An Assessment of the Distribution of Deep-Sea Corals in Atlantic Canada by Using Both Scientific and Local Forms of Knowledge
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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. -
Author's Accepted Manuscript
Author’s Accepted Manuscript This is the accepted version of the following article: Rakka, M., Bilan, M., Godinho, A., Movilla, J., Orejas, C., & Carreiro-Silva, M. (2019). First description of polyp bailout in cold-water octocorals under aquaria maintenance. Coral Reefs, 38(1), 15-20, which has been published in final form at https://doi.org/10.1007/s00338-018-01760- x. This article may be used for non-commercial purposes in accordance with Springer Terms and Conditions for Use of Self-Archived Versions 1 First description of polyp bail-out in cold-water octocorals under aquaria maintenance Maria Rakka1,2,3, Meri Bilan1,2,3, Antonio Godinho1,2,3,Juancho Movilla4,5, Covadonga Orejas4, Marina Carreiro-Silva1,2,3 1 MARE – Marine and Environmental Sciences Centre and Centre of the Institute of Marine Research 2 IMAR – University of the Azores, Rua Frederico Machado 4, 9901-862 Horta, Portugal 3 OKEANOS Research Unit, Faculty of Science and Technology, University of the Azores, 9901-862, Horta, Portugal 4 Instituto Español de Oceanografía, Centro Oceanográfico de Baleares, Moll de Ponent s/n, 07015 Palma, Spain 5 Instituto de Ciencias del Mar (ICM-CSIC). Passeig Maritim de la Barceloneta 37-49, 08003 Barcelona, Spain Corresponding author: Maria Rakka, [email protected], +351915407062 2 Abstract Cnidarians, characterized by high levels of plasticity, exhibit remarkable mechanisms to withstand or escape unfavourable conditions including reverse development which describes processes of transformation of adult stages into early developmental stages with higher mobility. Polyp bail-out is a stress-escape response common among scleractinian species, consisting of massive detachment of live polyps and subsequent death of the mother colony. -
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. -
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. -
Deep-Sea Coral Taxa in the U.S. Northeast Region: Depth and Geographical Distribution (V
Deep-Sea Coral Taxa in the U.S. Northeast Region: Depth and Geographical Distribution (v. 2020) by David B. Packer1, Martha S. Nizinski2, Stephen D. Cairns3, 4 and Thomas F. Hourigan 1. NOAA Habitat Ecology Branch, Northeast Fisheries Science Center, Sandy Hook, NJ 2. NOAA National Systematics Laboratory Smithsonian Institution, Washington, DC 3. National Museum of Natural History, Smithsonian Institution, Washington, DC 4. NOAA Deep Sea Coral Research and Technology Program, Office of Habitat Conservation, Silver Spring, MD This annex to the U.S. Northeast chapter in “The State of Deep-Sea Coral and Sponge Ecosystems of the United States” provides a revised and updated list of deep-sea coral taxa in the Phylum Cnidaria, Class Anthozoa, known to occur in U.S. waters from Maine to Cape Hatteras (Figure 1). Deep-sea corals are defined as azooxanthellate, heterotrophic coral species occurring in waters 50 meters deep or more. Details are provided on the vertical and geographic extent of each species (Table 1). This list is adapted from Packer et al. (2017) with the addition of new species and range extensions into Northeast U.S. waters reported through 2020, along with a number of species previously not included. No new species have been described from this region since 2017. Taxonomic names are generally those currently accepted in the World Register of Marine Species (WoRMS), and are arranged by order, then alphabetically by family, genus, and species. Data sources (references) listed are those principally used to establish geographic and depth distributions. The total number of distinct deep-sea corals documented for the U.S. -
Deep-Sea Coral Taxa in the U.S. Southeast Region: Depth and Geographic Distribution (V
