Arctic Coral Reefs an Undiscovered Environment
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Methane Cold Seeps As Biological Oases in the High‐
LIMNOLOGY and Limnol. Oceanogr. 00, 2017, 00–00 VC 2017 The Authors Limnology and Oceanography published by Wiley Periodicals, Inc. OCEANOGRAPHY on behalf of Association for the Sciences of Limnology and Oceanography doi: 10.1002/lno.10732 Methane cold seeps as biological oases in the high-Arctic deep sea Emmelie K. L. A˚ strom€ ,1* Michael L. Carroll,1,2 William G. Ambrose, Jr.,1,2,3,4 Arunima Sen,1 Anna Silyakova,1 JoLynn Carroll1,2 1CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway 2Akvaplan-niva, FRAM – High North Research Centre for Climate and the Environment, Tromsø, Norway 3Division of Polar Programs, National Science Foundation, Arlington, Virginia 4Department of Biology, Bates College, Lewiston, Maine Abstract Cold seeps can support unique faunal communities via chemosynthetic interactions fueled by seabed emissions of hydrocarbons. Additionally, cold seeps can enhance habitat complexity at the deep seafloor through the accretion of methane derived authigenic carbonates (MDAC). We examined infaunal and mega- faunal community structure at high-Arctic cold seeps through analyses of benthic samples and seafloor pho- tographs from pockmarks exhibiting highly elevated methane concentrations in sediments and the water column at Vestnesa Ridge (VR), Svalbard (798 N). Infaunal biomass and abundance were five times higher, species richness was 2.5 times higher and diversity was 1.5 times higher at methane-rich Vestnesa compared to a nearby control region. Seabed photos reveal different faunal associations inside, at the edge, and outside Vestnesa pockmarks. Brittle stars were the most common megafauna occurring on the soft bottom plains out- side pockmarks. -
Vulnerable Marine Ecosystems – Processes and Practices in the High Seas Vulnerable Marine Ecosystems Processes and Practices in the High Seas
ISSN 2070-7010 FAO 595 FISHERIES AND AQUACULTURE TECHNICAL PAPER 595 Vulnerable marine ecosystems – Processes and practices in the high seas Vulnerable marine ecosystems Processes and practices in the high seas This publication, Vulnerable Marine Ecosystems: processes and practices in the high seas, provides regional fisheries management bodies, States, and other interested parties with a summary of existing regional measures to protect vulnerable marine ecosystems from significant adverse impacts caused by deep-sea fisheries using bottom contact gears in the high seas. This publication compiles and summarizes information on the processes and practices of the regional fishery management bodies, with mandates to manage deep-sea fisheries in the high seas, to protect vulnerable marine ecosystems. ISBN 978-92-5-109340-5 ISSN 2070-7010 FAO 9 789251 093405 I5952E/2/03.17 Cover photo credits: Photo descriptions clockwise from top-left: Acanthagorgia spp., Paragorgia arborea, Vase sponges (images courtesy of Fisheries and Oceans, Canada); and Callogorgia spp. (image courtesy of Kirsty Kemp, the Zoological Society of London). FAO FISHERIES AND Vulnerable marine ecosystems AQUACULTURE TECHNICAL Processes and practices in the high seas PAPER 595 Edited by Anthony Thompson FAO Consultant Rome, Italy Jessica Sanders Fisheries Officer FAO Fisheries and Aquaculture Department Rome, Italy Merete Tandstad Fisheries Resources Officer FAO Fisheries and Aquaculture Department Rome, Italy Fabio Carocci Fishery Information Assistant FAO Fisheries and Aquaculture Department Rome, Italy and Jessica Fuller FAO Consultant Rome, Italy FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2016 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Symbionts and Environmental Factors Related to Deep-Sea Coral Size and Health
