Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770Ma Isua Supracrustal Belt (West Greenland)

Earth and Planetary Science Letters

Volumn 363, Issue , 2013, Pages 192-203

  Czaja, Andrew D ^a   Johnson, Clark M ^a   Beard, Brian L ^a   Roden, Eric E ^a   Li, Weiqiang ^a   Moorbath, Stephen ^b  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

^b UNIVERSITY OF OXFORD   (United Kingdom)

Author keywords

Anoxygenic phototrophs; Early Archean; Fe isotopes; Fe oxidation; Femtosecond laser ablation; Isua Supracrustal Belt

Indexed keywords

ARCHEAN; FE ISOTOPES; FEMTOSECONDS; ISUA SUPRACRUSTAL BELTS; PHOTOTROPHS;

GALLIUM; HYDROTHERMAL SYNTHESIS; INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY; IRON ANALYSIS; IRON COMPOUNDS; LASER ABLATION; LASERS; LITHOLOGY; MAGNETITE; MASS SPECTROMETERS; OXIDATION; REDOX REACTIONS; SECONDARY ION MASS SPECTROMETRY; ULTRASHORT PULSES;

ISOTOPES;

AMPHIBOLITE FACIES; ARCHEAN; BANDED IRON FORMATION; DEPOSITION; IRON; ISOTOPIC ANALYSIS; ISOTOPIC COMPOSITION; LASER METHOD; MAGNETITE; METAMORPHISM; OXIDATION; PALEOENVIRONMENT; REDOX CONDITIONS; SEDIMENT CHEMISTRY; SUPRACRUSTAL ROCK;

ARCTIC; GREENLAND; ISUA GREENSTONE BELT;

BACTERIA (MICROORGANISMS);

EID: 84873868519     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.12.025     Document Type: Article

References (92)

