Imaging Intracellular Ph in a Reef Coral and Symbiotic Anemone

Total Page:16

File Type:pdf, Size:1020Kb

Imaging Intracellular Ph in a Reef Coral and Symbiotic Anemone Imaging intracellular pH in a reef coral and symbiotic anemone A. A. Venn1, E. Tambutte´ , S. Lotto, D. Zoccola, D. Allemand, and S. Tambutte´ Centre Scientifique de Monaco, Avenue Saint Martin, MC98000 Monaco Edited by Paul G. Falkowski, Rutgers, The State University of New Jersey, New Brunswick, NJ, and approved July 28, 2009 (received for review March 16, 2009) The challenges corals and symbiotic cnidarians face from global global climate change (12). Oceanic absorption of atmospheric environmental change brings new urgency to understanding fun- anthropogenic CO2 is decreasing both the availability of car- damental elements of their physiology. Intracellular pH (pHi) bonate ions and seawater pH potentially compromising coral influences almost all aspects of cellular physiology but has never calcification (13–15), while rising sea surface temperatures affect been described in anthozoans or symbiotic cnidarians, despite its photosynthesis and cause dysfunction in the symbiotic relation- pivotal role in carbon concentration for photosynthesis and calci- ship between corals and their intracellular algae (bleaching) (16, fication. Using confocal microscopy and the pH sensitive probe 17). Quantification of pHi is a key step toward determining the carboxy SNARF-1, we mapped pHi in short-term light and dark- mechanistic basis behind the vulnerability of these physiological incubated cells of the reef coral Stylophora pistillata and the processes to environmental change. symbiotic anemone Anemonia viridis. In all cells isolated from both Progress in the understanding of the physiology of symbiotic species, pHi was markedly lower than the surrounding seawater cnidarians like corals depends on the development of tools to pH of 8.1. In cells that contained symbiotic algae, mean values of examine their cell biology (2). In many other biological systems pHi were significantly higher in light treated cells than dark treated understanding of pHi regulation and other physiological param- -cells (7.41 ؎ 0.22 versus 7.13 ؎ 0.24 for S. pistillata; and 7.29 ؎ 0.15 eters has improved significantly by the application of intracel versus 7.01 ؎ 0.27 for A. viridis). In contrast, there was no signif- lular probes that emit fluorescence at 2 wavelengths which can icant difference in pHi in light and dark treated cells without algal be calibrated to the concentration of specific ions in the cell (e.g., symbionts. Close inspection of the interface between host cyto- Hϩ) (18–20). When coupled with confocal microscopy, this plasm and algal symbionts revealed a distinct area of lower pH approach allows the mapping of dynamic physiological processes adjacent to the symbionts in both light and dark treated cells, across cell structures (21, 22) and has enormous potential utility possibly associated with the symbiosome membrane complex. in physiological studies of symbiotic cnidarians, which harbor These findings are significant developments for the elucidation of intracellular algae and thus require excellent spatial resolution to models of inorganic carbon transport for photosynthesis and distinguish between animal and algal compartments. calcification and also provide a cell imaging procedure for future In the current study, we adapted a live cell imaging procedure investigations into how pHi and other fundamental intracellular that allowed us to make the first pHi measurements in symbiotic parameters in corals respond to changes in the external environ- cnidarians and anthozoans. To do this, we observed endoderm ment such as reductions in seawater pH. cells from the reef coral Stylophora pistillata and the symbiotic anemone Anemonia viridis exposed to both light and dark ͉ ͉ ͉ ͉ cell biology cnidaria symbiosis photosynthesis climate change conditions. pHi was determined by loading cells with the pH sensitive fluorescent probe, carboxyseminaphthorhodafluor-1 ymbiotic cnidarians form the structural foundation of coral (SNARF-1), and analysis by confocal microscopy. Our in vivo Sreefs, which rank among the most biodiverse and ecologically cell imaging procedure was developed to allow spatial separation important ecosystems. Despite their environmental significance, of cnidarian host and symbiont cell compartments and has a wide key elements of coral physiology such as calcification and the range of potential applications in the study of coral and cnidarian symbiotic interactions