Using SBSE for the study of organic compounds in submarine hydrothermal vents: from the research vessel to the lab

Size: px
Start display at page:

Download "Using SBSE for the study of organic compounds in submarine hydrothermal vents: from the research vessel to the lab"

Transcription

1 Using SBSE for the study of organic compounds in submarine hydrothermal vents: from the research vessel to the lab Cécile Konn, Sophie Chataing LGM, Ifremer, Brest 2 nd SBSE technical meeting, Paris, 11&12 February 2013

2 Ifremer: Institut français de recherche pour l exploitation de la mer (1984) a budget of about 243 millions 5 centers, 25 along the coastline of France and overseas over people, 450 specialities 8 research vessels (4 highseas) 1 submersible and 1 ROV ( m) 2 AUVs (autonomous vehicles) DISCOVERING THE OCEANS WITH IFREMER RESEARCH MONITORING OF COASTAL AND OCEANIC WATERS DEVELOPMENT, MANAGEMENT AND OPEN ACCESS TO LARGE RESEARCH INFRASTRUCTURES 2

3 Laboratory of Geochemistry and Metallogeny? Research interests Hydrothermal exploration Geochemistry and metallogeny of rocks Geochemistry of hydrothermal plumes and fluids Gas hydrates Cold seeps Study areas in all oceans and seas Margins Subduction zones Mid-Ocean Ridges Back arc basins 3

4 Hydrothermal system? Mn, CH 4, He, Fe Humphris and McCollum, Oceanus, 41 (2),

5 Where are hydrothermal vents located? Credits: S. Beaulieu, K. Joyce, and S.A. Soule (WHOI),

6 Hydrothermal plumes / vents search Ifremer / Stephane LESBATS Sampling bottles Sensors 6

7 Hydrothermal plumes / vents search 7

8 Sampling 8

9 Ultramafic-hosted? Underlying rocks = Mantle rocks = peridotites (olivine rich) Seawater / Mantle interaction = alteration of olivine serpentine SERPENTINISATION Mn, CH 4, He, Fe H 2 production reducing conditions Thermodynamically favorable for CO 2 CH 4 Organics Humphris and McCollum, Oceanus, 41 (2),

10 Origin of organic compounds in hydrothermal fluids H O C H H C C H H N H Rocks, minerals, metals, almost all gases, water Inorganic world Living world = organic world OXIDIZED Abiotic synthesis? REDUCED 10

11 Scientific stakes How did life start? Could part of the oil be renewable? Is abiotic synthesis of organic compounds occuring in submarine hydrothermal systems? Are there organic compounds in hydrothermal fluids? Where do they come from? 11

12 C. Konn et al., 2009, Chemical Geology Are there organic compounds in hydrothermal fluids? n Linear, methyl and branched hydrocarbons C9 C19 R1 R2 Cyclohexanes C9 C11 R O OH Fatty acids C9 C18 PolyAromatic Hydrocarbons (PAH) 12

13 C. Konn et al., 2012, Geochemical Transactions Alkanes 13

14 BTEX C. Konn et al., 2012, Geochemical Transactions 14

15 C. Konn et al., 2012, Geochemical Transactions PAHs 15

16 C. Konn et al., 2012, Geochemical Transactions Fatty acids (SW) 16

17 Original protocol: qualitative study 24 µl PDMS 300 rpm 60 min Light 10 ml sample Internal Standards Organic modifier Gas tight vials 17

18 Conclusions and perspectives Use of SBSE Preparation technique to be used on board a research vessel Detection of a wide range of dissolved organic compounds in seafloor hydrothermal fluids Understanding of the geochemical processes controlling the formation and distribution of the compounds Work to continue Quantification Determination of their origin In situ measurements Exploration!!! 18

19 Thank you for your attention 19

Hydrothermal vents from the Azores

Hydrothermal vents from the Azores Hydrothermal vents from the Azores Ana Colaço Center of IMAR from University of Azores Departement of Oceanography and Fisheries 1 Hydrothermal vents are zones of fluid expulsion from the sea floor, normally

More information

Serpentinization, Abiogenic Methane, and Extremophilic Archaea within the Seafloor

Serpentinization, Abiogenic Methane, and Extremophilic Archaea within the Seafloor Serpentinization, Abiogenic Methane, and Extremophilic Archaea within the Seafloor Michael J. Mottl Department of Oceanography NAI Winter School, Jan. 2005 Earth s mantle is 68% of its mass and 83% of

More information

Supplementary Materials

Supplementary Materials Supplementary Materials S1 : Mixing lines used for calculation of the end-member composition of the Fatu Kapa fluids. S2 : Modified after Von Damm et al. (1991). Plot of the molality of dissolved SiO 2

More information

Hydrothermal Vents. "oases. of life." Evolution Physiology Biodiversity. Barbara Zimmermann, Kirstin Claußen, Ulrich Markmann

