Chapter 35 Extent of Assessment of Marine Biological Diversity
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The 2016 SWFSC Billfish Newsletter
The SouthwestSWFSC Fisheries 2016 Billfish Science Newsletter Center’s 2016 Billfish Newsletter Global Tagging Map El Niño fishing conditions Catch-Photo-Release mobile phone application IGFA Great Marlin Race and satellite tagging 1 Top Anglers and Captains of 2015 SWFSC 2016 Billfish Newsletter Table of Contents Special Foreword …………………………………………………………….. 3 An Inside Look ……………………………………………………………..… 4 Prologue …………………………………………………………………….… 5 Introduction ……………………………………………………………..….… 5 The International Billfish Angler Survey ………………………………....... 7 Pacific blue marlin 9 Striped marlin 10 Indo-Pacific sailfish 11 Black marlin 13 Shortbill spearfish 13 Broadbill swordfish 14 The Billfish Tagging Program ……………………………………………..... 14 The Hawaiian Islands 16 2015 Tagging-at-a-Glance Map 17 Baja California and Guerrero, Mexico 18 Southern California 18 Western Pacific 18 Top Anglers and Captains Acknowledgements ……………………………. 19 Top Tagging Anglers 19 Top Tagging Captains 21 Tag Recoveries ……………………………………………………………….. 21 Science in Action: “The IGFA Great Marlin Race and Marlin Tagging” 23 Acknowledgements ………………………………………………………....... 25 Angler Photos ……………………………………………………………..….. 26 Congratulations to Captain Teddy Hoogs of the Bwana for winning this year’s cover photo contest! Teddy photographed this spectacular marlin off the coast of Hawaii. Fish on! 2 Special Forward James Wraith, director of the SWFSC Cooperative Billfish Tagging Program since 2007, recently left the SWFSC to move back to Australia. James was an integral part of the Highly Migratory Species (HMS) program. In addition to day-to-day work, James planned and organized the research cruises for HMS at the SWFSC and was involved in tagging thresher, blue, and mako sharks in the Southern California Bight for many years. We are sad to see him go but are excited for his future opportunities and thankful for his many contributions to the program over the last 10 years. -
Striped Marlin (Kajikia Audax)
I & I NSW WILD FISHERIES RESEARCH PROGRAM Striped Marlin (Kajikia audax) EXPLOITATION STATUS UNDEFINED Status is yet to be determined but will be consistent with the assessment of the south-west Pacific stock by the Scientific Committee of the Central and Western Pacific Fisheries Commission. SCIENTIFIC NAME STANDARD NAME COMMENT Kajikia audax striped marlin Previously known as Tetrapturus audax. Kajikia audax Image © I & I NSW Background lengths greater than 250cm (lower jaw-to-fork Striped marlin (Kajikia audax) is a highly length) and can attain a maximum weight of migratory pelagic species distributed about 240 kg. Females mature between 1.5 and throughout warm-temperate to tropical 2.5 years of age whilst males mature between waters of the Indian and Pacific Oceans.T he 1 and 2 years of age. Striped marlin are stock structure of striped marlin is uncertain multiple batch spawners with females shedding although there are thought to be separate eggs every 1-2 days over 4-41 events per stocks in the south-west, north-west, east and spawning season. An average sized female of south-central regions of the Pacific Ocean, as about 100 kg is able to produce up to about indicated by genetic research, tagging studies 120 million eggs annually. and the locations of identified spawning Striped marlin spend most of their time in grounds. The south-west Pacific Ocean (SWPO) surface waters above the thermocline, making stock of striped marlin spawn predominately them vulnerable to surface fisheries.T hey are during November and December each year caught mostly by commercial longline and in waters warmer than 24°C between 15-30°S recreational fisheries throughout their range. -
Vmes on the Corner Seamounts] NAFO
