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The oxidation state of sulfur in lunar apatite

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Published/Copyright: January 23, 2019
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Abstract

Lunar apatites contain hundreds to thousands of parts per million of sulfur. This is puzzling because lunar basalts are thought to form in low oxygen fugacity (fO2) conditions where sulfur can only exist in its reduced form (S2–), a substitution not previously observed in natural apatite. We present measurements of the oxidation state of S in lunar apatites and associated mesostasis glass that show that lunar apatites and glass contain dominantly S2–, whereas natural apatites from Earth are only known to contain S6+. It is likely that many terrestrial and martian igneous rocks contain apatites with mixed sulfur oxidation states. The S6+/S2– ratios of such apatites could be used to quantify the fO2 values at which they crystallized, given information on the portioning of S6+ and S2– between apatite and melt and on the S6+/S2– ratios of melts as functions of fO2 and melt composition. Such a well-calibrated oxybarometer based on this the oxidation state of S in apatite would have wide application.

Keywords: Moon; oxygen; apatite; sulfur
  1. Funding

    This research was performed at GeoSoilEnviroCARS (The University of Chicago, Sector 13), APS ANL. GeoSoilEnviroCARS is supported by the National Science Foundation—Earth Sciences (EAR-1634415) and Department of Energy—GeoSciences (DE-FG02-94ER14466). This research used resources of APS, a U.S. Department of Energy (DOE) Office of Science user facility operated for the DOE Office of Science by ANL under Contract No. DE-AC02-06CH11357. Support for this research was provided by the University of California and by NASA’s Planetary Science Research Program.

Acknowledgments

We thank A. Lanzirotti and M. Newville for assistance in beamline operations at the Advanced Photon Source, Argonne National Laboratory (APS ANL). We also thank the curatorial staff at NASA Johnson Space Center for allocations of Apollo samples for this study. We thank A. Bell, G. Ustunisik, and an anonymous reviewer for constructive comments.

References cited

Beaty, D.W., and Albee, A.L. (1978) Comparative petrology and possible genetic relations among the Apollo 11 basalts. Proceedings of the Ninth Planetary Science Conference, 1, 359–463.Search in Google Scholar

Botcharnikov, R.E., Linnen, R.L., Wilke, M., Holtz, F., Jugo, P.J., and Berndt, J. (2010) High gold concentrations in sulphide-bearing magma under oxidizing conditions. Nature Geoscience, 4, 112.10.1038/ngeo1042Search in Google Scholar

Boyce, J.W., Liu, Y., Rossman, G.R., Guan, Y., Eiler, J.M., Stolper, E.M., and Taylor, L.A. (2010) Lunar apatite with terrestrial volatile abundances. Nature, 466, 466.10.1038/nature09274Search in Google Scholar

Boyce, J.W., Tomlinson, S.M., McCubbin, F.M., Greenwood, J.P., and Treiman, A.H. (2014) The lunar apatite paradox. Science, 344, 400.10.1126/science.1250398Search in Google Scholar

Brett, R. (1976) Reduction of mare basalts by sulfur loss. Geochimica et Cosmo-chimica Acta, 40, 997–1004.10.1016/0016-7037(76)90042-9Search in Google Scholar

Brounce, M., Stolper, E., and Eiler, J. (2017) Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation. Proceedings of the National Academy of Sciences, 114, 8997–9002.10.1073/pnas.1619527114Search in Google Scholar PubMed PubMed Central

Bunch, T.E., Keils, K., and Prinz, M. (1972) Mineralogy, petrology and chemistry of lunar rock 12039. Meteoritics, 7, 245–255.10.1111/j.1945-5100.1972.tb00439.xSearch in Google Scholar

Carmichael, I.S.E. (1991) The redox states of basic and silicic magmas: a reflection of their source regions? Contributions to Mineralogy and Petrology, 106, 129–141.10.1007/BF00306429Search in Google Scholar

Chen, Y., Zhang, Y., Liu, Y., Guan, Y., Eiler, J., and Stolper, E.M. (2015) Water, fluorine, and sulfur concentrations in the lunar mantle. Earth and Planetary Science Letters, 427, 37–46.10.1016/j.epsl.2015.06.046Search in Google Scholar

El Goresy, A. (1976) Oxide minerals in lunar rocks. Reviews in Mineralogy and Geochemistry, 3, 47–72.Search in Google Scholar