Hydrothermal Vents. oases. of life. Evolution Physiology Biodiversity. Barbara Zimmermann, Kirstin Claußen, Ulrich Markmann Hydrothermal Vents "oases of life." Evolution Physiology Biodiversity Barbara Zimmermann, Kirstin Claußen, Ulrich Markmann Hydrothermal vents are geysers on the seafloor. They continuously spew super-hot,

More information

Marine Science and Oceanography

Marine Science and Oceanography Marine Science and Oceanography Marine geology- study of the ocean floor Physical oceanography- study of waves, currents, and tides Marine biology study of nature and distribution of marine organisms Chemical

More information

Science Drivers. Spectroscopic Sensors. In Situ Sensors. Development of autonomous and remote platforms

Science Drivers. Spectroscopic Sensors. In Situ Sensors. Development of autonomous and remote platforms Science Drivers In Situ Sensors Spectroscopic Sensors Development of autonomous and remote platforms ROVs, AUVs Cabled observatories Desire to analyze targets with discrete stability regions in the deep

More information

Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor

Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor. Shape of the seafloor Multibeam echo sounders - Research vessel Scripps Institution of Oceanography R/V Roger Revelle depth Source: Scripps Institution of Oceanography http://woodshole.er.usgs.gov/project-pages/caribbean/movie1.html

More information

General Oceanography Geology 105 Expedition 14 Dive & Discover Explorations of the Seafloor See Due Date in Greensheet or in Module Area of Canvas

General Oceanography Geology 105 Expedition 14 Dive & Discover Explorations of the Seafloor See Due Date in Greensheet or in Module Area of Canvas General Oceanography Name Geology 105 Expedition 14 Dive & Discover Explorations of the Seafloor See Due Date in Greensheet or in Module Area of Canvas Expedition Objective: In this expedition, we will

More information

14.2 Ocean Floor Features Mapping the Ocean Floor

14.2 Ocean Floor Features Mapping the Ocean Floor 14.2 Ocean Floor Features Mapping the Ocean Floor The ocean floor regions are the continental margins, the ocean basin floor, and the mid-ocean ridge. 14.2 Ocean Floor Features Continental Margins A continental

More information

Metamorphic Environments. Contact (or thermal) Hydrothermal Burial Regional Shock (impact) Fault Zone

Metamorphic Environments. Contact (or thermal) Hydrothermal Burial Regional Shock (impact) Fault Zone Metamorphic Environments Contact (or thermal) Hydrothermal Burial Regional Shock (impact) Fault Zone Contact Metamorphism Contact or thermal metamorphism occurs when an intrusive magma heats the surrounding

More information

4. In areas where tectonic plates collide, the seafloor has deep. 5. In areas where tectonic plates separate, the seafloor has mid- ocean

4. In areas where tectonic plates collide, the seafloor has deep. 5. In areas where tectonic plates separate, the seafloor has mid- ocean Name Date Hour Table Chapter 14 Lesson One- General Directions: Use the word bank below to complete each statement. NOT all terms are used. abyssal plains brackish water condensation energy freshwater

More information

Deep-Sea and Sub-Seafloor Resources: A Polymetallic Sulphide and Co-Mn Crust Perspective. Stephen Roberts

Deep-Sea and Sub-Seafloor Resources: A Polymetallic Sulphide and Co-Mn Crust Perspective. Stephen Roberts Deep-Sea and Sub-Seafloor Resources: A Polymetallic Sulphide and Co-Mn Crust Perspective by Stephen Roberts The LRET Research Collegium Southampton, 16 July 7 September 2012 1 Deep-Sea and Sub-Seafloor

More information

Magma Formation and Behavior

Magma Formation and Behavior Magma Formation and Behavior Introduction: The study of body waves as they pass through Earth's interior provides strong evidence that the Earth's mantle is composed almost entirely of solid ultramafic

More information

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE!

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! WHAT PROMINENT FEATURE CAN YOU IDENTIFY IN THIS PICTURE? What do you think the different colors represent? Who might find such a picture

More information

(my) Current understanding of plate divergence processes at mid-oceanic ridges (in 24 slides)

(my) Current understanding of plate divergence processes at mid-oceanic ridges (in 24 slides) (my) Current understanding of plate divergence processes at mid-oceanic ridges (in 24 slides) q 1962-2018 mid-ocean ridge processes (magmatism, tectonics, hydrothermalism) : discoveries, evolving concepts,

More information

Prospects and Status of Exploration for Polymetallic Sulphides. Georgy Cherkashov VNIIOkeangeologia St.Petersburg, RUSSIA

Prospects and Status of Exploration for Polymetallic Sulphides. Georgy Cherkashov VNIIOkeangeologia St.Petersburg, RUSSIA Prospects and Status of Exploration for Polymetallic Sulphides Georgy Cherkashov VNIIOkeangeologia St.Petersburg, RUSSIA Introduction Outline Hydrothermal processes and seafloor massive sulfides (SMS):

More information

Magma Formation and Behavior

Magma Formation and Behavior Magma Formation and Behavior Questions What causes mantle rock to melt, resulting in magma formation? Why is magma formation restricted to specific plate tectonic settings? Why are mafic (basaltic) magmas