Vulnerable Marine Ecosystems Database Newfoundland Seamounts Geographical reference Northwest Atlantic Management Body/Authority Northwest Atlantic Fisheries Organization (NAFO) Area Type Seamount closure (NAFO) Closed since 2007-01-01 until 2021-12-31 Habitat and Biology General Biology Seamounts are uniquely complex habitats that rise into bathyal and epi-pelagic depths. In general seamounts, owing to their isolation tend to support endemic populations and unique faunal assemblages. Physical description of the environment: Seamounts Newfoundland Seamounts consist of 6 peaks with summits all deeper than 2400 m, with most of the area being deeper than 3500m. The Newfoundland seamounts were volcanically active in the late Cretaceous period. Named seamounts include Shredder and Scruntion. Map FAO Fisheries and Aquaculture Department Disclaimer The boundaries and names shown and the designations used on this map do not imply the expression of any opinion whatsoever on the part of FAO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers and boundaries. Dashed lines on maps represent approximate border lines for which there may not yet be full agreement. Management Measures specific to this area Area closed to bottom fishing from 1 Jan 2007 to 31 Dec 2010. Provisions for exploratory fishery, encounters and temporary closures. (Art 15.5-10) Period in force: 2007-01-01 to 2010-12-31 Source of information NAFO Conservation and Enforcement Measures 2010 (NAFO FC Doc. 10/1 Serial No. N5740) http://archive.nafo.int/open/fc/2010/fcdoc10-01.pdf 2010 NAFO. 2010. Scientific Council Meeting, 20-24 Sep 2010. -
Black Marlin (Makaira Indica) Blue Marlin (Makaira Nigricans) Blue
Black marlin (Makaira indica) Blue marlin (Makaira nigricans) Blue shark (Prionace glauca) Opah (Lampris guatus) Shorin mako shark (Isurus oxyrinchus) Striped marlin (Kaijkia audax) Western Central Pacific, North Pacific, South Pacific Pelagic longline July 12, 2016 Alexia Morgan, Consulng Researcher Disclaimer Seafood Watch® strives to have all Seafood Reports reviewed for accuracy and completeness by external sciensts with experse in ecology, fisheries science and aquaculture. Scienfic review, however, does not constute an endorsement of the Seafood Watch® program or its recommendaons on the part of the reviewing sciensts. Seafood Watch® is solely responsible for the conclusions reached in this report. Table of Contents Table of Contents 2 About Seafood Watch 3 Guiding Principles 4 Summary 5 Final Seafood Recommendations 5 Introduction 8 Assessment 10 Criterion 1: Impacts on the species under assessment 10 Criterion 2: Impacts on other species 22 Criterion 3: Management Effectiveness 45 Criterion 4: Impacts on the habitat and ecosystem 55 Acknowledgements 58 References 59 Appendix A: Extra By Catch Species 69 2 About Seafood Watch Monterey Bay Aquarium’s Seafood Watch® program evaluates the ecological sustainability of wild-caught and farmed seafood commonly found in the United States marketplace. Seafood Watch® defines sustainable seafood as originang from sources, whether wild-caught or farmed, which can maintain or increase producon in the long-term without jeopardizing the structure or funcon of affected ecosystems. Seafood Watch® makes its science-based recommendaons available to the public in the form of regional pocket guides that can be downloaded from www.seafoodwatch.org. The program’s goals are to raise awareness of important ocean conservaon issues and empower seafood consumers and businesses to make choices for healthy oceans. -
Age Progressive Volcanism in the New England Seamounts and the Opening of the Central Atlantic Ocean
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 89, NO. B12, PAGES 9980-9990, NOVEMBER 10, 1984 AGEPROGRESSIVE VOLCANISM IN THENEW ENGLAND SEAMOUNTS AND THE OPENING OF THE CENTRAL ATLANTIC OCEAN R. A. Duncan College of Oceanography, Oregon State University, Corvallis Abstract. Radiometric ages (K-Ar and •øAr- transient featur e•s that allow calculations of 39Ar methods) have been determined on dredged relative motions only. volcanic rocks from seven of the New England The possibility that plate motions may be Seamounts, a prominent northwest-southeast trend- recorded by lines of islands and seamounts in the ing volcanic lineament in the northwestern ocean basins is attractive in this regard. If, Atlantic Ocean. The •øAr-39Ar total fusion and as the Carey-Wilson-Morgan model [Carey, 1958; incren•ental heating ages show an increase in Wilson, 1963; Morgan, 19•1] proposes, sublitho- seamount construction age from southeast to spheric, thermal anomalies called hot spots