Geochemistry and Cosmochemistry Group
✦ Cameca 6F ion microprobe of the Geochemistry/Cosmochemistry Group, DTM. (photo: Steve Shirey)
DTM's Geochemistry/Cosmochemistry Group
“The DTM Geochemistry and Cosmochemistry Group —united by their ability to exploit sophisticated analytical instruments— is expert in the discovery and characterization of presolar grains; the chemistry and chronology of early solar system material, including meteorites, interplanetary dusk particles (IDPs), and samples from cometary and planetary bodies; chemical processing on Earth associated with early global differentiation, continent formation, and subduction; and dynamical mixing in the Earth's mantle revealed by products of mantle melting.” (Former Director, Sean Solomon, describing the G/CG to Carnegie trustees)
The Geochemistry/Cosmochemistry Group has four current staff members, Conel Alexander, Larry Nittler, Anat Shahar, and Steven Shirey and two emeritus staff members, Rick Carlson and Fouad Tera. Our group recently lost long-time staff member Erik Hauri. With the support of chemistry lab manager, Michelle Jordan, mass spectrometer lab manager, Tim Mock, and ion probe specialist, Jianhua Wang, research projects involving the staff can range from a short, informal nature to those that are long term. Research collaborations are welcome on almost any professional level: as an intern, a pre-doctoral fellow, a post-doctoral fellow, a visiting scientist, or a Tuve Fellow. Many projects are NSF or NASA funded, but with the Carnegie Institution’s high level of ongoing lab support, important scientific questions can be attacked without the proposal lead-time that NSF or NASA funding requires. The most fruitful collaborations are those that align with the interests of the staff and the type of analyses suited to our facilities (see below).
The scientific environment at DTM is stimulating and the Washington area is the best in the world as a supportive environment for science. The Washington area hosts a remarkable collection of institutions and laboratories with which joint research projects often can be carried out: Geophysical Lab, Goddard Space Flight Center, National Institute of Standards and Technology, Naval Research Laboratory, Smithsonian Institution, US Geological Survey, and University of Maryland. Many have ongoing programs in Earth and Planetary Science. Interested in the possibilities? Please contact any one of the staff directly and/or see Academic Opportunities page.
Available Analytical Facilities
Thermal ionization mass spectrometer: Thermo-Fisher Triton
Inductively-coupled plasma mass spectrometer: Nu Plasma HR, Nu Plasma II, Thermo iCap Qc
Secondary ion mass spectrometer: NanoSIMS 50L, Cameca IMS 6f
Scanning electron microscope: JOEL SX-6500,
Available with Geophysical Lab: JOEL Field Emission EPMA, Zeiss Auriga SEM, FEI plasma FIB, WiTec confocal Raman
Chemistry labs: Multiple clean-room facility equipped for all aspects of sample preparation
Supporting labs: Optical microscopy lab, microsampling, rock room, machine shop, electronics lab
A Tradition of Groundbreaking Research
As of March 2019, the 5-person Geochemistry and Cosmochemistry Group staff had authored some 60 separate, independent papers in Science and Nature –highly cited journals known for publishing groundbreaking research. This accomplishment highlights the intellectual vitality of our group and indeed the whole Carnegie Institution model for carrying out scientific research. A list of these papers with links to their PDF's can be seen below.
Tot (w/ no dups)
Nature (17)
Science (43)
Alexander
2
10
Carlson
8
11
Hauri
5
7
Nittler
1
16
Shirey
6
10
Geochemistry/Cosmochemistry Group Papers in Science and Nature
Alexander, C. M. O’D., A. P. Boss, and R. W. Carlson, Cosmochemistry - The early evolution of the inner solar system: a meteoritic perspective, Science 293 (no. 5527), 64-68, 2001. http://dx.doi.org/10.1126/science.105287
Alexander, C. M. O'D., R. Bowden, M. L. Fogel, K. T. Howard, C. D. K. Herd, L. R. Nittler, The Provenances of Asteroids, and Their Contributions to the Volatile Inventories of the Terrestrial Planets. Science 337, 721- 723 (2012)
Alexander, C. M. O’D., J. N. Grossman, D. S. Ebel, and F. J. Ciesla, The formation conditions of chondrules and chondrites, Science 320 (no. 5883), 1617-1619, 2008. http://dx.doi.org/10.1126/science.1156561
Blewett, D. T., N. L. Chabot, B. W. Denevi, C. M. Ernst, J. W. Head, N. R. Izenberg, S. L. Murchie, S. C. Solomon, L. R. Nittler, T. J. McCoy, Z. Y. Xiao, D. M. H. Baker, C. I. Fassett, S. E. Braden, J. Oberst, F. Scholten, F. Preusker, and D. M. Hurwitz, Hollows on Mercury: MESSENGER evidence for geologically recent volatile-related activity, Science 333 (no. 6051), 1856-1859, 2011. http://dx.doi.org/10.1126/science.1211681
