and Demospongiae) that evolved first from the Urmetazoa during the Proterozoic: a review” by W. E. G. Müller et al. W. E. G. Müller et al. Received and published: 3 April 2007 3rd April 2007 Full Screen / Esc From : Prof. Dr. W.E.G. Müller, Institut für Physiologische Chemie, Abteilung Ange- wandte Molekularbiologie, Universität, Duesbergweg 6, 55099 Mainz; GERMANY. tel.: Printer-friendly Version +49-6131-392-5910; fax.: +49-6131-392-5243; E-mail: [email protected] To the Editorial Board Interactive Discussion MS-NR: bgd-2006-0069 Discussion Paper S262 EGU Dear colleagues: BGD Thank you for your email from April 2nd informing me that our manuscript entitled: 4, S262–S276, 2007 The unique skeleton of siliceous sponges (Porifera; Hexactinellida and Demospongiae) that evolved first from the Urmetazoa during the Proterozoic: a review by: Werner E.G. Müller, Jinhe Li, Heinz C. Schröder, Li Qiao and Xiaohong Wang Interactive Comment which we submit for the Journal Biogeosciences must be revised. In the following we discuss point for point the arguments raised by the referees/reader. In detail: Interactive comment on “The unique skeleton of siliceous sponges (Porifera; Hex- actinellida and Demospongiae) that evolved first from the Urmetazoa during the Pro- terozoic: a review” by W. E. G. Müller et al. By: M. -
Hexasterophoran Glass Sponges of New Zealand (Porifera: Hexactinellida: Hexasterophora): Orders Hexactinosida, Aulocalycoida and Lychniscosida
Hexactinellida: Hexasterophora): Orders Hexactinosida, Aulocalycoida and Lychniscosida Aulocalycoida and Lychniscosida Hexactinellida: Hexasterophora): Orders Hexactinosida, The Marine Fauna of New Zealand: Hexasterophoran Glass Sponges Zealand (Porifera: ISSN 1174–0043; 124 Henry M. Reiswig and Michelle Kelly The Marine Fauna of New Zealand: Hexasterophoran Glass Sponges of New Zealand (Porifera: Hexactinellida: Hexasterophora): Orders Hexactinosida, Aulocalycoida and Lychniscosida Henry M. Reiswig and Michelle Kelly NIWA Biodiversity Memoir 124 COVER PHOTO Two unidentified hexasterophoran glass sponge species, the first possibly Farrea onychohexastera n. sp. (frilly white honeycomb sponge in several bushy patches), and the second possibly Chonelasma lamella, but also possibly C. chathamense n. sp. (lower left white fan), attached to the habitat-forming coral Solenosmilia variabilis, dominant at 1078 m on the Graveyard seamount complex of the Chatham Rise (NIWA station TAN0905/29: 42.726° S, 179.897° W). Image captured by DTIS (Deep Towed Imaging System) onboard RV Tangaroa, courtesy of NIWA Seamounts Programme (SFAS103), Oceans2020 (LINZ, MFish) and Rob Stewart, NIWA, Wellington (Photo: NIWA). This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NATIONAL INSTITUTE OF WATER AND ATMOSPHERIC RESEARCH (NIWA) The Marine Fauna of New Zealand: Hexasterophoran Glass Sponges of New Zealand (Porifera: Hexactinellida: -
An Integrative Systematic Framework Helps to Reconstruct Skeletal
Dohrmann et al. Frontiers in Zoology (2017) 14:18 DOI 10.1186/s12983-017-0191-3 RESEARCH Open Access An integrative systematic framework helps to reconstruct skeletal evolution of glass sponges (Porifera, Hexactinellida) Martin Dohrmann1*, Christopher Kelley2, Michelle Kelly3, Andrzej Pisera4, John N. A. Hooper5,6 and Henry M. Reiswig7,8 Abstract Background: Glass sponges (Class Hexactinellida) are important components of deep-sea ecosystems and are of interest from geological and materials science perspectives. The reconstruction of their phylogeny with molecular data has only recently begun and shows a better agreement with morphology-based systematics than is typical for other sponge groups, likely because of a greater number of informative morphological characters. However, inconsistencies remain that have far-reaching implications for hypotheses about the evolution of their major skeletal construction types (body plans). Furthermore, less than half of all described extant genera have been sampled for molecular systematics, and several taxa important for understanding skeletal evolution are still missing. Increased taxon sampling for molecular phylogenetics of this group is therefore urgently needed. However, due to their remote habitat and often poorly preserved museum material, sequencing all 126 currently recognized extant genera will be difficult to achieve. Utilizing morphological data to incorporate unsequenced taxa into an integrative systematics framework therefore holds great promise, but it is unclear which methodological approach best suits this task. Results: Here, we increase the taxon sampling of four previously established molecular markers (18S, 28S, and 16S ribosomal DNA, as well as cytochrome oxidase subunit I) by 12 genera, for the first time including representatives of the order Aulocalycoida and the type genus of Dactylocalycidae, taxa that are key to understanding hexactinellid body plan evolution. -