are northwest that is consistent with northwestward active and fixed with respect to one another in motion of the North American plate over a New the earth's upper mantle, they would then consti- England hot spot between 103 and 82 Ma. A linear tute a reference frame for directly and precisely volcano migration rate of 4.7 cm/yr fits the measuring plate motions. Ancient longitudes as seamount age distribution. These ages fall well as latitudes would be determined from vol- Within a longer age progression from the Corner cano construction ages along the tracks left by Seamounts (70 to 75 Ma), at the eastern end of hot spots and, providing relative plate motions the New England Seamounts, to the youngest phase are also known, quantitative estimates of conver- of volcanism in the White Mountain Igneous gent plate motions can be calculated [Engebretson Province, New England (100 to 124 Ma). -
A Black Marlin, Makaira Indica, from the Early Pleistocene of the Philippines and the Zoogeography of Istiophorid B1llfishes
BULLETIN OF MARINE SCIENCE, 33(3): 718-728,1983 A BLACK MARLIN, MAKAIRA INDICA, FROM THE EARLY PLEISTOCENE OF THE PHILIPPINES AND THE ZOOGEOGRAPHY OF ISTIOPHORID B1LLFISHES Harry L Fierstine and Bruce 1. Welton ABSTRACT A nearly complete articulated head (including pectoral and pelvic girdles and fins) was collected from an Early Pleistocene, upper bathyal, volcanic ash deposit on Tambac Island, Northwest Central Luzon, Philippines. The specimen was positively identified because of its general resemblance to other large marlins and by its rigid pectoral fin, a characteristic feature of the black marlin. This is the first fossil billfish described from Asia and the first living species of billfi sh positively identified in the fossil record. The geographic distribution of the two living species of Makaira is discussed, Except for fossil localities bordering the Mediterranean Sea, the distribution offossil post-Oligocene istiophorids roughly corresponds to the distribution of living adult forms. During June 1980, we (Fierstine and Welton, in press) collected a large fossil billfish discovered on the property of Pacific Farms, Inc., Tambac Island, near the barrio of Zaragoza, Bolinao Peninsula, Pangasinan Province, Northwest Cen tral Luzon, Philippines (Fig. 1). In addition, associated fossils were collected and local geological outcrops were mapped. The fieldwork continued throughout the month and all specimens were brought to the Natural History Museum of the Los Angeles County for curation, preparation, and distribution to specialists for study. The fieldwork was important because no fossil bony fish had ever been reported from the Philippines (Hashimoto, 1969), fossil billfishes have never been described from Asia (Fierstine and Applegate, 1974), a living species of billfish has never been positively identified in the fossil record (Fierstine, 1978), and no collection of marine macrofossils has ever been made under strict stratigraphic control in the Bolinao area, if not in the entire Philippines. -
Status of Billfish Resources and the Billfish Fisheries in the Western
SLC/FIAF/C1127 (En) FAO Fisheries and Aquaculture Circular ISSN 2070-6065 STATUS OF BILLFISH RESOURCES AND BILLFISH FISHERIES IN THE WESTERN CENTRAL ATLANTIC Source: ICCAT (2015) FAO Fisheries and Aquaculture Circular No. 1127 SLC/FIAF/C1127 (En) STATUS OF BILLFISH RESOURCES AND BILLFISH FISHERIES IN THE WESTERN CENTRAL ATLANTIC by Nelson Ehrhardt and Mark Fitchett School of Marine and Atmospheric Science, University of Miami Miami, United States of America FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Bridgetown, Barbados, 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. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. ISBN 978-92-5-109436-5 © FAO, 2016 FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate DFNQRZOHGJHPHQWRI)$2DVWKHVRXUFHDQGFRS\ULJKWKROGHULVJLYHQDQGWKDW)$2¶VHQGRUVHPHQWRI XVHUV¶YLHZVSURGXFWVRUVHUYLFHVLVQRWLPSOLHGLQDQ\ZD\ All requests for translation and adaptation rights, and for resale and other commercial use rights should be made via www.fao.org/contact-us/licence-request or addressed to [email protected]. -
Biodiversity and the Future of the Gulf of Maine Area Lewis Incze and Peter Lawton Genes
