Marine Conservation Planning in Practice: Lessons Learned from the Gulf of California
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Shrimp Fishing in Mexico
235 Shrimp fishing in Mexico Based on the work of D. Aguilar and J. Grande-Vidal AN OVERVIEW Mexico has coastlines of 8 475 km along the Pacific and 3 294 km along the Atlantic Oceans. Shrimp fishing in Mexico takes place in the Pacific, Gulf of Mexico and Caribbean, both by artisanal and industrial fleets. A large number of small fishing vessels use many types of gear to catch shrimp. The larger offshore shrimp vessels, numbering about 2 212, trawl using either two nets (Pacific side) or four nets (Atlantic). In 2003, shrimp production in Mexico of 123 905 tonnes came from three sources: 21.26 percent from artisanal fisheries, 28.41 percent from industrial fisheries and 50.33 percent from aquaculture activities. Shrimp is the most important fishery commodity produced in Mexico in terms of value, exports and employment. Catches of Mexican Pacific shrimp appear to have reached their maximum. There is general recognition that overcapacity is a problem in the various shrimp fleets. DEVELOPMENT AND STRUCTURE Although trawling for shrimp started in the late 1920s, shrimp has been captured in inshore areas since pre-Columbian times. Magallón-Barajas (1987) describes the lagoon shrimp fishery, developed in the pre-Hispanic era by natives of the southeastern Gulf of California, which used barriers built with mangrove sticks across the channels and mouths of estuaries and lagoons. The National Fisheries Institute (INP, 2000) and Magallón-Barajas (1987) reviewed the history of shrimp fishing on the Pacific coast of Mexico. It began in 1921 at Guaymas with two United States boats. -
Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
Inner Sound of Stroma, Pentland Firth (Scotland, UK)
3rd International Conference on Ocean Energy, 6 October, Bilbao An Operational Hydrodynamic Model of a key tidal-energy site: Inner Sound of Stroma, Pentland Firth (Scotland, UK) M.C. Easton 1, D.K. Woolf 1, and S. Pans 2 1 Environmental Research Institute North Highland College, UHI Millenium Institute Thurso, Caithness, KW14 7JD, Scotland Email: [email protected] 2 DHI Representative UK (Scotland) DHI Agern Allé 5, DK-2970 Hørsholm, Denmark E-mail: [email protected] Abstract mutual influence of tidal ranges and phases between North Atlantic to the West and the North Sea to the As a result of significant progress towards the East act to setup strong currents [2] where spring tides delivery of tidal-stream power the industry is commonly exceed 5 ms-1 [3-4]. moving swiftly towards the deployment of pre- Seeking to capitalise on these unique conditions and commercial arrays. Meanwhile important sites, accelerate the delivery of large-scale tidal-stream such as the Pentland Firth, are being made available energy, in March 2010 the organisation controlling the for development. It is now crucial that we consider seabed in the United Kingdom, the Crown Estate, how the installation of tidal-stream devices will awarded leases for up to 600 MW of installed tidal interact with their host environment. Surveying energy capacity within the Pentland Firth-Orkney and modelling of the marine system prior to region [5]. An additional 200 MW is expected to be development is a prerequisite to identifying any awarded later in 2010 [6]. This announcement of the significant changes associated with tidal energy first large-scale deployment of tidal energy devices deployment. -
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. -
The Gulf of Mexico Workshop on International Research, March 29–30, 2017, Houston, Texas
OCS Study BOEM 2019-045 Proceedings: The Gulf of Mexico Workshop on International Research, March 29–30, 2017, Houston, Texas U.S. Department of the Interior Bureau of Ocean Energy Management Gulf of Mexico OCS Region OCS Study BOEM 2019-045 Proceedings: The Gulf of Mexico Workshop on International Research, March 29–30, 2017, Houston, Texas Editors Larry McKinney, Mark Besonen, Kim Withers Prepared under BOEM Contract M16AC00026 by Harte Research Institute for Gulf of Mexico Studies Texas A&M University–Corpus Christi 6300 Ocean Drive Corpus Christi, TX 78412 Published by U.S. Department of the Interior New Orleans, LA Bureau of Ocean Energy Management July 2019 Gulf of Mexico OCS Region DISCLAIMER Study collaboration and funding were provided by the US Department of the Interior, Bureau of Ocean Energy Management (BOEM), Environmental Studies Program, Washington, DC, under Agreement Number M16AC00026. This report has been technically reviewed by BOEM, and it has been approved for publication. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the US Government, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. REPORT AVAILABILITY To download a PDF file of this report, go to the US Department of the Interior, Bureau of Ocean Energy Management website at https://www.boem.gov/Environmental-Studies-EnvData/, click on the link for the Environmental Studies Program Information System (ESPIS), and search on 2019-045. CITATION McKinney LD, Besonen M, Withers K (editors) (Harte Research Institute for Gulf of Mexico Studies, Corpus Christi, Texas). -