1. Albarède F., Beard B.L., Johnson C.M. Analytical methods for non-traditional isotopes. Geochemistry of Non-Traditional Stable Isotopes 2004, 113-152. Mineralogical Society of America and Geochemical Society, Washington, DC. J.J. Rosso (Ed.).
2. Anbar A.D., Duan Y., Lyons T.W., Arnold G.L., Kendall B., Creaser R.A., Kaufman A.J., Gordon G.W., Scott C., Garvin J., Buick R. A whiff of oxygen before the Great Oxidation Event?. Science 2007, 317:1903-1906.
3. André L., Cardinal D., Alleman L.Y., Moorbath S. Silicon isotopes in ~3.8Ga West Greenland rocks as clues to the Eoarchaean supracrustal Si cycle. Earth Planet. Sci. Lett. 2006, 245:162-173.
4. Appel P.W.U., Fedo C.M., Moorbath S., Myers J.S. Early Archaean Isua supracrustal belt, West Greenland: pilot study of the Isua Multidisciplinary Research Project. Geol. Greenland Surv. Bull. 1998, 180:94-99.
5. Appel P.W.U., Fedo C.M., Moorbath S., Myers J.S. Recognizable primary volcanic and sedimentary features in a low-strain domain of the highly deformed, oldest known (≈3.7-3.8 Gyr) Greenstone Belt, Isua, West Greenland. Terra Nova 1998, 10:57-62.
6. 55Fe diffusion in magnetite crystals at 500°C and its relevance to oxidation of iron. J. Mater. Sci. 1983, 18:2371-2379.
7. Beard B.L., Czaja A.D., Li W., Schauer J.J., Olson M., Johnson C.M. Iron isotope fractionation during femtosecond laser ablation of magnetite determined by aerosol size sorting experiments. Mineral. Mag. 2012, 76:1462.
8. Beard B.L., Handler R.M., Scherer M.M., Wu L.L., Czaja A.D., Heimann A., Johnson C.M. Iron isotope fractionation between aqueous ferrous iron and goethite. Earth Planet. Sci. Lett. 2010, 295:241-250.
9. Beard B.L., Johnson C.M. High precision iron isotope measurements of terrestrial and lunar materials. Geochim. Cosmochim. Acta 1999, 63:1653-1660.
10. Beard B.L., Johnson C.M. Inter-mineral Fe isotope variations in mantle-derived rocks and implications for the Fe geochemical cycle. Geochim. Cosmochim. Acta 2004, 68:4727-4743.
11. Beard B.L., Johnson C.M., Skulan J.L., Nealson K.H., Cox L., Sun H. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe. Chem. Geol. 2003, 195:87-117.
12. Beukes N.J. Palaeoenvironmental setting of iron-formations in the depositional basin of the Transvaal Supergroup, South Africa. Iron-Formation: Facts and Problems 1983, 131-209. Elsevier, Amsterdam. A.F. Trendall, R.C. Morris (Eds.).
13. Boak J.L., Dymek R.F. Metamorphism of the ca. 3800Ma supracrustal rocks at Isua, West Greenland: implications for early Archean crustal evolution. Earth Planet. Sci. Lett. 1982, 59:155-176.
14. 2+-significance for banded iron formations. Nature 1983, 303:163-164.
15. Brocks J.J., Logan G.A., Buick R., Summons R.E. Archean molecular fossils and the early rise of eukaryotes. Science 1999, 285:1033-1036.
16. Cloud P.E. Atmospheric and hydrospheric evolution on the primitive earth. Science 1968, 160:729-736.
17. Craddock P.R., Dauphas N. Iron and carbon isotope evidence for microbial iron respiration throughout the Archean. Earth Planet. Sci. Lett. 2011, 303:121-132.
18. Croal L.R., Johnson C.M., Beard B.L., Newman D.K. Iron isotope fractionation by Fe(II)-oxidizing photoautotrophic bacteria. Geochim. Cosmochim. Acta 2004, 68:1227-1242.
19. Crowe S.A., Jones C., Katsev S., Magen C., O'Neill A.H., Sturm A., Canfield D.E., Haffner G.D., Mucci A., Sundby B., Fowle D.A. Photoferrotrophs thrive in an Archean Ocean analogue. Proc. Natl. Acad. Sci. USA 2008, 105:15938-15943.
20. Crowley J.L., Myers J.S., Dunning G.R. Timing and nature of multiple 3700-3600Ma tectonic events in intrusive rocks north of the Isua greenstone belt, southern West Greenland. Geol. Soc. Amer. Bull. 2002, 114:1311-1325.
21. Czaja A.D., Johnson C.M., Beard B.L., Eigenbrode J.L., Freeman K.H., Yamaguchi K.E. Iron and carbon isotope evidence for ecosystem and environmental diversity in the ~2.7 to 2.5Ga Hamersley Province, Western Australia. Earth Planet. Sci. Lett. 2010, 292:170-180.
22. Czaja A.D., Johnson C.M., Roden E.E., Beard B.L., Voegelin A.R., Nägler T.F., Beukes N.J., Wille M. Evidence for free oxygen in the Neoarchean ocean based on coupled iron-molybdenum isotope fractionation. Geochim. Cosmochim. Acta. 2012, 86:118-137.
23. Dauphas N., Cates N.L., Mojzsis S.J., Busigny V. Identification of chemical sedimentary protoliths using iron isotopes in the >3750Ma Nuvvuagittuq supracrustal belt, Canada. Earth Planet. Sci. Lett. 2007, 254:358-376.