Fleet, M.E. (2005) XANES spectroscopy of sulfur in Earth materials. Canadian Mineralogist, 43, 1811–1838.10.2113/gscanmin.43.6.1811Search in Google Scholar

Green, D.H., Ringwood, A.E., Ware, N.G., Hibberson, W.O., Major, A., and Kiss, E. (1971) Experimental petrology and petrogenesis of Apollo 12 basalts. Proceedings of the Second Planetary Science Conference, 1, 601–615.10.1007/978-94-010-2861-5_14Search in Google Scholar

Greenwood, J.P., Itoh, S., Sakamoto, N., Warren, P., Taylor, L., and Yurimoto, H. (2011) Hydrogen isotope ratios in lunar rocks indicate delivery of cometary water to the Moon. Nature Geoscience, 4, 79.10.1038/ngeo1050Search in Google Scholar

Guggisberg, S., Eberhardt, P., Geiss, J., Grogler, N., and Stettler, A. (1979) Classification of the Apollo-11 mare basalts according to Ar39-Ar40 ages and petrological properties. Proceedings of the Tenth Planetary Science Conference, 1–39.Search in Google Scholar

Haggerty, S.E., and Meyer, H.O.A. (1970) Apollo 12: Opaque oxides. Earth and Planetary Science Letters, 9, 379–387.10.1016/0012-821X(70)90001-4Search in Google Scholar

Hauri, E.H., Weinreich, T., Saal, A.E., Rutherford, M.C., and Van Orman, J.A. (2011) High pre-eruptive water contents preserved in lunar melt inclusions. Science, 333, 213.10.1126/science.1204626Search in Google Scholar

Helz, R.T., Cottrell, E., Brounce, M.N., and Kelley, K.A. (2017) Olivine-melt relationships and syneruptive redox variations in the 1959 eruption of Kilauea volcano as revealed by XANES. Journal of Volcanology and Geothermal Research, 333, 1–14.10.1016/j.jvolgeores.2016.12.006Search in Google Scholar

Henning, P.A., Adolfsson, E., and Grins, J. (2000) The chalcogenide phosphate apatites Ca10(PO46S, Sr10(PO46S, Ba10(PO46S and Ca10(PO46Se. Zeitschrift für Kristallographie—Crystalline Materials, 215, 226–230.10.1524/zkri.2000.215.4.226Search in Google Scholar

Herd, C.D., Borg, L.E., Jones, J.H., and Papike, J.J. (2002) Oxygen fugacity and geochemical variations in the martian basalts: implications for martian basalt petrogenesis and the oxidation state of the upper mantle of Mars. Geochimica et Cosmochimica Acta, 66, 2025–2036.10.1016/S0016-7037(02)00828-1Search in Google Scholar

Jugo, P.J., Wilke, M., and Botcharnikov, R.E. (2010) Sulfur K-edge XANES analysis of natural and synthetic basaltic glasses: Implications for S speciation and S content as function of oxygen fugacity. Geochimica et Cosmochimica Acta, 74, 5926–5938.10.1016/j.gca.2010.07.022Search in Google Scholar

Karner, J.M., Sutton, S.R., Papike, J.J., Shearer, C.K., Jones, J.H., and Newville, M. (2006) Application of a new vanadium valence oxybarometer to basaltic glasses from the Earth, Moon, and Mars. American Mineralogist, 91, 270–277.10.2138/am.2006.1830Search in Google Scholar

Kelley, K.A., and Cottrell, E. (2009) Water and the oxidation state of subduction zone magmas. Science, 325, 605–607.10.1126/science.1174156Search in Google Scholar PubMed

Kim, Y., Konecke, B., Fiege, A., Simon, A., and Becker, U. (2017) An ab-initio study of the energetics and geometry of sulfide, sulfite, and sulfate incorporation into apatite: The thermodynamic basis for using this system as an oxybarometer. American Mineralogist, 102, 1646–1656.10.2138/am-2017-6044Search in Google Scholar

Klein, C. (1972) Lunar materials: Their mineralogy, petrology and chemistry. Earth-Science Reviews, 8, 169–204.10.1016/0012-8252(72)90083-9Search in Google Scholar

Klimm, K., Kohn, S.C., and Botcharnikov, R.E. (2012) The dissolution mechanism of sulphur in hydrous silicate melts. II: Solubility and speciation of sulphur in hydrous silicate melts as a function of fO2 Chemical Geology, 322– 323, 250–267.10.1016/j.chemgeo.2012.04.028Search in Google Scholar