More information

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR Earth / Environmental Science Ch. 14 THE OCEAN FLOOR The Blue Planet Nearly 70% of the Earth s surface is covered by the global ocean It was not until the 1800s that the ocean became an important focus

More information

Fluid-Rock Interactions and the Sub-Seafloor Biosphere

Fluid-Rock Interactions and the Sub-Seafloor Biosphere Fluid-Rock Interactions and the Sub-Seafloor Biosphere BACKGROUND DATA Examples of Key Scientific Questions (OOI Science Plan) Scientific Priorities (San Juan Meeting) Example ORION Experiments (San Juan

More information

Lecture 13. Hydrothermal Circulation

Lecture 13. Hydrothermal Circulation Lecture 13. Hydrothermal Circulation The discovery of hot springs on the ocean floor during the 1970s was one of the most exciting events in the history of oceanography. Although hydrothermal activity

More information

UNIT SIX: Earth s Structure. Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes

UNIT SIX: Earth s Structure. Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes UNIT SIX: Earth s Structure Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes Chapter Twenty: Earthquakes and Volcanoes 20.1 Earthquakes 20.2 Volcanoes

More information

Destabilization of Carbon Dioxide Hydrates in the Ocean. Resherle Verna Department of Earth Science, University of Southern California

Destabilization of Carbon Dioxide Hydrates in the Ocean. Resherle Verna Department of Earth Science, University of Southern California Verna 1 Destabilization of Carbon Dioxide Hydrates in the Ocean Resherle Verna Department of Earth Science, University of Southern California I. ABSTRACT This paper features the investigation of the change

More information

Suzanne Picazo, Mathilde Cannat, Adelie Delacour, Javier Escartın, Stephane Roumejon, and Serguei Silantyev

Suzanne Picazo, Mathilde Cannat, Adelie Delacour, Javier Escartın, Stephane Roumejon, and Serguei Silantyev Correction Volume 14, Number 8 16 August 2013 doi: ISSN: 1525-2027 Correction to Deformation associated with the denudation of mantle-derived rocks at the Mid- Atlantic Ridge 13 15 N: The role of magmatic

More information

Diving along the mid-ocean ridge at 21 N on. How to Build a Black Smoker Chimney. The Formation of Mineral Deposits At Mid-Ocean Ridges

Diving along the mid-ocean ridge at 21 N on. How to Build a Black Smoker Chimney. The Formation of Mineral Deposits At Mid-Ocean Ridges How to Build a Black Smoker Chimney Alvin s manipulator reaches toward a black smoker chimney, seen through the sub s viewport, at 17 S on the East Pacific Rise. Hot hydrothermal fluids surge through the

More information

IMPORTANT FACTS HYDROTHERMAL VENTS OCCUR WHERE HIGH TEMPERATURE WATER IS COMING INTO THE OCEANS. First discovered in 1977 by Bob Ballard.

IMPORTANT FACTS HYDROTHERMAL VENTS OCCUR WHERE HIGH TEMPERATURE WATER IS COMING INTO THE OCEANS. First discovered in 1977 by Bob Ballard. HYDROTHERMAL VENTS IMPORTANT FACTS HYDROTHERMAL VENTS OCCUR WHERE HIGH TEMPERATURE WATER IS COMING INTO THE OCEANS. First discovered in 1977 by Bob Ballard. HOW THEY WORK * COLD OVERLYING SEAWATER PENETRATES

More information

Olivine Aqueous Alteration Under Low T Conditions in the Presence of Ammonia A Case for Ocean Moons

Olivine Aqueous Alteration Under Low T Conditions in the Presence of Ammonia A Case for Ocean Moons Olivine Aqueous Alteration Under Low T Conditions in the Presence of Ammonia A Case for Ocean Moons Objectives Understand the alteration processes at work under Low T/P and their dynamics when subjected

More information

NOAA and the National Deep Submergence Facility DEep Submergence Science Committee Meeting NOAA 2006 Report

NOAA and the National Deep Submergence Facility DEep Submergence Science Committee Meeting NOAA 2006 Report NOAA and the National Deep Submergence Facility DEep Submergence Science Committee Meeting NOAA 2006 Report November 9, 2006 Seattle, WA Image courtesy of the MTS 04 science team, IFE, URI/IAO NOAA and

More information

Metals in geothermal fluids and metal precipitations in surface pipelines in Iceland can these been utilized?