Symbionts and environmental factors related to deep-sea coral size and health Erin Malsbury, University of Georgia Mentor: Linda Kuhnz Summer 2018 Keywords: deep-sea coral, epibionts, symbionts, ecology, Sur Ridge, white polyps ABSTRACT We analyzed video footage from a remotely operated vehicle to estimate the size, environmental variation, and epibiont community of three types of deep-sea corals (class Anthozoa) at Sur Ridge off the coast of central California. For all three of the corals, Keratoisis, Isidella tentaculum, and Paragorgia arborea, species type was correlated with the number of epibionts on the coral. Paragorgia arborea had the highest average number of symbionts, followed by Keratoisis. Epibionts were identified to the lowest possible taxonomic level and categorized as predators or commensalists. Around twice as many Keratoisis were found with predators as Isidella tentaculum, while no predators were found on Paragorgia arborea. Corals were also measured from photos and divided into size classes for each type based on natural breaks. The northern sites of the mound supported larger Keratoisis and Isidella tentaculum than the southern portion, but there was no relationship between size and location for Paragorgia arborea. The northern sites of Sur Ridge were also the only place white polyps were found. These polyps were seen mostly on Keratoisis, but were occasionally found on the skeletons of Isidella tentaculum and even Lillipathes, an entirely separate subclass of corals from Keratoisis. Overall, although coral size appears to be impacted by 1 environmental variables and location for Keratoisis and Isidella tentaculum, the presence of symbionts did not appear to correlate with coral size for any of the coral types. -
Brochure.Pdf
Two Little Fishies Two Little Fishies Inc. 4016 El Prado Blvd., Coconut Grove, Florida 33133 U.S.A. Tel (+01) 305 661.7742 Fax (+01) 305 661.0611 eMail: [email protected] ww w. t w o l i t t l e f i s h i e s . c o m © 2004 Two Little Fishies Inc. Two Little Fishies is a registered trademark of Two Little Fishies Inc.. All illustrations, photos and specifications contained in this broc h u r e are based on the latest pr oduct information available at the time of publication. Two Little Fishies Inc. res e r ves the right to make changes at any time, without notice. Printed in USA V.4 _ 2 0 0 4 Simple, Elegant, Practical,Solutions Useful... Two Little Fishies Two Little Fishies, Inc. was founded in 1991 to pr omote the reef aquarium hobby with its in t ro d u c t o r y video and books about ree f aquariums. The company now publishes and distributes the most popular reef aquarium ref e r ence books and identification guides in English, German French and Italian, under the d.b.a. Ricordea Publishing. Since its small beginning, Two Little Fishies has also grown to become a manufacturer and im p o r ter of the highest quality products for aquariums and water gardens, with interna t i o n a l distribution in the pet, aquaculture, and water ga r den industries. Two Little Fishies’ prod u c t line includes trace element supplements, calcium supplements and buffers, phosphate- fr ee activated carbon, granular iron - b a s e d phosphate adsorption media, underwa t e r bonding compounds, and specialty foods for fish and invertebrates. -
Biological Structures As a Source of Habitat Heterogeneity and Biodiversity on the Deep Ocean Margins Lene Buhl-Mortensen1, Ann Vanreusel2, Andrew J
Marine Ecology. ISSN 0173-9565 SPECIAL TOPIC Biological structures as a source of habitat heterogeneity and biodiversity on the deep ocean margins Lene Buhl-Mortensen1, Ann Vanreusel2, Andrew J. Gooday3, Lisa A. Levin4, Imants G. Priede5,Pa˚ l Buhl-Mortensen1, Hendrik Gheerardyn2, Nicola J. King5 & Maarten Raes2 1 Institute of Marine Research, Benthic habitat group, Bergen, Norway 2 Ghent University, Marine Biology research group, Belgium 3 National Oceanography Centre Southampton, Southampton, UK 4 Integrative Oceanography Division, Scripps Institution of Oceanography, University of California, La Jolla, CA, USA 5 Oceanlab, University of Aberdeen, Newburgh, Aberdeenshire, UK Keywords Abstract Biodiversity; biotic structures; commensal; continental slope; deep sea; deep-water coral; Biological structures exert a major influence on species diversity at both local and ecosystem engineering; sponge reefs; regional scales on deep continental margins. Some organisms use other species as xenophyophores. substrates for attachment, shelter, feeding or parasitism, but there may also be mutual benefits from the association. Here, we highlight the structural attributes Correspondence and biotic effects of the habitats that corals, sea pens, sponges and xenophyo- Lene Buhl-Mortensen, Institute of Marine phores offer other organisms. The environmental setting of the biological struc- Research, Benthic habitat group, P.O. Box 1870 Nordnes, N-5817 Bergen, Norway tures influences their species composition. The importance of benthic species as E-mail: [email protected] substrates seems to increase with depth as the complexity of the surrounding geological substrate and food supply decline. There are marked differences in the Accepted: 30 December 2009 degree of mutualistic relationships between habitat-forming taxa. This is espe- cially evident for scleractinian corals, which have high numbers of facultative doi:10.1111/j.1439-0485.2010.00359.x associates (commensals) and few obligate associates (mutualists), and gorgonians, with their few commensals and many obligate associates. -
