Biotextbookch21-29.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
(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. -
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. -
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. -
Paleo-The Story of Life
PALEO: THE STORY OF LIFE Life on Earth has not always existed as it currently does. The fact that life began on Earth in the first place is miraculous due to the environmental factors needed for its beginnings and sustainability. The relentless pursuit of life over billions of years from small living molecules to complex creatures roaming, flying and swimming throughout the Earth has culminated into the current state of life’s existence as we know it on the planet we call home. Paleo: The Story of Life is a 3,000-square-foot exhibit, spanning 4.6 billion years in scope. The exhibit presents casts of 128 rare fossils, including Lucy, Archaeopteryx and T rex, among many others. Drawn from the world’s foremost fossil collections, the Paleo exhibit showcases casts of rare fossils from the Americas, Europe, Asia, Africa and Australia – skeletons, skulls, claws and eggs gathered from prestigious museums, including the Smithsonian Institution, American Museum of Natural History, Royal Ontario Museum and Carnegie Museum, among others. Rarely available for viewing outside of their respective museums, these compelling artifacts are presented exclusively in Paleo: The Story of Life. Fossils range from the earliest invertebrate marine life through the Triassic, Jurassic and Cretaceous dinosaurs to mammals and prehistoric humans. Paleo: The Story of Life explores the comprehensive story of prehistoric life on Earth. The Paleo exhibit is a visiting exhibit and will be on display through Thursday, May 31, 2018. It is located in the Horowitz Traveling Exhibit Area. The MOST presents Paleo: The Story of Life in association with the International Museum Institute, Inc. -
In Search of the Kingdom's Ediacarans
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/274730804 IN SEARCH OF THE KINGDOM'S EDIACARANS: THE FIRST GENUINE METAZOANS (MACROSCOPIC BODY AND TRACE FOSSILS) FROM THE NEOPROTEROZOIC JIBALAH GROUP (VENDIAN/EDIACARAN) ON THE ARABIAN SHI... ARTICLE · JANUARY 2013 CITATIONS READS 2 69 18 AUTHORS, INCLUDING: Patricia Vickers Rich Peter Robert. Johnson Monash University (Australia) 45 PUBLICATIONS 1,271 CITATIONS 79 PUBLICATIONS 1,250 CITATIONS SEE PROFILE SEE PROFILE Tom Rich Museum Victoria 92 PUBLICATIONS 1,703 CITATIONS SEE PROFILE Ulf Linnemann Senckenberg Naturhistorische Sammlunge… 144 PUBLICATIONS 1,914 CITATIONS SEE PROFILE Available from: Tom Rich Retrieved on: 11 February 2016 In Search of the Kingdom’s Ediacarans: The First Genuine Metazoans on the Arabian Shield IN SEARCH OF THE KINGDOM’S EDIACARANS: THE FIRST GENUINE METAZOANS (MACROSCOPIC BODY AND TRACE FOSSILS) FROM THE NEOPROTEROZOIC JIBALAH GROUP (VENDIAN/EDIACARAN) ON THE ARABIAN SHIELD BY PATRICIA VICKERS-RICH, ANDREI IVANTSOV, FAYEK H. KATTAN, PETER R. JOHNSON, ASHRAF AL QUBSANI, WADEE KASHGHARI, MAXIM LEONOV, THOMAS RICH, ULF LINNEMANN, MANDY HOFMANN, PETER TRUSLER, JEFF SMITH, ABDULLAH YAZEDI, BEN RICH, SAAD M. AL GARNI, ABDULLA SHAMARI, ADEEB AL BARAKATI, AND MOHAMMAD H. AL KAFF Cenozoic basalt draped Neoproterozoic sequence with Cambrian Saq Sandstone overlying the Neoproterozoic Jibalah Group as a Backdrop, Northwestern Arabian Shield www.sgs.org.sa TECHNICAL REPORT SGS-TR-2013-5 1434 H 2013 G Saudi Geological Survey Technical Report - SGS-TR-2013-5 i In Search of the Kingdom’s Ediacarans: The First Genuine Metazoans on the Arabian Shield A Technical Report prepared by the Saudi Geological Survey, Jeddah, Kingdom of Saudi Arabia The work on which this report is based was performed in support of Saudi Geological Survey Subproject Subproject - The Eastern Arabian Shield: Window into Supercontinental Assembly at the Dawn of Animal Life. -
Phylum Porifera
790 Chapter 28 | Invertebrates updated as new information is collected about the organisms of each phylum. 