Deep-Sea Coral Taxa in the U.S. Southeast Region: Depth and Geographic Distribution (v. 2020) by Thomas F. Hourigan1, Stephen D. Cairns2, John K. Reed3, and Steve W. Ross4 1. NOAA Deep Sea Coral Research and Technology Program, Office of Habitat Conservation, Silver Spring, MD 2. National Museum of Natural History, Smithsonian Institution, Washington, DC 3. Cooperative Institute of Ocean Exploration, Research, and Technology, Harbor Branch Oceanographic Institute, Florida Atlantic University, Fort Pierce, FL 4. Center for Marine Science, University of North Carolina, Wilmington This annex to the U.S. Southeast chapter in “The State of Deep-Sea Coral and Sponge Ecosystems in the United States” provides a list of deep-sea coral taxa in the Phylum Cnidaria, Classes Anthozoa and Hydrozoa, known to occur in U.S. waters from Cape Hatteras to the Florida Keys (Figure 1). Deep-sea corals are defined as azooxanthellate, heterotrophic coral species occurring in waters 50 meters deep or more. Details are provided on the vertical and geographic extent of each species (Table 1). This list is an update of the peer-reviewed 2017 list (Hourigan et al. 2017) and includes taxa recognized through 2019, including one newly described species. Taxonomic names are generally those currently accepted in the World Register of Marine Species (WoRMS), and are arranged by order, and alphabetically within order by family, genus, and species. Data sources (references) listed are those principally used to establish geographic and depth distribution. Figure 1. U.S. Southeast region delimiting the geographic boundaries considered in this work. The region extends from Cape Hatteras to the Florida Keys and includes the Jacksonville Lithoherms (JL), Blake Plateau (BP), Oculina Coral Mounds (OC), Miami Terrace (MT), Pourtalès Terrace (PT), Florida Straits (FS), and Agassiz/Tortugas Valleys (AT). -
Deep-Sea Corals from O'higgins I Seamount
Lat. Am. J. Aquat. Res., 40(2): 467-472, 2012 Colonial life on O’Higgins I seamount 467 DOI: 10.3856/vol40-issue2-fulltext-23 Short Communication Colonial life under the Humboldt Current System: deep-sea corals from O’Higgins I seamount Juan I. Cañete1 & Verena Häussermann2,3 1Facultad de Ciencias, Universidad de Magallanes, P.O. Box 113-D, Punta Arenas, Chile 2Escuela de Ciencias del Mar, Pontificia Universidad Católica de Valparaíso Avda. Altamirano 1480, Valparaíso, Chile 3Fundación San Ignacio de Huinay, P.O. Box 462, Puerto Montt, Chile ABSTRACT. A benthic community constituted by an assemblage of at least four species of deep-sea corals collected in only one trawl carried-out on the summit of the O’Higgins I seamount, central Chile. The corals were collected in only one trawl carried-out during a Chilean-Japanese cruise onboard the R/V” Koyo Maru” in December 29, 2004. Presence of oxygenated and cold Antarctic Intermediate Water (>400 m depth) on the plateau was recorded under of the Equatorial Subsurface Water associated to the oxygen-minimum zone -1 (OMZ, <1 mL O2 L ). The biogeographic origin of the fauna evidenced a mix of Subantarctic and central Chile continental margin species. The assemblage is represented by two species of anthipatarians (Leiopathes sp. and Chrysopathes sp.), one unidentified species of Paragorgiidae and one species of Isididae (Acanella chilensis). The study demonstrated that deep-water corals of the O’Higgins seamount provide crucial habitat for commercially important crustacean exploited along continental margin off central Chile such as nylon shrimp (Heterocarpus reedi). This resource as well as some fishes such as alfonsino (Beryx splendens) and orange roughy (Hoplostethus atlanticus) could drawing the commercial fishing industry to these fragile areas poorly known Chilean marine benthic communities. -
Crustaceans Associated with the Deep-Water Gorgonian Corals Paragorgia Arborea (L., 1758) and Primnoa Resedaeformis (Gunn., 1763) L
JOURNAL OF NATURAL HISTORY, 0000, 00, 1–15 Crustaceans associated with the deep-water gorgonian corals Paragorgia arborea (L., 1758) and Primnoa resedaeformis (Gunn., 1763) L. BUHL-MORTENSEN and P. B. MORTENSEN Department of Fisheries and Oceans, Marine Environmental Sciences Division, Bedford Institute of Oceanography, PO Box 1006, Dartmouth, NS B2Y 4A2, Canada; e-mail: [email protected] (Accepted 4 February 2003) To explore the crustacean fauna associated with deep-water gorgonian corals, suction samples were taken from colonies of Paragorgia arborea and Primnoa resedaeformis using a Remotely Operated Vehicle. Seven colonies of P. arborea and eight of P. resedaeformis were sampled from 330–500 m depth in the Northeast Channel off Nova