between cnidarians and their intracellular physiology. algae (Symbiodinium) are poorly understood, largely due to knowledge gaps in fundamental aspects of cnidarian cell biology Results (1–3). Observation of Cell Preparations. Cell preparations isolated from Intracellular pH (pHi) modulates virtually all aspects of cell A. viridis and S. pistillata included a variety of cell types including metabolism, including membrane channel functioning, the struc- endoderm cells that contained 1 to 3 algae and cells without algal tural and functional properties of enzymes, intracellular signal- symbionts (Fig. 1). ing, and ion availability (4, 5). As a consequence, pHi must be Cells that contained 2 algae were the most suitable for tightly controlled and changes in pHi are minimized by intra- measurements of pHi in algae-containing cells for 2 reasons. cellular buffers and regulation by ion carriers on the cell First, this cell type contained a larger area of host cytoplasm membrane (6, 7). In symbiotic cnidarians such as corals, pHi is available for pHi measurements than single alga cells [in which thought to be linked to processes of photosynthesis and calcifi- the cytoplasm was closely stretched around the alga (Fig. 1, cation by influencing the flux of ions between host, symbiont, and the surrounding environment (6, 8). This particularly con- cerns the transport of dissolved organic carbon (DIC) between Author contributions: A.A.V., D.A., and S.T. designed research; A.A.V., E.T., S.L., D.Z., and Ϫ cell layers and the speciation of DIC between CO2, HCO3 , and S.T. performed research; A.A.V., E.T., and S.T. analyzed data; and A.A.V., D.A., and S.T. 2Ϫ wrote the paper. CO3 (9–11). Measurements of pHi in cnidarian cells are therefore an essential step for elucidating how DIC is transferred The authors declare no conflict of interest. from the surrounding seawater to the respective sites of photo- This article is a PNAS Direct Submission. synthesis and calcification. See Commentary on page 16541. Understanding the links between pHi and processes of calci- 1To whom correspondence should be addressed. E-mail: alex@centrescientifique.mc. fication and photosynthesis is becoming increasingly important This article contains supporting information online at www.pnas.org/cgi/content/full/ given the challenges corals and symbiotic cnidarians face under 0902894106/DCSupplemental. 16574–16579 ͉ PNAS ͉ September 29, 2009 ͉ vol. 106 ͉ no. 39 www.pnas.org͞cgi͞doi͞10.1073͞pnas.0902894106 Downloaded by guest on September 28, 2021 SEE COMMENTARY Fig. 1. Cnidarian endoderm cells isolated from A. viridis with and without symbiotic algae. (Row A–D) Different cell types: (A) endoderm cells without symbiotic algae. (B) endoderm cells containing one alga. C ϭ animal cytoplasm A ϭ intracellular symbiotic alga. (C) endoderm cells with 2 algae. (D) endoderm cells with 3 algae. (Column 1) TEM images. (Column 2) confocal images of cells stained with Hoechst 33342 and Rhodamine 123. (Column 3) Confocal images of cells loaded with SNARF-1 a.m. Colors in confocal images represent the following: Red ϭ autofluorescence of chlorophyll in intracellular algae, blue ϭ nuclei stained with Hoechst 33342, green ϭ mitochondria stained with Rhodamine 123, yellow ϭ cnidarian cytoplasm stained with SNARF-1. SCIENCES RowB)] and secondly, double cells were more numerous in cell curves of pHi with the SNARF-1 signal are given for S. pistillata APPLIED BIOLOGICAL preparations than cells that contained 3 algae. and A. viridis as supporting information (SI) Fig. S1. In the case of A. viridis preparations, cells with no intracellular Analysis of vertically-stacked horizontal slices through the cell algae could be identified to be of endodermal origin because the (z stack profiles) showed that pHi was stable (Ϯ pH 0.1) toward isolation procedure allowed separation of this layer from other the center of most cells where SNARF-1 fluorescence was host tissues. The presence of these cells allowed comparisons of greatest (Fig. 2). Exceptions to this rule occurred with the pHi to be made between endoderm cells with and without presence of acidic vacuoles which had a pH of 6 or below the intracellular algae. limits of our calibration. Analysis by TEM and staining with Hoecsht 33342 and Using this approach, pHi was determined in endoderm cells of rhodamine 123 identified the presence of nuclei and mitochon- S. pistillata and A. viridis that had been incubated for 20 min under light or dark conditions (Table 1). In both species, pHi was dria in all cell types, which were generally located between the significantly higher in light-incubated cells that contained algal algal cells in host cells with 2 or more algae (Fig. 1, Column 2). symbionts than dark-incubated symbiont-containing cells (one The cytoplasm of host cells stained evenly with SNARF-1 with way ANOVA, F5,114 ϭ 8.135, P Ͻ 0.001). However, when light little or no exclusion or concentration of the dye within cell and dark-incubated symbiont free cells isolated from A. viridis compartments such as nuclei or mitochondria (Fig. 1, Column 3), were compared, no significant difference in pHi was found although