24. Dauphas N., Rouxel O. Mass spectrometry and natural variations of iron isotopes. Mass Spectrom. Rev. 2006, 25:515-550.
25. Dauphas N., van Zuilen M., Busigny V., Lepland A., Wadhwa M., Janney P.E. Iron isotope, major and trace element characterization of early Archean supracrustal rocks from SW Greenland: protolith identification and metamorphic overprint. Geochim. Cosmochim. Acta. 2007, 71:4745-4770.
26. Dauphas N., van Zuilen M., Wadhwa M., Davic A.M., Marty B., Janney P.E. Clues from Fe isotope variations on the origin of Early Archean BIFs from Greenland. Science 2004, 306:2077-2080.
27. Dieckmann R., Schmalzried H. Defects and cation diffusion in magnetite (I). Ber. Bunsenges. Phys. Chem. 1977, 81:344-347.
28. Dymek R.F., Klein C. Chemistry, petrology and origin of banded iron-formation lithologies from the 3800Ma Isua Supracrustal Belt, West Greenland. Precambrian Res. 1988, 39:247-302.
29. Eigenbrode J.L., Freeman K.H., Summons R.E. Methylhopane biomarker hydrocarbons in Hamersley Province sediments provide evidence for Neoarchean aerobiosis. Earth Planet. Sci. Lett. 2008, 273:323-331.
30. Farquhar J., Bao H., Thiemens M. Atmospheric influence of Earth's earliest sulfur cycle. Science 2000, 289:756-758.
31. Fedo C.M., Myers J.S., Appel P.W.U. Depositional setting and paleogeographic implications of earth's oldest supracrustal rocks, the>3.7Ga Isua Greenstone belt, West Greenland. Sediment. Geol. 2001, 141:61-77.
32. Gallagher P.K., West K.W., Warne S.S.J. Use of the Mössbauer effect to study the thermal decomposition of siderite. Thermochim. Acta 1981, 50:41-47.
33. Grotzinger J.P., Kasting J.F. New constraints on Precambrian ocean composition. J. Geol. 1993, 101:235-243.
34. Heck P.R., Huberty J.M., Kita N.T., Ushikubo T., Kozdon R., Valley J.W. SIMS analyses of silicon and oxygen isotope ratios for quartz from Archean and Paleoproterozoic banded iron formations. Geochim. Cosmochim. Acta 2011, 75:5879-5891.
35. Hegler F., Posth N.R., Jiang J., Kappler A. Physiology of phototrophic iron(II)-oxidizing bacteria: implications for modern and ancient environments. FEMS Microbiol. Ecol. 2008, 66:250-260.
36. Heijlen W., Appel P.W.U., Frezzotti M.L., Horsewell A., Touret J.L.R. Metamorphic fluid flow in the northeastern part of the 3.8-3.7Ga Isua Greenstone Belt (SW Greenland): A re-evalution of fluid inclusion evidence for early Archean seafloor-hydrothermal systems. Geochim. Cosmochim. Acta. 2006, 70:3075-3095.
37. Heimann A., Johnson C.M., Beard B.L., Valley J.W., Roden E.E., Spicuzza M.J., Beukes N.J. Fe, C, and O isotope compositions of banded iron formation carbonates demonstrate a major role for dissimilatory iron reduction in ~2.5Ga marine environments. Earth Planet. Sci. Lett. 2010, 294:8-18.
38. Herrick, M.J., 2007. Isotopic Studies of the 3.7-3.8Ga Isua Banded iron Formations Provide Insight into the Early Archean Geochemical Cycles. M.s. Thesis. Department of Geology and Geophysics, University of Wisconsin, Madison, p. 73.
39. Hoashi M., Bevacqua D.C., Otake T., Watanabe Y., Hickman A.H., Utsunomiya S., Ohmoto H. Primary haematite formation in an oxygenated sea 3.46 billion years ago. Nat. Geosci. 2009, 2:301-306.
40. Holland H.D. The Chemical Evolution of the Atmosphere and Oceans 1984, Princeton University Press, Princeton, NJ.
41. 18O for magnetite and hematite by SIMS. Chem. Geol. 2010, 276:269-283.
42. Jackson M.J., Pollack H.N. On the sensitivity of parameterized convection to the rate of decay of internal heat sources. J. Geophys. Res. 1984, 89:103-108.
43. Johnson C.M., Beard B.L. Fe isotopes: an emerging technique for understanding modern and ancient biogeochemical cycles. GSA Today 2006, 16:4-10.
44. Johnson C.M., Beard B.L., Beukes N.J., Klein C., O'Leary J.M. Ancient geochemical cycling in the Earth as inferred from Fe isotope studies of banded iron formations from the Transvaal Craton. Contrib. Mineral. Petrol. 2003, 144:523-547.
45. Johnson C.M., Beard B.L., Klein C., Beukes N.J., Roden E.E. Iron isotopes constrain biologic and abiologic processes in banded iron formation genesis. Geochim. Cosmochim. Acta 2008, 72:151-169.
46. Johnson C.M., Beard B.L., Roden E.E. The iron isotope fingerprints of redox and biogeochemical cycling in the modern and ancient Earth. Annu. Rev. Earth Planet. Sci. 2008, 36:457-493.