Metals in geothermal fluids and metal precipitations in surface pipelines in Iceland can these been utilized? Metals in geothermal fluids and metal precipitations in surface pipelines in Iceland can these been utilized? Dr. Vigdís Hardardóttir, Iceland GeoSurvey - ÍSOR Msc. NordMin course Iceland Nov. 2016 Black

More information

Image courtesy Lau ISS Scientists. Donna Blackman, current chair of the R2K Steering Committee Scripps Institution of Oceanography

Image courtesy Lau ISS Scientists. Donna Blackman, current chair of the R2K Steering Committee Scripps Institution of Oceanography Image courtesy Lau ISS Scientists Donna Blackman, current chair of the R2K Steering Committee Scripps Institution of Oceanography 1 meter Endeavour hydrothermal vent chimneys, Juan de Fuca Ridge An integrated,

More information

Hydrothermal Vent Challenge

Hydrothermal Vent Challenge 2004 Ring of Fire Expedition Hydrothermal Vent Challenge FOCUS Chemistry of hydrothermal vents GRADE LEVEL 9-12 (Chemistry) FOCUS QUESTION What are common features of hydrothermal vent fluids, and how

More information

Earthquakes. Earthquakes are caused by a sudden release of energy

Earthquakes. Earthquakes are caused by a sudden release of energy Earthquakes Earthquakes are caused by a sudden release of energy The amount of energy released determines the magnitude of the earthquake Seismic waves carry the energy away from its origin Fig. 18.1 Origin

More information

John Breier. CURRICULUM VITAE 28 August 2007 ADDRESS AND TELEPHONE

John Breier. CURRICULUM VITAE 28 August 2007 ADDRESS AND TELEPHONE CURRICULUM VITAE 28 August 2007 John Breier ADDRESS AND TELEPHONE Woods Hole Oceanographic Institution Applied Ocean Physics & Engineering 266 Woods Hole Road Blake Building, Room 200 Woods Hole, MA, 02543

More information

DESSC Meeting December Jason Science User Reports

DESSC Meeting December Jason Science User Reports DESSC Meeting December 2008 Jason Science User Reports MAR 08 KNOX18RR 07/9-08/13 R/V Roger Revelle, ROV Jason II Rainbow, Lucky Strike, Lost city, TAG Reysenbach: Diversity and Distribution of Thermoacidophiles

More information

Lecture 6 - Determinants of Seawater Composition. Sets up electric dipole because O is more electronegative A o. Figure 3.

Lecture 6 - Determinants of Seawater Composition. Sets up electric dipole because O is more electronegative A o. Figure 3. 12.742 - Marine Chemistry Fall 2004 Lecture 6 - Determinants of Seawater Composition Prof. Scott Doney What is seawater? Water Dissolved inorganic salts (major ions) Trace species, organics, colloids,

More information

6th Grade Science Sample Assessment Items S6E3c.

6th Grade Science Sample Assessment Items S6E3c. Composition 6th Grade Science Sample Assessment Items Ocean water differs from freshwater in that it has. A. a lower temperature B. a higher temperature C. a higher concentration of silicon dioxide D.

More information

Alkaline Seafloor Hydrothermal Systems: Experimental Simulation of CO 2 -Peridotite-Seawater Reactions

Alkaline Seafloor Hydrothermal Systems: Experimental Simulation of CO 2 -Peridotite-Seawater Reactions Alkaline Seafloor Hydrothermal Systems: Experimental Simulation of CO 2 -Peridotite-Seawater Reactions Thomas M. Carpenter John P. Kaszuba Melissa Fittipaldo Michael Rearick Los Alamos National Laboratory

More information

Promoting Seafloor Observation in China -- A Meeting Report

Promoting Seafloor Observation in China -- A Meeting Report Promoting Seafloor Observation in -- A Meeting Report Introduction With its rapid development in economy, is now placing more emphasis on marine science and technology. Recently, construction of a sea-floor

More information

Table of Contents. Introduction 4. Chapter 1 Research and the Deep Oceans 6. Chapter 2 Physical Characteristics of the Ocean 10

Table of Contents. Introduction 4. Chapter 1 Research and the Deep Oceans 6. Chapter 2 Physical Characteristics of the Ocean 10 Table of Contents Introduction 4 Chapter 1 Research and the Deep Oceans 6 Chapter 2 Physical Characteristics of the Ocean 10 Chapter 3 Composition of the Oceans Waters 16 Chapter 4 Tides, Waves, and Currents

More information

Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p.

Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p. Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p. 2 Mid-Ocean Ridge Province p. 3 Benthic and Pelagic Provinces

More information

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor Earth s Continents and Seafloors GEOL100 Physical Geology Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types of crust Dense, thin,

More information

Cecile Konn 1,2*, Jean-Luc Charlou 1, Jean-Pierre Donval 1 and Nils G Holm 2

Cecile Konn 1,2*, Jean-Luc Charlou 1, Jean-Pierre Donval 1 and Nils G Holm 2 Konn et al. Geochemical Transactions 212, 13:8 RESEARCH ARTICLE Open Access Characterisation of dissolved organic compounds in hydrothermal fluids by stir bar sorptive extraction - gas chomatography -

More information

OIMB GK12 CURRICULUM HYDROTHERMAL VENT FORMATION

OIMB GK12 CURRICULUM HYDROTHERMAL VENT FORMATION 5 th Grade 60 minutes HYDROTHERMAL VENT FORMATION Adapted from For Sea Oregon Science Content Standards: 5.2 Interaction and Change: Force, energy, matter, and organisms interact within living and nonliving