Recommended publications
  • Checklist of Fish and Invertebrates Listed in the CITES Appendices
    JOINTS NATURE \=^ CONSERVATION COMMITTEE Checklist of fish and mvertebrates Usted in the CITES appendices JNCC REPORT (SSN0963-«OStl JOINT NATURE CONSERVATION COMMITTEE Report distribution Report Number: No. 238 Contract Number/JNCC project number: F7 1-12-332 Date received: 9 June 1995 Report tide: Checklist of fish and invertebrates listed in the CITES appendices Contract tide: Revised Checklists of CITES species database Contractor: World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge, CB3 ODL Comments: A further fish and invertebrate edition in the Checklist series begun by NCC in 1979, revised and brought up to date with current CITES listings Restrictions: Distribution: JNCC report collection 2 copies Nature Conservancy Council for England, HQ, Library 1 copy Scottish Natural Heritage, HQ, Library 1 copy Countryside Council for Wales, HQ, Library 1 copy A T Smail, Copyright Libraries Agent, 100 Euston Road, London, NWl 2HQ 5 copies British Library, Legal Deposit Office, Boston Spa, Wetherby, West Yorkshire, LS23 7BQ 1 copy Chadwick-Healey Ltd, Cambridge Place, Cambridge, CB2 INR 1 copy BIOSIS UK, Garforth House, 54 Michlegate, York, YOl ILF 1 copy CITES Management and Scientific Authorities of EC Member States total 30 copies CITES Authorities, UK Dependencies total 13 copies CITES Secretariat 5 copies CITES Animals Committee chairman 1 copy European Commission DG Xl/D/2 1 copy World Conservation Monitoring Centre 20 copies TRAFFIC International 5 copies Animal Quarantine Station, Heathrow 1 copy Department of the Environment (GWD) 5 copies Foreign & Commonwealth Office (ESED) 1 copy HM Customs & Excise 3 copies M Bradley Taylor (ACPO) 1 copy ^\(\\ Joint Nature Conservation Committee Report No.
    [Show full text]
  • Taxonomic Checklist of CITES Listed Coral Species Part II
    CoP16 Doc. 43.1 (Rev. 1) Annex 5.2 (English only / Únicamente en inglés / Seulement en anglais) Taxonomic Checklist of CITES listed Coral Species Part II CORAL SPECIES AND SYNONYMS CURRENTLY RECOGNIZED IN THE UNEP‐WCMC DATABASE 1. Scleractinia families Family Name Accepted Name Species Author Nomenclature Reference Synonyms ACROPORIDAE Acropora abrolhosensis Veron, 1985 Veron (2000) Madrepora crassa Milne Edwards & Haime, 1860; ACROPORIDAE Acropora abrotanoides (Lamarck, 1816) Veron (2000) Madrepora abrotanoides Lamarck, 1816; Acropora mangarevensis Vaughan, 1906 ACROPORIDAE Acropora aculeus (Dana, 1846) Veron (2000) Madrepora aculeus Dana, 1846 Madrepora acuminata Verrill, 1864; Madrepora diffusa ACROPORIDAE Acropora acuminata (Verrill, 1864) Veron (2000) Verrill, 1864; Acropora diffusa (Verrill, 1864); Madrepora nigra Brook, 1892 ACROPORIDAE Acropora akajimensis Veron, 1990 Veron (2000) Madrepora coronata Brook, 1892; Madrepora ACROPORIDAE Acropora anthocercis (Brook, 1893) Veron (2000) anthocercis Brook, 1893 ACROPORIDAE Acropora arabensis Hodgson & Carpenter, 1995 Veron (2000) Madrepora aspera Dana, 1846; Acropora cribripora (Dana, 1846); Madrepora cribripora Dana, 1846; Acropora manni (Quelch, 1886); Madrepora manni ACROPORIDAE Acropora aspera (Dana, 1846) Veron (2000) Quelch, 1886; Acropora hebes (Dana, 1846); Madrepora hebes Dana, 1846; Acropora yaeyamaensis Eguchi & Shirai, 1977 ACROPORIDAE Acropora austera (Dana, 1846) Veron (2000) Madrepora austera Dana, 1846 ACROPORIDAE Acropora awi Wallace & Wolstenholme, 1998 Veron (2000) ACROPORIDAE Acropora azurea Veron & Wallace, 1984 Veron (2000) ACROPORIDAE Acropora batunai Wallace, 1997 Veron (2000) ACROPORIDAE Acropora bifurcata Nemenzo, 1971 Veron (2000) ACROPORIDAE Acropora branchi Riegl, 1995 Veron (2000) Madrepora brueggemanni Brook, 1891; Isopora ACROPORIDAE Acropora brueggemanni (Brook, 1891) Veron (2000) brueggemanni (Brook, 1891) ACROPORIDAE Acropora bushyensis Veron & Wallace, 1984 Veron (2000) Acropora fasciculare Latypov, 1992 ACROPORIDAE Acropora cardenae Wells, 1985 Veron (2000) CoP16 Doc.
