Shrimp Fishing in Mexico
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Final Master Document Draft EFH EIS Gulf
Final Environmental Impact Statement for the Generic Essential Fish Habitat Amendment to the following fishery management plans of the Gulf of Mexico (GOM): SHRIMP FISHERY OF THE GULF OF MEXICO RED DRUM FISHERY OF THE GULF OF MEXICO REEF FISH FISHERY OF THE GULF OF MEXICO STONE CRAB FISHERY OF THE GULF OF MEXICO CORAL AND CORAL REEF FISHERY OF THE GULF OF MEXICO SPINY LOBSTER FISHERY OF THE GULF OF MEXICO AND SOUTH ATLANTIC COASTAL MIGRATORY PELAGIC RESOURCES OF THE GULF OF MEXICO AND SOUTH ATLANTIC VOLUME 1: TEXT March 2004 Gulf of Mexico Fishery Management Council The Commons at Rivergate 3018 U.S. Highway 301 North, Suite 1000 Tampa, Florida 33619-2266 Tel: 813-228-2815 (toll-free 888-833-1844), FAX: 813-225-7015 E-mail: [email protected] This is a publication of the Gulf of Mexico Fishery Management Council pursuant to National Oceanic and Atmospheric Administration Award No. NA17FC1052. COVER SHEET Environmental Impact Statement for the Generic Essential Fish Habitat Amendment to the fishery management plans of the Gulf of Mexico Draft () Final (X) Type of Action: Administrative (x) Legislative ( ) Area of Potential Impact: Areas of tidally influenced waters and substrates of the Gulf of Mexico and its estuaries in Texas, Louisiana, Mississippi, Alabama, and Florida extending out to the limit of the U.S. Exclusive Economic Zone (EEZ) Agency: HQ Contact: Region Contacts: U.S. Department of Commerce Steve Kokkinakis David Dale NOAA Fisheries NOAA-Strategic Planning (N/SP) (727)570-5317 Southeast Region Building SSMC3, Rm. 15532 David Keys 9721 Executive Center Dr. -
Translation Series No.1375
FISHERIES RESEARCH BOARD OF CANADA Translation Series No. 1375 Bioebenoses and biomass of benthos of the Newfoundland-Labrador region. By Ki1N. Nesis Original title: Biotsenozy i biomassa bentosa N'yufaund- • .lendskogo-Labradorskogo raiona.. From: Trudy Vsesoyuznogo Nauchno-Issledovatel'skogo •Instituta Morskogo Rybnogo Khozyaistva Okeanografii (eNIRO), 57: 453-489, 1965. Translated by the Translation Bureau(AM) Foreign Languages Division Department of the Secretary of State of Canada Fisheries Research Board of Canada • Biological Station , st. John's, Nfld 1970 75 pages typescript 'r OEPARTMENT OF THE SECRETARY OF STATE SECRÉTARIAT D'ÉTAT TRANSLATION BUREAU BUREAU DES TRADUCTIONS FOREIGN LANGUAGES DIVISION DES LANGUES DIVISION ° CANADA ÉTRANGÈRES TRANSLATED FROM - TR,ADUCTION DE INTO - EN Russian English 'AUTHOR - AUTEUR Nesis K.N. TITLE IN ENGLISH - TITRE ; ANGLAIS Biocoenoses and biomas of benthos of the Newfolindland-Labradoriregion Title . in foreign_iangnage---(tranalitarate_foreisn -ottantatere) Biotsenozy i biomassa bentosa N i yufaundlendSkogo-Labradorskogoraiona. , .ReF5RENCE IN FOREIGN ANGUA2E (NAME OF BOOK OR PUBLICATION) IN FULL. TRANSLITERATE FOREIGN CFiA,IRACTERS. • REFERENCE' EN LANGUE ETRANGERE (NOM DU LIVRE OU PUBLICATION), AU COMPLET. TRANSCRIRE EN CARACTERES PHONETIQUEL •. Trudylesesoyuznogo nauchno-iàsledovaterskogo instituta morskogo — rybnogo khozyaistva i okeanogràfii - :REFEREN CE IN ENGLISH - RÉFÉRENCE EN ANGLAIS • Trudy of the 40.1-Union Scientific-Research Instituteof Marine . Fiseriés and Oceanography. PUBLISH ER ÉDITEUR PAGE,NUMBERS IN ORIGINAL DATE OF PUBLICATION NUMEROS DES PAGES DANS DATE DE PUBLICATION . L'ORIGINAL YE.tR ISSUE.NO . 36 VOLUME ANNEE NUMERO PLACE OF PUBLICATION NUMBER OF TYPED PAGES LIEU DE PUBLICATION NOMBRE DE PAG.ES DACTY LOGRAPHIEES 1965 5 7 REQUEr IN G• DEPA RTMENT Fisheries Research Board TRANSLATION BUREAU NO. -
Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
Marine Stewardship Council Pre-Assessment
