Endeavour Hydrothermal Vents: Canada's First Marine Protected Area
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Geologists Suggest Horseshoe Abyssal Plain May Be Start of a Subduction Zone 8 May 2019, by Bob Yirka
Geologists suggest Horseshoe Abyssal Plain may be start of a subduction zone 8 May 2019, by Bob Yirka against one another. Over by the Iberian Peninsula, the opposite appears to be happening—the African and Eurasian plates are pulling apart as the former creeps east toward the Americas. Duarte noted that back in 2012, other researchers conducting seismic wave tests found what appeared to be a dense mass of unknown material beneath the epicenter of the 1969 quake. Some in the field suggested it could be the start of a subduction zone. Then, last year, another team conducted high-resolution imaging of the area and also found evidence of the mass, confirming that it truly existed. Other research has shown that the area just above the mass experiences routine tiny earthquakes. Duarte suggests the evidence to date indicates that the bottom of the plate is peeling away. This could happen, he explained, due to serpentinization in which water percolates through plate fractures and reacts with material beneath the surface, resulting A composite image of the Western hemisphere of the in the formation of soft green minerals. The soft Earth. Credit: NASA mineral layer, he suggests, is peeling away. And if that is the case, then it is likely the area is in the process of creating a subduction zone. He reports that he and his team members built models of their A team of geologists led by João Duarte gave a ideas and that they confirmed what he suspected. presentation at this past month's European The earthquakes were the result of the process of Geosciences Union meeting that included a birthing a new subduction zone. -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats. -
The C-Floor and Zones
The C-Floor and zones Table of Contents ` ❖ The ocean zones ❖ Sunlight zone and twilight zone ❖ Midnight and Abyssal zone ❖ The hadal zone ❖ The c-floor ❖ The c-floor definitions ❖ The c-floor definitions pt.2 ❖ Cites ❖ The end The ocean zones 200 meters deep 1,000 Meters deep 4,000 Meters deep 6,000 Meters deep 10,944 meters deep Sunlight zone Twilight zone ❖ The sunlight zone is 200 meters from the ocean's ❖ The twilight zone is about 1,000 meters surface deep from the ❖ Animals that live here ocean's surface sharks, sea turtles, ❖ Animals that live jellyfish and seals here are gray ❖ Photosynthesis normally whales, greenland occurs in this part of the Shark and clams ocean ❖ The twilight get only a faint amount of sunlight DID YOU KNOW Did you know That no plants live That the sunlight zone in the twilight zone could be called as the because of the euphotic and means well lit amount of sunlight in greek Midnight zone Abyssal zone ❖ The midnight zone is ❖ The abyssal zone is 4,000 meters from 6,000 meters from the the ocean's surface ocean’s surface ❖ Animals that live in ❖ Animals that live in the the midnight zone Abyssal zone are fangtooth fish, pacific are, vampire squid, viperfish and giant snipe eel and spider crabs anglerfish ❖ Supports only ❖ Animals eat only the DID YOU KNOW invertebrates and DID YOU KNOW leftovers that come That only 1 percent of light fishes That most all the way from the travels through animals are sunlight zone to the the midnight zone either small or midnight zone bioluminescent The Hadal Zone (Trench ● The Hadal Zone is 10,944 meters under the ocean ● Snails, worms, and sea cucumbers live in the hadal zone ● It is pitch black in the Hadal Zone The C-Floor The C-Floor Definitions ❖ The Continental Shelf - The flat part where people can walk. -
Ocean Zones Adapted from USC Sea Grant “Island Explorers” by Dr