    [Show full text]
  • SEDIMENTARY FRAMEWORK of Lmainland FRINGING REEF DEVELOPMENT, CAPE TRIBULATION AREA
    GREAT BARRIER REEF MARINE PARK AUTHORITY TECHNICAL MEMORANDUM GBRMPA-TM-14 SEDIMENTARY FRAMEWORK OF lMAINLAND FRINGING REEF DEVELOPMENT, CAPE TRIBULATION AREA D.P. JOHNSON and RM.CARTER Department of Geology James Cook University of North Queensland Townsville, Q 4811, Australia DATE November, 1987 SUMMARY Mainland fringing reefs with a diverse coral fauna have developed in the Cape Tribulation area primarily upon coastal sedi- ment bodies such as beach shoals and creek mouth bars. Growth on steep rocky headlands is minor. The reefs have exten- sive sandy beaches to landward, and an irregular outer margin. Typically there is a raised platform of dead nef along the outer edge of the reef, and dead coral columns lie buried under the reef flat. Live coral growth is restricted to the outer reef slope. Seaward of the reefs is a narrow wedge of muddy, terrigenous sediment, which thins offshore. Beach, reef and inner shelf sediments all contain 50% terrigenous material, indicating the reefs have always grown under conditions of heavy terrigenous influx. The relatively shallow lower limit of coral growth (ca 6m below ADD) is typical of reef growth in turbid waters, where decreased light levels inhibit coral growth. Radiocarbon dating of material from surveyed sites confirms the age of the fossil coral columns as 33304110 ybp, indicating that they grew during the late postglacial sea-level high (ca 5500-6500 ybp). The former thriving reef-flat was killed by a post-5500 ybp sea-level fall of ca 1 m. Although this study has not assessed the community structure of the fringing reefs, nor whether changes are presently occur- ring, it is clear the corals present today on the fore-reef slope have always lived under heavy terrigenous influence, and that the fossil reef-flat can be explained as due to the mid-Holocene fall in sea-level.
    [Show full text]
  • Commentary Cellular Mechanisms of Cnidarian Bleaching: Stress Causes the Collapse of Symbiosis
    3059 The Journal of Experimental Biology 211, 3059-3066 Published by The Company of Biologists 2008 doi:10.1242/jeb.009597 Commentary Cellular mechanisms of Cnidarian bleaching: stress causes the collapse of symbiosis Virginia M. Weis Department of Zoology, Oregon State University, Corvallis, OR, 97331, USA e-mail: [email protected] Accepted 6 August 2008 Summary Cnidarian bleaching is a breakdown in the mutualistic symbiosis between host Cnidarians, such as reef building corals, and their unicellular photosynthetic dinoflagellate symbionts. Bleaching is caused by a variety of environmental stressors, most notably elevated temperatures associated with global climate change in conjunction with high solar radiation, and it is a major contributor to coral death and reef degradation. This review examines the underlying cellular events that lead to symbiosis dysfunction and cause bleaching, emphasizing that, to date, we have only some pieces of a complex cellular jigsaw puzzle. Reactive oxygen species (ROS), generated by damage to both photosynthetic and mitochondrial membranes, is shown to play a central role in both injury to the partners and to inter-partner communication of a stress response. Evidence is presented that suggests that bleaching is a host innate immune response to a compromised symbiont, much like innate immune responses in other host–microbe interactions. Finally, the elimination or exit of the symbiont from host tissues is described through a variety of mechanisms including exocytosis, host cell detachment and host cell apoptosis. Key words: coral bleaching, symbiosis, coral, Symbiodinium, oxidative stress, reactive oxygen species, nitric oxide, apoptosis. Introduction ability of the corals to deposit their massive calcium carbonate Symbioses between a variety of marine invertebrates, including skeletons that form the reef structure.