Konecke, B.A., Fiege, A., Simon, A.C., Parat, F., and Stechern, A. (2017a) Co-variability of S6+ S4+ and S2- in apatite as a function of oxidation state: Implications for a new oxybarometer. American Mineralogist, 102, 548–557.10.2138/am-2017-5907Search in Google Scholar

Konecke, B.A., Fiege, A., Simon, A.C., and Holtz, F. (2017b) Cryptic metasomatism during late-stage lunar magmatism implicated by sulfur in apatite. Geology, 45, 739–742.10.1130/G39249.1Search in Google Scholar

Lyons, J.I. (1988) Volcanogenic iron oxide deposits, Cerro de Mercado and vicinity, Durango. Economic Geology, 83, 1886–1906.10.2113/gsecongeo.83.8.1886Search in Google Scholar

McCubbin, F.M., and Jones, R.H. (2015) Extraterrestrial apatite: Planetary geochemistry to astrobiology. Elements, 11, 183–188.10.2113/gselements.11.3.183Search in Google Scholar

McCubbin, F.M., and Ustunisik, G. (2018) Experimental investigation of F and Cl partitioning between apatite and Fe-rich basaltic melt at 0 GPa and 950–1050 °C: Evidence for steric controls on apatite-melt exchange equilibria in OH-poor apatite. American Mineralogist, 103, 1455–1467.10.2138/am-2018-6339Search in Google Scholar

McCubbin, F.M., Vander Kaaden, K.E., Tartèse, R., Klima, R.L., Liu, Y., Mortimer, J., Barnes, J.J., Shearer, C.K., Treiman, A.H., Lawrence, D.J., and others (2015) Magmatic volatiles (H, C, N, F, S, Cl) in the lunar mantle, crust, and regolith: Abundances, distributions, processes, and reservoirs. American Mineralogist, 100, 1668–1707.10.2138/am-2015-4934CCBYNCNDSearch in Google Scholar

Moussallam, Y., Edmonds, M., Scaillet, B., Peters, N., Gennaro, E., Sides, I., and Oppenheimer, C. (2016) The impact of degassing on the oxidation state of basaltic magmas: A case study of Kīlauea volcano. Earth and Planetary Science Letters, 450, 317–325.10.1016/j.epsl.2016.06.031Search in Google Scholar

Nyquist, L.E., Shih, C.-Y., Wooden, J.L., Bansal, B.M., and Wiesmann, H. (1979) The Sr and Nd isotopic record of Apollo 12 basalts: Implications for lunar geochemical evolution. Proceedings of the Tenth Planetary Science Conference, 77–114.Search in Google Scholar

Pan, Y., and Fleet, M.E. (2002) Compositions of the apatite-group minerals: substitution mechanisms and controlling factors. Reviews in Mineralogy and Geochemistry, 48, 13–49.10.1515/9781501509636-005Search in Google Scholar

Pernet-Fisher, J.F., Howarth, G.H., Liu, Y., Chen, Y., and Taylor, L.A. (2014) Estimating the lunar mantle water budget from phosphates: Complications associated with silicate-liquid-immiscibility. Geochimica et Cosmochimica Acta, 144, 326–341.10.1016/j.gca.2014.09.004Search in Google Scholar

Piccoli, P., and Candela, P.A. (2002) Apatite in igneous systems. Reviews in Mineralogy and Geochemistry, 48, 255–292.10.1515/9781501509636-009Search in Google Scholar

Rhodes, J.M., Blanchard, D.P., Dungan, M.A., Brannon, J.C., and Rodgers, K.V. (1977) Chemistry of Apollo 12 Mare basalts: Magma types and fractionation processes. Proceedings of the Eighth Planetary Science Conference, 1, 1305–1338.Search in Google Scholar

Roedder, E., and Weiblen, P.W. (1970) Silicate liquid immiscibility in lunar magmas, evidenced by melt inclusions in lunar rocks. Science, 167, 641.10.1126/science.167.3918.641Search in Google Scholar

Saal, A.E., Hauri, E.H., Cascio, M.L., Van Orman, J.A., Rutherford, M.C., and Cooper, R.F. (2008) Volatile content of lunar volcanic glasses and the presence of water in the Moon’s interior. Nature, 454, 192–195.10.1038/nature07047Search in Google Scholar

