Commission on the Limits of the Continental Shelf
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IOTC-2006-WPTT-10 Historical Database on Soviet Tuna Longline
IOTC-2006-WPTT-10 Historical database on Soviet tuna longline tuna research in the Indian and Atlantic oceans (first results of YugNIRO-NMFS data rescue project)① Evgeny Romanov1, 2, Gary Sakagawa3, Francis Marsac1, Natal’ya Romanova4 (1) IRD, UR 109 THETIS, Centre de Recherche Halieutique Mediterraneenne et Tropicale Avenue Jean Monnet – BP 171, 34203 Sete Cedex, France (corresponding author) (2) Southern Scientific Research Institute of Marine Fisheries & Oceanography (YugNIRO), Kerch, Crimea, Ukraine (3) Southwest Fisheries Science Center, 8640 La Jolla Shores Drive, La Jolla CA 92037 (4) 2, rue des Chasseurs, 34070, Montpellier, France Abstract YugNIRO (formerly AzCherNIRO, till 1988), Kerch, Ukraine started tuna research in the Indian Ocean in early 1960-ies and such studies continued till early 1990-ies. For research purposes medium-sized fishing trawlers converted for pelagic longlining were used. Recent data inventory accounted about 130 research, searching, and fishing pelagic longline cruises for 1961- 1989 targeted tunas (generally Thunnus), billfishes (Makaira, Tetrapturus, Xiphias gladius), pelagic sharks (Carcharhinus, Isurus, Alopias, Prionace glauca, Galeocerdo cuvier). Other pelagic species were recorded as bycatch. More than 5200 longline sets with about 2.5 millions nominal hooks were shot. For every research cruise the following data were colleted on set by set basis: number of hooks, hooks distribution by depth, total catch, and catch by species. Almost all the fish caught were measured, weighed, and analyzed. Estimated catch depth of every fish was recorded. Environmental data and MBT station data generally available. Due to lack of computer equipment and limited funding throughout years of data sampling this valuable data were stored on paper as logbooks of longline catches and biological analysis. -
Ocean Drilling Program Initial Reports Volume
Backman, J., Duncan, R. A., et al., 1988 Proceedings of the Ocean Drilling Program, Initial Reports, Vol. 115 1. INTRODUCTION1 Shipboard Scientific Party2 Leg 115 is the first of a nine-leg program of exploration of these volcanic islands and submarine (presumed volcanic) ridges the Indian Ocean. Previous drilling by the Deep Sea Drilling is consistent with northward motion of the Indian plate, fol- Program (DSDP), Legs 22 through 29 (1972-73), resulted in the lowed by northeastward motion of the African plate, over a first detailed information about the geologic and Oceanographic fixed melting anomaly at the location of Reunion during Ter- history of this major region of the oceans. Compared with the tiary time (Morgan, 1981; Duncan, 1981). In addition, this vol- Atlantic and Pacific Ocean Basins, however, the Indian Ocean is canic trail is parallel with the Ninetyeast Ridge, another subma- still relatively unexplored. During this multifaceted investiga- rine lineament linked to hotspot activity (now centered near the tion, we hoped to examine many fundamental questions. The Kerguelen Islands, Antarctic plate), and the two may record the scientific objectives of this leg fell into two main subject areas: northward motion of India during the opening of the Indian hotspot volcanism and paleoceanography. Ocean. Until Leg 115, however, the only accessible sampling loca- HOTSPOTS AND PLATE TECTONICS tions along the proposed Reunion hotspot track were the young An extraordinary feature of the Indian Ocean is the large volcanic islands at the southern end and the Deccan flood ba- number of elevated plateaus and ridges scattered throughout the salts at the northern end. -
The Indian Ocean 106 Worldwide Review of Bottom Fisheries in the High Seas
