MoMAR : a coordinated and multidisciplinary long-term study of hydrothermal ecosystems at the Mid-Atlantic Ridge close to the Azores archipelago. Hydrothermal.

Slides:



Advertisements
Similar presentations
Ocean Reference Time-Series Moorings: Acoustics By Bruce M. Howe Applied Physics Laboratory, University of Washington Reference Time-Series Science Team.
Advertisements

John A. Orcutt Deputy Director, SIO Ocean Observations Initiative NSF MREFC Chair, NSF/CORE DEOS Comm.
1 SWALIM Workshop, Nairobi June 2007 N. Hoepffner, M.Clerici, and S. Djavidnia* Global Environment Monitoring Unit EC-JRC, Ispra The African Marine.
Towards Cabled Integration at Seafloor Hydrothermal Vent Sites K. Ding, W. E. Seyfried.
MoMAR* : suivi à long terme des systèmes hydrothermaux de la dorsale Médio Atlantique près des Açores. * Monitoring the Mid Atlantic Ridge.
FROM THE MIDOCEAN RIDGES TO THE BLACK SMOKERS. What is it a midocean ridge? A midocean ridge it’s due to the divergence between two plates (e.g. The African.
Plate Tectonics.
Structure of Earth Earth has Four parts Seafloor Spreading.
Mid-Ocean Ridges: A Connected System Hydrothermal circulation links ocean, seafloor, and crust, including vent communities How is fluid circulation controlled.
Spatial and Temporal Variability of Hydrography in the Vicinity of the Main Endeavour Field Scott Veirs, Christian Sarason, Russell McDuff, Fritz Stahr,
State Partnerships: Coastal & Environmental Issues Facing the MACOORA States November 17, 2009 MACOORA Kate Zultner Coastal States Organization
* Institut de Physique du Globe Paris
Science Starter Turn to the next blank page in your ISN and cut and paste the handout that is located on the front desk. You will need colored pencils.
Oceanography Ocean Sciences 122. Oceans of the World 1.Pacific Ocean 2.Atlantic Ocean 3.Indian Ocean 4.Arctic Ocean 5.Southern Ocean.
MP 2 Review.
WORKSHOP ON CABLE-BASED OCEAN OBSERVATORIES,11-12 JUNE 2007, RADISSON SAS HOTEL NORGE, BERGEN Research topics within [Seafloor] Participants: Kuvvet AtakanJon.
OET Nautilus Workshop University of Rhode Island, ISC 6–9 May 2013 OET Nautilus Workshop University of Rhode Island, ISC 6–9 May 2013 AT25-04: Hydrogeologic,
Earth’s Interior Section1.
Formation, Transformation and Trace-element scavenging of Minerals in Deep-Sea Ferromanganese crusts: Implications for marine biogeochemical cycles and.
Work Package 2 / 3 TECHNOLOGIAL & PROCEDURAL HARMONISATION FixO3 General Assembly 14 th to the 16 th October 2014, Heraklion-CRETE Jérôme Blandin, IFREMER.
EXtreme ecosystem studies in the deep OCEan: Technological Developments : EXOCET/D P.-M. Sarradin, J. Sarrazin, J.F. Cadiou et al EUROPEAN Project FP6,
Sea Floor Mapping with Sonar and Magnetometers. Sonar SOund Navigation And Ranging Sound waves are directed to the bottom of the ocean and reflect back.
Jeopardy Q $100 Q $100 Q $100 Q $100 Q $100 Q $200 Q $200 Q $200
TOPIC 5: PLATE TECTONICS
Research Infrastructures in FP7 On behalf of : Anna Maria Johansson, Hervé Péro European Commission, DG RTD/B3 MarineERA workshop Feb
Life in Extreme Environments: A Study of the Prevalence of life in the Depths of an Underwater Rift Zone.
TFH Berlin Deployment technologies of seafloor observatories Hans W. Gerber Dept. Mechanical Engineering TFH Berlin, University of Applied Sciences, Germany.
ROSCOE Vicki Ferrini: Data Representative/Team Leader Breea Govenar: Research Scientist/Data Representative Laishona Vitelli: K-12 Educator David Reeder:
RAP 1. __ coolest layer of the Earth (Earth’s layers) 2.___ three types of volcanoes (types of volcanoes) 3.___instrument that is located at or near Earth’s.
EPOS a long term integration plan of research infrastructures for solid Earth Science in Europe Preparatory Phase Project
The HERMIONE project (Hotspot Ecosystem Research and Man’s Impact on European Seas) is a new interdisciplinary project co-ordinated.
GEOLOGY JEOPARDY JB Final Review Jeopardy PLATE TECTONICS SEAFLOOR SPREADING DEFORMATION OF THE CRUST MINERALSROCKRECORD
Seismic Hazard Map EPOS European Plate Observing System RESEARCH INFRASTRUCTURE AND E-SCIENCE FOR DATA AND OBSERVATORIES ON EARTHQUAKES, VOLCANOES, SURFACE.