The Unique Skeleton of Siliceous Sponges (Porifera; Hexactinellida and Demospongiae) That Evolved first from the Urmetazoa During the Proterozoic: a Review
Biogeosciences, 4, 219–232, 2007 www.biogeosciences.net/4/219/2007/ Biogeosciences © Author(s) 2007. This work is licensed under a Creative Commons License. The unique skeleton of siliceous sponges (Porifera; Hexactinellida and Demospongiae) that evolved first from the Urmetazoa during the Proterozoic: a review W. E. G. Muller¨ 1, Jinhe Li2, H. C. Schroder¨ 1, Li Qiao3, and Xiaohong Wang4 1Institut fur¨ Physiologische Chemie, Abteilung Angewandte Molekularbiologie, Duesbergweg 6, 55099 Mainz, Germany 2Institute of Oceanology, Chinese Academy of Sciences, 7 Nanhai Road, 266071 Qingdao, P. R. China 3Department of Materials Science and Technology, Tsinghua University, 100084 Beijing, P. R. China 4National Research Center for Geoanalysis, 26 Baiwanzhuang Dajie, 100037 Beijing, P. R. China Received: 8 January 2007 – Published in Biogeosciences Discuss.: 6 February 2007 Revised: 10 April 2007 – Accepted: 20 April 2007 – Published: 3 May 2007 Abstract. Sponges (phylum Porifera) had been considered an axial filament which harbors the silicatein. After intracel- as an enigmatic phylum, prior to the analysis of their genetic lular formation of the first lamella around the channel and repertoire/tool kit. Already with the isolation of the first ad- the subsequent extracellular apposition of further lamellae hesion molecule, galectin, it became clear that the sequences the spicules are completed in a net formed of collagen fibers. of sponge cell surface receptors and of molecules forming the The data summarized here substantiate that with the find- intracellular signal transduction pathways triggered by them, ing of silicatein a new aera in the field of bio/inorganic chem- share high similarity with those identified in other metazoan istry started. -
The Lower Bathyal and Abyssal Seafloor Fauna of Eastern Australia T
The lower bathyal and abyssal seafloor fauna of eastern Australia T. O’hara, A. Williams, S. Ahyong, P. Alderslade, T. Alvestad, D. Bray, I. Burghardt, N. Budaeva, F. Criscione, A. Crowther, et al. To cite this version: T. O’hara, A. Williams, S. Ahyong, P. Alderslade, T. Alvestad, et al.. The lower bathyal and abyssal seafloor fauna of eastern Australia. Marine Biodiversity Records, Cambridge University Press, 2020, 13 (1), 10.1186/s41200-020-00194-1. hal-03090213 HAL Id: hal-03090213 https://hal.archives-ouvertes.fr/hal-03090213 Submitted on 29 Dec 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. O’Hara et al. Marine Biodiversity Records (2020) 13:11 https://doi.org/10.1186/s41200-020-00194-1 RESEARCH Open Access The lower bathyal and abyssal seafloor fauna of eastern Australia T. D. O’Hara1* , A. Williams2, S. T. Ahyong3, P. Alderslade2, T. Alvestad4, D. Bray1, I. Burghardt3, N. Budaeva4, F. Criscione3, A. L. Crowther5, M. Ekins6, M. Eléaume7, C. A. Farrelly1, J. K. Finn1, M. N. Georgieva8, A. Graham9, M. Gomon1, K. Gowlett-Holmes2, L. M. Gunton3, A. Hallan3, A. M. Hosie10, P. -
Formation of Giant Spicules in the Deep-Sea Hexactinellid Monorhaphis Chuni (Schulze 1904): Electron-Microscopic and Biochemical Studies
Cell Tissue Res (2007) 329:363–378 DOI 10.1007/s00441-007-0402-x REGULAR ARTICLE Formation of giant spicules in the deep-sea hexactinellid Monorhaphis chuni (Schulze 1904): electron-microscopic and biochemical studies Werner E. G. Müller & Carsten Eckert & Klaus Kropf & Xiaohong Wang & Ute Schloßmacher & Christopf Seckert & Stephan E. Wolf & Wolfgang Tremel & Heinz C. Schröder Received: 25 November 2006 /Accepted: 19 February 2007 / Published online: 4 April 2007 # Springer-Verlag 2007 Abstract The siliceous sponge Monorhaphis chuni (Hexa- spicules; it harbors the axial filament and is surrounded by ctinellida) synthesizes the largest biosilica structures on an axial cylinder (100–150 μm) of electron-dense homo- earth (3 m). Scanning electron microscopy has shown that geneous silica. During dissolution of the spicules with these spicules are regularly composed of concentrically hydrofluoric acid, the axial filament is first