10051 5th Street N., Suite 105 St. Petersburg, Florida 33702-2211 Tel: (727) 563-9070 Fax: (727) 563-0207 Em ail: MRAG.Americas@m ragam ericas.com President: Andrew A. Rosenberg, Ph.D. Pre-Assessment of the Louisiana Shrimp Fishery Prepared for Louisiana Department of Wildlife and Fisheries Prepared by MRAG Americas, Inc. Robert J. Trumble January 2016 Table of Contents 1. Introduction .................................................................................................................... 2 1.1. Aims/scope of pre-assessment ............................................................................ 2 1.2 Constraints to the pre-assessment of the fishery ................................................. 3 1.3. Unit(s) of Assessment ......................................................................................... 3 1.4 Total Allowable Catch (TAC) and Catch Data ...................................................... 3 2. Description of the fishery ................................................................................................ 4 2.1. Scope of the fishery in relation to the MSC programme ....................................... 4 2.2. Overview of the fishery ........................................................................................ 4 2.3. Principle One: Target species background .......................................................... 4 2.4. Principle Two: Ecosystem background ................................................................ 5 2.5. Principle Three: Management system background -
Latin American Biogems: the Baker River Snakes Through Chilean Patagonia from the Glacial Lakes of the Andes to Fjords on the Pacific Coast
Facts Foott, 2009, The Patagonian Foundation and iLCP and Foundation Patagonian The 2009, Foott, The Baker River snakes through Chilean Patagonia from the glacial lakes of the Andes to fjords on the Pacific coast. Latin American BioGems: Saving Special Wild Places and Wildlife NRDC’s BioGems Initiative protects endangered wild regions and species throughout the Americas. In Latin America, NRDC has worked to preserve BioGems unspoiled ecosystems and threatened wildlife from Mexico’s Baja Peninsula to Chile’s Patagonia, working in partnership with communities and organizations to eliminate threats and to find environmentally sustainable alternatives. For more information, please contact: Baja California, n Cabo Pulmo: Cabo Pulmo National Marine Amanda Maxwell Mexico Park is home to the healthiest and most [email protected] To the east of the important coral reef of the Baja Peninsula, (202) 289-2368 Baja Peninsula, the home to humpback whales, dolphins, whale Gulf of California, sharks, Pacific manta rays and five species of sea Carolina Herrera which Jacques turtles, as well as more than 200 species of fish. [email protected] Cousteau called Hopkins Lee Ralph Now a Spanish real estate company is proposing (202) 289-2381 Humpback whale “the aquarium of a massive 9,500 acre resort complex next to the world,” provides shelter for hundreds of species the park. Since October 2010, NRDC has of fish, sea turtles and marine mammals. NRDC been working with a local coalition to stop this is working with Mexican partners to protect Baja’s industrial tourism development and to promote fragile marine life from a variety sustainable tourism alternatives. -
Why Did the Southern Gulf of California Rupture So Rapidly?—Oblique Divergence Across Hot, Weak Lithosphere Along a Tectonically Active Margin
Why did the Southern Gulf of California rupture so rapidly?—Oblique divergence across hot, weak lithosphere along a tectonically active margin breakup, is mainly dependent on the thermal structure, crust- Paul J. Umhoefer, Geology Program, School of Earth Sciences & Environmental Sustainability, Northern Arizona University, al thickness, and crustal strength of the lithosphere when Flagstaff, Arizona 86011, USA; [email protected] rifting begins (e.g., Buck, 2007), as well as forces at the base of the lithosphere and far-field plate interactions (Ziegler and Cloetingh, 2004). ABSTRACT Continental rupture at its two extremes creates either large Rifts in the interior of continents that evolve to form large ocean basins or small and narrow marginal seas depending oceans typically last for 30 to 80 m.y. and longer before com- largely on the tectonic setting of the rift. Rupture of a conti- plete rupture of the continent and onset of sea-floor spreading. nent that creates large oceans most commonly initiates as A distinct style of rifts form along the active tectonic margins of rifts in old, cold continental lithosphere or within former continents, and these rifts more commonly form marginal seas large collisional belts in the interior of large continents, part and terranes or continental blocks or slivers that are ruptured of the process known as the Wilson Cycle (Wilson, 1966). away from their home continent. The Gulf of California and the Rupture to create narrow marginal seas commonly occurs in Baja California microplate make up one of the best examples active continental margins and results in the formation of of the latter setting and processes. -