Sand Dunes Computer Animations and Paper Models by Tau Rho Alpha*, John P
Go Home U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Sand Dunes Computer animations and paper models By Tau Rho Alpha*, John P. Galloway*, and Scott W. Starratt* Open-file Report 98-131-A - This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this program has been used by the U.S. Geological Survey, no warranty, expressed or implied, is made by the USGS as to the accuracy and functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the USGS in connection therewith. * U.S. Geological Survey Menlo Park, CA 94025 Comments encouraged tralpha @ omega? .wr.usgs .gov [email protected] [email protected] (gobackward) <j (goforward) Description of Report This report illustrates, through computer animations and paper models, why sand dunes can develop different forms. By studying the animations and the paper models, students will better understand the evolution of sand dunes, Included in the paper and diskette versions of this report are templates for making a paper models, instructions for there assembly, and a discussion of development of different forms of sand dunes. In addition, the diskette version includes animations of how different sand dunes develop. Many people provided help and encouragement in the development of this HyperCard stack, particularly David M. Rubin, Maura Hogan and Sue Priest. -
Baja California Sur, Mexico)
Journal of Marine Science and Engineering Article Geomorphology of a Holocene Hurricane Deposit Eroded from Rhyolite Sea Cliffs on Ensenada Almeja (Baja California Sur, Mexico) Markes E. Johnson 1,* , Rigoberto Guardado-France 2, Erlend M. Johnson 3 and Jorge Ledesma-Vázquez 2 1 Geosciences Department, Williams College, Williamstown, MA 01267, USA 2 Facultad de Ciencias Marinas, Universidad Autónoma de Baja California, Ensenada 22800, Baja California, Mexico; [email protected] (R.G.-F.); [email protected] (J.L.-V.) 3 Anthropology Department, Tulane University, New Orleans, LA 70018, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-413-597-2329 Received: 22 May 2019; Accepted: 20 June 2019; Published: 22 June 2019 Abstract: This work advances research on the role of hurricanes in degrading the rocky coastline within Mexico’s Gulf of California, most commonly formed by widespread igneous rocks. Under evaluation is a distinct coastal boulder bed (CBB) derived from banded rhyolite with boulders arrayed in a partial-ring configuration against one side of the headland on Ensenada Almeja (Clam Bay) north of Loreto. Preconditions related to the thickness of rhyolite flows and vertical fissures that intersect the flows at right angles along with the specific gravity of banded rhyolite delimit the size, shape and weight of boulders in the Almeja CBB. Mathematical formulae are applied to calculate the wave height generated by storm surge impacting the headland. The average weight of the 25 largest boulders from a transect nearest the bedrock source amounts to 1200 kg but only 30% of the sample is estimated to exceed a full metric ton in weight. -
Richard Sullivan, President
Participating Organizations Alliance for a Living Ocean American Littoral Society Arthur Kill Coalition Clean Ocean Action www.CleanOceanAction.org Asbury Park Fishing Club Bayberry Garden Club Bayshore Regional Watershed Council Bayshore Saltwater Flyrodders Belford Seafood Co-op Main Office Institute of Coastal Education Belmar Fishing Club Beneath The Sea 18 Hartshorne Drive 3419 Pacific Avenue Bergen Save the Watershed Action Network P.O. Box 505, Sandy Hook P.O. Box 1098 Berkeley Shores Homeowners Civic Association Wildwood, NJ 08260-7098 Cape May Environmental Commission Highlands, NJ 07732-0505 Central Jersey Anglers Voice: 732-872-0111 Voice: 609-729-9262 Citizens Conservation Council of Ocean County Fax: 732-872-8041 Fax: 609-729-1091 Clean Air Campaign, NY Ocean Advocacy [email protected] Coalition Against Toxics [email protected] Coalition for Peace & Justice/Unplug Salem Since 1984 Coast Alliance Coastal Jersey Parrot Head Club Communication Workers of America, Local 1034 Concerned Businesses of COA Concerned Citizens of Bensonhurst Concerned Citizens of COA Concerned Citizens of Montauk Eastern Monmouth Chamber of Commerce Fisher’s Island Conservancy Fisheries Defense Fund May 31, 2006 Fishermen’s Dock Cooperative, Pt. Pleasant Friends of Island Beach State Park Friends of Liberty State Park, NJ Friends of the Boardwalk, NY Garden Club of Englewood Edward Bonner Garden Club of Fair Haven Garden Club of Long Beach Island Garden Club of Middletown US Army Corps of Engineers Garden Club of Morristown -
