Corals That Live on Mountaintops
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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. -
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). -
1 Creating a Species Inventory for a Marine Protected Area: the Missing
Katherine R. Rice NOAA Species Inventory Project Spring 2018 Creating a Species Inventory for a Marine Protected Area: The Missing Piece for Effective Ecosystem-Based Marine Management Katherine R. Rice ABSTRACT Over the past decade, ecosystem-based management has been incorporated into many marine- management administrations as a marine-conservation tool, driven with the objective to predict, evaluate and possibly mitigate the impacts of a warming and acidifying ocean, and a coastline increasingly subject to anthropogenic control. The NOAA Office of National Marine Sanctuaries (ONMS) is one such administration, and was instituted “to serve as the trustee for a network of 13 underwater parks encompassing more than 600,000 square miles of marine and Great Lakes waters from Washington state to the Florida Keys, and from Lake Huron to American Samoa” (NOAA, 2015). The management regimes for nearly all national marine sanctuaries, as well as other marine protected areas, have the goal of managing and maintaining biodiversity within the sanctuary. Yet none of those sanctuaries have an inventory of their known species nor a standardized protocol for measuring or monitoring species biodiversity. Here, I outline the steps required to compile a species inventory for an MPA, but also describe some of stumbling blocks that one might encounter along the way and offer suggestions on how to handle these issues (see Appendix A: Process for Developing the MBNMS Species Inventory (PD-MBNMS)). This project consists of three research objectives: 1. Determining what species inventory efforts exist, how they operate, and their advantages and disadvantages 2. Determining the process of creating a species inventory 3. -
2019 Annual Report a SUMMARY Climate Change a Triple Threat for the Ocean CO2 Burning Fossil Fuels, Deforestation and Industrial Agriculture Release
2019 Annual Report A SUMMARY Climate Change A triple threat for the ocean CO2 Burning fossil fuels, deforestation and industrial agriculture release carbon dioxide (CO2) and other heat-trapping gases into our atmosphere, causing our planet to warm. The ocean has buffered us from the worst impacts of climate > 90% ~25% HEAT change by absorbing more than 90 CO2 percent of this excess heat and about 25 percent of the CO2, but at the cost of causing significant harm to marine ecosystems. LESS MORE WARMER OXYGEN ACIDIC SEA LEVEL BLEACHING TOXIC ALGAE HABITATS ACIDIFICATION FISHERIES Sea level rise is Warm-water coral reefs Larger and more frequent Lower oxygen levels More acidic water Disruptions in fisheries accelerating, flooding (marine biodiversity blooms are making fish, are suffocating some harms animals that build affect the marine food coastal communities hotspots) could be lost if birds, marine mammals marine animals and shells, such as corals, web, local livelihoods, and and drowning the planet warms by and people sick. shrinking their habitats. clams, and oysters. global food security. wetland habitats. 2°C (3.6°F). In 2019, the Intergovernmental Panel on Climate Change report details the triple threat of climate change to ocean ecosystems: Warming, acidification, and deoxygenation. annualreport.mbari.org/2019 Illustration by Emily Hess Cover photo: Animation by Frame 48 Source: IPCC, 2019: Special Report on the Ocean and Cryosphere in a Changing Climate (SROCC) View from the Masthead Climate Change A triple threat for the ocean CO 2 Advancing science Burning fossil fuels, deforestation and industrial agriculture release and engineering for carbon dioxide (CO2) and other heat-trapping gases into our atmosphere, causing our planet to Earth’s final frontier warm. -
Publications Supported by NOAA's Office of Ocean Exploration And
