[1] Rudnick R L, Gao S. Composition of the continental crust[C]∥Rudnick R L, ed. Treaise on Geochemistry Volume 3: The crust.Amsterdam: Elsevier Press,2004:1-64.

[2] Beard B L, Johnson C M. Fe isotope variations in the modern and ancient earth and other planetary bodies[J]. Review Mineralogy & Geochemistry, 2004, 55: 319-357.

[3] Albarède F, Beard B L. Analytical methods for non-traditional isotopes[J]. Review Mineralogy & Geochemistry, 2004, 55: 113-151.

[4] Arnold G L, Weyer S, Anbar A D. Fe isotope variations in natural materials measured using high mass resolution multiple collector ICPMS [J]. Analytical Chemistry, 2004, 76: 322-327.

[5] Weyer S, Schwieters J B. High precision Fe isotope measurements with high mass resolution MCICPMS [J]. International Journal of Mass Spectrometry,2003,226:355-368.

[6] Beard B L, Johnson C M. High Precision iron isotope measurements of terrestrial and lunar material [J]. Geochimica et Cosmochimica Acta,1999, 63:1 653-1 660.

[7] Zhu X K, O′Nions R K, Guo Y, et al. Secular variation of iron isotopes in north Atlantic Deep Water [J]. Science,2000,287:2 000-2 002.

[8] Zhu X K, Guo Y, O'Nions R K, et al. Isotopic homogeneity of iron in the early solar nebula [J]. Nature,2001, 412:311-313.

[9] Johnson C M, Beard B L. Biogeochemical cycling of iron isotope [J]. Science,2005,309:1 025-1 027.

[10] Anbar A D. Iron stable isotopes: Beyond biosignatures [J]. Earth and Planetary Science Letter,2004, 217:223-236.

[11] Yu Jimin, Jiang Shaoyong. Recent adances in Fe isotope geochemistry [J]. Journal of Nanjing University (Natural Sciences), 2001, 37(3): 385-389.[于际民,蒋少涌. Fe 同位素地球化学进展 [J]. 南京大学学报:自然科学版,2001,37(3):385-389.]

[12] Jiang Shaoyong. Transition metal isotopes: analytical methods and geology applications [J]. Earth Science Frontiers, 2003, 10 (2): 269-278.[蒋少涌. 过渡族金属元素同位素分析方法及其地质应用 [J]. 地学前缘,2003,10(2):269-278.

[13] Skulan J L, Beard B L, Johnson C M, Kinetic and equilibrium Fe isotope fractionation between aqueous Fe(III) and hematite[J]. Geochimica et Cosmochimica Acta,2002,66:2 995-3 015.

[14] Beard B L, Johnson C M. High precision iron isotope measurements of terrestrial and lunar materials [J]. Geochimica et Cosmochimica Acta,1999, 63:1 653-1 660.

[15] Johnson K S, Gordon R M, Coale K H. What controls dissolved iron concentrations in the world ocean?[J]. Marine Chemistry,1997, 57:137-161.

[16] Wu J, Boyle E A, Wen L. Soluble and colloidal iron in the oligotrophic North Atlantic and North Pacific [J]. Science,2001,293: 847-849.

[17] Jickells T D, An Z S, Andersen K K, et al. Global iron connections between desert dust, ocean biogeochemistry, and climate[J]. Science,2005, 308: 67-71.

[18] Ussher S J, Achterberg E R, Worsfold P. Marine biogeochemistry of iron[J]. Environmental Chemistry, 2004, 1: 67-80.

[19] Alt J C. Hydrothermal fluxes at mid-ocean ridges and on ridge flanks, C R [J]. Geoscience, 2003, 335: 853-864.

[20] Bergquist B, Boyle E. Iron isotopic composition of Amazon River [N]. EOS(Transactions, American Geophysical Union),2002, 83: OS12C-0290.

[21] Fantle M S, DePaolo D J, The isotopic composition of continental iron and implications for the global Fe cycle [N]. EOS, Transactions, American Geophysical Union, 2002, 83: V22B-1234.

[22] Matthews A, Zhu X-K, O'Nions R K. Kinetic iron stable isotope fractionation between iron (-II) and (-III) complexes in solution[J]. Earth Planetary Science Letter, 2001, 192: 81-92.

[23] Rouxel O, Sholkovitz E. Large Scale Iron Isotope Fractionation in Subterranean Estuaries[J]. Geophysical Research Abstracts,2006,8:05141.