More information

GLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition

GLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition Grotzinger Jordan Understanding Earth Sixth Edition Chapter 4: IGNEOUS ROCKS Solids from Melts 2011 by W. H. Freeman and Company Chapter 4: Igneous Rocks: Solids from Melts 1 About Igneous Rocks Igneous

More information

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Oceans: The Last Frontier Foundations, 6e - Chapter 9 Stan Hatfield Southwestern Illinois College The vast world ocean Earth is often referred

More information

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:-

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- SEA-FLOOR SPREADING In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- Detailed bathymetric (depth) studies showed that there was an extensive submarine

More information

Chapter 20. Plate Tectonics

Chapter 20. Plate Tectonics Chapter 20 Plate Tectonics Early Evidence (Wegener) The geometric fit of the continents. The similarity in rock age groups between adjoining regions. The similarity in Paleozoic fossils between adjoining

More information

MAR110 Lecture #4 Fundamentals of Plate Tectonics

MAR110 Lecture #4 Fundamentals of Plate Tectonics 1 MAR110 Lecture #4 Fundamentals of Plate Tectonics The Ocean Sea Floor is formed Along the Mid-Ocean Ridge Spreading Centers The Ocean Sea Floor is destroyed in the Subduction Zones Figure 4.2 Convection

More information

5. Convergent boundaries produce a relatively low number of earthquakes compared to other boundaries. a. True

5. Convergent boundaries produce a relatively low number of earthquakes compared to other boundaries. a. True 1. Earth s crust is thinner than its mantle. ANSWER: True 2. The concept of isostacy states that high-density rock will stand higher than low-density rock, which explains the formation of subduction zones.

More information

Most mafic magmas come from the upper mantle and lower crust. This handout will address five questions:

Most mafic magmas come from the upper mantle and lower crust. This handout will address five questions: Geology 101 Origin of Magma From our discussions of the structure of the interior of the Earth, it is clear that the upper parts of the Earth (crust and mantle) are mostly solid because s-waves penetrate

More information

The Sea Floor. Chapter 2

The Sea Floor. Chapter 2 The Sea Floor Chapter 2 Geography of the Ocean Basins World ocean is the predominant feature on the Earth in total area Northern Hemisphere = 61% of the total area is ocean. Southern Hemisphere = about

More information

You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science:

You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science: Ocean History You should be able to identify a few of the key cultures, individuals and expeditions in the history of marine science: Phoenicians Arabs Micronesians Polynesians Aristotle Erikson Columbus

More information

Thermal-Mechanical Behavior of Oceanic Transform Faults

Thermal-Mechanical Behavior of Oceanic Transform Faults Presented at the COMSOL Conference 2008 Boston Thermal-Mechanical Behavior of Oceanic Transform Faults COMSOL Conference - Boston, Massachusetts October 2008 Emily C. Roland - MIT/WHOI Joint Program Mark

More information

Chapter 12 Lecture. Earth: An Introduction to Physical Geology. Eleventh Edition. Earth s Interior. Tarbuck and Lutgens Pearson Education, Inc.

Chapter 12 Lecture. Earth: An Introduction to Physical Geology. Eleventh Edition. Earth s Interior. Tarbuck and Lutgens Pearson Education, Inc. Chapter 12 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Earth s Interior Tarbuck and Lutgens Earth s Internal Structure Earth s interior can be divided into three major layers defined

More information

MAR110 Lecture #3 Ocean Bathymetry / Plate Tectonics

MAR110 Lecture #3 Ocean Bathymetry / Plate Tectonics 1 MAR110 Lecture #3 Ocean Bathymetry / Plate Tectonics Ocean Basin Geographic Zones The geographic zones of the North Atlantic are identified in the bird s eye view of the sea floor above. Below is shown

More information

high and ultrahigh pressures.

high and ultrahigh pressures. Stability of hydrous phases in serpentinites to high and ultrahigh pressures. Study of fluid and multiphase solid inclusions in high, very high pressure rocks and metamorphic veins The crust to mantle

More information

Origin and Evolution of the Ocean Floor

Origin and Evolution of the Ocean Floor Origin and Evolution of the Ocean Floor Outline Mapping the Ocean Floor Continental Margins Origin of Oceanic Lithosphere Structure of Ocean Crust Mapping the ocean floor Depth originally measured by lowering

More information

Early Career Scientists/Student Introduction. Part II

Early Career Scientists/Student Introduction. Part II Early Career Scientists/Student Introduction Part II Jeffrey Marlow // 4 th year (already?) grad student // Caltech Anaerobic Methane Oxidation Endolithic Activity & Community Diversity Methane Seep Proteomics

More information

JMRS11 Jan Mayen Ridge Sampling Survey 2011

JMRS11 Jan Mayen Ridge Sampling Survey 2011 JMRS11 Jan Mayen Ridge Sampling Survey 2011 JMRS11 Report Presentation VBPR/TGS, February 2012 Confidentiality Screen dumps and the underlying data in this document are confidential and proprietary to