    [Show full text]
  • Volume 2. Animals
    AC20 Doc. 8.5 Annex (English only/Seulement en anglais/Únicamente en inglés) REVIEW OF SIGNIFICANT TRADE ANALYSIS OF TRADE TRENDS WITH NOTES ON THE CONSERVATION STATUS OF SELECTED SPECIES Volume 2. Animals Prepared for the CITES Animals Committee, CITES Secretariat by the United Nations Environment Programme World Conservation Monitoring Centre JANUARY 2004 AC20 Doc. 8.5 – p. 3 Prepared and produced by: UNEP World Conservation Monitoring Centre, Cambridge, UK UNEP WORLD CONSERVATION MONITORING CENTRE (UNEP-WCMC) www.unep-wcmc.org The UNEP World Conservation Monitoring Centre is the biodiversity assessment and policy implementation arm of the United Nations Environment Programme, the world’s foremost intergovernmental environmental organisation. UNEP-WCMC aims to help decision-makers recognise the value of biodiversity to people everywhere, and to apply this knowledge to all that they do. The Centre’s challenge is to transform complex data into policy-relevant information, to build tools and systems for analysis and integration, and to support the needs of nations and the international community as they engage in joint programmes of action. UNEP-WCMC provides objective, scientifically rigorous products and services that include ecosystem assessments, support for implementation of environmental agreements, regional and global biodiversity information, research on threats and impacts, and development of future scenarios for the living world. Prepared for: The CITES Secretariat, Geneva A contribution to UNEP - The United Nations Environment Programme Printed by: UNEP World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge CB3 0DL, UK © Copyright: UNEP World Conservation Monitoring Centre/CITES Secretariat The contents of this report do not necessarily reflect the views or policies of UNEP or contributory organisations.
    [Show full text]
  • Scleractinia Fauna of Taiwan I
    Scleractinia Fauna of Taiwan I. The Complex Group 台灣石珊瑚誌 I. 複雜類群 Chang-feng Dai and Sharon Horng Institute of Oceanography, National Taiwan University Published by National Taiwan University, No.1, Sec. 4, Roosevelt Rd., Taipei, Taiwan Table of Contents Scleractinia Fauna of Taiwan ................................................................................................1 General Introduction ........................................................................................................1 Historical Review .............................................................................................................1 Basics for Coral Taxonomy ..............................................................................................4 Taxonomic Framework and Phylogeny ........................................................................... 9 Family Acroporidae ............................................................................................................ 15 Montipora ...................................................................................................................... 17 Acropora ........................................................................................................................ 47 Anacropora .................................................................................................................... 95 Isopora ...........................................................................................................................96 Astreopora ......................................................................................................................99
    [Show full text]
  • Summary Output
    AC29 Doc. 13.3 Annex 1 Summary output To comply with paragraph 1 a) of Resolution Conf. 12.8 (Rev. CoP17), a summary output of trade in wild-sourced specimens was produced from data extracted from the CITES Trade Database on 26th April 2017. An excel version of the data output is also available (see AC29 Doc Inf. 4), which details the trade levels for each individual country with direct exports over the five most recent years (2011-2015). Table 1. Data included for the summary output of ‘wild-sourced’ trade Data included CITES Trade Database Gross exports; report type Direct trade only (re-exports are excluded) Current Appendix Appendix II taxa and Appendix I taxa subject to reservation Source codes1 Wild (‘W’), ranched (‘R’), unknown (‘U’) and no reported source (‘-’) Purpose codes1 All Terms included Selected terms2: baleen, bodies, bones, carapaces, carvings, cloth, eggs, egg (live), fins, gall and gall bladders, horns and horn pieces, ivory pieces, ivory carvings, live, meat, musk (including derivatives for Moschus moschiferus), plates, raw corals, scales, shells, skin pieces, skins, skeletons, skulls, teeth, trophies, and tusks. Units of measure Number (unit = blank) and weight (unit = kilogram3) [Trade in other units of measure (e.g. litres, metres etc.) were excluded] Year range 2011-20154 Contextual The global conservation status and population trend of the species as published information in The IUCN Red List of Threatened Species; Whether the species/country combination was subject to the Review of Significant Trade process for the last three iterations (post CoP14, post CoP15 and post CoP16); Whether the taxon was reported in trade for the first time within the CITES Trade Database since 2012 (e.g.
