海洋地质与第四纪地质

参考文献

[1]曾志刚,陈帅,王晓媛,等.东马努斯海盆PACMANUS热液区SiFe-Mn羟基氧化物的矿物学和微形貌特征[J].中国科学:地球科学,2013, 43(1):61-71.[ZENG Zhigang, CHEN Shai, WANG Xiaoyuan,et al. Mineralogical and micromorphological characteristics of Si-FeMn oxyhydroxides from the PACMANUS hydrothermal field, Eastern Manus Basin. Science China:Earth Sciences[J], 2013, 43(1):61-71.]

[2]Alt J C. Hydrothermal oxide and nontronite deposits on seamounts in the Eastern Pacific[J]. Marine Geology, 1988, 81(1):227-239.

[3]Gini C, Jamieson J W, Reeves E P, et al. Iron oxyhydroxide-rich hydrothermal deposits at the high-temperature Favne Vent Field, Mohns Ridge[J]. Geochemistry, Geophysics, Geosystems, 2024, 25(6):e2024GC011481.

[4]Sun Z, Zhou H, Glasby G P, et al. Mineralogical characterization and formation of Fe-Si oxyhydroxide deposits from modern seafloor hydrothermal vents[J]. American Mineralogist, 2013, 98(1):85-97.

[5]Bishop C S, Lichtschlag A, Roberts S, et al. Fe-oxyhydroxide deposits at Semenov hydrothermal field(13°30′N), Mid-Atlantic ridge:insights into formation, modification and resource potential[J]. Mineralium Deposita, 2025, 0026-4598:1432-1866.

[6]Fallon E K, Petersen S, Brooker R A, et al. Oxidative dissolution of hydrothermal mixed-sulphide ore:an assessment of current knowledge in relation to seafloor massive sulphide mining[J]. Ore Geology Reviews, 2017, 86:309-337.

[7]孙治雷,何拥军,李军,等.洋底热液喷口系统的微生物成矿研究进展[J].海洋地质与第四纪地质, 2011, 31(3):123-132.[SUN Zhilei,HE Yongjun, LI Jun, et al. The recent progress of submarine hydrothermal biomineralization[J]. Marine Geology&Quaternary Geology,2011, 31(3):123-132.]

[8]石学法,符亚洲,李兵,等.我国深海矿产研究:进展与发现[J].矿物岩石地球化学通报, 2021, 40(2):305-318.[SHI Xuefa, FU Yazhou,LI Bing, et al. Research on Deep-sea Minerals in China:Progress and Discovery[J]. Bulletin of Mineralogy, Petrology and Geochemistry,2021, 40(2):305-318.]

[9]Hu S, Tao C, Liao S, et al. Transformation of minerals and mobility of heavy metals during oxidative weathering of seafloor massive sulfide and their environmental significance[J]. Science of the Total Environment, 2022, 819:153091.

[10]Knight R D, Roberts S, Cooper M J. Investigating monomineralic and polymineralic reactions during the oxidation of sulphide minerals in seawater:implications for mining seafloor massive sulphide deposits[J]. Applied Geochemistry, 2018, 90:63-74.

[11]Hannington M, Jonasson I. Physical and chemical processes of seafloor mineralization at mid-ocean ridges[M]. US:American Geophysical Union, 1995.

[12]Bilenker L D, Romano G Y, McKibben M A. Kinetics of sulfide mineral oxidation in seawater:implications for acid generation during in situ mining of seafloor hydrothermal vent deposits[J]. Applied Geochemistry, 2016, 75:20-31.

[13]Murr L E. Biological issues in materials science and engineering:interdisciplinarity and the bio-materials paradigm[J]. JOM, 2006, 58(7):23-33.

[14]Gartman A, Luther G W. Oxidation of synthesized sub-micron pyrite(FeS2)in seawater[J]. Geochimica et Cosmochimica Acta, 2014, 144:96-108.

[15]Ortiz-Castillo J E, Mirazimi M, Mohammadi M, et al. The role of microorganisms in the formation, dissolution, and transformation of secondary minerals in mine rock and drainage:a review[J]. Minerals,2021, 11(12):1349.

[16]Tivey M K. Generation of seafloor hydrothermal vent fluids and associated mineral deposits[J]. Oceanography, 2007, 20(1):50-65.

[17]翟世奎.现代海底热液活动的热和物质通量估算[J].海洋学报,2005(2):115-121.[ZHAI Shikui, WANG Xingtao, YU Zenghui, et al. Heat and mass flux estimation of modern seafloor hydrothermal activity[J]. Acta Oceanologica Sinica, 2005(2):115-121.]