Borg, L. E., J. N. Connelly, M. Boyet, and R. W. Carlson, Chronological evidence that the Moon is either young or did not have a global magma ocean, Nature 477 (no. 7362), 70-U150, 2011. http://dx.doi.org/10.1038/nature10328
Boyet, M., and R. W. Carlson, Nd-142 evidence for early (> 4.53 Ga) global differentiation of the silicate Earth, Science 309 (no. 5734), 576-581, 2005. http://dx.doi.org/10.1126/science.1113634
Brandon, A. D., R. A. Creaser, S. B. Shirey, and R. W. Carlson, Osmium recycling in subduction zones, Science 272 (no. 5263), 861-864, 1996. http://dx.doi.org/10.1126/science.272.5263.861
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Herd, C. D. K., A. Blinova, D. N. Simkus, Y. S. Huang, R. Tarozo, C. M. O. Alexander, F. Gyngard, L. R. Nittler, G. D. Cody, M. L. Fogel, Y. Kebukawa, A. L. D. Kilcoyne, R. W. Hilts, G. F. Slater, D. P. Glavin, J. P. Dworkin, M. P. Callahan, J. E. Elsila, B. T. De Gregorio, and R. M. Stroud, Origin and evolution of prebiotic organic matter as inferred from the Tagish Lake meteorite, Science 332 (no. 6035),1304-1307, 2011. http://dx.doi.org/10.1126/science.1203290
Jackson, M. G., and R. W. Carlson, An ancient recipe for flood-basalt genesis, Nature 476 (no. 7360), 316-U77, 2011. http://dx.doi.org/10.1038/nature10326
Jackson, M. G., R. W. Carlson, M. D. Kurz, P. D. Kempton, D. Francis, and J. Blusztajn, Evidence for the survival of the oldest terrestrial mantle reservoir, Nature 466 (no. 7308), 853-U84, 2010. http://dx.doi.org/10.1038/nature09287
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Lambert, D. D., J. W. Morgan, R. J. Walker, S. B. Shirey, R. W. Carlson, M. L. Zientek, and M. S. Koski, Rhenium-osmium and samarium-neodymium isotopic systematics of the Stillwater Complex, Science 244 (no. 4909), 1169-1174, 1989. http://dx.doi.org/10.1126/science.244.4909.1169
Lawrence, D. J., W. C. Feldman, J. O. Goldsten, S. Maurice, P. N. Peplowski, B. J. Anderson, D. Bazell, R. L. McNutt, L. R. Nittler, T. H. Prettyman, D. J. Rodgers, S. C. Solomon, S. Z. Weider, Evidence for Water Ice Near Mercury's North Pole from MESSENGER Neutron Spectrometer Measurements. Science 339, 292-296 (2013)
McKeegan, K. D., J. Aleon, J. Bradley, D. Brownlee, H. Busemann, A. Butterworth, M. Chaussidon, S. Fallon, C. Floss, J. Gilmour, M. Gounelle, G. Graham, Y. B. Guan, P. R. Heck, P. Hoppe, I. D. Hutcheon, J. Huth, H. Ishii, M. Ito, S. B. Jacobsen, A. Kearsley, L. A. Leshin, M. C. Liu, I. Lyon, K. Marhas, B. Marty, G. Matrajt, A. Meibom, S. Messenger, S. Mostefaoui, S. Mukhopadhyay, K. Nakamura-Messenger, L. Nittler, R. Palma, R. O. Pepin, D. A. Papanastassiou, F. Robert, D. Schlutter, C. J. Snead, F. J. Stadermann, R. Stroud, P. Tsou, A. Westphal, E. D. Young, K. Ziegler, L. Zimmermann, and E. Zinner, Isotopic compositions of cometary matter returned by Stardust, Science 314 (no. 5806),1724-1728, 2006. http://dx.doi.org/10.1126/science.1135992
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O’Neil, J., and R. W. Carlson. Building Archean cratons from Hadean mafic crust, Science (no. 6330), 1199-1202, 2017. http://dx.doi.org/10.1126/science.aah3823
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Saal,A.E, E. H. Hauri, J. A. Van Orman, M. J. Rutherford, Hydrogen Isotopes in Lunar Volcanic Glasses and Melt Inclusions Reveal a Carbonaceous Chondrite Heritage. Science 340, 1317-1320 (2013)
Sarafian, E., G. A. Gaetani, E. H. Hauri.,and A. R. Sarafian. Experimental constraints on the damp peridotite solidus and oceanic mantle potential temperature, Science 355 (no. 6328), 942-944, 2017. http://dx.doi.org/10.1126/science.aaj2165
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Smit, K.V., Shirey, S.B., Hauri, E.H., and Stern, R.A. (2019) Sulfur isotopes in diamonds reveal differences in continent construction. Science 364, 383-385. http://doi.org/10.1126/science.aaw9548
Smith, E. M., S. B. Shirey, F. Nestola, E. S. Bullock, J. H. Wang, S. H. Richardson, and W. Y. Wang. Large gem diamonds from metallic liquid in Earth’s deep mantle,Science 354 (no. 6318), 1403-1405, 2016. http://dx.doi.org/10.1126/science.aal1303
Smith, E. M., Shirey, S. B., Richardson S. H., Nestola, F., Bullock, E. S., Wang, J., & Wang, W. (2018). Blue boron-bearing diamonds from Earth’s lower mantle. Nature, 560, 84–87. http://doi.org/10.1038/s41586-018-0334-5
Steele,A., F. M. McCubbin, M. Fries, L. Kater, N. Z. Boctor, M. L. Fogel, P. G. Conrad, M. Glamoclija, M. Spencer, A. L. Morrow, M. R. Hammond, R. N. Zare, E. P. Vicenzi, S. Siljestrom, R. Bowden, C. D. K. Herd, B. O. Mysen, S. B. Shirey, H. E. F. Amundsen, A. H. Treiman, E. S. Bullock, A. J. T. Jull, A Reduced Organic Carbon Component in Martian Basalts. Science 337, 212-215 (2012)
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