[24] Elrod V A, Berelson W M, Coale K H, et al. The flux of iron from continental shelf sediments: A missing source for global budgets [J]. Geophysical Research Letter,2004,31:L12307. doi:10.1029/2004GL020216.

[25] Severmann S, Johnson C M, Beard B L, et al. The effect of early diagenesis on the Fe isotope compositions of poreeaters and authigenic minerals in continental margin sediments[J]. Geochimica et Cosmochimica Acta, 2006, in press.

[26] Beard B L, Johnson C M, Von Damm K L. Poulson RLIron isotope constraints on Fe cycling and mass balance in the oxygenated Earth oceans[J]. Geology,2003,31:629-632.

[27] Koschinsky A, Halback P. Sequential leaching of marine ferromanganese precipitates: Genetic implications[J]. Geochimica et Cosmochimica Acta,1995,59:5 113-5 132.

[28] Chu N C, Johnson C M, Beard B L, et al. Evidence for hydrothermal venting in the Fe isotope compositions of deep Pacific ocean through time[J]. Earth Planetary Science Letter,2006,in press.

[29] Yang Y M, Rouxel O, Shi X F, et al. Fe isotope composition of Fe-Mn crusts in Pacific and its significance for Paleoceanography[J]. Geophysical Research Abstracts,2006,8:08710.

[30] Levasseur S, Frank M, Hein, J R, et al. The global variation in the iron isotope composition of marine hydrogenetic ferromanganese deposits: implications for seawater chemistry?[J]. Earth and Planetary Science Letter, 2004, 224:91-105.

[31] Severmann S, Johnson C M, Beard B L, et al. The effect of plume processes on the Fe isotope composition of hydrothermally derieved Fe in the deep oceans as inferred from the Rainbow vent site, Mid-Atlantic Ridge, 36^o14'N [J]. Earth and Planetary Science Letter,2004,225(1/2):63-76.

[32] Polyakov V B, Mineev S D. The use of Mössbauer spectroscopy in stable isotope geochemistry [J]. Geochimica et Cosmochimica Acta,2000,64:849-865.

[33] Rouxel O, Fouquet Y, Ludden J N, Subsurface processes at the Lucky Strike Hydrothermal Field, Mid-Atlantic Ridge: Evidence from sulfur, selenium, and iron isotopes[J]. Geochimica et Cosmochimica Acta,2004,68:2 295-2 311.

[34] Sharma M, Polizzotto M, Anbar A D. Iron isotopes in hot springs along the Juan de Fuca Ridge [J]. Earth and Planetary Science Letter, 2001, 194:39-51.

[35] Graham S, Pearson N, Jackson S, et al. Tracing Cu and Fe from source to porphyry: In situ determination of Cu and Fe isotope ratios in sulfides from the Grasberg Cu Au deposit [J]. Chemical Geology,2004,207:147-169.

[36] Staudigel H, Plank, T, White B, et al. Geochemical fluxes during seafloor alteration of the basaltic upper oceanic crust: DSDP sites 418 and 417[C]∥Bebout G, et al. eds. Subduction: Top to bottom. Washington DC: Americal Geophysical Union, 1996:19-38.

[37] Rouxel O, Dobbek N, Ludden J, et al. Iron isotope fractionation during oceanic crust alteration[J]. Chemical  Geology,2003,202:155-182.

[38] Bekker A, Holland H D, Wang P-L, et al. Dating the rise of atmospheric oxygen [J]. Nature, 2004, 427:117-20.

[39] Canfield D E. A new model for Proterozoic ocean chemistry[J].Nature,1998, 396:450-453.

[40] Canfield D E. The early history of atmospheric oxygen: Homage to Robert M Gerrels. Annu[J]. Review in Earth Planetary Science,2005,33:1-36.

[41] Farquhar J, Bao H M, Thiemens M. Atmospheric influence of Earth's earliest sulfur cycle[J]. Science,2000, 289:756-58.

[42] Johnson C M, Beard B L, Beukes N J, et al. Ancient geochemical cycling in the Earth as inferred from Fe isotope studies of banded iron formations from the Transvaal Craton [J]. Contribution to Mineralogy and Petrology, 2003, 144:523-547.

[43] Rouxel O, Bekker A, Edwards K. Iron isotope constraints on the archean and Paleoproerozoic ocean redox state[J]. Science,2005,307:1 088-1 091.