Deep-Sea Life Issue 14, January 2020 Cruise News E/V Nautilus Telepresence Exploration of the U.S
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MARINE FAUNA and FLORA of BERMUDA a Systematic Guide to the Identification of Marine Organisms
MARINE FAUNA AND FLORA OF BERMUDA A Systematic Guide to the Identification of Marine Organisms Edited by WOLFGANG STERRER Bermuda Biological Station St. George's, Bermuda in cooperation with Christiane Schoepfer-Sterrer and 63 text contributors A Wiley-Interscience Publication JOHN WILEY & SONS New York Chichester Brisbane Toronto Singapore ANTHOZOA 159 sucker) on the exumbrella. Color vari many Actiniaria and Ceriantharia can able, mostly greenish gray-blue, the move if exposed to unfavorable condi greenish color due to zooxanthellae tions. Actiniaria can creep along on their embedded in the mesoglea. Polyp pedal discs at 8-10 cm/hr, pull themselves slender; strobilation of the monodisc by their tentacles, move by peristalsis type. Medusae are found, upside through loose sediment, float in currents, down and usually in large congrega and even swim by coordinated tentacular tions, on the muddy bottoms of in motion. shore bays and ponds. Both subclasses are represented in Ber W. STERRER muda. Because the orders are so diverse morphologically, they are often discussed separately. In some classifications the an Class Anthozoa (Corals, anemones) thozoan orders are grouped into 3 (not the 2 considered here) subclasses, splitting off CHARACTERISTICS: Exclusively polypoid, sol the Ceriantharia and Antipatharia into a itary or colonial eNIDARIA. Oral end ex separate subclass, the Ceriantipatharia. panded into oral disc which bears the mouth and Corallimorpharia are sometimes consid one or more rings of hollow tentacles. ered a suborder of Scleractinia. Approxi Stomodeum well developed, often with 1 or 2 mately 6,500 species of Anthozoa are siphonoglyphs. Gastrovascular cavity compart known. Of 93 species reported from Ber mentalized by radially arranged mesenteries. -
In the Long Island and It's Adjacent Areas in Middle Andaman, India
Indian Journal of Geo Marine Sciences Vol. 47 (01), January 2018, pp. 96-102 Diversity and distribution of gorgonians (Octocorallia) in the Long Island and it’s adjacent areas in Middle Andaman, India J. S. Yogesh Kumar1*, S. Geetha2, C. Raghunathan3 & R. Sornaraj2 1Marine Aquarium and Regional Centre, Zoological Survey of India, (Ministry of Environment, Forest and Climate Change), Government of India, Digha – 721428, West Bengal, India. 2Research Department of Zoology, Kamaraj College (Manonmaniam Sundaranar University), Thoothukudi – 628003, Tamil Nadu, India. 3Zoological Survey of India (Ministry of Environment, Forest and Climate Change), Government of India, M Block, New Alipore, Kolkata - 700 053,West Bengal, India. [E.mail: [email protected] ] Received 05 November 2015 ; revised 17 November 2016 The diversity and distribution of gorgonian were assessed at seven sites at Long Island and it’s adjusting areas in Middle Andaman during 2013 to 2015. A total of 28 species of gorgonians are reported in shallow reef areas. Maximum life form was observed in Guaiter Island and Minimum in Headlamp Patch. A significant positive correlation was observed between the Islands, the species diversity was high for the genera Junceella, Subergorgia and Ellisella. Principal Component Analysis also supported for this three genes. [Keywords: Diversity, Gorgonian, Octocoral, Long Island, Middle Andaman, Andaman and Nicobar, India] Introduction The gorgonians popularly called as sea In India, the study on gorgonians fans and sea whips are marine sessile taxonomy initiated by Thomson and coelenterates with colonial skeleton and living Henderson15,16 and 50 species were reported of polyps1. They are exceptionally productive and a which 26 species were new from oyster banks of valuable natural asset. -
Information Review for Protected Deep-Sea Coral Species in the New Zealand Region