Pandalus Platyceros Range: Spot Prawn Inhabit Alaska to San Diego
Fishery-at-a-Glance: Spot Prawn Scientific Name: Pandalus platyceros Range: Spot Prawn inhabit Alaska to San Diego, California, in depths from 150 to 1,600 feet (46 to 488 meters). The areas where they are of higher abundance in California waters occur off of the Farallon Islands, Monterey, the Channel Islands and most offshore banks. Habitat: Juvenile Spot Prawn reside in relatively hard-bottom kelp covered areas in shallow depths, and adults migrate into deep water of 60.0 to 200.0 meters (196.9 to 656.2 feet). Size (length and weight): The Spot Prawn is the largest prawn in the North Pacific reaching a total length of 25.3 to 30.0 centimeters (10.0 to 12.0 inches) and they can weigh up to 120 grams (0.26 pound). Life span: Spot Prawn have a maximum observed age estimated at more than 6 years, but there are considerable differences in age and growth of Spot Prawns depending on the research and the area. Reproduction: The Spot Prawn is a protandric hermaphrodite (born male and change to female by the end of the fourth year). Spawning occurs once a year, and Spot Prawn typically mate once as a male and once or twice as a female. At sexual maturity, the carapace length of males reaches 1.5 inches (33.0 millimeters) and females 1.75 inches (44.0 millimeters). Prey: Spot Prawn feed on other shrimp, plankton, small mollusks, worms, sponges, and fish carcasses, as well as being detritivores. Predators: Spot Prawn are preyed on by larger marine animals, such as Pacific Hake, octopuses, and seals, as well as humans. -
First Timer's Guide to Mexico 2018
LatitudeLatitude 38’s38’s FirstFirst Timer’sTimer’s GuideGuide MexicoMexicototo 20182018 Silver Anniversary Premier Partners - Mexico Tourism & Satellite Phone Store Sunday, November 18 4:00 p.m. - 7:00 p.m. Mexican Folk Dancing • Live Music • Food & Drinks FREE for fi rst fi fty! (2018 Baja Ha-Ha participants.) Door prizes and much more! Latitude 38's First Timer’s Guide to Mexico 25th Anniversary Baja Ha-Ha Produced by the Latitude 38 staff, who remind you to 'keep in touch’ during your travels. We encourage you to email us with reports — and photos! — about interesting places you visit, or letters about issues of interest to other cruisers. Email your contributions: For Baja Ha-HA [email protected] partipant information contact: For sponsorship information: Postal Mail: 417 South Hill St., Suite 646 [email protected] Los Angeles, CA 90013 Email: [email protected] Editorial & Sponsorship: 415-383-8202 Phone: 415-613-8200 www.latitude38.com www.baja-haha.com www.pacifi cpuddlejump.com www.socaltata.com www.deltadoodah.com — © Latitude 38 Media, LLC, 2018 — No part of this booklet may be reproduced without permission from Latitude 38 Media, LLC. First Timer's Guide to Mexico • 3 A WORLD OF ITS OWN Dear Baja Ha-Ha Sailors, We are very pleased to have this opportunity to support your adventure in Mexico with the 25th Annual Baja Ha-Ha Rally, and welcome you to the unique Mexico cruising lifestyle. Renowned as a haven for the world’s most discerning cruisers, Mexico’s harbors, marinas and attractions have garnered rave reviews from generations of cruisers and Baja Ha-Ha participants. -
Download Our Mexico & USA Brochure
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Physical Geography Research Project