    [Show full text]
  • Conservation of Reef Corals in the South China Sea Based on Species and Evolutionary Diversity
    Biodivers Conserv DOI 10.1007/s10531-016-1052-7 ORIGINAL PAPER Conservation of reef corals in the South China Sea based on species and evolutionary diversity 1 2 3 Danwei Huang • Bert W. Hoeksema • Yang Amri Affendi • 4 5,6 7,8 Put O. Ang • Chaolun A. Chen • Hui Huang • 9 10 David J. W. Lane • Wilfredo Y. Licuanan • 11 12 13 Ouk Vibol • Si Tuan Vo • Thamasak Yeemin • Loke Ming Chou1 Received: 7 August 2015 / Revised: 18 January 2016 / Accepted: 21 January 2016 Ó Springer Science+Business Media Dordrecht 2016 Abstract The South China Sea in the Central Indo-Pacific is a large semi-enclosed marine region that supports an extraordinary diversity of coral reef organisms (including stony corals), which varies spatially across the region. While one-third of the world’s reef corals are known to face heightened extinction risk from global climate and local impacts, prospects for the coral fauna in the South China Sea region amidst these threats remain poorly understood. In this study, we analyse coral species richness, rarity, and phylogenetic Communicated by Dirk Sven Schmeller. Electronic supplementary material The online version of this article (doi:10.1007/s10531-016-1052-7) contains supplementary material, which is available to authorized users. & Danwei Huang [email protected] 1 Department of Biological Sciences and Tropical Marine Science Institute, National University of Singapore, Singapore 117543, Singapore 2 Naturalis Biodiversity Center, PO Box 9517, 2300 RA Leiden, The Netherlands 3 Institute of Biological Sciences, Faculty of
    [Show full text]
  • Milleporidae, Stylasteridae, Scleractinia) in the National Museum of Natural History, Smithsonian Institution
    Catalog of the Type Specimens of Stony Corals (Milleporidae, Stylasteridae, Scleractinia) in the National Museum of Natural History, Smithsonian Institution STEPHEN D. CAIRNS W9\ I SMITHSONIAN CONTRIBUTIONS TO ZOOLOGY • NUMBER 514 SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of "diffusing knowledge" was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, commencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Folklife Studies Smithsonian Studies in Air and Space Smithsonian Studies in History and Technology In these series, the Institution publishes small papers and full-scale monographs that report the research and collections of its various museums and bureaux or of professional colleagues in the world of science and scholarship. The publications are distributed by mailing lists to libraries, universities, and similar institutions throughout the world. Papers or monographs submitted for series publication are received by the Smithsonian Institution Press, subject to its own review for format and style, only through departments of the various Smithsonian museums or bureaux, where the manuscripts are given substantive review.
    [Show full text]
  • RESEARCH ARTICLE Twilight Spectral Dynamics and the Coral Reef Invertebrate Spawning Response
    770 The Journal of Experimental Biology 214, 770-777 © 2011. Published by The Company of Biologists Ltd doi:10.1242/jeb.043406 RESEARCH ARTICLE Twilight spectral dynamics and the coral reef invertebrate spawning response Alison M. Sweeney1,*, Charles A. Boch1, Sonke Johnsen2 and Daniel E. Morse1 1Institute for Collaborative Biotechnologies, University of California, Santa Barbara, CA 93105, USA and 2Department of Biology, Duke University, Durham, NC 27708, USA *Author for correspondence ([email protected]) Accepted 11 November 2010 SUMMARY There are dramatic and physiologically relevant changes in both skylight color and intensity during evening twilight as the pathlength of direct sunlight through the atmosphere increases, ozone increasingly absorbs long wavelengths and skylight becomes increasingly blue shifted. The moon is above the horizon at sunset during the waxing phase of the lunar cycle, on the horizon at sunset on the night of the full moon and below the horizon during the waning phase. Moonlight is red shifted compared with daylight, so the presence, phase and position of the moon in the sky could modulate the blue shifts during twilight. Therefore, the influence of the moon on twilight color is likely to differ somewhat each night of the lunar cycle, and to vary especially rapidly around the full moon, as the moon transitions from above to below the horizon during twilight. Many important light-mediated biological processes occur during twilight, and this lunar effect may play a role. One particularly intriguing biological event tightly correlated with these twilight processes is the occurrence of mass spawning events on coral reefs. Therefore, we measured downwelling underwater hyperspectral irradiance on a coral reef during twilight for several nights before and after the full moon.