More information

GEOLOGY MEDIA SUITE Chapter 12

GEOLOGY MEDIA SUITE Chapter 12 UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 12 Volcanoes 2010 W.H. Freeman and Company Plate tectonics explains the global pattern of volcanism. Key Figure 12.20 (page

More information

7. Deep Sea Reducing Habitats. Deep-Sea Reducing Habitats

7. Deep Sea Reducing Habitats. Deep-Sea Reducing Habitats 7. Deep Sea Reducing Habitats History of Deep Sea Exploration Discovery of hydrothermal vents Hydrothermal Vents Living in reducing environments Chemosynthesis Life history strategies Other Reducing Habitats

More information

READING QUESTIONS: Chapter 11, Plate Tectonics GEOL 131 Fall pts

READING QUESTIONS: Chapter 11, Plate Tectonics GEOL 131 Fall pts READING QUESTIONS: Chapter 11, Plate Tectonics GEOL 131 Fall 2018 61 pts NAME DUE: Tuesday, November 20 Continental Drift: An Idea Before Its Time (p. 317-321) 1. Fill in the blanks in this sentence from

More information

Chapter 9 Lecture Outline. Oceans: The Last Frontier

Chapter 9 Lecture Outline. Oceans: The Last Frontier Chapter 9 Lecture Outline Oceans: The Last Frontier The Vast World Ocean Earth is referred to as the blue planet 71% of Earth s surface is oceans and marginal seas Continents and islands comprise the remaining

More information

GD3.3/GM3.3/GMPV16/TS4.7

GD3.3/GM3.3/GMPV16/TS4.7 GD Geodynamics Orals and PICOs MO1, 08:30 10:00 MO2, 10:30 12:00 MO3, 13:30 15:00 MO4, 15:30 17:00 TU1, 08:30 10:00 TU2, 10:30 12:00 TU3, 13:30 15:00 Monday, 08 April Medal Lecture) (co-organized), 08:30

More information

PHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION)

PHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION) Chapter 2: Plate Tectonics Chapter Summary: Plate tectonics is a theory that suggests Earth's surface is divided into several large plates that change position and size. Intense geologic activity occurs

More information

Controlled-source electromagnetic imaging of the Middle America Trench o"shore Nicaragua

Controlled-source electromagnetic imaging of the Middle America Trench oshore Nicaragua Controlled-source electromagnetic imaging of the Middle America Trench o"shore Nicaragua Kerry Key Scripps Institution of Oceanography Collaborators: Samer Naif (SIO, now LDEO), Steven Constable (SIO),

More information

Biodiversity of Hydrothermal Vents at Brothers Volcano

Biodiversity of Hydrothermal Vents at Brothers Volcano Biodiversity of Hydrothermal Vents at Brothers Volcano Background One measure of biodiversity of an ecosystem is the species diversity, which is a combination of both species richness and species evenness.

More information

Chapter 2: Plate Tectonics: A Unifying Theory

Chapter 2: Plate Tectonics: A Unifying Theory Chapter 2: Plate Tectonics: A Unifying Theory Chapter Outline 2.1 Introduction 2.2 Early Ideas About Continental Drift 2.3 What Is the Evidence for Continental Drift? 2.4 Features of the Seafloor 2.5 Earth

More information

Lecture Outlines PowerPoint. Chapter 13 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 13 Earth Science 11e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 13 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

More information

Web Supplement

Web Supplement Web Supplement 19.4.6 Economic Deposits including Ores Some of the mounds of metalliferous sediment contain enough metals in high concentrations to be of economic interest. For example, the TAG (Trans-Atlantic

More information

Lecture 4 What Controls the Composition of Seawater

Lecture 4 What Controls the Composition of Seawater Lecture 4 What Controls the Composition of Seawater Seawater is salty! Why? What controls the composition of seawater? Do Chemical Equilibrium reactions control the composition of the Ocean? What is meant

More information

Marine Geosciences / Oceanography Fields and disciplines

Marine Geosciences / Oceanography Fields and disciplines Marine Geosciences / Oceanography Fields and disciplines Marine Geosciences; Oceanography Chemical Oceanography Marine chemistry; marine geochemistry Biological Oceanography Marine biology; marine biogeochemistry

More information

Yev Kontar. Illinois State Geological Survey, University of Illinois at Urbana-Champaign

Yev Kontar. Illinois State Geological Survey, University of Illinois at Urbana-Champaign Addressing Caribbean Geophysical Hazards through the Continuously Operating Caribbean GPS Observational Network (COCONet) and International Ocean Drilling Program (IODP) Yev Kontar Illinois State Geological

More information

LAB 6: TRINIDAD BEACH FIELD TRIP

LAB 6: TRINIDAD BEACH FIELD TRIP OBJECTIVES: LAB 6: TRINIDAD BEACH FIELD TRIP 1) to develop your powers of observation, especially of geological phenomena; 2) to identify the rocks exposed at Trinidad Beach; 3) to reconstruct some of

More information

Mesosaurus. Fresh water reptile Permian Period million years ago South America, Africa Approximately 16 inches long

