WING Boswell
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Earth & Planetary Sciences boswell.wing@mcgill.ca |
Ph.D., Johns Hopkins University Maryland, U.S.A. (2004)
Department of Earth and Planetary Sciences, McGill University
Publications
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Articles GEOTOP:
Fiorentini, M.L., Bekker, A., Rouxwl, O., Wing, B.A., Maier, W., Rumble, D. 2012. Multiple sulfur and iron isotope composition of magmatic Ni-Cu-(PGE) sulfide mineralization from eastern Botswana. Economic Geology, 107 (1), 105-116.
Masterson, A.L., Farquhar, J., Wing, B.A., In press. Sulfur mass-independent fractionation patterns in the broadband UV photolysis of sulfur dioxide: Pressure and third body effects, Earth and Planetary Science Letters.
Shen, Y., Farquhar, J., Zhang, H., Masterson, A., Zhang, T., Wing, B.A., 2011. Multiple S-isotopic evidence for episodic shoaling of anoxic water during Late Permian mass extinction, Nature Communications, 2(1), 210. pdf
Cartigny, P., Farquhar, J., Thomassot, E., Harris, J.W., Wing, B., Masterson, A., McKeegan, K., Stachel, T., 2009. A mantle origin for Paleoarchean peridotitic diamonds from the Panda kimberlite, Slave craton: Evidence from 13C-, 15N- and 33,34S- stable isotope systematics, Lithos, 112, 852-864. pdf
Guo, Q., Strauss, H., Kaufman, A.J., Schröder, S., Gutzmer, J., Wing, B., Baker, M.A., Bekker, A., Jin, Q., Kim, S.-T., Farquhar, J., 2009. Reconstructing Earth's surface oxidation across the Archean-Proterozoic transition, Geology, 37 (5), 399-402. pdf
Penniston-Dorland, S.C., Wing, B.A., Nex, P.A.M., Kinnaird, J.A., Farquhar, J., Brown, M., Sharman, E.R., 2008. Multiple sulfur isotopes reveal a magmatic origin for the Platreef platinum group element deposit, Bushveld Complex, South Africa, Geology, 36 (12), 979-982. pdf
Bindeman, I.N., Eiler, J.M., Wing B.A., Farquhar, J., 2007. Rare sulfur and triple oxygen isotope geochemistry of volcanogenic sulfate aerosols, Geochimica et Cosmochimica Acta, 71(9), 2326-2343. GEOTOP Publication n° 2007-0039. pdf
Farquhar, J., Johnston, D.T., Wing, B.A., 2007. Implications of conservation of mass effects on mass-dependent isotope fractionations: Influence of network structure on sulfur isotope phase space of dissimilatory sulfate reduction, Geochimica et Cosmochimica Acta, 71 (24), pp. 5862-5875. pdf
Teng, F., McDonough, W.F., Rudnick, R.L., Wing, B.A., 2007. Limited lithium isotopic fractionation during progressive metamorphic dehydration in metapelites: A case study from the Onawa contact aureole, Maine. Chem. Geol., 239, 1-12. pdf
Wing, B.A., Ferry, J.M., 2007. Magnitude and geometry of reactive fluid flow from direct inversion of spatial patterns of geochemical alteration, American Journal of Science, 307 (5), 793-832. pdf
Jamieson, J.W., Wing, B.A., Hannington, M.D., Farquhar, J., 2006. Evaluating isotopic equilibrium among sulfide mineral pairs in Archean ore deposits: Case Study from the Kidd Creek VMS deposit, Ontario, Canada. Economic Geol., 101, 1055-1061.
Johnston, D.T., Poulton, S.W., Fralick, P.W., Wing, B.A., Canfield, D.E., Farquhar, J., 2006. Evolution of the oceanic sulfur cycle at the end of the Paleoproterozoic, Geochimica et Cosmochimica Acta, 70(23 SPEC. ISS.), 5723-5739. pdf
Autres articles:
Tyra, M.A., Farquhar, J., Wing, B.A., Benedix, G.K., Jull, A.J.T., Jackson, T., and Thiemens, M.H., 2007. Terrestrial alteration of carbonate in a suite of Antarctic CM chondrites: Evidence from oxygen and carbon isotopes, Geochimica et Cosmochimica Acta, 71(3), 782-795. pdf
Ono, S., Wing, B., Johnston, D., Farquhar, J., and Rumble, D., 2006. Mass-dependent fractionation of quadruple stable sulfur isotope system as a new tracer of sulfur biogeochemical cycles, Geochimica et Cosmochimica Acta, 70(9), 2238-2252. pdf
Ono, S., Wing, B., Rumble, D., and Farquhar, J., 2006. High precision analysis of all four stable isotopes of sulfur (32S, 33S, 34S and 36S) at nanomole levels using a laser fluorination isotope-ratio-monitoring gas chromatography-mass spectrometry, Chemical Geology, 225(1-2), 30-39. pdf
Ferry, J.M., Rumble III, D., Wing, B.A., Penniston-Dorland, S.C., 2005. A new interpretation of centimetre-scale variations in the progress of infiltration-driven metamorphic reactions: Case study of carbonated metaperidotite, Val d'Efra, Central Alps, Switzerland, Journal of Petrology, 46(8), 1725-1746. pdf
Johnston, D. T., Farquhar, J., Wing, B. A., Kaufman, A. J., Canfield, D. E., Habicht, K.S., 2005. Multiple Sulfur Isotope Fractionations in Biological systems: a case study with Sulfate Reducers and Sulfur Disproportionators, American Journal of Science, 305, 645-660. pdf.