THE INDIAN OCEAN 106 Worldwide review of bottom fisheries in the high seas 30°E 40°E 50°E 60°E 70°E 80°E 90°E 100°E 110°E 120°E P h A a il i p A r a b i a n n f f e p 57.1 d h i 51.3 n S e a a S t e y o ngal m T G ha u u S °N a l e °N Ba Be f i a n n l a u a o o 10 f l 10 n n a S d S u e S e a i S 57.7 h C 51.5 0° 0° M i d - I n d i 51.a n R 4i d g e J a v a Banda 57.2 S 57.2 e a Sea Mascarene °S Plateau °S 10 Saya De T i m o r 10 e u Malha Bank q Malha Bank S e a i l MozambiqueMo Ridge b e m 57.5.1 zambique Ridge a n n z a n o h 51.6 a C 51.6 °S e °S M c 20 O 20 51.7 57.3 Ninetyeast Ridge Ninetyeast Ridge n °S Madagascar a °S 51.8 Broken Ridge 30 Ridge i 30 d 57.5.2 °S n °S 40 Southwest Indian Ridge 40 I Southeast57.4 Indian Ridge °S °S 50 50 30°E 40°E 50°E 60°E 70°E 80°E 90°E 100°E 110°E 120°E 200 nautical miles arcs Higigh-seas deep sea fishing grounds SIOFA Competence Area Map Projection: Cylindrical equal area FAO Fishing Areas FAO, 2008 MAP 1 Main high seas deep-sea fishing grounds in the Indian Ocean and area of competence of the Southern Indian Ocean Fisheries Agreement (SIOFA) 107 Indian Ocean FAO Statistical Areas 51 and 57 GEOGRAPHIC DESCRIPTION OF THE REGION The Indian Ocean is the third largest of the earth’s five oceans. -
Briefing on Human Trafficking in the Intl Fishing Industry
December 19, 2016 BRIEFING ON GREENPEACE’S REPORT ‘TURN THE TIDE’ AND CENTER FOR AMERICAN PROGRESS’ REPORT ‘SEAFOOD SLAVERY: HUMAN TRAFFICKING IN THE INTERNATIONAL FISHING INDUSTRY’ TURN THE TIDE Summary In December 2016, Greenpeace released ‘Turn the Tide’, a year-long investigation into human rights abuses and illegal fishing in Thailand’s distant water fishing fleet. In the report, Greenpeace alleges that recent crackdowns on illegal fishing in Indonesia and Papua New Guinea forced offending vessels into the Saya de Malha bank area, a large, shallow, biodiverse tropical ecosystem. Due to inadequate enforcement in Saya de Malha – regulated by Mauritius and the Seychelles – Greenpeace claims that illegal fishing and human rights abuses have flourished. Greenpeace monitored the activity of large refrigerated fishing vessels (also known as “reefers”) in Saya de Malha from 2015 to 2016. Greenpeace alleges that there, beyond enforcement, instances of illegal fishing, human rights, and labor abuses occur on vessels. Abuses documented by Greenpeace include 22 hour workdays, a lack of employment contracts, lying about the cost of documents such as passports, and other violations. Unfortunately, Greenpeace also found that – once the vessel returns to port in Thailand – inspections by the Royal Thai Navy may not adequately identify potential trafficking victims due to coercive tactics by senior crew on these vessels. In addition to the aforementioned abuses, Greenpeace found other health risks present for fishers. The vessels monitored by Greenpeace are able to stay out at sea for months or years at a time in part due to transshipment, a practice in which a reefer supplies the vessel with food, fuel, and other supplies. -
The Saya De Malha Banks March Introduction the Indian Ocean Is the Third Largest of the Earth’S Five Oceans
Madagascar Marine Programme FACTSHEET The Saya de Malha Banks MARCH Introduction The Indian Ocean is the third largest of the earth’s five oceans. The topography of the sea bed on the high 2011 seas of the Indian Ocean is characterized by large areas of abyssal plane with extensive ridge systems and numerous seamounts, Banks, plateaus and other underwater features. Among the deep-sea ridge systems, the Mascarene Ridge includes the Saya de Malha Banks, which in some areas is less than 20 metres deep and is mostly in international waters between Mauritius and Seychelles. Named by Portuguese sailors more than 500 years ago for the carpets of seagrass that extend across the Banks, the Saya de Malha Banks in the Western Indian Ocean are home to the least explored and what is believed to be the largest seagrass meadow in the world (Hilbertz et al. 2002). Site Description The Mascarene Plateau, including the Saya de Malha Banks is consid- ered to be a remnant of the ancient supercontinent Gondwana, going back to the continental break-up some 120 million years ago and sub- sequent separation and rifting of the African and Indian continental plates. The seafloor of the area is geologically complex and character- ized by a series of plateaus, Banks, shoals and islands, surmounted in the north by the granitic islands of the Republic of Seychelles and in the south by the Mascarene Islands including Mauritius. The Saya de Malha Bankss are located between 8°30 - 12° S and 59°30 - 62.30° E in the western Indian Ocean along the submerged, crescent-shaped Mascarene Ridge that runs between the Republic of Seychelles to the north and the Republic of Mauritius to the south. -