2011 COSEE-West Introduction to Ocean Zones Adapted from USC Sea Grant “Island Explorers” by Dr. Rachel Kennison, COSEE West Co- Director Grade: K-12 Group Size: 30 students Time: 55 minutes BACKGROUND In order to begin to understand life below the seafloor, it is essential to grasp that the ocean has many different habitats that are defined by the physical and chemical properties that exist at different depths. The purpose of this activity is to identify and describe different zones of the ocean and the organisms that live there. The ocean is divided into 5 main zones from the surface to the depths where light can no longer penetrate. These zones are characterized by different physical and chemical properties, such as quantity and quality of light, pressure and temperature. These properties affect what life forms can exist within those limitations. This activity introduces the microbial environment in the deep ocean, and can be the foundation to explain geothermal processes, and the evolution of bacteria. Labels and features to include on diagram: Photic (sunlit) zone Aphotic (no light) zone Neritic system Benthic realm Pelagic realm Bathyal zone Abyssal zone Hadal zone Shoreline Sea level Coral reef Continental Shelf Continental slope Continental rise Submarine Canyon Abyssal Plain Seamount Guyot Trench Mid-ocean Ridge Rift Valley Hydrothermal vent Sub-seafloor sediment Sub-seafloor aquifer A useful reference for your ocean zones diagram is at http://geosci.sfsu.edu/courses/geol102/ex9.html Two basic guides for the zones: (Source: Sea -
For Creative Minds
For Creative Minds The For Creative Minds educational section may be photocopied or printed from our website by the owner of this book for educational, non-commercial uses. Cross-curricular teaching activities, interactive quizzes, and more are available online. Go to ArbordalePublishing.com and click on the book’s cover to explore all the links. Deep Ocean Habitats Things change the deeper you go in the ocean: light disappears, temperatures grow increasingly colder, and pressure gets much higher. The amount of oxygen in the water sunlight zone decreases with depth but then gets higher again at the bottom! Because these changes twilight zone affect the types of organisms that can survive there, the ocean is divided into five layers by depth called life zones. Only the sunlight zone receives enough sunlight for algae to convert light into energy midnight zone (photosynthesis). Because almost all food webs start with plants or algae, this is the zone where the most animals live. The twilight zone still gets some sunlight, but not enough for photosynthesis. The animals that live here either travel to the sunlight zone to feed or depend on food falling from above. There is no light in the midnight zone. Most abyssal zone of the animals that live here produce their own light through bioluminescence. The abyssal zone is pitch black, almost freezing cold, and has little oxygen and incredibly high pressure, yet animals still live here. In the deep trenches is the hadal zone. It is like the abyssal zone, except with even more hadal zone immense -
Global Open Oceans and Deep Seabed (Goods) - Biogeographic Classification
CBD Distr. GENERAL UNEP/CBD/SBSTTA/14/INF/10 29 April 2010 ORIGINAL: ENGLISH SUBSIDIARY BODY ON SCIENTIFIC, TECHNICAL AND TECHNOLOGICAL ADVICE Fourteenth meeting Nairobi, 10-21 May 2010 Item 3.1.3 of the provisional agenda * GLOBAL OPEN OCEANS AND DEEP SEABED (GOODS) - BIOGEOGRAPHIC CLASSIFICATION Note by the Executive Secretary 1. The Executive Secretary is circulating herewith, for the information of participants in the fourteenth meeting of the Subsidiary Body on Scientific, Technical and Technological Advice, IOC Technical Series No.84 on Global Open Oceans and Deep Seabed (GOODS) - Biogeographic Classification, submitted by the United Nations Educational, Scientific and Cultural Organization/Intergovernmental Oceanographic Commission, pursuant to paragraph 6of decision IX/20. 2. This report was also considered by the CBD Expert Workshop on Scientific and Technical Guidance on the Use of Biogeographic Classification Systems and Identification of Marine Areas Beyond National Jurisdiction in Need of Protection, held in Ottawa, from 29 September to 2 October 2009. 3. The document is circulated in the form and language in which it was received by the Secretariat of the Convention on Biological Diversity. * UNEP/CBD/SBSTTA/14/1 /... In order to minimize the environmental impacts of the Secretariat’s processes, and to contribute to the Secretary-General’s initiative f or a C-Neutral UN, this document is printed in limited numbers. Delegates are kindly requested to bring their copies to meetings and not to request additional copies. Global Open Oceans and Deep Seabed (GOODS) biogeographic classification Global Open Oceans and Deep Seabed (GOODS) biogeographic classification Edited by: Marjo Vierros (UNU-IAS), Ian Cresswell (Australia), Elva Escobar Briones (Mexico), Jake Rice (Canada), and Jeff Ardron (Germany) UNESCO 2009 goods inside 2.indd 1 24/03/09 14:55:52 Global Open Oceans and Deep Seabed (GOODS) biogeographic classification Authors Contributors Vera N. -