Scotia. A total of 17 species were identified as be- ing associated with the corals. The P. arborea-fauna was richer than the P. resedaeformis fauna in both abundance and number of species, with 1303 versus 102 individuals and 16 versus seven species, respectively. However, 13 of the species associated with P. arborea were from hydroids attached to the coral. Amphipods dominated the fauna both in abundance and numbers of species and the most common species were Metopa bruzelii, Stenopleustes malmgreni, Proboloides calcarata and Aeginella spinosa. The isopod Munna boecki and the cirripede Ornatoscalpellum stroemii were also quite common. The most strongly associated crustaceans were two parasitic poecilostomatid copepods; these are common also on tropical gorgonians and are most likely obligate associates. The frequently occurring shrimp Pandalus propinquus probably avoids predation by seeking protection among the coral branches. Shrimp counts from video records showed that visual inspection without physically disturbing colonies will generally not reveal the crustaceans hidden in coral colonies. -
Genetic Analysis of Bamboo Corals (Cnidaria: Octocorallia: Isididae): Does Lack of Colony Branching Distinguish Lepidisis from Keratoisis?
BULLETIN OF MARINE SCIENCE, 81(3): 323–333, 2007 Genetic analYsis of bamboo corals (CniDaria: Octocorallia: ISIDIDae): Does lacK of colonY brancHing DistinguisH LEPIDISIS from KERATOISIS? Scott C. France Abstract Bamboo corals (family Isididae) are among the most easily recognized deep-water octocorals due to their articulated skeleton comprised of non-sclerite calcareous in- ternodes alternating with proteinaceous nodes. Most commonly encountered in the deep-sea are species in the subfamily Keratoisidinae, including the genera Acanella Gray, 1870, Isidella Gray, 1857, Keratoisis Wright, 1869, and Lepidisis Verrill, 1883. Systematists have debated whether Lepidisis and Keratoisis should be defined on the basis of “colony branching.” Although recent taxonomic keys use “colonies un- branched” to distinguish Lepidisis, the original description of the genus included both branched and unbranched morphologies, with both forms also classified in Keratoisis. This study analyzed mitochondrialD NA sequence variation from isidids collected between 500–2250 m depth to address the following question: are un- branched, whip-like bamboo corals in the subfamily Keratoisidinae monophyletic? DNA sequences of the msh1 gene (1426 nucleotides) from 32 isidids were used to construct a phylogeny. Coding of gaps provided additional informative characters for taxon discrimination. The results show five well-supported clades, all grouping both branched and unbranched colony morphologies; there was no single mono- phyletic clade of unbranched Keratoisidinae. The msh1 phylogeny suggests that the distinction between the genera Lepidisis and Keratoisis should not be based on whether or not colonies branch. Bamboo corals (Family Isididae) are common in deep-sea habitats. The family is characterized by its axial skeleton, which is composed of calcareous internodes alter- nating with proteinaceous, sclerite-free nodes (Fig. -
Character Lability in Deep-Sea Bamboo Corals (Octocorallia, Isididae, Keratoisidinae)
Vol. 397: 11–23, 2009 MARINE ECOLOGY PROGRESS SERIES Published December 17 doi: 10.3354/meps08307 Mar Ecol Prog Ser Contribution to the Theme Section ‘Conservation and management of deep-sea corals and coral reefs’ OPENPEN ACCESSCCESS Character lability in deep-sea bamboo corals (Octocorallia, Isididae, Keratoisidinae) Luisa F. Dueñas, Juan A. Sánchez* Departamento de Ciencias Biológicas-Facultad de Ciencias, Laboratorio de Biología Molecular Marina (BIOMMAR), Universidad de los Andes, Carrera 1 #18A–10, Bogotá, Colombia ABSTRACT: Morphological traits that appear multiple times when mapped onto molecular phyloge- nies have been associated with character lability. In an ecological context, functional characters, if labile, could confer advantages for adaptation to specific habitats. Bamboo corals are long-lived, deep-sea octocorals characterized by an obvious modularity, which affords diverse branching mor- phologies in the Keratoisidinae subfamily. We reconstructed molecular phylogenies using 16S (mito- chondrial) and ITS2 (nuclear) ribosomal DNA, and