Biodiversity and the Future of the Gulf of Maine Area Lewis Incze and Peter Lawton Genes Biodiversity is the diversity of life at all levels of organization, from genes to species, communities and ecosystems. Species Nearshore Offshore Bank Basin Slope GoMA: Ecosystem Field Project Habitats and Seamount Communities Abyssal Plain From microbes to whales, and from fundamental biodiversity to EBM GoMA Areas of Work: Species in the Gulf of Maine Area Ecology: past and present Technology Synthesizing Knowledge Linkages to EBM Outreach Today’s Agenda: 08:45-09:45 Presentation: The Global Census and GoMA: What did we do? What did we learn? 09:45-10:00 Q&A 10:00-10:20 BREAK 10:20-11:00 Presentation: Pathways to EBM 11:00-11:45 Discussion Programs of the Census of Marine Life ArCoD Arctic CMarZ Zooplankton CAML Antarctic Creefs Coral Reefs CenSeam Seamounts GoMA Gulf of Maine Area CheSS Chemosynthetic Systems ICOMM Microbes COMARGE Continental margins MAR-ECO Mid-Ocean Ridges CeDAMAR Abyssal Plains NaGISA Intertidal/Shallow Subtidal CenSeam Seamounts TOPP Top Predators HMAP History of Marine Animal Populations FMAP Future of “ “ “ OBIS Ocean Biogeographic Information System Collaborators/Affiliated programs Great Barrier Reef Gulf of Mexico BarCode of Life Encyclopedia of Life Oceans film 10 years (2000-2010) 80 countries, 2700 scientists 17 projects, 14 field projects + OBIS, HMAP Xxx cruises, xxxx days at sea, and FMAP ~ $77m leveraged ~ $767 m --need to 5 affiliated projects (field and technology) check 9 national and regional committees >2,500 scientific papers (many covers) books special journal volumes ~1,200 new species identified >1,500 species in waiting Collection in PLoS-ONE, 2010, incl. -
Red Sea Large Marine Ecosystem (Lme
III-6 Red Sea: LME #33 S. Heileman and N. Mistafa The Red Sea LME is bordered by Djibouti, Egypt, Eritrea, Israel, Jordan, Saudi Arabia, Sudan and Yemen. It has a surface area of 458,620 km2, of which 2.33% is protected and includes 3.8% of the world’s coral reefs (Sea Around Us 2007). It is characterised by dense, salty water formed by net evaporation with rates up to 1.4 - 2.0 m yr-1 (Hastenrath & Lamb 1979) and deep convection in the northern sector resulting in the formation of a deep water mass flowing out into the Gulf of Aden underneath a layer of less saline inflowing water (Morcos 1970). A dominant phenomenon affecting the oceanography and meteorology of the region is the Arabian monsoon. In winter, northeast monsoon winds extend well into the Gulf of Aden and the southern Red Sea, causing a seasonal reversal in the winds over this entire region (Patzert 1974). The seasonal monsoon reversal and the local coastal configuration combine in summer to force a radically different circulation pattern composed of a thin surface outflow, an intermediate inflowing layer of Gulf of Aden thermocline water and a vastly reduced (often extinguished) outflowing deep layer (Patzert 1974). Within the basin itself, the general surface circulation is cyclonic (Longhurst 1998). High evaporation and low precipitation maintain the Red Sea LME as one of the most saline water masses of the world oceans, with a mean surface salinity of 42.5 ppt and a mean temperature of 30° C during the summer (Sofianos et al. -
Fisheries in Large Marine Ecosystems: Descriptions and Diagnoses
Fisheries in Large Marine Ecosystems: Descriptions and Diagnoses D. Pauly, J. Alder, S. Booth, W.W.L. Cheung, V. Christensen, C. Close, U.R. Sumaila, W. Swartz, A. Tavakolie, R. Watson, L. Wood and D. Zeller Abstract We present a rationale for the description and diagnosis of fisheries at the level of Large Marine Ecosystems (LMEs), which is relatively new, and encompasses a series of concepts and indicators different from those typically used to describe fisheries at the stock level. We then document how catch data, which are usually available on a smaller scale, are mapped by the Sea Around Us Project (see www.seaaroundus.org) on a worldwide grid of half-degree lat.