Shallow Seamounts Represent Speciation Islands for Circumglobal
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Skeletal Development and Mineralization Pattern of The
e Rese tur arc ul h c & a u D q e A v e f l o o Mesa-Rodríguez et al., J Aquac Res Development 2014, 5:6 l p a m n Journal of Aquaculture r e u n o t DOI: 10.4172/2155-9546.1000266 J ISSN: 2155-9546 Research & Development Research Article OpenOpen Access Access Skeletal Development and Mineralization Pattern of the Vertebral Column, Dorsal, Anal and Caudal Fin Complex in Seriola Rivoliana (Valenciennes, 1833) Larvae Mesa-Rodríguez A*, Hernández-Cruz CM, Socorro JA, Fernández-Palacios H, Izquierdo MS and Roo J Aquaculture Research Group, Science and Technology Park, University of Las Palmas de Gran Canaria, P. O. Box 56, 35200 Telde, Canary Islands, Spain Abstract Bone and fins development in Seriola rivoliana were studied from cleared and stained specimens from 3 to 33 days after hatching. The vertebral column began to mineralize in the neural arches at 4.40 ± 0.14 mm Standard Length (SL), continued with the haemal arches and centrums following a cranial-caudal direction. Mineralization of the caudal fin structures started with the caudal rays by 5.12 ± 0.11 mm SL, at the same time that the notochord flexion occurs. The first dorsal and anal fin structures were the hard spines (S), and lepidotrichium (R) by 8.01 ± 0.26 mm SL. The metamorphosis was completed by 11.82 ± 0.4 mm SL. Finally, the fin supports (pterygiophores) and the caudal fins were completely mineralized by 16.1 ± 0.89 mm SL. In addition, the meristic data of 23 structures were provided. -
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. -
Identity Crisis Or Split Personality? Trans-Ocean Distances and Not Within Individual Regions
Journal of Biogeography (J. Biogeogr.) (2007) 34, 2001–2008 GUEST Seamounts: identity crisis or split EDITORIAL personality? Craig R. McClain* Monterey Bay Aquarium Research Institute, ABSTRACT 7700 Sandholdt Road, Moss Landing, CA At present, researchers propose that over 14,000 seamounts exist and, like their 95039, USA terrestrial analogues, function like islands. In addition, seamounts are described as oases, biodiversity hotspots, and lush coral/sponge gardens. Here I discuss the extent to which these tenets regarding seamounts may be inappropriate, suffer from a lack of support, and be over-generalizations of a broad range of envi- ronmental types encountered on seamounts. Ultimately, for seamount science to progress, we need to challenge our conventional wisdom on these habitats and the extent to which all seamounts function in a similar manner. *Correspondence: Craig R. McClain, Monterey Bay Aquarium Research Institute, 7700 Keywords Sandholdt Road, Moss Landing, CA, 95039, USA. Biodiversity, conservation, coral, deep sea, ecological oasis, endemism, hotspot, E-mail: [email protected] island biogeography, isolation, seamount. biological communities that support highly unique and INTRODUCTION endemic faunas’. In ‘Toward a strategy for high seas marine There is no such things as mountains and valleys on the deep-sea protected areas’, Gjerde & Breide (2003) notes that ‘Sea- bottom. mounts are areas of high endemic biodiversity with little Mosely (1880), p. 343 overlap in community composition between seamount Less than 100 years after Mosely’s statement, Hubbs (1959) clusters’. contemplated the ‘scientific interests, particularly in respect Alternatively, others suggest that seamounts are unique to zoogeography and speciation’ of recently discovered habitats for reasons not related to their ‘islandness’. -
Cnidaria, Hydrozoa) from the Vema and Valdivia Seamounts (SE Atlantic)
European Journal of Taxonomy 758: 49–96 ISSN 2118-9773 https://doi.org/10.5852/ejt.2021.758.1425 www.europeanjournaloftaxonomy.eu 2021 · Gil M. & Ramil F. This work is licensed under a Creative Commons Attribution License (CC BY 4.0). Research article urn:lsid:zoobank.org:pub:7CA6D8AC-2312-47F9-8C17-528B94E4C8A7 Hydroids (Cnidaria, Hydrozoa) from the Vema and Valdivia seamounts (SE Atlantic) Marta GIL 1,* & Fran RAMIL 2 1,2 CIM-UVigo – Centro de Investigación Mariña, Facultade de Ciencias do Mar, Universidade de Vigo, Spain. 