Sato, M. (1979) The driving mechanism of lunar pyroclastic eruptions inferred from the oxygen fugacity behavior of Apollo 17 orange glass. Proceedings of the Tenth Planetary Science Conference, 311–325.Search in Google Scholar

Sato, M., Hickling, N.L., and McLane, J.E. (1973) Oxygen fugacity values of Apollo 12, 14, and 15 lunar samples and reduced state of lunar magmas. Proceedings of the Fourth Lunar Science Conference, 1, 1061–1079.Search in Google Scholar

Shearer, C.K., McKay, G., Papike, J.J., and Karner, J.M. (2006) Valence state partitioning of vanadium between olivine-liquid: Estimates of the oxygen fugacity of Y980459 and application to other olivine-phyric martian basalts. American Mineralogist, 91, 1657–1663.10.2138/am.2006.2155Search in Google Scholar

Shearer, C.K., Sharp, Z.D., Burger, P.V., McCubbin, F.M., Provencio, P.P., Brearley, A.J., and Steele, A. (2014) Chlorine distribution and its isotopic composition in “rusty rock” 66095. Implications for volatile element enrichments of “rusty rock” and lunar soils, origin of “rusty” alteration, and volatile element behavior on the Moon. Geochimica et Cosmochimica Acta, 139, 411–433.10.1016/j.gca.2014.04.029Search in Google Scholar

Steele, A.M., Colson, R.O., Korotev, R.L., and Haskin, L.A. (1992) Apollo 15 green glass: Compositional distribution and petrogenesis. Geochimica et Cosmochimica Acta, 56, 4075–4090.10.1016/0016-7037(92)90017-DSearch in Google Scholar

Suitch, P.R., Taitai, A., Lacout, J.L., and Young, R.A. (1986) Structural consequences of the coupled substitution of Eu,S in calcium sulfoapatite. Journal of Solid State Chemistry, 63, 267–277.10.1016/0022-4596(86)90177-5Search in Google Scholar

Taitai, A., and Lacout, J.L. (1989) On the coupled introduction of Eu3+ and S2-ions into strontium apatites. Journal of Physics and Chemistry of Solids, 50, 851–855.10.1016/0022-3697(89)90066-8Search in Google Scholar

Taylor, L.A., Williams, R.J., and McCallister, R.H. (1972) Stability relations of ilmenite and ulvöspinel in the Fe-Ti-O system and application of these data to lunar mineral assemblages. Earth and Planetary Science Letters, 16, 282–288.10.1016/0012-821X(72)90204-XSearch in Google Scholar

Taylor, L.A., Patchen, A., Mayne, R.G., and Taylor, D.-H. (2004) The most reduced rock from the moon, Apollo 14 basalt 14053: Its unique features and their origin. American Mineralogist, 89, 1617–1624.10.2138/am-2004-11-1205Search in Google Scholar

Treiman, A., Boyce, J.W., Gross, J., Gao, Y., Eiler, J.M., and Stolper, E.M. (2014) Phosphate-halogen metasomatism of lunar granulite 79215: Impact-induced fractionation of volatiles and incompatible elements. American Mineralogist, 99, 1860–1870.10.2138/am-2014-4822Search in Google Scholar

Turner, G. (1970) Argon-40/ Argon-39 Dating of Lunar Rock Samples. Science, 167, 466.10.1126/science.167.3918.466Search in Google Scholar PubMed

Wadhwa, M. (2008) Redox conditions on small bodies, the Moon and Mars. Reviews in Mineralogy and Geochemistry, 68, 493–510.10.1515/9781501508509-017Search in Google Scholar

Wetzel, D.T., Rutherford, M.J., Jacobsen, S.D., Hauri, E.H., and Saal, A.E. (2013) Degassing of reduced carbon from planetary basalts. Proceedings of the National Academy of Sciences, 110, 8010.10.1073/pnas.1219266110Search in Google Scholar PubMed PubMed Central

Wetzel, D.T., Hauri, E.H., Saal, A.E., and Rutherford, M. J. (2015) Carbon content and degassing history of the lunar volcanic glasses. Nature Geoscience, 8, 755.10.1038/ngeo2511Search in Google Scholar

Received: 2018-08-31
Accepted: 2018-11-01
Published Online: 2019-01-23
Published in Print: 2019-02-25

© 2019 Walter de Gruyter GmbH, Berlin/Boston

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