1 Publications Supported by NOAA’s Office of Ocean Exploration and Research Compiled by Chris Belter, NOAA Central Library Accurate as of 17 April 2012 Journal Articles (n=454) Ahyong ST. 2008. Deepwater crabs from seamounts and chemosynthetic habitats off eastern New Zealand (Crustacea : Decapoda : Brachyura). Zootaxa(1708):1-72. Aig D, Haywood K. 2008. Through the Sea Snow: The Central Role of Videography in the Deep Gulf Wrecks Mission. International Journal of Historical Archaeology 12(2):133-145. doi:10.1007/s10761-008-0049-7 Andrews AH, Stone RP, Lundstrom CC, DeVogelaere AP. 2009. Growth rate and age determination of bamboo corals from the northeastern Pacific Ocean using refined Pb-210 dating. Marine Ecology-Progress Series 397:173-185. doi:10.3354/meps08193 Angel MV. 2010. Towards a full inventory of planktonic Ostracoda (Crustacea) for the subtropical Northwestern Atlantic Ocean. Deep-Sea Research Part Ii-Topical Studies in Oceanography 57(24-26):2173-2188. doi:10.1016/j.dsr2.2010.09.020 Arellano SM, Young CM. 2009. Spawning, Development, and the Duration of Larval Life in a Deep-Sea Cold-Seep Mussel. Biological Bulletin 216(2):149-162. Auster PJ. 2007. Linking deep-water corals and fish populations. Bulletin of Marine Science 81:93-99. Auster PJ, Gjerde K, Heupel E, Watling L, Grehan A, Rogers AD. 2011. Definition and detection of vulnerable marine ecosystems on the high seas: problems with the "move-on" rule. ICES Journal of Marine Science 68(2):254-264. doi:10.1093/icesjms/fsq074 Auster PJ, Watling L. 2010. Beaked whale foraging areas inferred by gouges in the seafloor. -
360. How Many Hours in a Day? 24
With this in mind we can discuss how one can finds one longitude. How many degrees are there in a circle? 360. How many hours in a day? 24. So how many degrees are there in an hour? (divide 360 by 24 and the answer is 15). So for every hour away from the p rime meridian you are 15 degrees away from it. Ships would take a chronometer or a clock on the ship set at the time at the Prime Meridian. When the sun was directly overhead on the ship, the navigator would know it was “noon” and look at the clock which might say 1300 hours (1 p.m.) So there is an hour difference in time between the ship and London. This would mean that the ship is 15 degrees west of the prime meridian. Charles Darwin Darwin traveled on a ship called “The Beagle” captained by Robert Fitzroy. The ship was to undertake a journey that would last nearly 5 years. The ship left on 27 Dec, 1831. Charles Darwin as naturalist whose job, basically was to disprove the idea of evolution which was growing in popularity at the time. Darwin made two significant hypotheses on the trip. One had to do with his theory of reef formation, The other had to do with the idea of biological evolution. We deal here with the first of the two – reef formation First. What is a reef made of? Largely coral. What is coral? Coral is an animal belonging to a phylum called Cnidaria. This phylum contains animals which are sessile (don’t move) like sea anemones and corals and well as some organisms which are motile (can move) like jelly fish. -
National Oceanic and Atmospheric Administration
STATE OF CALIFORNIA—THE RESOURCES AGENCY ARNOLD SCHWARZENEGGER, GOVERNOR CALIFORNIA COASTAL COMMISSION 45 FREMONT, SUITE 2000 SAN FRANCISCO, CA 94105-2219 VOICE AND TDD (415) 904-5200 FAX (415) 904-5400 F4c STAFF REPORT AND RECOMMENDATION ON CONSISTENCY DETERMINATION Consistency Determination No. CD-011-07 Staff: CLT-SF File Date: 2/28/2007 60th Day: 4/29/2007 75th Day: 5/14/2007 Extended to: 8/17/2007 Commission Meeting: 8/10/2007 FEDERAL AGENCY: National Oceanic and Atmospheric Administration PROJECT LOCATION: The Monterey Bay National Marine Sanctuary extends from Marin County to Cambria (San Luis Obispo County), encompassing nearly 300 miles of shoreline and 5,322 square miles of ocean extending an average of twenty-five miles from shore (Exhibit 1). PROJECT DESCRIPTION: Revised management plan and revised set of regulations for the Monterey Bay National Marine Sanctuary. SUBSTANTIVE FILE DOCUMENTS: See page 37. CD-011-07 (NOAA) Monterey Bay National Marine Sanctuary Page 2 EXECUTIVE SUMMARY The National Oceanic and Atmospheric Administration (NOAA) submitted a consistency determination for the revised management plan and set of regulations governing activities in the Monterey Bay National Marine Sanctuary (MBNMS or Sanctuary). NOAA states that the proposed measures would afford better protection to the natural and cultural resources of the MBNMS. NOAA describes the proposed set of regulations as including both new regulations as well as changes to existing regulations, as follows: Proposed new regulations include prohibitions on: -