The Ocean Floor Word Find Activity
The Ocean Floor Word Find Activity Beneath the ocean is a landscape, which has similar features to what we see on land. The ocean floor is generally divided into the continental shelf, the continental slope and the deep ocean floor. The land from the continent or an island gently extends out underneath the water to form a large area called the continental shelf. The continental shelf is a very important area under the ocean as a lot of marine life thrives there. The area can also contain petroleum, natural gas as well as minerals under the seafloor which are very valuable. The continental slope is the point where the shelf area plunges down into the deepest parts of the oceans. This part of the ocean floor is marked with deep canyons. Below the continental slopes sediment can often collect over time to form gental slopes called continental rises. The continental shelf, slope and rises are known as the continental margin. In many parts of the bottom of the ocean there are flat areas covered with sediment. This area is called the abyssal plain. The abyssal plain is usually found at depths between 3000 and 6000 metres below sea level. The abyssal plain is broken by mid ocean ridges, which are like long mountain ranges under the ocean. The entire global mid ocean ridge system is the longest mountain chain on earth and has formed where oceanic plates are continuously separating. These areas include the Mid-Atlantic ridge, the Pacific rise, as well as trenches such as the Marina Trench in the Pacific Ocean. -
45. Sedimentary Facies and Depositional History of the Iberia Abyssal Plain1
Whitmarsh, R.B., Sawyer, D.S., Klaus, A., and Masson, D.G. (Eds.), 1996 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 149 45. SEDIMENTARY FACIES AND DEPOSITIONAL HISTORY OF THE IBERIA ABYSSAL PLAIN1 D. Milkert,2 B. Alonso,3 L. Liu,4 X. Zhao,5 M. Comas,6 and E. de Kaenel4 ABSTRACT During Leg 149, a transect of five sites (Sites 897 to 901) was cored across the rifted continental margin off the west coast of Portugal. Lithologic and seismostratigraphical studies, as well as paleomagnetic, calcareous nannofossil, foraminiferal, and dinocyst stratigraphic research, were completed. The depositional history of the Iberia Abyssal Plain is generally characterized by downslope transport of terrigenous sedi- ments, pelagic sedimentation, and contourite sediments. Sea-level changes and catastrophic events such as slope failure, trig- gered by earthquakes or oversteepening, are the main factors that have controlled the different sedimentary facies. We propose five stages for the evolution of the Iberia Abyssal Plain: (1) Upper Cretaceous and lower Tertiary gravitational flows, (2) Eocene pelagic sedimentation, (3) Oligocene and Miocene contourites, (4) a Miocene compressional phase, and (5) Pliocene and Pleistocene turbidite sedimentation. Major input of terrigenous turbidites on the Iberia Abyssal Plain began in the late Pliocene at 2.6 Ma. INTRODUCTION tured by both Mesozoic extension and Eocene compression (Pyrenean orogeny) (Boillot et al., 1979), and to a lesser extent by Miocene com- Leg 149 drilled a transect of sites (897 to 901) across the rifted mar- pression (Betic-Rif phase) (Mougenot et al., 1984). gin off Portugal over the ocean/continent transition in the Iberia Abys- Previous studies of the Cenozoic geology of the Iberian Margin sal Plain. -
Deep-Sea Ecosystems: Pristine Biodiversity Reservoir and Technological Challenges
The Exploration of Marine Biodiversity Scientific and Technological Challenges Carlos M. Duarte (ed.) Offprint of the Chapter 3. DEEP-SEA ECOSYSTEMS: PRISTINE BIODIVERSITY RESERVOIR AND TECHNOLOGICAL CHALLENGES by Eva Ramírez Llodra1,2 and David S. M. Billett2 1 Institute of Marine Sciences (CMIMA-CSIC), Barcelona, Spain 2 National Oceanography Centre (NOC), Southampton, UK © Fundación BBVA, 2006 www.fbbva.es ISBN: 978-84-96515-27-7 3. DEEP-SEA ECOSYSTEMS: PRISTINE BIODIVERSITY RESERVOIR AND TECHNOLOGICAL CHALLENGES 3.1. INTRODUCTION THE DEEP SEA is the largest ecosystem on Earth, with approximately 50% of the surface of the Earth covered by ocean more than 3,000 metres deep. It sup- ports one of the largest reservoirs of