1 Instituto Español de Oceanografía, Centro Oceanográfi co de Vigo, Spain. * Corresponding author: [email protected] 2 Email: [email protected] 1 urn:lsid:zoobank.org:author:FFF187EB-84CE-4A54-9A01-4E4326B5CD26 2 urn:lsid:zoobank.org:author:67BAF0B6-E4D5-4A2D-8C03-D2D40D522196 Abstract. In this report, we analyse the benthic hydroids collected on the Vema and Valdivia seamounts during a survey conducted in 2015 in the SEAFO Convention Area, focused on mapping and analysing the occurrence and abundance of benthopelagic fi sh and vulnerable marine ecosystem (VMEs) indicators on selected Southeast Atlantic seamounts. A total of 27 hydroid species were identifi ed, of which 22 belong to Leptothecata and only fi ve to Anthoathecata. Monostaechoides gen. nov. was erected within the family Halopterididae to accommodate Plumularia providentiae Jarvis, 1922, and a new species, Monotheca bergstadi sp. nov., is also described. Campanularia africana is recorded for the fi rst time from the Atlantic Ocean, and the Northeast Atlantic species Amphinema biscayana, Stegopoma giganteum and Clytia gigantea are also recorded from the South Atlantic. -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
Seriola Dumerili (Greater Amberjack)
UWI The Online Guide to the Animals of Trinidad and Tobago Diversity Seriola dumerili (Greater Amberjack) Family: Carangidae (Jacks and Pompanos) Order: Perciformes (Perch and Allied Fish) Class: Actinopterygii (Ray-finned Fish) Fig. 1. Greater amberjack, Seriola dumerili. [http://portal.ncdenr.org/web/mf/amberjack_greater downloaded 20 October 2016] TRAITS. The species Seriola dumerili displays rapid growth during development as a juvenile progressing to an adult. It is the largest species of the family of jacks. At adulthood, S. dumerili would typically weigh about 80kg and reach a length of 1.8-1.9m. Sexual maturity is achieved between the age of 3-5 years, and females may live longer and grow larger than males (FAO, 2016). S. dumurili are rapid-moving predators as shown by their body form (Fig. 1) (FLMNH, 2016). The adult is silvery-bluish in colour, whereas the juvenile is yellow-green. It has a characteristic goldish side line, as well as a dark band near the eye, as seen in Figs 1 and 2 (FAO, 2016; MarineBio, 2016; NCDEQ, 2016). DISTRIBUTION. S. dumerili is native to the waters of Trinidad and Tobago. Typically pelagic, found between depths of 10-360m, the species can be described as circumglobal. In other words, it is found worldwide, as seen in Fig. 3, though much more rarely in some areas, for example the eastern Pacific Ocean (IUCN, 2016). Due to this distribution, there is no threat to the population of the species, despite overfishing in certain locations. Migrations do occur, which are thought to be linked to reproductive cycles. -
Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats. -
World Ocean Thermocline Weakening and Isothermal Layer Warming
applied sciences Article World Ocean Thermocline Weakening and Isothermal Layer Warming Peter C. Chu * and Chenwu Fan Naval Ocean Analysis and Prediction Laboratory, Department of Oceanography, Naval Postgraduate School, Monterey, CA 93943, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-831-656-3688 Received: 30 September 2020; Accepted: 13 November 2020; Published: 19 November 2020 Abstract: This paper identifies world thermocline weakening and provides an improved estimate of upper ocean warming through replacement of the upper layer with the fixed depth range by the isothermal layer, because the upper ocean isothermal layer (as a whole) exchanges heat with the atmosphere and the deep layer. Thermocline gradient, heat flux across the air–ocean interface, and horizontal heat advection determine the heat stored in the isothermal layer. Among the three processes, the effect of the thermocline gradient clearly shows up when we use the isothermal layer heat content, but it is otherwise when we use the heat content with the fixed depth ranges such as 0–300 m, 0–400 m, 0–700 m, 0–750 m, and 0–2000 m. A strong thermocline gradient exhibits the downward heat transfer from the isothermal layer (non-polar regions), makes the isothermal layer thin, and causes less heat to be stored in it. On the other hand, a weak thermocline gradient makes the isothermal layer thick, and causes more heat to be stored in it. In addition, the uncertainty in estimating upper ocean heat content and warming trends using uncertain fixed depth ranges (0–300 m, 0–400 m, 0–700 m, 0–750 m, or 0–2000 m) will be eliminated by using the isothermal layer. -
Morphological Development of Embryo, Larvae and Juvenile in Yellowtail Kingfish, Seriola Lalandi