Guide to Translocating Coral Fragments for Deep-Sea Restoration
Guide to Translocating Coral Fragments for Deep-sea Restoration June 2020 | sanctuaries.noaa.gov | National Marine Sanctuaries Conservation Science Series ONMS-20-10 U.S. Department of Commerce Wilbur Ross, Secretary National Oceanic and Atmospheric Administration Neil A. Jacobs, Ph.D. Assistant Secretary of Commerce for Environmental Observation and Prediction National Ocean Service Nicole LeBoeuf, Assistant Administrator (Acting) Office of National Marine Sanctuaries John Armor, Director Report Authors: Charles A. Boch1, Andrew DeVogelaere2, Erica J. Burton2, Chad King2, Christopher Lovera1, Kurt Buck1, Joshua Lord3, Linda Kuhnz1, Michelle Kaiser4, Candace Reid-Rose4, and James P. Barry1 1Monterey Bay Aquarium Research Institute, 7700 Sandholdt Road, Moss Landing, CA 95039, USA 2Monterey Bay National Marine Sanctuary, National Ocean Service, National Oceanic and Atmospheric Administration, 99 Pacific Street, Bldg. 455A, Monterey, CA 93940, USA 3Moravian College, Bethlehem, PA, 18018, USA 4Monterey Bay Aquarium, 886 Cannery Row, Suggested Citation: Boch, C.A., A. DeVogelaere, E.J. Burton, C. King, C. Monterey, CA 93940, USA Lovera, K. Buck, J. Lord, L. Kuhnz, M. Kaiser, C. Reid- Rose, and J. P. Barry. Guide to translocating coral fragments for deep-sea restoration. National Marine Sanctuaries Conservation Series ONMS-20-10. U.S. Department of Commerce, National Oceanic and Atmospheric Administration, Office of National Marine Sanctuaries, Silver Spring, MD. 25 pp. Cover Photo: The seven coral species investigated for developing deep-sea coral restoration methods at Sur Ridge, Monterey Bay National Marine Sanctuary. Photos: MBARI About the National Marine Sanctuaries Conservation Series The Office of National Marine Sanctuaries, part of the National Oceanic and Atmospheric Administration, serves as the trustee for a system of underwater parks encompassing more than 600,000 square miles of ocean and Great Lakes waters. -
First Observations of the Cold-Water Coral Lophelia Pertusa in Mid-Atlantic Canyons of the USA
Deep-Sea Research II 104 (2014) 245–251 Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr2 First observations of the cold-water coral Lophelia pertusa in mid-Atlantic canyons of the USA Sandra Brooke a,n, Steve W. Ross b a Florida State University Coastal and Marine Laboratory, 3618 Coastal Highway 98, St. Teresa, FL 32358, USA b University of North Carolina at Wilmington, Center for Marine Science, 5600 Marvin Moss Lane, Wilmington, NC 28409, USA article info abstract Available online 26 June 2013 The structure-forming, cold-water coral Lophelia pertusa is widely distributed throughout the North fi Keywords: Atlantic Ocean and also occurs in the South Atlantic, North Paci c and Indian oceans. This species has fl USA formed extensive reefs, chie y in deep water, along the continental margins of Europe and the United Norfolk Canyon States, particularly off the southeastern U.S. coastline and in the Gulf of Mexico. There were, however, no Baltimore Canyon records of L. pertusa between the continental slope off Cape Lookout, North Carolina (NC) (∼341N, 761W), Submarine canyon and the rocky Lydonia and Oceanographer canyons off Cape Cod, Massachusetts (MA) (∼401N, 681W). Deep water During a research cruise in September 2012, L. pertusa colonies were observed on steep walls in both Coral Baltimore and Norfolk canyons. These colonies were all approximately 2 m or less in diameter, usually New record hemispherical in shape and consisted entirely of live polyps. The colonies were found between 381 m Lophelia pertusa and 434 m with environmental observations of: temperature 6.4–8.6 1C; salinity 35.0–35.6; and dissolved oxygen 2.06–4.41 ml L−1, all of which fall within the range of known L. -
Ch. 9: Ocean Biogeochemistry