INFORMATION REVIEW FOR PROTECTED DEEP-SEA CORAL SPECIES IN THE NEW ZEALAND REGION NIWA Client Report: WLG2006-85 November 2006 NIWA Project: DOC06307 INFORMATION REVIEW FOR PROTECTED DEEP-SEA CORAL SPECIES IN THE NEW ZEALAND REGION Authors Mireille Consalvey Kevin MacKay Di Tracey Prepared for Department of Conservation NIWA Client Report: WLG2006-85 November 2006 NIWA Project: DOC06307 National Institute of Water & Atmospheric Research Ltd 301 Evans Bay Parade, Greta Point, Wellington Private Bag 14901, Kilbirnie, Wellington, New Zealand Phone +64-4-386 0300, Fax +64-4-386 0574 www.niwa.co.nz © All rights reserved. This publication may not be reproduced or copied in any form without the permission of the client. Such permission is to be given only in accordance with the terms of the client's contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Contents Executive Summary iv 1. Introduction 1 2. Corals 1 3. Habitat 3 4. Corals as a habitat 3 5. Major taxonomic groups of deep-sea corals in New Zealand 5 6. Distribution of deep-sea corals in the New Zealand region 9 7. Systematics of deep-sea corals in New Zealand 18 8. Reproduction and recruitment of deep-sea corals 20 9. Growth rates and deep-sea coral ageing 22 10. Fishing effects on deep-sea corals 24 11. Other threats to deep-sea corals 29 12. Ongoing research into deep-sea corals in New Zealand 29 13. Future science and challenges to deep-sea coral research in New Zealand 30 14. -
The Malacostracan Fauna of Two Arctic Fjords (West Spitsbergen): the Diversity And
+ Models OCEANO-95; No. of Pages 24 Oceanologia (2017) xxx, xxx—xxx Available online at www.sciencedirect.com ScienceDirect j ournal homepage: www.journals.elsevier.com/oceanologia/ ORIGINAL RESEARCH ARTICLE The malacostracan fauna of two Arctic fjords (west Spitsbergen): the diversity and distribution patterns of its pelagic and benthic components Joanna Legeżyńska *, Maria Włodarska-Kowalczuk, Marta Gluchowska, Mateusz Ormańczyk, Monika Kędra, Jan Marcin Węsławski Institute of Oceanology, Polish Academy of Sciences, Sopot, Poland Received 14 July 2016; accepted 6 January 2017 KEYWORDS Summary This study examines the performance of pelagic and benthic Malacostraca in two Malacostraca; glacial fjords of west Spitsbergen: Kongsfjorden, strongly influenced by warm Atlantic waters, Arctic; and Hornsund which, because of the strong impact of the cold Sørkapp Current, has more of Svalbard; an Arctic character. The material was collected during 12 summer expeditions organized from Diversity; 1997 to 2013. In all, 24 pelagic and 116 benthic taxa were recorded, most of them widely Distribution distributed Arctic-boreal species. The advection of different water masses from the shelf had a direct impact on the structure of the pelagic Malacostraca communities, resulting in the clear dominance of the sub-arctic hyperiid amphipod Themisto abyssorum in Kongsfjorden and the great abundance of Decapoda larvae in Hornsund. The taxonomic, functional and size compositions of the benthic malacostracan assemblages varied between the two fjords, and also between the glacier-proximate inner bays and the main fjord basins, as a result of the varying dominance patterns of the same assemblage of species. There was a significant drop in species richness in the strongly disturbed glacial bays of both fjords, but only in Hornsund was this accompanied by a significant decrease in density and diversity, probably due to greater isolation and poorer quality of sediment organic matter in its innermost basin. -
Bath Vnectes ~ I ~ E R I T