Dev. Reprod. Vol. 20, No. 2, 131~140, June, 2016 http://dx.doi.org/10.12717/DR.2016.20.2.131 ISSN 2465-9525 (Print) ISSN 2465-9541 (Online) Morphological Development of Embryo, Larvae and Juvenile in Yellowtail Kingfish, Seriola lalandi Sang Geun Yang1, Sang Woo Hur2, Seung Cheol Ji1, Sang Gu Lim1, Bong Seok Kim1, Minhwan Jeong1, Chi Hoon Lee2 and †Young-Don Lee2 1Jeju Fisheries Research Institute, National Institute of Fisheries Science, Jeju 63610, Korea 2Marine Science Institute, Jeju National University, Jeju 63333, Korea ABSTRACT : This study monitored the morphological development of embryo, larvae and juvenile yellowtail kingfish, Seriola lalandi, for their aquaculture. The fertilized eggs obtained by natural spawning were spherical shape and buoyant. Fertilized eggs were transparent and had one oil globule in the yolk, with an egg diameter of 1.35 ± 0.04 mm and an oil globule diameter of 0.32 ± 0.02 mm. The fertilized eggs hatched 67–75 h after fertilization in water at 20 ± 0.5°C. The total length (TL) of the hatched larvae was 3.62 ± 0.16 mm. During hatching, the larvae, with their mouth and anus not yet opened. The yolk was completely absorbed 3 days after hatching (DAH), while the TL of post-larvae was 4.72 ± 0.07 mm. At 40 DAH, the juveniles had grown to 30.44 ± 4.07 mm in TL, body depth increased, the body color changed to a black, yellow, and light gray-blue color, and 3–4 vertical stripes appeared. At 45 DAH, the juveniles were 38.67 ± 5.65 mm in TL and 10.10 ± 0.94 mm in body depth. -
Morphological Development of Embryo, Larvae and Juvenile in Yellowtail Kingfish, Seriola Lalandi
Dev. Reprod. Vol. 20, No. 2, 109~118, June, 2016 http://dx.doi.org/10.12717/DR.2016.20.2.109 ISSN 2465-9525 (Print) ISSN 2465-9541 (Online) Morphological Development of Embryo, Larvae and Juvenile in Yellowtail kingfish, Seriola lalandi Sang Geun Yang1, Sang Woo Hur2, Seung Cheol Ji1, Sang Gu Lim1, Bong Seok Kim1, Minhwan Jeong1, Chi Hoon Lee2 and †Young-Don Lee2 1Jeju Fisheries Research Institute, National Institute of Fisheries Science, Jeju 63610, Korea 2Marine Science Institute, Jeju National University, Jeju 63333, Korea ABSTRACT : This study monitored the morphological development of embryo, larvae and juvenile yellowtail kingfish, Seriola lalandi, for their aquaculture. The fertilized eggs obtained by natural spawning were spherical shape and buoyant. Fertilized eggs were transparent and had one oil globule in the yolk, with an egg diameter of 1.35 ± 0.04 mm and an oil globule diameter of 0.32 ± 0.02 mm. The fertilized eggs hatched 67–75 h after fertilization in water at 20 ± 0.5°C. The total length (TL) of the hatched larvae was 3.62 ± 0.16 mm. During hatching, the larvae, with their mouth and anus not yet opened. The yolk was completely absorbed 3 days after hatching (DAH), while the TL of post-larvae was 4.72 ± 0.07 mm. At 40 DAH, the juveniles had grown to 30.44 ± 4.07 mm in TL, body depth increased, the body color changed to a black, yellow, and light gray-blue color, and 3–4 vertical stripes appeared. At 45 DAH, the juveniles were 38.67 ± 5.65 mm in TL and 10.10 ± 0.94 mm in body depth. -
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. -
© Iccat, 2007
A5 By-catch Species APPENDIX 5: BY-CATCH SPECIES A.5 By-catch species By-catch is the unintentional/incidental capture of non-target species during fishing operations. Different types of fisheries have different types and levels of by-catch, depending on the gear used, the time, area and depth fished, etc. Article IV of the Convention states: "the Commission shall be responsible for the study of the population of tuna and tuna-like fishes (the Scombriformes with the exception of Trichiuridae and Gempylidae and the genus Scomber) and such other species of fishes exploited in tuna fishing in the Convention area as are not under investigation by another international fishery organization". The following is a list of by-catch species recorded as being ever caught by any major tuna fishery in the Atlantic/Mediterranean. Note that the lists are qualitative and are not indicative of quantity or mortality. Thus, the presence of a species in the lists does not imply that it is caught in significant quantities, or that individuals that are caught necessarily die. Skates and rays Scientific names Common name Code LL GILL PS BB HARP TRAP OTHER Dasyatis centroura Roughtail stingray RDC X Dasyatis violacea Pelagic stingray PLS X X X X Manta birostris Manta ray RMB X X X Mobula hypostoma RMH X Mobula lucasana X Mobula mobular Devil ray RMM X X X X X Myliobatis aquila Common eagle ray MYL X X Pteuromylaeus bovinus Bull ray MPO X X Raja fullonica Shagreen ray RJF X Raja straeleni Spotted skate RFL X Rhinoptera spp Cownose ray X Torpedo nobiliana Torpedo