47. Kappler A., Johnson C.M., Crosby H.A., Beard B.L., Newman D.K. Evidence for equilibrium iron isotope fractionation by nitrate-reducing iron(II)-oxidizing bacteria. Geochim. Cosmochim. Acta 2010, 74:2826-2842.
48. Kappler A., Pasquero C., Konhauser K.O., Newman D.K. Deposition of banded iron formations by anoxygenic phototrophic Fe(II)-oxidizing bacteria. Geology 2005, 33:865-868.
49. Kato Y., Suzuki K., Nakamura K., Hickman A.H., Nedachi M., Kusakabe M., Bevacqua D.C., Ohmoto H. Hematite formation by oxygenated groundwater more than 2.76 billion years ago. Earth Planet. Sci. Lett. 2009, 278:40-49.
50. Kaufman A.J., Johnston D.T., Farquhar J., Masterson A.L., Lyons T.W., Bates S., Anbar A.D., Arnold G.L., Garvin J., Buick R. Late Archean biospheric oxygenation and atmospheric evolution. Science 2007, 317:1900-1903.
51. Kendall B., Reinhard C.T., Lyons T.W., Kaufman A.J., Poulton S.W., Anbar A.D. Pervasive oxygenation along late Archaean ocean margins. Nat. Geosci. 2010, 3:647-652.
52. Kita N.T., Huberty J.M., Kozdon R., Beard B.L., Valley J.W. High-precision SIMS oxygen, sulfur and iron stable isotope analyses of geological materials: accuracy, surface topography and crystal orientation. Surf. Interface Anal. 2011, 43:427-431.
53. Klein C. Some Precambrian banded iron-formations (BIFs) from around the world: their age, geologic setting, mineralogy, metamorphism, geochemistry, and origin. Am. Mineral. 2005, 90:1473-1499.
54. Klein C., Beukes N.J. Time distribution, stratigraphy, and sedimentologic setting, and geochemistry of precambrian iron-formations. The Proterozoic Biosphere, A Multidisciplinary Study 1992, Cambridge University Press, New York, pp. 139-146.
55. Konhauser K.O., Amskold L., Lalonde S.V., Posth N.R., Kappler A., Anbar A. Decoupling photochemical Fe(II) oxidation from shallow-water BIF deposition. Earth Planet. Sci. Lett. 2007, 258:87-100.
56. Konhauser K.O., Hamade T., Raiswell R., Morris R.C., Ferris F.G., Southam G., Canfield D.E. Could bacteria have formed the Precambrian banded iron formations?. Geology 2002, 30:1079-1082.
57. Li W., Johnson C.M., Beard B.L. U-Th-Pb isotope data indicate phanerozoic age for oxidation of the 3.4Ga Apex Basalt. Earth Planet. Sci. Lett. 2012, 319:197-206.
58. Lovley D.R., Stolz J.F., Nord G.L., Phillips E.J.P. Anaerobic production of magnetite by a dissimilatory iron-reducing microorganism. Nature 1987, 330:252-254.
59. Mojzsis S.J., Coath C.D., Greenwood J.P., McKeegan K.D., Harrison T.M. Mass-independent isotope effects in Archean (2.5 to 3.8Ga) sedimentary sulfides determined by ion microprobe analysis. Geochim. Cosmochim. Acta 2003, 67:1635-1658.
60. Moorbath S., Onions R.K., Pankhurs R.J. Early Archaean age for Isua iron formation, West Greenland. Nature 1973, 245:138-139.
61. Myers J.S. Protoliths of the 3.8-3.7Ga Isua greenstone belt, West Greenland. Precambrian Res. 2001, 105:129-141.
62. Nutman A.P. Early Archean crustal evolution of the Isukasia area, southern West Greenland. Precambrian Tectonics Illustrated 1984, 79-93. E. Schweizerbart'sche Verlagsbuchhandlung (Nägele u. Obermiller), Germany, Stuttgart. A. Kröner, R. Greiling (Eds.).
63. Nutman A.P., Allaart J.H., Bridgwater D., Dimroth E., Rosing M. Stratigraphic and geochemical evidence for the depositional environment of the Early Archean Isua Supracrustal Belt, southern West Greenland. Precambrian Res. 1984, 25:365-396.
64. Nutman A.P., Bridgwater D. Early Archean Amîtsoq tonalites and granites of the Isukasia area, southern West Greenland: development of the oldest-known sial. Contrib. Mineral. Petrol. 1986, 94:137-148.
65. 2-rich atmosphere before ~1.8 billion years ago. Nature 2004, 429:395-399.
66. Planavsky N., Rouxel O., Bekker A., Shapiro R., Fralick P., Knudsen A. Iron-oxidizing microbial ecosystems thrived in late Paleoproterozoic redox-stratified oceans. Earth Planet. Sci. Lett. 2009, 286:230-242.
67. Polat A., Frei R. The origin of early Archean banded iron formations and of continental crust, Isua, southern West Greenland. Precambrian Res. 2005, 138:151-175.
68. Polyakov V.B., Clayton R.N., Horita J., Mineev S.D. Equilibrium iron isotope fractionation factors of minerals: reevaluation from the data of nuclear inelastic resonant X-ray scattering and Mössbauer spectroscopy. Geochim. Cosmochim. Acta 2007, 71:3833-3846.