Mesosaurus. Fresh water reptile Permian Period million years ago South America, Africa Approximately 16 inches long Explorers Alfred Wegener Mesosaurus Fresh water reptile Permian Period 286-245 million years ago South America, Africa Approximately 16 inches long Glossopteris Plant fossil Permian Period 286-245 million

More information

TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April

TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April MO1, 08:30 10:00 MO2, 10:30 12:00 MOL, 12:15 13:15 MO3, 13:30 15:00 MO4, 15:30 17:00 GD3.3/GM3.3/GMPV16/TS4.7, The evolution of plate

More information

Non-living Resources of the OCS. Harald Brekke NPD

Non-living Resources of the OCS. Harald Brekke NPD Non-living Resources of the OCS Harald Brekke NPD The Continental Shelf and the Area http://www.grida.no/publications/shelf-last-zone/ Outer Continental Shelf Example http://www.grida.no/publications/shelf-last-zone/

More information

Appendix 10: Non-Potential of Natural Gas Hydrate Occurrence in Queen Charlotte Basin8

Appendix 10: Non-Potential of Natural Gas Hydrate Occurrence in Queen Charlotte Basin8 British Columbia Offshore Hydrocarbon Development Appendix 10: Non-Potential of Natural Gas Hydrate Occurrence in Queen Charlotte Basin8 Natural gases such as methane, ethane, propane typically occur as

More information

Ch 9.1 Notes. Objective: Be able to explain the theory of plate tectonics and be able to explain evidence that supports it.

Ch 9.1 Notes. Objective: Be able to explain the theory of plate tectonics and be able to explain evidence that supports it. Ch 9.1 Notes Objective: Be able to explain the theory of plate tectonics and be able to explain evidence that supports it. Pangaea Alfred Wegener proposed that land on Earth formed a single, huge landmass.

More information

Lecture 26: Marine Geology Read: Chapter 21 Homework due December 3

Lecture 26: Marine Geology Read: Chapter 21 Homework due December 3 Learning Objectives (LO) Lecture 26: Marine Geology Read: Chapter 21 Homework due December 3 What we ll learn today:! 1. Describe the world s five oceans! 2. Understand patterns of ocean circulation! 3.

More information

Earth as a planet: Interior and Surface layers

Earth as a planet: Interior and Surface layers Earth as a planet: Interior and Surface layers Bibliographic material: Langmuir & Broecker (2012) How to build a habitable planet Internal structure of the Earth: Observational techniques Seismology Analysis

More information

The Ocean Floor Earth Science, 13e Chapter 13

The Ocean Floor Earth Science, 13e Chapter 13 The Ocean Floor Earth Science, 13e Chapter 13 Stanley C. Hatfield Southwestern Illinois College The vast world ocean Earth is often referred to as the blue planet Seventy-one percent of Earth s surface

More information

RV Tethys II 20 campaigns to the DYFAMED site from July 2007 to May 2009

RV Tethys II 20 campaigns to the DYFAMED site from July 2007 to May 2009 DYCOMED Dynamics of chemical contaminants in the Mediterranean Sea: An integrated investigation from the atmosphere to the sea bed Lars-Eric Heimbürger 1,2 Scientific supervisors: Daniel Cossa 1 and Christophe

More information

PLATE TECTONIC PROCESSES

PLATE TECTONIC PROCESSES Lab 9 Name Sec PLATE TECTONIC PROCESSES 1. Fill in the blank spaces on the chart with the correct answers. Refer to figures 2.3, 2.4 p.33 (2.2 and 2.3 on p. 23) as needed. 2. With your knowledge of different

More information

Ocean Basins, Bathymetry and Sea Levels

Ocean Basins, Bathymetry and Sea Levels Ocean Basins, Bathymetry and Sea Levels Chapter 4 Please read chapter 5: sediments for next class and start chapter 6 on seawater for Thursday Basic concepts in Chapter 4 Bathymetry the measurement of

More information

Earth s Seafloors. Ocean Basins and Continental Margins. Introductory Oceanography Ray Rector - Instructor

Earth s Seafloors. Ocean Basins and Continental Margins. Introductory Oceanography Ray Rector - Instructor Earth s Seafloors Ocean Basins and Continental Margins Introductory Oceanography Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types

More information

Are seafloor hydrothermal sulphides deposits valuable mineral resources? Bramley J Murton

Are seafloor hydrothermal sulphides deposits valuable mineral resources? Bramley J Murton Are seafloor hydrothermal sulphides deposits valuable mineral resources? Bramley J Murton Outline Why do we need new sources of metals? What are seafloor mineral deposits Where do they occur and why: Why

More information

Backarc basin Spreading axis* Magmatic front. Convecting asthenosphere. Distance from trench (km)

Backarc basin Spreading axis* Magmatic front. Convecting asthenosphere. Distance from trench (km) Backarc basin preading axis M agmatic arc Magmatic front basin Accretionary prism Outer trench high Depth (km) 0 50 00 50 400 Arc crust Lithospheric mantle Indicates feature that may or may not be present