MARINE ECOLOGY PROGRESS SERIES Vol. 98: 107-113,1993 Published August 5 Mar. Ecol. Prog. Ser. Epibionts and intermoult duration in the crab Bath vnectes ~i~eritus Josep-Maria Gili, Pere Abello, Roger Villanueva Institut de Cihncies del Mar (CSIC). Passeig Nacional sln, E-08039 Barcelona. Spain ABSTRACT: Crustacean carapaces act as semipermanent hard substrata and can provide useful information on moulting and other biological characteristics of the host. The patterns of epibiosis on the portunid crab Bathynectes pipentus were stuhed from samples collected by trawling off southern Namibia between September 1987 and December 1988. Four species were identified as epibionts of this crab: the hydroid Stegopoma plicatile, the polychaete Spirorbis patagonicus, the pedunculate cirriped Poecilasma kaempfen and the bryozoan Nolella annectens. The patterns of distribution of the 4 epibionts were studied on the carapaces of 318 adult male crabs. The number of individuals or colonies of each epibiont species was noted within each of 4 carapace areas. The hydroid occurred preferentially on the anterior part (46.9 %) of the carapace, whereas the cirriped was found most commonly on the posterior (45.7 %) The polychaete was more common on the inferior parts (53.1 %) as was the bryozoan (80.3 %). The relationships between the size of the crab and the number of polyps (hydranths), the number of colonies and the number of gonothecae of S. plicatde were also analyzed, since these parameters could give an estimate of the intermoult period of the host. Based on the identification of 3 cohorts in both the hydroid and cirriped populations, and talung into account their probable age, a minimal time for the intermoult period can be defined. -
EXPLORING DEEP SEA HYDROTHERMAL VENTS on EARTH and OCEAN WORLDS. P. Sobron1,2, L. M. Barge3, the Invader Team. 1Impossible Sensing, St
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 2505.pdf EXPLORING DEEP SEA HYDROTHERMAL VENTS ON EARTH AND OCEAN WORLDS. P. Sobron1,2, L. M. Barge3, the InVADER Team. 1Impossible Sensing, St. Louis, MO ([email protected]) 2SETI Institute, Mtn. View, CA, , 3Jet Propulsion Laboratory, Pasadena, CA The Mission: InVADER (In-situ Vent Analysis precipitates showing exposed minerals and organic Divebot for Exobiology Research, Figure 4.1, content. The UNOLS ROV will use our coring tool and https://invader-mission.org/) is NASA’s most advanced its own manipulator and cameras to take ground truth subsea sensing payload, a tightly integrated imaging and samples as part of the InVADER deplotment. laser Raman spectroscopy/laser-induced breakdown In contrast to existing methods, InVADER allows spectroscopy/laser induced native fluorescence in-situ, autonomous, non-destructive measurements of instrument capable of in-situ, rapid, long-term these vent characteristics. InVADER will fill these gaps, underwater analyses of vent fluid and precipitates. and advance readiness in vent exploration on Earth and Such analyses are critical for finding and studying Ocean Worlds by simplifying operational strategies for life and life’s precursors at vent systems on Ocean identifying and characterizing seafloor environments. Worlds. To demonstrate the scientific potential and We will use statistical analysis tools for the fusion of functionality of the instrument, in July 2021 our team multi-sensor datasets, and develop real-time science will deploy InVADER on the Ocean Observatories data evaluation and payload control routines to Initiative’s (OOI) Regional Cabled Array (RCA), a establish, and then validate, adaptive science operations power/data distribution network off the Oregon coast, at strategies that maximize science return in a mission-like the underwater hydrothermal systems of Axial scenario. -
Significant Dissipation of Tidal Energy in the Deep Ocean Inferred from Satellite Altimeter Data