Historical Biogeography of the Late Cretaceous Vertebrates of India: Comparison of Geophysical and Paleontological Data
Khosla, A. and Lucas, S.G., eds., 2016, Cretaceous Period: Biotic Diversity and Biogeography. New Mexico Museum of Natural History and Science Bulletin 71. 317 HISTORICAL BIOGEOGRAPHY OF THE LATE CRETACEOUS VERTEBRATES OF INDIA: COMPARISON OF GEOPHYSICAL AND PALEONTOLOGICAL DATA OMKAR VERMA1, ASHU KHOSLA2, FRANCISCO J. GOIN3 AND JASDEEP KAUR2 1Geology Discipline Group, School of Sciences, Indira Gandhi National Open University, New Delhi – 110 068, India, e-mail: omkarverma@ ignou.ac.in; 2Department of Geology, Centre for Advanced Studies, Panjab University, Sector-14, Chandigarh – 160014, India, e-mail: [email protected], e-mail: [email protected]; 3Consejo Nacional de Investigaciones Científicas y Técnicas and División Paleontología Vertebrados, Museo de Ciencias Naturales de La Plata, B1900FWA La Plata, Argentina, e-mail: [email protected] Abstract—The Cretaceous was a special time for the Indian plate as it was separated from Gondwana landmasses and started its northward journey across the Tethys Sea towards the Equator. The northward movement of this plate implied shifting latitudes and climate belts, until it finally collided with Asia during the early Cenozoic. Geophysical data and plate tectonic models show that after splitting from Gondwana, the Indian plate remained as an isolated continent for more than 45 Ma during the Cretaceous; thus, it predicts a remarkable biotic endemism for the continent. Paleontological data on the Cretaceous vertebrates of India is best known for Maastrichtian time; in turn, the pre-Maastrichtian record is very poor—it contains very few fossils of fishes and marine reptiles. The Maastrichtian fossil record comprises vertebrates of Gondwana and Laurasian affinities and some endemic, ancient lineages as well. -
Fisheries Research
1. Fisheries Research 1.1 Coastal (artisanal) fishery The monitoring of the artisanal fishery for the island of Mauritius was pursued and data on catch, effort, fish species and gear type were collected. Out of the 61 fish landing stations, around 25 fish landing stations were randomly selected on a monthly basis for data collection. 1.1.1 Catch, effort and catch per fisherman day The estimated total production was 950 tonnes of fresh fish comprising 579 tonnes from the lagoon and 371 tonnes from off-lagoon areas. The catch from the lagoon was slightly higher compared to last year whereas that of the off-lagoon showed a slight decrease and the overall mean catch per fisherman-day (CPFD) increased from 4.1 to 4.4 kg with a corresponding decrease in fisherman days. Table 1.1, Figure 1.1 and 1.2 show the catch, number of fisherman days and CPFD. Table 1.1: Catch, fisherman days and CPFD Year Catch (t) Fisherman days CPFD (kg) L OL Total L OL Total L OL M 2002 704 598 1 302 192 116 108 708 300 824 3.7 5.5 4.3 2003 704 462 1 166 189 988 83 362 273 350 3.7 5.5 4.3 2004 699 344 1 043 195 087 68 516 263 603 3.6 5.0 4.2 2005 545 402 947 153 771 77 429 231 200 3.5 5.2 4.1 2006 579 371 950 145 089 68 961 214 050 4.0 5.4 4.4 L=lagoon, OL= off-lagoon, M= mean, CPFD= catch per fisherman day 350 1400 300 1200 250 1000 200 800 150 600 Catch (t) 100 400 50 200 Fisherman days ('000) 0 0 2002 2003 2004 2005 2006 Year Fisherman days Catch (t) Figure 1.1: Fisherman days and total catch 6 5 ) 4 3 CPFD (kg CPFD 2 1 0 2002 2003 2004 2005 2006 Year L OL M Figure 1.2: Catch per fisherman day 1.1.2 Monthly landings The monthly production of fresh fish in the lagoon and off-lagoon, value of catch, effort and CPFD are presented in table 1.2. -