-long. cells. The time series of catches thus obtained for over 180,000 half-degree cells can be regrouped on any larger scale, here that of LMEs. This yields catch time series by species (groups) and LME, which began in 1950 when the FAO started collecting global fisheries statistics, and ends in 2004 with the last update of these datasets. The catch data by species, multiplied by ex-vessel price data and then summed, yield the value of the fishery for each LME, here presented as time series by higher (i.e., commercial) groups. Also, these catch data can be used to evaluate the primary production required (PPR) to sustain fisheries catches. PPR, when related to observed primary production, provides another index for assessing the impact of the countries fishing in LMEs. The mean trophic level of species caught by fisheries (or ‘Marine Trophic Index’) is also used, in conjunction with a related indicator, the Fishing-in-Balance Index (FiB), to assess changes in the species composition of the fisheries in LMEs. -
IATTC-94-01 the Tuna Fishery, Stocks, and Ecosystem in the Eastern
INTER-AMERICAN TROPICAL TUNA COMMISSION 94TH MEETING Bilbao, Spain 22-26 July 2019 DOCUMENT IATTC-94-01 REPORT ON THE TUNA FISHERY, STOCKS, AND ECOSYSTEM IN THE EASTERN PACIFIC OCEAN IN 2018 A. The fishery for tunas and billfishes in the eastern Pacific Ocean ....................................................... 3 B. Yellowfin tuna ................................................................................................................................... 50 C. Skipjack tuna ..................................................................................................................................... 58 D. Bigeye tuna ........................................................................................................................................ 64 E. Pacific bluefin tuna ............................................................................................................................ 72 F. Albacore tuna .................................................................................................................................... 76 G. Swordfish ........................................................................................................................................... 82 H. Blue marlin ........................................................................................................................................ 85 I. Striped marlin .................................................................................................................................... 86 J. Sailfish -
Resolving Geographic Expansion in the Marine Trophic Index
Vol. 512: 185–199, 2014 MARINE ECOLOGY PROGRESS SERIES Published October 9 doi: 10.3354/meps10949 Mar Ecol Prog Ser Contribution to the Theme Section ‘Trophodynamics in marine ecology’ FREEREE ACCESSCCESS Region-based MTI: resolving geographic expansion in the Marine Trophic Index K. Kleisner1,3,*, H. Mansour2,3, D. Pauly1 1Sea Around Us Project, Fisheries Centre, University of British Columbia, 2202 Main Mall, Vancouver, BC V6T 1Z4, Canada 2Earth and Ocean Sciences, University of British Columbia, 2207 Main Mall, Vancouver, BC V6T 1Z4, Canada 3Present address: NOAA, Northeast Fisheries Science Center, 166 Water St., Woods Hole, MA 02543, USA ABSTRACT: The Marine Trophic Index (MTI), which tracks the mean trophic level of fishery catches from an ecosystem, generally, but not always, tracks changes in mean trophic level of an ensemble of exploited species in response to fishing pressure. However, one of the disadvantages of this indicator is that declines in trophic level can be masked by geographic expansion and/or the development of offshore fisheries, where higher trophic levels of newly accessed resources can overwhelm fishing-down effects closer inshore. Here, we show that the MTI should not be used without accounting for changes in the spatial and bathymetric reach of the fishing fleet, and we develop a new index that accounts for the potential geographic expansion of fisheries, called the region-based MTI (RMTI). To calculate the RMTI, the potential catch that can be obtained given the observed trophic structure of the actual catch is used to assess the fisheries in an initial (usu- ally coastal) region. When the actual catch exceeds the potential catch, this is indicative of a new fishing region being exploited.