Name Date Physical Geography Research Project Your small group will be assigned one of the following examples. Use the provided websites to conduct research and answer the questions for your assigned example. Example 1: The North Sea Humans have divided land into governed territories for centuries. But what happens when a body of water needs to be divided up because of a natural resource? That is what happened in the North Sea after oil was discovered in the 1960s. The countries that surround the North Sea include the United Kingdom, France, Belgium, the Netherlands, Germany, Denmark, and Norway. Research how the countries that border the North Sea have divided up the claim. If possible, find information on the United Nations Law of the Sea Treaty and exclusive economic zones (EEZ). 1. Do you think the way the North Sea was split was fair to all countries involved? Why or why not? ____________________________________________________________________________________ ____________________________________________________________________________________ ____________________________________________________________________________________ 2. How do you think dividing up a claim like this affects the relationships between the countries involved? Support your opinion with evidence. __________________________________________ ____________________________________________________________________________________ ____________________________________________________________________________________ 3. Are there other areas of Europe where natural resources -
6 North Sea 6.1 Ecosystem Overview 6.1.1 Ecosystem Components
6 North Sea 6.1 Ecosystem overview 6.1.1 Ecosystem components Seabed topography and substrates The topography of the North Sea can be broadly described as having a shallow (<50 m) southeastern part, which is sharply separated by the Dogger Bank from a much deeper (50–100 m) central part that runs north along the British coast. The central northern part of the shelf gradually slopes down to 200 m before reaching the shelf edge. Another main feature is the Norwegian Trench running east along the Norwegian coast into the Skagerrak with depths up to 500 m. Further to the east, the Norwegian Trench ends abruptly, and the Kattegat is of depths similar to the main part of the North Sea (Figure 6.1.1). The substrates are dominated by sands in the southern and coastal regions and fine muds in deeper and more central parts (Figure 6.1.2). Sands become generally coarser to the east and west, with patches of gravel and stones existing as well. In the shallow southern part, concentrations of boulders may be found locally, originating from transport by glaciers during the ice ages. This specific hard-bottom habitat has become scarcer, because boulders caught in beam trawls are often brought ashore. The area around, and to the west of the Orkney/Shetland archipelago is dominated by coarse sand and gravel. The deep areas of the Norwegian Trench are covered with extensive layers of fine muds, while some of the slopes have rocky bottoms. Several underwater canyons extend further towards the coasts of Norway and Sweden. -
Amphipod Cell Lineages
Development 129, 5789-5801 5789 © 2002 The Company of Biologists Ltd doi:10.1242/dev.00155 Cell lineage analysis of the amphipod crustacean Parhyale hawaiensis reveals an early restriction of cell fates Matthias Gerberding1,3, William E. Browne2 and Nipam H. Patel1,3,* 1Department of Organismal Biology and Anatomy, University of Chicago, Chicago, IL 60637, USA 2Department of Molecular Genetics and Cell Biology, University of Chicago, Chicago, IL 60637, USA 3Howard Hughes Medical Institute, University of Chicago, Chicago, IL 60637, USA *Author for correspondence (e-mail: [email protected]) Accepted 11 September 2002 SUMMARY In the amphipod crustacean, Parhyale hawaiensis, the endoderm and the fourth micromere generates the first few embryonic cleavages are total and generate a germline. These findings demonstrate for the first time a stereotypical arrangement of cells. In particular, at the total cleavage pattern in an arthropod which results in an eight-cell stage there are four macromeres and four invariant cell fate of the blastomeres, but notably, the cell micromeres, and each of these cells is uniquely identifiable. lineage pattern of Parhyale reported shows no clear We describe our studies of the cell fate pattern of these resemblance to those found in spiralians, nematodes or eight blastomeres, and find that the eight clones resulting deuterostomes. Finally, the techniques we have developed from these cells set up distinct cell lineages that differ in for the analysis of Parhyale development suggest that this terms of proliferation, migration and cell fate. Remarkably, arthropod may be particularly useful for future functional the cell fate of each blastomere is restricted to a single analyses of crustacean development.