Uplift of Quaternary Shorelines in Eastern Patagonia: Darwin Revisited
Uplift of Quaternary shorelines in Eastern Patagonia: Darwin revisited Kevin Pedoja, Vincent Regard, Laurent Husson, Joseph Martinod, Benjamin Guillaume, Enrique Fucks, Maximiliano Iglesias, Pierre Weill To cite this version: Kevin Pedoja, Vincent Regard, Laurent Husson, Joseph Martinod, Benjamin Guillaume, et al.. Uplift of Quaternary shorelines in Eastern Patagonia: Darwin revisited. Geomorphology, Elsevier, 2011, 127 (3-4), pp.121-142. 10.1016/j.geomorph.2010.08.003. insu-00610899 HAL Id: insu-00610899 https://hal-insu.archives-ouvertes.fr/insu-00610899 Submitted on 6 Mar 2019 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. Distributed under a Creative Commons Attribution| 4.0 International License Uplift of quaternary shorelines in eastern Patagonia: Darwin revisited Kevin Pedoja a,⁎, Vincent Regard b,c,d, Laurent Husson e,f, Joseph Martinod b,c,d, Benjamin Guillaume g, Enrique Fucks h, Maximiliano Iglesias i, Pierre Weill a a Laboratoire de Morphodynamique Continentale et Côtière, CNRS, Université de Caen, 14000 Caen, France b Université de Toulouse ; UPS (OMP) ; LMTG ; 14 Av Edouard Belin, F-31400 Toulouse, France c IRD ; LMTG ; F-31400 Toulouse, France d CNRS ; LMTG ; F-31400 Toulouse, France e CNRS UMR 6118, Géosciences Rennes, 35042 Rennes, France f CNRS UMR 6112, Laboratoire de Planétologie et Géodynamique de Nantes, France g Dip. -
Gulf of California - Sea of Cortez Modern Sailing Expeditions
Gulf of California - Sea of Cortez Modern Sailing Expeditions November 24 to December 4, 2019 Modern Sailing School & Club Cpt Blaine McClish (415) 331 – 8250 Trip Leader THE BOAT — Coho II, 44’ Spencer 1330 Coho II is MSC’s legendary offshore racer/cruiser. She has carried hundreds of MSC students and sailors under the Golden Gate Bridge and onto the Pacific Ocean. At 44.4 feet overall length and 24,000 pounds of displacement, Coho II is built for crossing oceans with speed, seakindly motion, and good performance in both big winds and light airs. • Fast and able bluewater cruiser • Fully equipped for the offshore sailing and cruising experience TRAVEL ARRANGEMENTS You are responsible for booking your own airfare. Direct flights from SFO to La Paz, and Los Cabos to SFO are available but are limited. Flights with layovers in San Diego or Los Angeles will cost less than direct flights. If you would like to use a travel agent to book your flights, we suggest Bob Entwisle at E&E Travel at (415) 819-5665. WHAT TO BRING Luggage Travel light. Your gear should fit in a medium duffel bag and small carry-on bag. Your carry-on should be less than 15 pounds. We recommend using a dry bag or backpack. Both bags should be collapsible for easy storage on the boat in small space. Do not bring bags with hard frames as they are difficult to stow. Gear We have found that people often only use about half of what they bring. A great way to bring only what you use is to lay all your items out and reduce it by 50%. -
Chapter 10. a First Look at Nunatsiavut Kangidualuk ('Fjord') Ecosystems
Chapter 10. A first look at Nunatsiavut Kangidualuk (‘fjord’) ecosystems Lead author Tanya Brown1,2,3, Ken Reimer3, Tom Sheldon4, Trevor Bell5 1Department of Biochemistry and Microbiology, University of Victoria, Victoria, BC; 2Institute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, BC; 3Environmental Sciences Group, Royal Military College of Canada, Kingston, ON; 4Nunatsiavut Government, Nain, NF; 5Memorial University of Newfoundland, St. John’s, NF Contributing authors S. Bentley, R. Pienitz, M. Gosselin, M. Blais, M. Carpenter, E. Estrada, T. Richerol, E. Kahlmeyer, S. Luque, B. Sjare, A. Fisk, S. Iverson Abstract Long marine inlets that are classified as either fjords or fjards indent the Labrador coast. Along the moun- tainous north coast a classic fjord landscape dominates, with deep (up to ~300 m) muddy basins separated by rocky sills and flanked by high (up to 1,000 m), steep sidewalls. In contrast, the fjards of the central and southern coast are generally shallow (150 m), irregularly shaped inlets with gently sloping sidewalls and large intertidal zones. These fjords and fjards are important feeding grounds for marine mammals and seabirds and are commonly used by Inuit for hunting and travel. Despite their ecological and socio-cultural importance, these marine ecosystems are largely understudied. The Nunatsiavut Nuluak project has, as a primary goal, to undertake baseline inventories and comparative assessments of representative marine ecosystems in Labrador, including benthic and pelagic community composition, distribution and abun- dance, fjord processes, and oceanographic conditions. A case study demonstrating ecosystem resilience to anthropogenic disturbance is examined. This information provides a foundation for further research and monitoring as climate change and anthropogenic pressures alter recent baselines.