28.1 | Phylum Porifera By the end of this section, you will be able to do the following: • Describe the organizational features of the simplest multicellular organisms • Explain the various body forms and bodily functions of sponges As we have seen, the vast majority of invertebrate animals do not possess a defined bony vertebral endoskeleton, or a bony cranium. However, one of the most ancestral groups of deuterostome invertebrates, the Echinodermata, do produce tiny skeletal “bones” called ossicles that make up a true endoskeleton, or internal skeleton, covered by an epidermis. We will start our investigation with the simplest of all the invertebrates—animals sometimes classified within the clade Parazoa (“beside the animals”). This clade currently includes only the phylum Placozoa (containing a single species, Trichoplax adhaerens), and the phylum Porifera, containing the more familiar sponges (Figure 28.2). The split between the Parazoa and the Eumetazoa (all animal clades above Parazoa) likely took place over a billion years ago. We should reiterate here that the Porifera do not possess “true” tissues that are embryologically homologous to those of all other derived animal groups such as the insects and mammals. This is because they do not create a true gastrula during embryogenesis, and as a result do not produce a true endoderm or ectoderm. But even though they are not considered to have true tissues, they do have specialized cells that perform specific functions like tissues (for example, the external “pinacoderm” of a sponge acts like our epidermis). -
Challenges in Indian Palaeobiology
Challenges in Indian Palaeobiology Current Status, Recent Developments and Future Directions © BIRBAL SAHNI INSTITUTE OF PALAEOBOTANY, LUCKNOW 226 007, (U.P.), INDIA Published by The Director Birbal Sahni Institute of Palaeobotany Lucknow 226 007 INDIA Phone : +91-522-2740008/2740011/ 2740399/2740413 Fax : +91-522-2740098/2740485 E-mail : [email protected] [email protected] Website : http://www.bsip.res.in ISBN No : 81-86382-03-8 Proof Reader : R.L. Mehra Typeset : Syed Rashid Ali & Madhavendra Singh Produced by : Publication Unit Printed at : Dream Sketch, 29 Brahma Nagar, Sitapur Road, Lucknow November 2005 Patrons Prof. V. S. Ramamurthy Secretary, Department of Science & Technology, Govt. of India Dr. Harsh K. Gupta Formerly Secretary, Department of Ocean Development, Govt. of India Prof. J. S. Singh Chairman, Governing Body, BSIP Prof. G. K. Srivastava Chairman, Research Advisory Committee, BSIP National Steering Committee Dr. N. C. Mehrotra, Director, BSIP - Chairman Prof. R.P. Singh, Vice Chancellor, Lucknow University - Member Prof. Ashok Sahni, Geology Department, Panjab University - Member Prof. M.P. Singh, Geology Department, Lucknow University - Member Dr. M. Sanjappa, Director, Botanical Survey of India - Member Dr. D. K. Pandey, Director (Exlporation), ONGC, New Delhi - Member Dr. P. Pushpangadan, Director, NBRI - Member Prof. S.K. Tandon, Geology Department, Delhi University - Member Dr. Arun Nigvekar, Former Chairman, UGC - Member Dr. K.P.N. Pandiyan, Joint Secretary & Financial Adv., DST - Member Local Organizing Committee Dr. N. C. Mehrotra, Director - Chairman Dr. Jayasri Banerji, Scientist ‘F’ - Convener Dr. A. K. Srivastava, Scientist ‘F’ - Member Dr. Ramesh K. Saxena, Scientist ‘F’ - Member Dr. Archana Tripathi, Scientist ‘F’ - Member Dr. -
Whole-Ocean Changes in Silica and Ge/Si Ratios During The
Originally published as: Jochum, K. P., Schuessler, J. A., Wang, X.‐H., Stoll, B., Weis, U., Müller, W. E. G., Haug, G. H., Andreae, M. O., Froelich, P. N. (2017): Whole‐Ocean Changes in Silica and Ge/Si Ratios During the Last Deglacial Deduced From Long‐Lived Giant Glass Sponges. ‐ Geophysical Research Letters, 44, 22, pp. 11555—11564. DOI: http://doi.org/10.1002/2017GL073897 PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Whole-Ocean Changes in Silica and Ge/Si Ratios 10.1002/2017GL073897 During the Last Deglacial Deduced From Long- Key Points: Lived Giant Glass Sponges • Si isotope and Ge measurements in the deep-sea sponge Monorhaphis K. P. Jochum1,2 , J. A. Schuessler3 , X.-H. Wang4, B. Stoll1,2, U. Weis1,2 , W. E. G. Müller4, chuni provide an archive of climate 2 1,5 6 change, reaching back to at least 17 G. H. Haug , M. O. Andreae , and P. N. Froelich ka B.P. 1 2 • Our data suggest that at the onset of Biogeochemistry Department, MPIC Max Planck Institute for Chemistry, Mainz, Germany, Climate Geochemistry the last deglaciation, deep Pacific Department, MPIC Max Planck Institute for Chemistry, Mainz, Germany, 3GFZ German Research Centre for Geosciences, Ocean dissolved silica was higher and Potsdam, Germany, 4ERC Advanced Grant Research Group at the Institute for Physiological Chemistry, University Medical Ge/Si lower than at present Center of the Johannes Gutenberg University Mainz, Mainz, Germany, 5Scripps Institution of Oceanography, University of California. San Diego, La Jolla, CA, USA, 6Nicholas School of the Environment, Duke University, Durham, NC, USA Supporting Information: • Supporting Information S1 Abstract Silicon is a keystone nutrient in the ocean for understanding climate change because of the Correspondence to: importance of Southern Ocean diatoms in taking up CO2 from the surface ocean-atmosphere system and K.