6/3/13 Ch. 9: Ocean Biogeochemistry NOAA photo gallery Overview • The Big Picture • Ocean Circulation • Seawater Composition • Marine NPP • Particle Flux: The Biological Pump • Carbon Cycling • Nutrient Cycling • Time Pemitting: Hydrothermal venting, Sulfur cycling, Sedimentary record, El Niño • Putting It All Together Slides borrowed from Aradhna Tripati 1 6/3/13 Ocean Circulation • Upper Ocean is wind-driven and well mixed • Surface Currents deflected towards the poles by land. • Coriolis force deflects currents away from the wind, forming mid-ocean gyres • Circulation moves heat poleward • River influx is to surface ocean • Atmospheric equilibrium is with surface ocean • Primary productivity is in the surface ocean Surface Currents 2 6/3/13 Deep Ocean Circulation • Deep and Surface Oceans separated by density gradient caused by differences in Temperature and Salinity • This drives thermohaline deep circulation: * Ice forms in the N. Atlantic and Southern Ocean, leaving behind cold, saline water which sinks * Oldest water is in N. Pacific * Distribution of dissolved gases and nutrients: N, P, CO2 Seawater Composition • Salinity is defined as grams of salt/kg seawater, or parts per thousand: %o • Major ions are in approximately constant concentrations everywhere in the oceans • Salts enter in river water, and are removed by porewater burial, sea spray and evaporites (Na, Cl). • Calcium and Sulfate are removed in biogenic sediments • Magnesium is consumed in hydrothermal vents, in ionic exchange for Ca in rock. • Potassium adsorbs in clays. 3 6/3/13 Major Ions in Seawater The Two-Box Model of the Ocean Precipitation Evaporation River Flow Upwelling Downwelling Particle Flux Sedimentation 4 6/3/13 Residence time vs. -
CNIDARIA Corals, Medusae, Hydroids, Myxozoans
FOUR Phylum CNIDARIA corals, medusae, hydroids, myxozoans STEPHEN D. CAIRNS, LISA-ANN GERSHWIN, FRED J. BROOK, PHILIP PUGH, ELLIOT W. Dawson, OscaR OcaÑA V., WILLEM VERvooRT, GARY WILLIAMS, JEANETTE E. Watson, DENNIS M. OPREsko, PETER SCHUCHERT, P. MICHAEL HINE, DENNIS P. GORDON, HAMISH J. CAMPBELL, ANTHONY J. WRIGHT, JUAN A. SÁNCHEZ, DAPHNE G. FAUTIN his ancient phylum of mostly marine organisms is best known for its contribution to geomorphological features, forming thousands of square Tkilometres of coral reefs in warm tropical waters. Their fossil remains contribute to some limestones. Cnidarians are also significant components of the plankton, where large medusae – popularly called jellyfish – and colonial forms like Portuguese man-of-war and stringy siphonophores prey on other organisms including small fish. Some of these species are justly feared by humans for their stings, which in some cases can be fatal. Certainly, most New Zealanders will have encountered cnidarians when rambling along beaches and fossicking in rock pools where sea anemones and diminutive bushy hydroids abound. In New Zealand’s fiords and in deeper water on seamounts, black corals and branching gorgonians can form veritable trees five metres high or more. In contrast, inland inhabitants of continental landmasses who have never, or rarely, seen an ocean or visited a seashore can hardly be impressed with the Cnidaria as a phylum – freshwater cnidarians are relatively few, restricted to tiny hydras, the branching hydroid Cordylophora, and rare medusae. Worldwide, there are about 10,000 described species, with perhaps half as many again undescribed. All cnidarians have nettle cells known as nematocysts (or cnidae – from the Greek, knide, a nettle), extraordinarily complex structures that are effectively invaginated coiled tubes within a cell. -
Host-Microbe Interactions in Octocoral Holobionts - Recent Advances and Perspectives Jeroen A
van de Water et al. Microbiome (2018) 6:64 https://doi.org/10.1186/s40168-018-0431-6 REVIEW Open Access Host-microbe interactions in octocoral holobionts - recent advances and perspectives Jeroen A. J. M. van de Water* , Denis Allemand and Christine Ferrier-Pagès Abstract Octocorals are one of the most ubiquitous benthic organisms in marine ecosystems from the shallow tropics to the Antarctic deep sea, providing habitat for numerous organisms as well as ecosystem services for humans. In contrast to the holobionts of reef-building scleractinian corals, the holobionts of octocorals have received relatively little attention, despite the devastating effects of disease outbreaks on many populations. Recent advances have shown that octocorals possess remarkably stable bacterial communities on geographical and temporal scales as well as under environmental