Template for Submission of Scientific Information to Describe Areas Meeting Scientific Criteria for Ecologically Or Biologically Significant Marine Areas
Template for Submission of Scientific Information to Describe Areas Meeting Scientific Criteria for Ecologically or Biologically Significant Marine Areas Title/Name of the area: Canyons and Seamounts of the Northwest Atlantic Ocean within and beyond national jurisdiction Presented by: Lisa Speer, Director, International Oceans Program, Natural Resources Defense Council Peter Auster, Senior Research Scientist, Sea Research Foundation and Research Professor Emeritus, University of Connecticut. Introduction: Submarine canyons and seamounts off the Atlantic coast of the United States and Canada provide foraging, breeding, and/or nursery habitats for hundreds of fish and crustacean species, including swordfish, tuna, and sharks; marine mammals including endangered sperm whale, beaked whales, and dolphins; and isolated invertebrate communities including those dominated by deep sea corals and sponges. Location: Submarine canyons off the Atlantic coast of the United States and Canada occur mostly within the zones of national jurisdiction. Four of the New England Seamounts are within the jurisdiction of the United States. The remaining New England Seamounts and all of the Corner Rise Seamounts are located in ABNJ. See maps (links below). Feature description of the proposed area The varied seafloor topography and complex oceanographic influences of canyons and seamounts combine to create unique habitat for many species of corals, sponges and other invertebrates on the benthos and fish, marine mammals and birds in the pelagic realm. Deepwater canyons are a striking feature of the continental margin off the east coast of the United States and Canada. There are 15 major canyons in the United States alone, ranging in depth from about 200 meters to about 3,500 meters. -
Burton 2013 Cultural History of Davidson Seamount
Cultural History of Davidson Seamount: A Characterization of Mapping, Research, and Fishing Erica J. Burton Monterey Bay National Marine Sanctuary Technical Report August 2013 Cultural History of Davidson Seamount MBNMS Technical Report COVER IMAGES Top left: Davidson Seamount, the first undersea feature to be officially termed a seamount by the U.S. Board on Geographic Names. This feature was surveyed by the C&GS in 1933 and named in honor of the great Coast Survey West Coast pioneer George Davidson, 1825-1911. Latitude should range from 35 to 36 degrees. Image Credit: NOAA Central Library Historical Collection (NOAA Photo Library) and original chart credit: Association of Commissioned Officers (1933). Top right: George Davidson (circa 1883). Credit: NOAA, B.A. Colonna Album (NOAA Photo Library) Bottom: Monterey Bay Aquarium Research Institute’s ROV Tiburon. Credit: T. Trejo for NOAA. SUGGESTED CITATION Burton, E.J. 2013. Cultural History of Davidson Seamount: A Characterization of Mapping, Research, and Fishing. MBNMS Technical Report, 21 p. 2 Cultural History of Davidson Seamount MBNMS Technical Report TABLE OF CONTENTS INTRODUCTION .......................................................................................................................................4 MAPPING ................................................................................................................................................................................ 5 RESEARCH AND MONITORING ................................................................................................................................ -
Biodiversity of Bear Seamount, New England Seamount Chain: Results of Exploratory Trawling