Detailed Structure and Plate Reconstructions of the Central Indian Ocean Between 83.0 and 42.5 Ma (Chrons 34 and 20) V
Detailed Structure and Plate Reconstructions of the Central Indian Ocean Between 83.0 and 42.5 Ma (Chrons 34 and 20) V. Yatheesh, J. Dyment, G. Bhattacharya, J. Royer, K. Kamesh Raju, T. Ramprasad, A. Chaubey, P. Patriat, K. Srinivas, Y. Choi To cite this version: V. Yatheesh, J. Dyment, G. Bhattacharya, J. Royer, K. Kamesh Raju, et al.. Detailed Structure and Plate Reconstructions of the Central Indian Ocean Between 83.0 and 42.5 Ma (Chrons 34 and 20). Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2019, 124 (5), pp.4305-4322. 10.1029/2018JB016812. hal-02390146 HAL Id: hal-02390146 https://hal.archives-ouvertes.fr/hal-02390146 Submitted on 8 Dec 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. RESEARCH ARTICLE Detailed Structure and Plate Reconstructions of the 10.1029/2018JB016812 Central Indian Ocean Between 83.0 and 42.5 Ma Key Points: • We mapped high‐resolution (Chrons 34 and 20) magnetic isochrons in the Central V. Yatheesh1 , J. Dyment2, G. C. Bhattacharya1, J. Y. Royer3, K. A. Kamesh Raju1, T. Ramprasad1, Indian Ocean between 83.0 and 1 2 1 2 42.5 Ma A. -
The Geochemistry and Petrology of the Rodrigues Ridge (Western Indian Ocean)
The Geochemistry and Petrology of the Rodrigues Ridge (Western Indian Ocean). By Susan H. Mellor BSc. MSc. F.G.S. A thesis submitted in partial fulfilment of the requirements of the University of Greenwich for a Doctorate in Philosophy December 1998 \ Gravity Anomaly Map of the West Central Indian Ocean This false colour map covers 56° 00' E - 74° 00' E and 6° 00' S - 24° 00' S. False colour scale (red) +90 - -90 mgal (purple), colour bands are 15 mgal wide. Green - yellow boundary = 0 mgal. The map clearly shows the fracture zones of the Central Indian Ridge (CIR), the Mascarene Plateau (MP), Seychelles Bank (SB) and the Rodrigues Ridge(RR). Source: Scharroo R., No Date. Gravity Anomaly Atlas of the Indian Ocean [on line] Netherlands: DEOS. Available from: http://dutlru8.1r.tudelft.nl/img/indian.map?232,205.p.l5. [Accessed 21 March 1997]. The Geochemistry, Petrology and Petrogenesis of the Rodrigues Ridge (Western Indian Ocean). by Susan H. Mellor BSc. MSc. F.G.S. Abstract The Rodrigues Ridge is a linear east-west trending volcanic ridge, located between 18°S and 20°S in the western Indian Ocean. The trend of the Rodrigues Ridge is contrary to the ocean floor fabric of the underlying crust, which formed on the Central Indian Ridge (CIR) between ca. 48 My and 10 My. Dating of dredged basalts from the Rodrigues Ridge showed them to be 8-10 My, with no systematic variations with longitude. All samples recovered from the Rodrigues Ridge were olivine and plagioclase phyric with traces of chrome spinel. -
Ridges and Hotspots Around the Mascarene Islands
Jointly organized by InterRidge - international cooperation in ridge-crest studies http://www.interridge.org/ CNRS - Centre National de la Recherche Scientifique, France http://www.insu.cnrs.fr/ MOI - Mauritius Oceanography Institute, Mauritius http://moi.gov.mu/ International Conference Ridges and Hotspots around the Mascarene Islands 3-7 September 2012, Hotel Tamassa (LUX Island Resorts, Mauritius Organizing Committee: Dass Bissessur (Mauritius Oceanography Institute, Mauritius), Jérôme Dyment (CNRS and Institut de Physique du Globe de Paris, France) Debbie Milton (InterRidge) Scientific Committee: Patrick Bachélery (Université de La Réunion, France) Mitrasen Bhikajee (Mauritius Oceanography Institute, Mauritius) John Chen (Peking University, Beijing, China) Christophe Hémond (Université de Brest, France) K.A. Kamesh Raju (National Institute of Oceanography, Goa, India) Marcia Maia (CNRS & Université de Brest, France) Bramley Murton (National Oceanography Centre, Southampton, UK) Kyoko Okino (University of Tokyo, Japan) Kensaku Tamaki† (University of Tokyo, Japan) William White (Cornell University, USA) † deceased 1 This meeting is dedicated to the memory of our colleague and friend Kensaku Tamaki. Kensaku Tamaki in his office, Tokyo, February 2005. Kensaku led several cruises in the Western Indian Ocean, and he participated (himself or through Japanese colleagues, engineers, students, and/or even instruments) in many others. His interest in this area started in 1993 with the exploration of the Rodrigues Triple Junction, where he took advantage of a new generation of instruments to build on previous American, French, British and German efforts on this peculiar plate tectonic feature. He later focused on the ultra-slow Southwest Indian Ridge, an effort that culminated with cruise FUJI (France- UK-Japan-InterRidge) in 1997. -
Managing Marine Protected Areas: a Toolkit for the Western Indian Ocean
ManagingManaging MarineMarine ProtectedProtected AreasAreas A TOOLKIT for the Western Indian Ocean 2004 PUBLISHED BY IUCN Eastern African Regional Programme in collaboration with Western Indian Ocean Marine Science Association (WIOMSA) United Nations Environment Programme (UNEP) World Wide Fund for Nature (WWF) Coastal Zone Management Centre (CZMC) Coastal Zone Management This Centre, Netherlands publication has been made possible by funding from the Norwegian Agency for Development Cooperation (NORAD) The designation of geographical entities in this toolkit, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN, WIOMSA, UNEP, WWF, CZMC and NORAD concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN, WIOMSA, UNEP, WWF, CZMC and NORAD. This publication has been made possible by funding from the Norwegian Agency for Development Cooperation (NORAD). Published by: IUCN Eastern African Regional Programme, Nairobi, Kenya, in collaboration with the Western Indian Ocean Marine Science Association (WIOMSA), United Nations Environment Programme (UNEP), World Wide Fund for Nature (WWF), and the Coastal Zone Management Centre (CZMC), Netherlands. Coastal Zone Management Centre, Netherlands Copyright: © 2004 International Union for Conservation of Nature and Natural Resources. This publication may be reproduced in whole or part and in any form for education or non-profit uses, without special permission from the copyright holder, provided acknowledgement of the source is made. IUCN would appreciate receiving a copy of any publication which uses this publication as a source. -
New Heat-Flow Observations in a Hotspot Swell: the Reunion-Mascarene Plateau
New Heat-Flow Observations in a Hotspot Swell: the Reunion-Mascarene Plateau P. Chiozzi1, M. Verdoya1, C. Pasqua1,2 1University of Genoa, Depart. of Earth, Environment and Life Sciences, Genoa, Italy 2ELC – Electroconsult, Milan, Italy • Terrestrial heat-flow data, generally derived from sea-bottom measurements, can be important to validate theories on the origin of hotspot swells (e.g. Crough, 1978; Courtney and White, 1986; Watson and McKenzie, 1991; Sleep, 1994). • Strikingly, hotspots are generally characterised by the lack of high heat-flow values. This is often argument against reheating of the oceanic lithosphere as a mechanismforming swells (e.g. Von Herzen et al., 1989). • However, it was recently argued that the thermal signature of hotspots can be widely obscured by fluid circulation (e.g. Harris and McNutt, 2007). • Other analyses conclude that hydrothermal flow may redistribute heat only near the swell axes and that the small heat-flow anomalies indicate that the mechanisms producing hotspots do not significantly perturb the thermal state of the lithosphere (e.g. Stein and Von Herzen, 2007). • Closely spaced heat-flow determinations (1-2 km or less) can be useful to discriminate environments in which heat is transferred by conduction or advection • The heat-flow data analysis also may benefit from seismic profiles providing details of sediment interfaces; the occurrence of fluid flow can be better understood • So far, these requirements are satisfied in only for two hot spot swells: the Hawaii-Emperor chain and the Reunion-Mascarene