letters to nature 3. Rein, M. Phenomena of liquid drop impact on solid and liquid surfaces. Fluid Dynamics Res. 12, 61± water is created at high latitudes12. It has thus been suggested that 93 (1993). much of the mixing required to maintain the abyssal strati®cation, 4. Fukai, J. et al. Wetting effects on the spreading of a liquid droplet colliding with a ¯at surface: experiment and modeling. Phys. Fluids 7, 236±247 (1995). and hence the large-scale meridional overturning, occurs at 5. Bennett, T. & Poulikakos, D. Splat±quench solidi®cation: estimating the maximum spreading of a localized `hotspots' near areas of rough topography4,16,17. Numerical droplet impacting a solid surface. J. Mater. Sci. 28, 963±970 (1993). modelling studies further suggest that the ocean circulation is 6. Scheller, B. L. & Bous®eld, D. W. Newtonian drop impact with a solid surface. Am. Inst. Chem. Eng. J. 18 41, 1357±1367 (1995). sensitive to the spatial distribution of vertical mixing . Thus, 7. Mao, T., Kuhn, D. & Tran, H. Spread and rebound of liquid droplets upon impact on ¯at surfaces. Am. clarifying the physical mechanisms responsible for this mixing is Inst. Chem. Eng. J. 43, 2169±2179, (1997). important, both for numerical ocean modelling and for general 8. de Gennes, P. G. Wetting: statics and dynamics. Rev. Mod. Phys. 57, 827±863 (1985). understanding of how the ocean works. One signi®cant energy 9. Hayes, R. A. & Ralston, J. Forced liquid movement on low energy surfaces. J. Colloid Interface Sci. 159, 429±438 (1993). source for mixing may be barotropic tidal currents. -
Morphology and Significance of the Luminous Organs in Alepocephaloid Fishes
Uiblein, F., Ott, J., Stachowitsch,©Akademie d. Wissenschaften M. (Eds), Wien; 1996: download Deep-sea unter www.biologiezentrum.at and extreme shallow-water habitats: affinities and adaptations. - Biosystematics and Ecology Series 11:151-163. Morphology and significance of the luminous organs in alepocephaloid fishes Y. I. SAZONOV Abstract: Alepocephaloid fishes, or slickheads (two families, Alepocephalidae and Platytroctidae), are deep-sea fishes distributed in all three major oceans at depths of ca. 100-5000 m, usually between ca. 500 and 3000 m. Among about 150 known species, 13 alepocephalid and all (ca. 40) platytroctid species have diverse light organs: 1) postcleithral luminous gland (all platytroctids); it releases a luminescent secredon which presumably startles or blinds predators and allows the fish to escape; 2) relatively large, regulär photophores on the head and ventral parts of the body in the alepocephalid Microphotolepis and in 6 (of 14) platytroctid genera. These organs may serve for countershading and possibly for giving signals to other individuals of the same species; 3) small "simple" or "secondary" photophores covering the whole body and fins in 5 alepocephalid genera, and a few such structures in 1 platytroctid; these organs may be used for Camouflage in the glow of spontaneous bioluminescence; 4) the mental light organ in 2 alepocephalid genera from the abyssal zone (Bathyprion and Mirognathus) may be used as a Iure to attract prey. Introduction Alepocephaloid fishes, or slickheads, comprise two families of isospondyl- ous fishes (Platytroctidae and Alepocephalidae). The group is one of the most diverse among oceanic bathypelagic fishes (about 35 genera with 150 species), and these fishes play a significant role in the communities of meso- and bathypelagic animals. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Guide to the Identification of Precious and Semi-Precious Corals in Commercial Trade
'l'llA FFIC YvALE ,.._,..---...- guide to the identification of precious and semi-precious corals in commercial trade Ernest W.T. Cooper, Susan J. Torntore, Angela S.M. Leung, Tanya Shadbolt and Carolyn Dawe September 2011 © 2011 World Wildlife Fund and TRAFFIC. All rights reserved. ISBN 978-0-9693730-3-2 Reproduction and distribution for resale by any means photographic or mechanical, including photocopying, recording, taping or information storage and retrieval systems of any parts of this book, illustrations or texts is prohibited without prior written consent from World Wildlife Fund (WWF). Reproduction for CITES enforcement or educational and other non-commercial purposes by CITES Authorities and the CITES Secretariat is authorized without prior written permission, provided the source is fully acknowledged. Any reproduction, in full or in part, of this publication must credit WWF and TRAFFIC North America. The views of the authors expressed in this publication do not necessarily reflect those of the TRAFFIC network, WWF, or the International Union for Conservation of Nature (IUCN). The designation of geographical entities in this publication and the presentation of the material do not imply the expression of any opinion whatsoever on the part of WWF, TRAFFIC, or IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The TRAFFIC symbol copyright and Registered Trademark ownership are held by WWF. TRAFFIC is a joint program of WWF and IUCN. Suggested citation: Cooper, E.W.T., Torntore, S.J., Leung, A.S.M, Shadbolt, T. and Dawe, C. -