General Assembly Meeting – SA Session | Crete Oct SA 14.2 MOMAR - CENTRAL NORTH ATLANTIC DEEP SEA HYDROTHERMAL ECOSYSTEM OBSERVATION: SEISMIC, ACOUSTIC.
Strategy for building the infrastructure of EMSO - Norwegian node - Bénédicte Ferré & Jürgen Mienert Institute of Geology University of Tromsø All Regions.
Earth & its Layers Allison Morton Adv. Earth Science 2 ND Period.
Class 1: Plate Tectonics Review Today’s topics:  Earth’s compositional layers  Plate tectonics: theory & actions.
Laura Beranzoli Istituto Nazionale di Geofisica e Vulcanologia October 5-7, 2009ESONET NoE - 2nd All Region Workshop WP4 – Demonstration Missions.
Earth’s Interior. The Earth’s Core Much of the information scientists have about the Earth’s interior has come not only from complex instruments but also.
IES Integration of research activities on a long-term perspective Co-operation between universities, research institutes, enterprises and technology organisations.
MAR-ECO: PATTERNS AND PROCESSES OF THE ECOSYSTEMS OF THE NORTHERN MID-ATLANTIC after Garrison, 1993 Ridge-associated non-vent macro-and megafauna.
MoMAR : a coordinated and multidisciplinary long-term study of hydrothermal environments at the Mid- Atlantic Ridge / MoMAR-Fr The MOMAR (“Monitoring the.
ICOS status report, Oct The current Carboeurope atmospheric network Stars = vertical profiles Blue circles = continuous observatories Yellow diamonds.
EPOS where we are, where we go ! Massimo Cocco INGV Rome September EPOS Meeting.
The Science Requirements for Coastal and Marine Spatial Planning Dr. Robert B. Gagosian President and CEO September 24, 2009.
SUSTAINABLE DEVELOPMENT, GLOBAL CHANGE AND ECOSYSTEMS July Sub-Priority 6.3 “Global Change and Ecosystems” FP6 4 th Call for Proposals European.
ILIAS Project Summary ILIAS is an Integrated Infrastructure Initiative that has pulled together all of Europe's leading infrastructures in Astroparticle.
Metrology to enable improved underwater EMC testing MU- EMC Raúl Caballero Santos (CEM) Joaquin del Río (UPC) Albert Garcia (UPC)
E u r o p e a n C o m m i s s i o nCommunity Research Global Change and Ecosystems Malta, 27 January 2004 Alan Edwards EUROPEAN COMMISSION GMES – Implications.
5-7 Oct.2009All Regions Workshop #2 IBERIAN NODE Jorge Miguel Miranda University of Lisbon - IDL
DO NOW 1.___ name one cause of water pollution (water pollution) 2. __ coolest layer of the Earth (Earth’s layers) 3.___energy source that burns wood or.
Introduction Diffuse flow is detected using remote acoustic imaging. It is traditionally difficult to measure because it has a lower temperature and velocity.
Music: Beatles, “Octopus’s Garden” F First Midterm Exam will be April 23 F In class, closed book F Study Guide will be posted this Friday.
Hydrothermal Vents By Taylor, Jarrad and David What are Hydrothermal Vents A hypothermal vent is based on the ocean floor and is known as a hot spring,
  Long term (~30 yrs) scientific knowledge on deep- sea ecosystems (i.e. cold seeps, vents, cold water corals, slopes and abyssal plains…)  Vast experience.
Dynamic Planet I-3 AYR Answers. Question 1 What are the conditions that cause convection cells in a fluid? What are the conditions that cause convection.
Importance of Oceanography Oceanography is the study of the ocean, including its physical, chemical, geological, and biological aspects.
European Multidisciplinary Seafloor and Water Column Observatory - Portugal (EMSO-PT) Nuno Lourenço – (on behalf of Miguel Miranda)
InterRidge Chair, Leibniz-Institute of Marine Sciences, Kiel, Germany
Warm-up Directions Take Cornell notes in your lab journal on slides #2 – 9. Turn the title into a question and summarize the information on each.
PLATE TECTONICS.
Earth’s Materials and Processes-Part 8 Investigating Earth’s Interior
Hydrothermal Vents.
Earth’s Interior.
Science Starter Turn to the next blank page in your ISN and cut and paste the handout that is located on the front desk. You will need colored pencils.
Earth’s Interior.
7th EU Research FP has ten themes defined in order:
Alteration of Rocks by Temperature and Pressure
Part 1: Earth’s Dynamic Interior
Earth’s Interior.
Presentation transcript:

MoMAR : a coordinated and multidisciplinary long-term study of hydrothermal ecosystems at the Mid-Atlantic Ridge close to the Azores archipelago. Hydrothermal circulation at mid- ocean ridges is a fundamental process that impacts the transfer of energy and matter from the interior of the Earth to the crust, hydrosphere and biosphere. Seawater circulates through the permeable upper oceanic crust at mid-ocean ridges, exchanges chemicals with the surrounding rocks, and is heated up to temperatures of a few hundred degrees Celsius. This hot fluid flows up and is expelled at hydrothermal sites, in the form of black smokers, or diffuse vents. The unique faunal communities that develop near these vents are sustained by chemosynthetic microbes that use the chemicals in the hot fluids as a source of energy. The MoMAR area : # Slow-spreading Mid-Atlantic Ridge - 36°to 40°N # In proximity to the Azores harbours and shore-based facilities # 4 known vent fields / 3 distinct hydrothermal environments # Has been the target of over 20 scientific cruises under projects funded by EC MAST II, MAST III, FP4, FP5, FP6 leading to 15 years of multidisciplinary data. International participation to MoMAR: Strong european participation (14 labs in 8 countries), 3 funded FP6 initiatives have MoMAR-related objectives (MCRTN MoMARnet, STREP EXOCET/D & IP NEREIS). Selected as Integrated Study Site by the US Ridge 2000 Program. International coordination under the auspices of the InterRidge Program. MoMAR Objective : to constrain the dynamics of hydrothermal vent ecosystems at the Mid-Atlantic Ridge

Lucky Strike observatory design The objective there is to set up a permanent seafloor observatory to record and relate seismicity, seafloor deformation, fluid flow, temperature and composition, with the dynamics of vent communities (including microbes) The design shown above reflects planning by international partners at the recent MoMAR meeting in Lisbon. Implementation will begin in for seafloor deformation, near vents faunal communities monitoring, vent fluid temperature, and seismicity. In a first stage, sensors will be autonomous or linked acoustically to an ASSEM junction box. The ultimate objective (>2010) is to implement an integrated monitoring infrastructure with real time data satellite transmission (stage 1) followed by cable energy supply and data transmission (stage 2). The objective there is to turn the vent field into a natural laboratory for the study of ultramafic-hosted, iron-rich hydrothermal ecosystems. The experimental design at Rainbow involves instrumented IODP drilling of the hydrothermal stockwerk, as well as extensive site surveys and repeated sampling. Rainbow is an exceptionnal target for the study of ultramafic-hosted ridge hydrothermal systems. This site is characterized by the abundance of iron, an element which plays a major role at all scales in the ecosystem. Strategy : (as last updated at the MoMAR International Workshop of Lisbon in april 2005) Support comparative studies of hydrothermal vents in MoMAR area. Focus on the Rainbow and Lucky Strike vent fields, with IODP instrumented drilling planned at Rainbow and integrated & multiscale long-term monitoring at Lucky Strike. Actions in : IODP proposal submitted. Three cruises have taken place in Two are scheduled for 2006, that will deploy the first elements of the long- term seafloor observatory at Lucky Strike. In addition, three coordinated cruise proposals are currently examined by NSF. Contacts : MoMAR Web Page : Chair of International MoMAR steering group: Dr Javier Escartin Contact for MoMAR Integrated Site for the RIDGE 2000 US Program: Dr Susan Humphris Coordinator of FP6-STREP EXOCET/D: Dr Pierre Marie Sarradin Contacts for the Portuguese MoMAR program: Dr M. Miranda & Dr Ricardo Santos Contact for the French MoMAR program & coordinator of FP6-MCRTN MoMARnet: Dr Mathilde Cannat Rimicaris exoculata: a new type of symbiosis based on iron oxidation The Lucky Strike vent field is located on top of the volcanoe. It comprises more than 40 individual vents, with a remarkable density of faunal communities. It is part of a planned Marine Protected Area within portuguese ZEE. Sketch of proposed Lucky Strike observatory design Lucky Strike is the selected MoMAR site for integrated & multiscale long-term monitoring of ridge hydrothermal processes and ecosystems. Lucky Strike central volcanoe (bathymetry, viewed from SW, east wall of rift valley in background)