released arranged lamellae (width: 3–10 μm). Between 400 and 600 followed by the release of a proteinaceous tubule. Two lamellae have been counted in one giant basal spicule. An major proteins (150 kDa and 35 kDa) have been visualized, axial canal (diameter: ~2 μm) is located in the center of the together with a 24-kDa protein that cross-reacts with antibodies against silicatein. The spicules are surrounded by a collagen net, and the existence of a hexactinellidan Carsten Eckert was previously with the Museum für Naturkunde, collagen gene has been demonstrated by cloning it from Invalidenstrasse 43, 10115 Berlin, Germany. Aphrocallistes vastus. During the axial growth of the The collagen sequence from Aphrocallistes vastus reported here, viz., spicules, silicatein or the silicatein-related protein is [COL_APHRO] APHVACOL (accession number AM411124), has been deposited in the EMBL/GenBank data base. -
An Annotated Checklist of the Marine Macroinvertebrates of Alaska David T
NOAA Professional Paper NMFS 19 An annotated checklist of the marine macroinvertebrates of Alaska David T. Drumm • Katherine P. Maslenikov Robert Van Syoc • James W. Orr • Robert R. Lauth Duane E. Stevenson • Theodore W. Pietsch November 2016 U.S. Department of Commerce NOAA Professional Penny Pritzker Secretary of Commerce National Oceanic Papers NMFS and Atmospheric Administration Kathryn D. Sullivan Scientific Editor* Administrator Richard Langton National Marine National Marine Fisheries Service Fisheries Service Northeast Fisheries Science Center Maine Field Station Eileen Sobeck 17 Godfrey Drive, Suite 1 Assistant Administrator Orono, Maine 04473 for Fisheries Associate Editor Kathryn Dennis National Marine Fisheries Service Office of Science and Technology Economics and Social Analysis Division 1845 Wasp Blvd., Bldg. 178 Honolulu, Hawaii 96818 Managing Editor Shelley Arenas National Marine Fisheries Service Scientific Publications Office 7600 Sand Point Way NE Seattle, Washington 98115 Editorial Committee Ann C. Matarese National Marine Fisheries Service James W. Orr National Marine Fisheries Service The NOAA Professional Paper NMFS (ISSN 1931-4590) series is pub- lished by the Scientific Publications Of- *Bruce Mundy (PIFSC) was Scientific Editor during the fice, National Marine Fisheries Service, scientific editing and preparation of this report. NOAA, 7600 Sand Point Way NE, Seattle, WA 98115. The Secretary of Commerce has The NOAA Professional Paper NMFS series carries peer-reviewed, lengthy original determined that the publication of research reports, taxonomic keys, species synopses, flora and fauna studies, and data- this series is necessary in the transac- intensive reports on investigations in fishery science, engineering, and economics. tion of the public business required by law of this Department. -
Zootaxa 20 Years: Phylum Porifera
Zootaxa 4979 (1): 038–056 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Review ZOOTAXA Copyright © 2021 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4979.1.8 http://zoobank.org/urn:lsid:zoobank.org:pub:3409F59A-0552-44A8-89F0-4F0230CB27E7 Zootaxa 20 years: Phylum Porifera JOHN N.A. HOOPER1,2*, GERT WÖRHEIDE3,4,5, EDUARDO HAJDU6, DIRK ERPENBECK3,5, NICOLE J. DE VOOGD7,8 & MICHELLE KLAUTAU9 1Queensland Museum, PO Box 3300, South Brisbane 4101, Brisbane, Queensland, Australia [email protected], https://orcid.org/0000-0003-1722-5954 2Griffith Institute for Drug Discovery, Griffith University, Brisbane 4111, Queensland, Australia 3Department of Earth- and Environmental Sciences, Ludwig-Maximilians-Universität, Richard-Wagner Straße 10, 80333 Munich, Germany 4SNSB-Bavarian State Collection of Palaeontology and Geology, Richard-Wagner Straße 10, 80333 Munich, Germany 5GeoBio-Center, Ludwig-Maximilians-Universität München, Richard-Wagner Straße 10, 80333 Munich, Germany [email protected], https://orcid.org/0000-0002-6380-7421 [email protected], https://orcid.org/0000-0003-2716-1085 6Museu Nacional/UFRJ, TAXPO - Depto. Invertebrados, Quinta da Boa Vista, s/n 20940-040, Rio de Janeiro, RJ, BRASIL [email protected], https://orcid.org/0000-0002-8760-9403 7Naturalis Biodiversity Center, Dept. Marine Biodiversity, P.O. Box 9617, 2300 RA Leiden, The Netherlands [email protected], https://orcid.org/0000-0002-7985-5604 8Institute of Environmental Sciences, Leiden University, Leiden, The Netherlands 9Universidade Federal do Rio de Janeiro, Instituto de Biologia, Departamento de Zoologia, Av. Carlos Chagas Filho, 373, CEP 21941- 902, Rio de Janeiro, RJ, Brasil.