A Green Fluorescent Protein with Photoswitchable Emission from the Deep Sea
A Green Fluorescent Protein with Photoswitchable Emission from the Deep Sea Alexander Vogt1, Cecilia D’Angelo1, Franz Oswald2, Andrea Denzel1, Charles H. Mazel3, Mikhail V. Matz4, Sergey Ivanchenko5, G. Ulrich Nienhaus5,6,Jo¨ rg Wiedenmann1,7* 1 Institute of General Zoology and Endocrinology, University of Ulm, Ulm, Germany, 2 Department of Internal Medicine I, University of Ulm, Ulm, Germany, 3 NightSea, Andover, Massachusetts, United States of America, 4 Integrative Biology, University of Texas in Austin, Austin, Texas, United States of America, 5 Institute of Biophysics, University of Ulm, Ulm, Germany, 6 Department of Physics, University of Illinois at Urbana-Champaign, Urbana, Illinois, United States of America, 7 National Oceanography Centre, University of Southampton, Southampton, United Kingdom Abstract A colorful variety of fluorescent proteins (FPs) from marine invertebrates are utilized as genetically encoded markers for live cell imaging. The increased demand for advanced imaging techniques drives a continuous search for FPs with new and improved properties. Many useful FPs have been isolated from species adapted to sun-flooded habitats such as tropical coral reefs. It has yet remained unknown if species expressing green fluorescent protein (GFP)-like proteins also exist in the darkness of the deep sea. Using a submarine-based and -operated fluorescence detection system in the Gulf of Mexico, we discovered ceriantharians emitting bright green fluorescence in depths between 500 and 600 m and identified a GFP, named cerFP505, with bright fluorescence emission peaking at 505 nm. Spectroscopic studies showed that ,15% of the protein bulk feature reversible ON/OFF photoswitching that can be induced by alternating irradiation with blue und near- UV light. -
Okeanos Explorer ROV Dive Summary
Okeanos Explorer ROV Dive Summary Dive Information Dive Map Site Name Carondelet Reef Expedition Coordinator(s) Brian RC Kennedy, Nick Pawlenko ROV Lead(s) Karl McLetchie Science Team Lead(s) Amanda Demopoulos and Steven Auscavitch General Area Descriptor Phoenix Islands Protected Area ROV Dive Name Cruise EX-17-03 Leg 0 Dive Number 03 Equipment Deployed ROV Deep Discoverer (D2) Camera Platform Seirios CTD Depth Altitude Scanning Sonar USBL Position Heading ROV Measurements Pitch Roll HD Camera 1 HD Camera 2 Low Res Cam 1 Low Res Cam 2 Low Res Cam 3 Low Res Cam 4 Low Res Cam 5 Equipment Malfunctions Dive Summary: EX1703_DIVE03 ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^ In Water: 2017-03-10T18:25:08.463000 05°, 38.029' S ; 173°, 50.379' W Out Water: 2017-03-11T02:34:14.648000 05°, 37.629' S ; 173°, 50.105' W Off Bottom: 2017-03-11T01:37:19.059000 ROV Dive Summary 05°, 37.685' S ; 173°, 50.365' W (from processed ROV data) On Bottom: 2017-03-10T19:36:06.783000 05°, 37.936' S ; 173°, 50.260' W Dive duration: 8:9:6 Bottom Time: 6:1:12 Max. depth: 1842.3 m Special Notes Name Affiliation Email Address Scientists Involved University of (please provide name, Abby Lapointe Hawaii [email protected] location, affiliation, email) NOAA Fisheries Allen Andrews - PIFSC [email protected] 2 Amanda Demopoulos USGS [email protected] Amanda Netburn NOAA OER [email protected] FLorida State Amy Baco-Taylor University [email protected] UnderWater Andrea Pierce World Guam [email protected] Chiba Institute Asako of Technology Matsumoto