More information

Geology 1 st Semester Exam YSBAT

Geology 1 st Semester Exam YSBAT 1. What is the role of a geologist? Geology 1 st Semester Exam YSBAT 2016-2017 2. Earth is subdivided into three main layers based on what? 3. What features do you find at divergent boundaries? 4. Rock

More information

Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics

Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics clementaged.weebly.com Name: ODD Period: Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics Monday Tuesday Wednesday Thursday Friday 7 No School 8 E 9 O *Vocabulary *Frayer Vocab *Continental Drift Notes

More information

Plate Tectonics. A. Continental Drift Theory 1. Early development 2. Alfred Wegener s mechanism

Plate Tectonics. A. Continental Drift Theory 1. Early development 2. Alfred Wegener s mechanism Plate Tectonics A. Continental Drift Theory 1. Early development 2. Alfred Wegener s mechanism B. Seafloor Spreading 1. Earthquakes and volcanoes 2. Seafloor maps and dates 3. Continental drift revisited

More information

1 Volcanoes and Plate Tectonics

1 Volcanoes and Plate Tectonics CHAPTER 13 SECTION Volcanoes 1 Volcanoes and Plate Tectonics KEY IDEAS As you read this section, keep these questions in mind: What three conditions can cause magma to form? What is volcanism? What are

More information

CO 2 -water-rock reactivity at hydrothermal temperatures: The BigRig2 experiment

CO 2 -water-rock reactivity at hydrothermal temperatures: The BigRig2 experiment CO 2 -water-rock reactivity at hydrothermal temperatures: The BigRig2 experiment C.A. ROCHELLE 1 *, K. BATEMAN 1, A. LACINSKA 1, D. WAGNER 1, J. LIONS 2 AND I. GAUS 2 1 British Geological Survey, Keyworth,

More information

Geol. 656 Isotope Geochemistry

Geol. 656 Isotope Geochemistry HYDROTHERMAL ACTIVITY, METAMORPHISM, AND ORE DEPOSITS II SULFUR ISOTOPE FRACTIONATION IN LOW-TEMPERATURE SYSTEMS 2 - At temperatures below about 400 C, sulfate (SO 4 ) species becomes the dominant form

More information

Lecture Marine Provinces

Lecture Marine Provinces Lecture Marine Provinces Measuring bathymetry Ocean depths and topography of ocean floor Sounding Rope/wire with heavy weight Known as lead lining Echo sounding Reflection of sound signals 1925 German

More information

OCEANOGRAPHY CURRICULUM. Unit 1: Introduction to Oceanography

OCEANOGRAPHY CURRICULUM. Unit 1: Introduction to Oceanography Chariho Regional School District - Science Curriculum September, 2016 OCEANOGRAPHY CURRICULUM Unit 1: Introduction to Oceanography OVERVIEW Summary In this unit students will be introduced to the field

More information

1/27/2011 C H A P T E R 4 P L A T E T E C T O N I C S. Plate Tectonics. Highest pt=mt Everest, ft, 8848 m. Lowest pt. Marianas trench, -11,000 m

1/27/2011 C H A P T E R 4 P L A T E T E C T O N I C S. Plate Tectonics. Highest pt=mt Everest, ft, 8848 m. Lowest pt. Marianas trench, -11,000 m C H A P T E R 4 P L A T E T E C T O N I C S Highest pt=mt Everest, 29029 ft, 8848 m Lowest pt. Marianas trench, -11,000 m Plate Tectonics A Revolution in Geology The Plate Tectonic Model 1 A Revolution

More information

Chapter 1: Introduction...1 Chapter 2: Energy, Entropy and Fundamental Thermodynamic Concepts...24

Chapter 1: Introduction...1 Chapter 2: Energy, Entropy and Fundamental Thermodynamic Concepts...24 Table of Contents Part I: The Geochemical Toolbox Chapter 1: Introduction...1 Geochemistry...1 This Book...2 The Philosophy of Science...4 Building Scientific Understanding...4 The Scientist as Skeptic...5

More information

Part A GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES. Name

Part A GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES. Name GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES Name Part A 1. The rough, jumbled blocky or jagged surface of a lava flow is called a. pahoehoe b. lahar c. aa d. phreatic 2. The Cascade volcanoes like Mt. St.

More information

Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth - Chapter 13 Stan Hatfield Southwestern Illinois College

Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth - Chapter 13 Stan Hatfield Southwestern Illinois College Divergent Boundaries: Origin and Evolution of the Ocean Floor Earth - Chapter 13 Stan Hatfield Southwestern Illinois College Mapping the Ocean Floor Depth was originally measured by lowering weighted lines

More information

Hydrothermal Chemistry/ Reverse Weathering. Marine Chemistry Seminar

Hydrothermal Chemistry/ Reverse Weathering. Marine Chemistry Seminar Hydrothermal Chemistry/ Reverse Weathering Marine Chemistry Seminar 1974 Drever, The Sea Chapter 10:The Magnesium Problem 1979 Edmonds et al., Ridge Crest Hydrothermal Activity and the Balances of Major

More information