stress. This may be the result of their high capacity to regulate their microbiome through the production of antimicrobial and quorum-sensing interfering compounds. Despite decades of research relating to octocoral-microbe interactions, a synthesis of this expanding field has not been conducted to date. We therefore provide an urgently needed review on our current knowledge about octocoral holobionts. Specifically, we briefly introduce the ecological role of octocorals and the concept of holobiont before providing detailed overviews of (I) the symbiosis between octocorals and the algal symbiont Symbiodinium; (II) the main fungal, viral, and bacterial taxa associated with octocorals; (III) the dominance of the microbial assemblages by a few microbial species, the stability of these associations, and their evolutionary history with the host organism; (IV) octocoral diseases; (V) how octocorals use their immune system to fight pathogens; (VI) microbiome regulation by the octocoral and its associated microbes; and (VII) the discovery of natural products with microbiome regulatory activities. -
The State of Knowledge of Deep-Sea Corals in the New Zealand Region Di Tracey1 and Freya Hjorvarsdottir2 (Eds, Comps) © 2019
The state of knowledge of deep-sea corals in the New Zealand region Di Tracey1 and Freya Hjorvarsdottir2 (eds, comps) © 2019. All rights reserved. The copyright for this report, and for the data, maps, figures and other information (hereafter collectively referred to as “data”) contained in it, is held by NIWA is held by NIWA unless otherwise stated. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. While NIWA uses all reasonable endeavours to ensure the accuracy of the data, NIWA does not guarantee or make any representation or warranty (express or implied) regarding the accuracy or completeness of the data, the use to which the data may be put or the results to be obtained from the use of the data. Accordingly, NIWA expressly disclaims all legal liability whatsoever arising from, or connected to, the use of, reference to, reliance on or possession of the data or the existence of errors therein. NIWA recommends that users exercise their own skill and care with respect to their use of the data and that they obtain independent professional advice relevant to their particular circumstances. NIWA SCIENCE AND TECHNOLOGY SERIES NUMBER 84 ISSN 1173-0382 Citation for full report: Tracey, D.M. & Hjorvarsdottir, F. (eds, comps) (2019). The State of Knowledge of Deep-Sea Corals in the New Zealand Region. NIWA Science and Technology Series Number 84. 140 p. Recommended citation for individual chapters (e.g., for Chapter 9.: Freeman, D., & Cryer, M. (2019). Current Management Measures and Threats, Chapter 9 In: Tracey, D.M. -
Ocean Primary Production
Learning Ocean Science through Ocean Exploration Section 6 Ocean Primary Production Photosynthesis very ecosystem requires an input of energy. The Esource varies with the system. In the majority of ocean ecosystems the source of energy is sunlight that drives photosynthesis done by micro- (phytoplankton) or macro- (seaweeds) algae, green plants, or photosynthetic blue-green or purple bacteria. These organisms produce ecosystem food that supports the food chain, hence they are referred to as primary producers. The balanced equation for photosynthesis that is correct, but seldom used, is 6CO2 + 12H2O = C6H12O6 + 6H2O + 6O2. Water appears on both sides of the equation because the water molecule is split, and new water molecules are made in the process. When the correct equation for photosynthe- sis is used, it is easier to see the similarities with chemo- synthesis in which water is also a product. Systems Lacking There are some ecosystems that depend on primary Primary Producers production from other ecosystems. Many streams have few primary producers and are dependent on the leaves from surrounding forests as a source of food that supports the stream food chain. Snow fields in the high mountains and sand dunes in the desert depend on food blown in from areas that support primary production. The oceans below the photic zone are a vast space, largely dependent on food from photosynthetic primary producers living in the sunlit waters above. Food sinks to the bottom in the form of dead organisms and bacteria. It is as small as marine snow—tiny clumps of bacteria and decomposing microalgae—and as large as an occasional bonanza—a dead whale.