    [Show full text]
  • Scleractinian Corals and Reefs of Vietnam As a Part of the Pacific Reef Ecosystem
    Open Journal of Marine Science, 2011, 1, 50-68 http://dx.doi.org/10.4236/ojms.2011.12006 Published Online July 2011 (http://www.SciRP.org/journal/ojms) Scleractinian Corals and Reefs of Vietnam as a Part of the Pacific Reef Ecosystem Yuri Ya Latypov A. V. Zhirmunsky Institute of Marine Biology, Far East Branch of the Russian Academy of Sciences, Vladivostok, Russia E-mail: [email protected] Received May 12, 2011; revised June 1, 2011; accepted June 10, 2011 Abstract The paper analyzes both published and unpublished results of the investigations of Vietnamese reef building corals and reefs performed in the last decades of the twentieth century and first decades twenty-first. The state of the art in the study of reef-building scleractinian corals and reefs is presented. The scleractinian fauna of Vietnam is shown to match in species diversity (350 species of 80 genera) the tropical coral fauna of the Indonesian–Malacca fertile center, from which Indo-Pacific reef-building corals originated. The whole Vietnam coast from the Gulf of Tonkin to the Gulf of Siam is a biogeographically single whole and is a part of the Indo-Polynesian Province of the Indo-Pacific Area. Keywords: Vietnam, Reefs, Reef-Building Corals, Pacific Reef Ecosystem 1. Introduction till September, and the dry northeast, occurring in Octo- ber-April. Heavy rain showers during the wet monsoon 1.1. Brief the Ecological Characteristic and a period result in a huge (5 - 400 million m3) freshwater History of Studying influx and a substantial (up to 200 thous. tons) terri- genous sediment influx into the sea.
    [Show full text]
  • Tonga SUMA Report
    BIOPHYSICALLY SPECIAL, UNIQUE MARINE AREAS OF TONGA EFFECTIVE MANAGEMENT Marine and coastal ecosystems of the Pacific Ocean provide benefits for all people in and beyond the region. To better understand and improve the effective management of these values on the ground, Pacific Island Countries are increasingly building institutional and personal capacities for Blue Planning. But there is no need to reinvent the wheel, when learning from experiences of centuries of traditional management in Pacific Island Countries. Coupled with scientific approaches these experiences can strengthen effective management of the region’s rich natural capital, if lessons learnt are shared. The MACBIO project collaborates with national and regional stakeholders towards documenting effective approaches to sustainable marine resource management and conservation. The project encourages and supports stakeholders to share tried and tested concepts and instruments more widely throughout partner countries and the Oceania region. This report outlines the process undertaken to define and describe the special, unique marine areas of Tonga. These special, unique marine areas provide an important input to decisions about, for example, permits, licences, EIAs and where to place different types of marine protected areas, locally managed marine areas and Community Conservation Areas in Tonga. For a copy of all reports and communication material please visit www.macbio-pacific.info. MARINE ECOSYSTEM MARINE SPATIAL PLANNING EFFECTIVE MANAGEMENT SERVICE VALUATION BIOPHYSICALLY SPECIAL, UNIQUE MARINE AREAS OF TONGA AUTHORS: Ceccarelli DM1, Wendt H2, Matoto AL3, Fonua E3, Fernandes L2 SUGGESTED CITATION: Ceccarelli DM, Wendt H, Matoto AL, Fonua E and Fernandes L (2017) Biophysically special, unique marine areas of Tonga. MACBIO (GIZ, IUCN, SPREP), Suva.
    [Show full text]