W&M ScholarWorks VIMS Articles Virginia Institute of Marine Science 9-2003 Biodiversity of Bear Seamount, New England Seamount chain: Results of exploratory trawling JA Moore M Vecchione R Gibbons JK Galbraith M Turnipseed Virginia Institute of Marine Science See next page for additional authors Follow this and additional works at: https://scholarworks.wm.edu/vimsarticles Part of the Aquaculture and Fisheries Commons, and the Marine Biology Commons Recommended Citation Moore, JA; Vecchione, M; Gibbons, R; Galbraith, JK; Turnipseed, M; Southworth, M; and Watkins, E, Biodiversity of Bear Seamount, New England Seamount chain: Results of exploratory trawling (2003). Journal of Northwest Atlantic Fishery Science, 31, 363-372. https://scholarworks.wm.edu/vimsarticles/1970 This Article is brought to you for free and open access by the Virginia Institute of Marine Science at W&M ScholarWorks. It has been accepted for inclusion in VIMS Articles by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Authors JA Moore, M Vecchione, R Gibbons, JK Galbraith, M Turnipseed, M Southworth, and E Watkins This article is available at W&M ScholarWorks: https://scholarworks.wm.edu/vimsarticles/1970 J Northw Atl Fish Sci, Vol 31: 363372 Biodiversity of Bear Seamount, New England Seamount Chain: Results of Exploratory Trawling J A Moore Florida Atlantic University, Honors College, Jupiter, FL 33458, USA M Vecchione, B B Collette and R Gibbons National Marine Fisheries Service, National Systematics Laboratory, -
SPOTLIGHT 4 New England and Corner Rise Seamounts
CORE Metadata, citation and similar papers at core.ac.uk or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The approval Oceanography portionthe ofwith any articlepermitted only photocopy by is of machine, reposting, this means or collective or other redistirbution This article has This been published in Provided Mby WoodsOU HoleNT OpenAI AccessNS ServerIN THE Sea SPOTLIGHT 4 New England and Corner Rise Seamounts Oceanography By Timothy M. Shank , Volume 23, Number 1, a quarterly journal of The 23, NumberOceanography 1, a quarterly , Volume One of the longest seamount tracks in with ~ 75 morphotypes unique to the for understanding the changes in North the Atlantic Ocean was formed by the Corner Rise and ~ 60 unique to the Atlantic open-ocean circulation through Great Meteor or New England hotspot. New England Seamounts (Cho, 2008). time and the impact these changes have This more than 3000-km-long hotspot Interestingly, a variety of invertebrates on population connectivity. For example, track formed both the New England and are revealing differing levels of specificity corals in the northern North Atlantic Corner Rise seamounts, with a pause to their host corals, ranging from “facul- prospered during past interglacial in volcanism 83 million years ago as tative” to “obligate” (see Shank, 2010). periods and in particular throughout evidenced by the morphological gap For example, the galatheid Uroptychus the past 11,000 years, yet apparently between chains (Figure 1). The New has been observed only on the antipatha- disappeared during glacial times England and Corner Rise seamounts rian Parantipathes sp., and the ophiuroid (above 50°N). -
Telepresence-Enabled Exploration of The
! ! ! ! 2014 WORKSHOP TELEPRESENCE-ENABLED EXPLORATION OF THE !EASTERN PACIFIC OCEAN WHITE PAPER SUBMISSIONS ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! TABLE OF CONTENTS ! ! NORTHERN PACIFIC! Deep Hawaiian Slopes 7 Amy Baco-Taylor (Florida State University) USS Stickleback (SS-415) 9 Alexis Catsambis (Naval History and Heritage Command's Underwater Archaeology Branch) Sunken Battlefield of Midway 10 Alexis Catsambis (Naval History and Heritage Command's Underwater Archaeology Branch) Systematic Mapping of the California Continental Borderland from the Northern Channel Islands to Ensenada, Mexico 11 Jason Chaytor (USGS) Southern California Borderland 16 Marie-Helene Cormier (University of Rhode Island) Expanded Exploration of Approaches to Pearl Harbor and Seabed Impacts Off Oahu, Hawaii 20 James Delgado (NOAA ONMS Maritime Heritage Program) Gulf of the Farallones NMS Shipwrecks and Submerged Prehistoric Landscape 22 James Delgado (NOAA ONMS Maritime Heritage Program) USS Independence 24 James Delgado (NOAA ONMS Maritime Heritage Program) Battle of Midway Survey and Characterization of USS Yorktown 26 James Delgado (NOAA ONMS Maritime Heritage Program) Deep Oases: Seamounts and Food-Falls (Monterey Bay National Marine Sanctuary) 28 Andrew DeVogelaere (Monterey Bay National Marine Sanctuary) Lost Shipping Containers in the Deep: Trash, Time Capsules, Artificial Reefs, or Stepping Stones for Invasive Species? 31 Andrew DeVogelaere (Monterey Bay National Marine Sanctuary) Channel Islands Early Sites and Unmapped Wrecks 33 Lynn Dodd (University of Southern