Status and Highlights of the Geochemistry Program Several important research findings: Developed techniques that allows in-situ analysis of 67 elements.

Slides:



Advertisements
Similar presentations
Earth Science Chapter 21 Section 3
Advertisements

Mantle composition 1800s meteorites contain similar minerals to terrestrial rocks Hypothesis that meteorites come from asteroid belt and originate from.
Earth’s Spheres & Branches of Earth Science
Soil Carbonates as a Key to the Past Ca +2 + H 2 O + CO 2 = CaCO 3 + 2H + Calcium derived from weathering or atmospheric inputs C in carbonate from soil.
1. Scottish Association for Marine Science, Scottish Marine Institute, Oban, Scotland, UK New developments in seawater trace metal analysis at SAMS: Automated.
Corals as paleoclimatic archives Jens Zinke PROPER June 2004, VU Amsterdam.
GeoSoilEnviroCARS Matt Newville, Steve Sutton, Mark Rivers Applications: XANES EXAFS Techniques: Near-neighbor distances and coordination environment.
Kyger C “Kacey” Lohmann Professor Department of Geological Sciences Sedimentary Geochemistry Changes in Ocean Chemistry over the last billion years of.
Micro fossil in a meteorite ? (R. Hoover 2011). Lecture 7: Geologic History of Life Oldest signatures of life in sedimentary rocks: Microfossils Molecular.
NSF Research Day University of Vermont - June 6, 2008 Directorate for Geosciences Margaret Cavanaugh Deputy Assistant Director.
Marine Geology and Geochemistry Division MGGD folks –14 Oceanography Departmental Graduate Faculty –~10 Research faculty and postdocs –~15 graduate students.
Science of the Physical Universe 30: Life as a Planetary Phenomenon.
The Biogeochemical Sulfur Cycle
Ge/Ay133 When and how did the cores of terrestrial planets form?
Integrated Ecosystem Assessment for the Gulf of Mexico Becky Allee Gulf Coast Services Center.
When and how did the cores of terrestrial planets form?
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Climate Change in Earth’s Polar Regions
Name: Period: Science 6th Grade
Core Course Science A-54: Life as a Planetary Phenomenon.
Sulfur isotopes in the rock record
Chapter 2 frontispiece. The crescent moon as seen through Earth’s thin upper atmosphere E.A. Mathez, 2009, Climate Change: The Science of Global Warming.
Discovering Past Climates
Climate Systems Chapter 15. Clicker Question What is the approximate CO 2 content of the atmosphere? –A % (40 ppm) –B. 0.04% (400 ppm) –C. 0.4%
Mineral Exploration Tel: (07) Fax: (07)
Star Formation. Formation of the First Materials Big-Bang Event   Initial event created the physical forces, atomic particle building blocks, photons,
Global Warming By Jennifer Nucum Chemistry 106 how chemicals have hurt the earth.
GEOS-Chem Chemical Transport Model: Current Status and Future Plans Daniel J. Jacob, GEOS-Chem Model Scientist Harvard University.
Earth Science: CST Review Day #2 CST Released Questions # d, 1e, 1f, 2a, 2c, 2d YM 2010.
1. Overview About Washington University / Planetary Data Systems Geosciences Node Initial and continued interactions in China NASA-CNSA Bilateral (July.
@earthscience92. What is a System? Systems – a group of interacting parts that work to together to do a job or to form a whole. Open Systems Closed Systems.
AQA GCSE Science & Additional Science Chemistry 1 Topic 7 Hodder Education Revision Lessons Changes in the Earth and its atmosphere Click to continue.
Mass spectroscopy – learning objectives Outline the early developments in mass spectrometry. Outline the use of mass spectrometry in the determination.
Mars Geochemistry and Future Experiment Needs Mark A. Bullock August 7, 2002.
Global Warming And the Planetary Water Cycle Ruth Curry Woods Hole Oceanographic Institution Ruth Curry Woods Hole Oceanographic Institution Global Warming.
WATER ON EARTH Alessandro Morbidelli CNRS, Observatoire de la Cote d’Azur, Nice.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 1: An Introduction Don Wuebbles Department of Atmospheric Sciences University of Illinois,
Welcome and Introduction Departmental Research & Education Overview.
Overview Paleoclimate research at Georgia Tech seeks to understand how and why climate has changed in the past. Looking back beyond the instrumental record.
Ocean Response to Global Warming/Global Change William Curry Woods Hole Oceanographic Institution Environmental Defense May 12, 2005 Possible changes in.
What is Climate Change?. Climate change refers to any significant change in the measures of climate lasting for an extended period of time. In other words,
Lydie Dupont Enno Schefuß, Florian Rommerskirchen, Sebastian Hoetzel, Gerlinde Jung, Gesine Mollenhauer Climate and Vegetation Change in South Africa and.
Abundance of the Elements UNIVERSE by atom Abundance of the Elements ATMOSPHERE 78% N 2 and 21% O 2 CRUST OCEAN ATMOSPHERE by mass.
 C/N ratios in the sediment will more closely resemble that of overlying aquatic vegetation  C/N ratios of lake sediments reflect that of aquatic vegetation,
Weather, Climate, and Me Lesson 6 What make the wind?
Nitrous Oxide Focus Group Nitrous Oxide Focus Group launch event Friday February 22 nd, 2008 Dr Jan Kaiser Dr Parvadha Suntharalingam The stratospheric.
Warm Up: Label all the continents and oceans on your maps. South Southern Ocean North What is this body of water? Gulf of Mexico Caribbean Sea.
The Origin of the Earth The Origin of the Earth. Explanations About the Earth’s Origins Throughout history there has been numerous ideas, theories, legends,
Iron Isotopes in Achondrite Meteorites By Elizabeth Dybal Mentor Meenakshi Wadhwa.
Outstanding issues(think, research topics for weeks 3 & 4) the composition of the lower mantle (major elements) proportion of ferro-periclase (0% to 20%)
DAVINCI: Deep Atmosphere Venus Investigation of Noble Gas, Chemistry, and Imaging One out five NASA’s Discovery-class missions for Phase A studies. A 63.
Section Climate Change
Agata Nicolau-Kuklińska Karol Seweryn
John Christie Office of Technology Transfer
Formation and Composition of Earth’s Core Beyond the Current Paradigms
Volatile Element Compositions of Minerals in Meteorites
Who is responsible for global warming: Government or Public?
Isotopes of Hg 196Hg 0.1% 198Hg 10% 199Hg 17% 200Hg 23% 201Hg 13%
Zinc Isotopes Provide Clues to Volatile Loss During Moon Formation
Chapter 9.
What’s the difference between weather and climate?
When and how did the cores of terrestrial planets form?
Zinc Isotopes Provide Clues to Volatile Loss During Moon Formation
Lesson 2 LT: I can use mass number and atomic number to
Paleo Climate Change.
Nathan R. Thorp and Erik A. Hobbie
Cover Slide: (well decorated)
CLIMATE CHANGE.
Presentation transcript:

Status and Highlights of the Geochemistry Program Several important research findings: Developed techniques that allows in-situ analysis of 67 elements in less than 5 minutes. In Journal of Analytical Atomic Spectroscopy Discovery of in-vivo mercury isotope fractionation in fish 1. In Geochemistry, Geophysics, Geosystems. Palladium partition experiments that indicate that there is no need to call on a late veneer of meteorites (after core formation) to explain the high abundances of platinum group elements in the silicate Earth 2. In Nature Geoscience Record of expansion of C4 plants in Central Inner Mongolia shows a shift in the monsoon pattern in Eastern Asia during the Cenozoic 3. In Earth and Planetary Science Letters Determined rates of methane production in boreal and subarctic peatlands and the consequences for methane flux to the atmosphere 4. In Global Biogeochemical Cycles Since Jan 1, 2008 awarded $1.45M NSF (Earth, Ocean and Atmospheric Sciences Divisions), $750k NASA, $1M NOAA,and $150k from EPRI 5. Collaborations with Georgia Tech, University of Miami and Woods Hole Oceanographic Institution. Our main outside users 6 were awarded $2.2M 7 since Jan 1, 2008.

Vision for the Geochemistry Program as of summer 2010, mid-point in current award period Maintain our research profile which includes high-temperature geochemistry and cosmochemistry, aquatic chemistry, and low-T geochemistry and global warming Take advantage of research funding related to the oil spill in he Gulf of Mexico Expansion into biogeochemistry and the interaction of metals with organic matter in the environment 1. Replace inductively coupled plasma mass spectrometer 2. Continue to look at possibilities for natural overlap interests with other parts of the NHMFL. Potential areas are: Mössbauer spectroscopy Micro analytical facility for in-situ analyses of elemental abundances and isotopic compositions 3.

References for Slide 1 Reference list (NHMFL affiliated authors in bold): Humayun, M, Davis, D A and Hirschmann, M M (2010) Major element analysis of natural silicates by laser ablation ICP-MS, J. Anal. At. Spectrom., 25, 998–1005. Das, R, Salters, V J M, Odom, A L (2009) A case for in vivo mass-indeoendent fractionation of mercury isotopes in fish, Geochem, Geophys, Geosys, 10, Q11012 Righter, K, Humayun, M, Danielson, L (2008) Partitioning of palladium at high pressures and temperatures during core formation, Nature Geosciences, 1, Zhang, C, Wang, Y, Deng, T, Wang, X, Biasatti, D, Xu, Y, Li, Q (2009) C4 expansion in the central Inner Mongolia during the latest Miocene and early Pliocene, Earth Plan. Sci. Lett. 287, Chanton, J P, Glaser, P H, Chasar, L S, Burdige, D J, Hines, M E, Siegel, D I, Tremblay, L B and Cooper, W T (2008) Radiocarbon evidence for the importance of surface vegetation on fermentation and methanogenesis in contrasting types of boreal peatlands, Global Biogeochem. Cycles, 22, GB402.