69. Rollinson H. The metamorphic history of the Isua Greenstone Belt, West Greenland. The Early Earth: Physical, Chemical, and Biological Development 2002, 329-350. Geological Society, London, Special Publications. C.M.R. Fowler, C.J. Ebinger, C.J. Hawkesworth (Eds.).
70. Rollinson H. Metamorphic history suggested by garnet-growth chronologies in the Isua Greenstone Belt, West Greenland. Precambrian Res. 2003, 126:181-196.
71. 13C-depleted carbon microparticles in >3700-Ma sea-floor sedimentary rocks from west Greenland. Science 1999, 283:674-676.
72. Rosing M.T., Frei R. U-rich Archaean sea-floor sediments from Greenland-indications of >3700Ma oxygenic photosynthesis. Earth Planet. Sci. Lett. 2004, 217:237-244.
73. Rosing M.T., Rose N.M., Bridgwater D., Thomsen H.S. Earliest part of Earth's stratigraphic record: a reappraisal of the >3.7Ga Isua (Greenland) supracrustal sequence. Geology 1996, 24:43-46.
74. Rouxel O.J., Bekker A., Edwards K.J. Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state. Science 2005, 307:1088-1091.
75. 2+(aq) with carbonate minerals. Geochim. Cosmochim. Acta 2010, 74:6301-6323.
76. 9-yr-old Isua sediments, West Greenland: implications for the Archaean carbon and oxygen cycles. Geochim. Cosmochim. Acta 1979, 43:189-199.
77. Steinhoefel G., von Blanckenburg F., Horn I., Konhauser K.O., Beukes N.J., Gutzmer J. Deciphering formation processes of banded iron formations from the Transvaal and the Hamersley successions by combined Si and Fe isotope analysis using UV femtosecond laser ablation. Geochim. Cosmochim. Acta. 2010, 74:2677-2696.
78. Stüeken E.E., Catling D.C., Buick R. Contributions to late Archaean sulphur cycling by life on land. Nat. Geosci. 2012, 5:722-725.
79. Tangalos G.E., Beard B.L., Johnson C.M., Alpers C.N., Shelobolina E.S., Xu H., Konishi H., Roden E.E. Microbial production of isotopically light iron(II) in a modern chemically precipitated sediment and implications for isotopic variations in ancient rocks. Geobiology 2010, 8:197-208.
80. Trendall A.F. The Hamersley Basin. Iron-Formation: Facts and Problems 1983, 69-129. Elsevier, Amsterdam. A.F. Trendall, R.C. Morris (Eds.).
81. Trendall A.F. The significance of iron-formation in the Precambrian stratigraphic record. Spec. Publ. Int. Assoc. Sedimentol. 2002, 33:33-66.
82. Trendall A.F., Blockley J.G. The iron formations of the Precambrian Hamersley Group, Western Australia, GSWA Bulletin 119 1970, Geological Survey of Western Australia, Perth, p. 366.
83. Tronc E., Belleville P., Jolivet J.P., Livage J. Transformation of ferric hydroxide into spinel by Fe(II) adsorption. Langmuir 1992, 8:313-319.
84. Waldbauer J.R., Sherman L.S., Sumner D.Y., Summons R.E. Late Archean molecular fossils from the Transvaal Supergroup record the antiquity of microbial diversity and aerobiosis. Precambrian Res. 2009, 169:28-47.
85. Walker J.C.G. Possible limits on the composition of the Archaean ocean. Nature 1983, 302:518-520.
86. Whitehouse M.J., Fedo C.M. Microscale heterogeneity of Fe isotopes in >3.71Ga banded iron formation from the Isua Greenstone Belt, Southwest Greenland. Geology 2007, 35:719-722.
87. Whitehouse M.J., Kamber B.S., Fedo C.M., Lepland A. Integrated Pb- and S-isotope investigation of sulphide minerals from the early Archaean of southwest Greenland. Chem. Geol. 2005, 222:112-131.
88. Widdel F., Schnell S., Heising S., Ehrenreich A., Assmus B., Schink B. Ferrous iron oxidation by anoxygenic phototrophic bacteria. Nature 1993, 362:834-836.
89. Wiesli R.A., Beard B.L., Johnson C.M. Experimental determination of Fe isotope fractionation between aqueous Fe(II), siderite and "green rust" in abiotic systems. Chem. Geol. 2004, 211:343-362.
90. Wu L., Beard B.L., Roden E.E., Johnson C.M. Stable iron isotope fractionation between aqueous Fe(II) and hydrous ferric oxide. Environ. Sci. Technol. 2011, 45:1847-1852.
91. Wu L., Percak-Dennett E.M., Beard B.L., Roden E.E., Johnson C.M. Stable iron isotope fractionation between aqueous Fe(II) and model Archean ocean Fe-Si coprecipitates and implications for iron isotope variations in the ancient rock record. Geochim. Cosmochim. Acta. 2012, 84:14-28.
92. Yamaguchi K.E., Johnson C.M., Beard B.L., Ohmoto H. Biogeochemical cycling of iron in the Archean-Paleoproterozoic Earth: constraints from iron isotope variations in sedimentary rocks from the Kaapvaal and Pilbara Cratons. Chem. Geol. 2005, 218:135-169.