Johnston D. T., Wing B. A., Farquhar J., Kaufman A. J., Strauss H., Lyons T.W., Kah L. C. & Canfield D. E. 2005. Active microbial sulfur disproportionation in the Mesoproterozoic, Science, 310, 1477-1479. pdf.
Farquhar, J., Wing, B. A., 2005. The terrestrial record of stable sulfur isotopes: a reviea of implications for evolution of Earth’s sulfur cycle. in McDonald, I., Boyce, A.J., Butler, I.B., Herrington, R.J & Polya, D.A. (eds), 2005, Mineral Deposits and Earth Evolution, Geol. Soc. London Spec. Pub., 248, 167-177. pdf.
Ferry, J. M., Rumble III, D., Wing, B. A., Penniston-Dorland, S.C., 2005. A new interpretation of centimeter-scale variations in the progress of infiltration-driven metamorphic reactions: Case study of carbonated metaperidotite, Val d'Efra, Central Alps, Switzerland, J. Petrol., 46, 1725-1746. pdf.
Johnson, T., Brown, M., Gibson, R., Wing, B. A., 2004. Spinel-cordierite symplectites replacing andalusite: Evidence for melt-assisted diapirism in the Bushveld Complex, South Africa, J. Met. Geol., 22, 529-545. pdf.
Farquhar, J., Wing, B. A., 2003. Multiple sulfur isotopes and the evolution of the atmosphere, Earth Plan. Sci. Lett., 213, 1-13. pdf.
Wing, B. A., Ferry, J. M., Harrison, T. M., 2003. Prograde destruction and formation of monazite and allanite during contact and regional metamorphism of pelites: petrology and geochronology, Contrib. Mineral. Petrol., 145, 228-250. pdf.
Farquhar, J., Johnston, D.T., Wing, B. A., Habicht, K. S., Canfield, D. E., Airieau, S., Thiemens, M.H., 2003. Multiple sulphur isotopic interpretations of biosynthetic pathways: implications for biological signatures in the sulphur isotope record, Geobiol., 1, 27-36. pdf.
Wing, B. A., Ferry, J. M., 2002. Three-dimensional geometry of metamorphic fluid flow during Barrovian regional metamorphism from an inversion of combined petrologic and stable isotopic data, Geology, 30, 639-642. pdf.
Farquhar, J., Wing, B. A., McKeegan, K. D., Harris, J. W., Cartigny, P., Thiemens, M. H., 2002. Mass-independent sulfur of inclusions in diamond and sulfur recycling on early Earth, Science, 298, 2369-2372. pdf.
Ferry, J. M., Wing, B. A., Penniston-Dorland, S.C., Rumble III, D., 2002. The direction of fluid flow during contact metamorphism of siliceous carbonate rocks: new data for the Monzoni and Predazzo aureoles, northern Italy, and a global review, Contrib. Mineral. Petrol., 142, 679-699. pdf.
Ferry, J. M., Wing, B. A., Rumble III, D., 2001. Formation of wollastonite by chemically reactive fluid flow during contact metamorphism, Mt. Morrison pendant, Sierra Nevada, California, USA, J. Petrol., 42, 1705-1728. pdf.
Thèmes de recherche
Mots clé: géochimie d'isotopes stables, évolution atmosphérique, biogéochimie du Précambrien
Les processus qui agissent sur les différents systèmes terrestres laissent des traces géochimiques de leurs actions. Pour cerner la présence et l’intensité de ces processus dans le passé et de nos jours, ma recherche exploite la persistance de cette mémoire dans les archives géologique (roches plus ou moins anciennes) et la capacité unique des isotopes stables à la faire apparaître.
Mes récents sujets de recherche sont variés et s’étendent de l’étude des gaz traces atmosphériques qui contrôlent la capacité d’habiter la planète à l’étude des fluides crustaux de grandes profondeurs impliqués dans le métamorphisme et la construction de montagnes. De nouvelles recherches utiliseront des mesures de haute précision de concentrations isotopiques en oxygène (16O, 17O, 18O) et en soufre (32S, 33S, 34S, 36S) pour
i) examiner la biogéochimie microbienne sous une atmosphère anoxique (sous oxygénée) archéenne (> 2,5 milliards d’années),
ii) pour contraindre les fluxes de masse dans le cycle géologique du soufre au Phanérozoïque (540 millions à 2,5 milliards d’années) et
iii) pour rechercher les processus qui contrôlent les oxydants polluants et nettoyants (OH, O3) dans l’atmosphère moderne.
Étudiants
Bui, Thi Hao: PhD., McGill University
Sujet de recherche:Sulfur cycle in sediments at gas hydrate sites
Hryciuk, Matthew: M.Sc. in Earth and Planetary sciences, McGill University
Sujet de recherche: Intrusive-host rock interactions in the Franklin LIP, Victoria Island
Pellerin, André: PhD.McGill University
Sujet de recherche: Sulfur isotope fractionation by bacteria
Sharmann-Harris, Elizabeth: PhD., McGill University
Sujet de recherche: Multiple sulphur isotope study of volcanogenic massif sulphide – type deposits focussing on the Abitibi Belt