biodiversity on the planet, but remains one of the least studied ecosystems because of its remoteness and the techno- logical challenges for its investigation. The HMS Challenger Expedition (1872-1876) marked the beginning of the “heroic” age of deep-sea exploration, and our knowledge has progressed since in parallel with technological devel- opments. The deep-sea floor extends from around 200 m depth down the continental slope to the abyssal plains (3,000-6,000 m) and reaches the deepest part of the oceans in the Marianas Trench (11,000 m). These ecosystems are characterised by the absence of light, increasing pressure with depth and low temperature waters (with some exceptions). The deep sea contains extremely large habitats such as abyssal plains (millions km2) and mid-ocean ridges (65,000 km long). At the same time, it encloses relatively small, localised geological features such as canyons, seamounts, deep-water coral reefs, hydrothermal vents and cold seeps, which support unique microbial and animal communities. -
Oceans 11 Teaching Resources Vol 1
Oceans 11 A Teaching Resource Volume 1 1 Foreword Oceans 11 curriculum was developed by the Nova Scotia Department of Education as part of a joint project with the federal Department of Fisheries and Oceans. This curriculum reflects the framework described in Foundation for the Atlantic Canada Science Curriculum. Oceans 11 satisfies the second science credit requirement for high school graduation. Oceans 11 includes the following modules: Structure and Motion, Marine Biome, Coastal Zone, Aquaculture, and Fisheries. Oceans 11: A Teaching Resource, Volume 1 is intended to complement the curriculum guide, Oceans 11. The sample activities in this resource address the outcomes described in Oceans 11 for the three compulsory modules: Structure and Motion, Marine Biome, and Coastal Zone. Oceans 11: A Teaching Resource, Volume 2 is intended to complement Oceans 11. The sample activities in it address the outcomes for the modules Aquaculture and Fisheries. Teachers may choose to do one of these units or to divide their class into groups that focus on a unit. 2 Contents Structure and Motion Introduction Materials The Ocean Industry in Nova Scotia The Ocean Industry in Nova Scotia, Teacher Notes When Humans and the Ocean Meet When Humans and the Ocean Meet, Teacher Notes Bodies of Water Bodies of Water, Teacher Notes Bathymetric Profile Sketching Bathymetric Profile Sketching, Teacher Notes Water Facts Water Facts, Teacher Notes Comparing Densities of Fresh Water and Seawater Comparing Densities of Fresh Water and Seawater, Teacher Notes The Effects -
Abyssal Plain Faunal Carbon Flows Remain Depressed 26 Years After A
Biogeosciences, 15, 4131–4145, 2018 https://doi.org/10.5194/bg-15-4131-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Abyssal plain faunal carbon flows remain depressed 26 years after a simulated deep-sea mining disturbance Tanja Stratmann1, Lidia Lins2,a, Autun Purser3, Yann Marcon3,b, Clara F. Rodrigues4, Ascensão Ravara4, Marina R. Cunha4, Erik Simon-Lledó5, Daniel O. B. Jones5, Andrew K. Sweetman6, Kevin Köser7, and Dick van Oevelen1 1NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, P.O. Box 140, 4400 AC Yerseke, the Netherlands 2Marine Biology Research Group, Ghent University, Krijgslaan 281 S8, 9000 Ghent, Belgium 3Deep Sea Ecology and Technology, Alfred Wegener Institute, Am Handelshafen 12, 27570 Bremerhaven, Germany 4Departamento de Biologia & Centro de Estudos do Ambiente e do Mar (CESAM), Departamento de Biologia, Universidade de Aveiro, Campus de Santiago, 3810-193 Aveiro, Portugal 5National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK 6Marine Benthic Ecology, Biogeochemistry and In-situ Technology Research Group, The Lyell Centre for Earth and Marine Science and Technology, Heriot-Watt University, Edinburgh EH14 4AS, UK 7GEOMAR Helmholtz Centre for Ocean Research, FE Marine Geosystems, Wischhofstr 1–3, 24148 Kiel, Germany apresent address: Senckenberg Research Institute, Senckenberganlage 25, 60325 Frankfurt am Main, Germany bpresent address: MARUM – Center for Marine Environmental Sciences, General Geology – Marine Geology, University of Bremen, 28359 Bremen, Germany Correspondence: Tanja Stratmann ([email protected]) Received: 5 April 2018 – Discussion started: 9 April 2018 Revised: 25 June 2018 – Accepted: 27 June 2018 – Published: 6 July 2018 Abstract.