obtained 39 ITS2 and 22 16S sequences from 22 different specimens. The molecular topologies showed Keratoisidinae genera as polyphyletic. Twelve morphological characters were chosen to make the ancestral character reconstruction, none of which exhibited character states forming monophyletic groups when mapped onto molecular phy- logenies. The different character states appeared as having been gained and lost multiple times. Modular organisms such as bamboo corals could have higher character evolvability than unitary organisms. Complexity arising from simple body plans is a typical characteristic in most modular organisms, such as plants and colonial marine invertebrates. However, bamboo corals may also exhibit phenotypic plasticity associated with continuous characters, given that they can respond to extrinsic controls. -
Light and Vision in the Deep-Sea Benthos: I
Nova Southeastern University NSUWorks Marine & Environmental Sciences Faculty Articles Department of Marine and Environmental Sciences 10-1-2012 Light and Vision in the Deep-Sea Benthos: I. Bioluminescence at 500-1000 m Depth in the Bahamian Islands Sönke Johnsen Duke University Tamara M. Frank Nova Southeastern University, [email protected] Steven H.D. Haddock Monterey Bay Aquarium Research Institute Edith A. Widder Ocean Research and Conservation Association Charles G. Messing Nova Southeastern University, [email protected] Find out more information about Nova Southeastern University and the Halmos College of Natural Sciences and Oceanography. Follow this and additional works at: https://nsuworks.nova.edu/occ_facarticles Part of the Marine Biology Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons Recommended Citation Johnsen, Sönke, Tamara M. Frank, Steven HD Haddock, Edith A. Widder, and Charles G. Messing. "Light and vision in the deep-sea benthos: I. Bioluminescence at 500–1000 m depth in the Bahamian Islands." The ourJ nal of experimental biology 215, no. 19 (2012): 3335-3343. This Article is brought to you for free and open access by the Department of Marine and Environmental Sciences at NSUWorks. It has been accepted for inclusion in Marine & Environmental Sciences Faculty Articles by an authorized administrator of NSUWorks. For more information, please contact [email protected]. 3335 The Journal of Experimental Biology 215, 3335-3343 © 2012. Published by The Company of Biologists Ltd doi:10.1242/jeb.072009 RESEARCH ARTICLE Light and vision in the deep-sea benthos: I. Bioluminescence at 500–1000m depth in the Bahamian Islands Sönke Johnsen1,*, Tamara M. -
Scs18-23 WG-ESA Report 2018
Northwest Atlantic Fisheries Organization Serial No N6900 NAFO SCS Doc. 18/23 SC WORKING GROUP ON ECOSYSTEM SCIENCE AND ASSESSMENT – NOVEMBER 2018 Report of the 11th Meeting of the NAFO Scientific Council Working Group on Ecosystem Science and Assessment (WG-ESA) NAFO Headquarters, Dartmouth, Canada 13 - 22 November 2018 Contents Introduction ........................................................................................................................................................................................................3 Theme 1: spatial considerations................................................................................................................................................................4 1.1. Update on VME indicator species data and distribution .............................................................................4 1.2 Progress on implementation of workplan for reassessment of VME fishery closures. .................9 1.3. Discussion on updating Kernel Density Analysis and SDM’s .....................................................................9 1.4. Update on the Research Activities related to EU-funded Horizon 2020 ATLAS Project ...............9 1.5. Non-sponge and non-coral VMEs (e.g. bryozoan and sea squirts). ..................................................... 14 1.6 Ecological diversity mapping and interactions with fishing on the Flemish Cap .......................... 14 1.7 Sponge removal by bottom trawling in the Flemish Cap area: implications for ecosystem functioning ...................................................................................................................................................................