[18]Hou X, Han X, Hu X, et al. Formation mechanism of Fe oxyhydroxides and behavior of metals during the oxidation of submarine sulfides at the Wocan-1 Hydrothermal Field, Carlsberg Ridge[J]. Ore Geology Reviews, 2024, 174:106307.

[19]Fortin D, Ferris F G, Scott S D. Formation of Fe-silicates and Fe-oxides on bacterial surfaces in samples collected near hydrothermal vents on the Southern Explorer Ridge in the Northeast Pacific Ocean[J].American Mineralogist, 1998, 83:1399-1408.

[20]曾湘,邵宗泽.深海热液区微生物矿化过程的功能群和分子机制[J].微生物学通报, 2017, 44(4):890-901.[ZENG Xiang, SHAO Zongze.Microbial functional groups and molecular mechanisms for biomineralization in hydrothermal vents[J]. Microbiology China, 2017, 44(4):890-901.]

[21]Chan M A, Hinman N W, Potter-McIntyre S L, et al. Deciphering biosignatures in planetary contexts[J]. Astrobiology, 2019, 19(9):1075-1102.

[22]Kappler A, Bryce C, Mansor M, et al. An evolving view on biogeochemical cycling of iron[J]. Nature Reviews Microbiology, 2021,19(6):360-374.

[23]Edwards K J, Bach W, McCollom T M, et al. Neutrophilic iron-oxidizing bacteria in the ocean:their habitats, diversity, and roles in mineral deposition, rock alteration, and biomass production in the deep-sea[J].Geomicrobiology Journal, 2004, 21(6):393-404.

[24]McAllister S M, Davis R E, McBeth J M, et al. Biodiversity and emerging biogeography of the neutrophilic iron-oxidizing Zetaproteobacteria[J]. Applied and Environmental Microbiology, 2011, 77(15):5445-5457.

[25]Ta K, Chen S, Du M, et al. Iron oxides(oxyhydroxides)associated with biogenic iron-organic framework structures in deep-sea hydrothermal vents of the Indian Ocean[J]. Chemical Geology, 2024, 650:121980.

[26]Boyd T, Scott S. Microbial and hydrothermal aspects of ferric oxyhydroxides and ferrosic hydroxides:the example of Franklin Seamount,Western Woodlark Basin, Papua New Guinea[J]. Geochemical Transactions, 2001, 2(1):45.

[27]Sun Z, Zhou H, Glasby G P, et al. Formation of Fe-Mn-Si oxide and nontronite deposits in hydrothermal fields on the Valu Fa Ridge, Lau Basin[J]. Journal of Asian Earth Sciences, 2012, 43(1):64-76.

[28]Rouxel O, Toner B, Germain Y, et al. Geochemical and iron isotopic insights into hydrothermal iron oxyhydroxide deposit formation at Loihi Seamount[J]. Geochimica et Cosmochimica Acta, 2018, 220:449-482.

[29]Meng X, Jin X, Li X, et al. Mineralogy and geochemistry of secondary minerals and oxyhydroxides from the Xunmei Hydrothermal Field,southern Mid-Atlantic Ridge(26°S):insights for metal mobilization during the oxidation of submarine sulfides[J]. Marine Geology, 2021,442:106654.

[30]Li J, Sun M, Qi W, et al. Geochemical and Sr-Nd-Pb-Fe isotopic constraints on the formation of Fe-Si oxyhydroxide deposits at the ultraslow-spreading southwest Indian ridge[J]. Geochemistry, Geophysics, Geosystems, 2024, 25(2):e2023GC011185.

[31]Hekinian R, Hoffert M, Larque P, et al. Hydrothermal Fe and Si oxyhydroxide deposits from South Pacific intraplate volcanoes and East Pacific Rise axial and off-axial regions[J]. Economic Geology, 1993,88(8):2099-2121.

[32]Maslennikov V V, Cherkashov G A, Firstova A V, et al. Trace element assemblages of pseudomorphic iron oxyhydroxides of the Pobeda-1 Hydrothermal Field, 17°08.7′N, Mid-Atlantic Ridge:the development of a halmyrolysis model from LA-ICP-MS data[J]. Minerals, 2023, 13(1):4.

[33]Dekov V M, Petersen S, Garbe-Schonberg C D, et al. Fe-Si-oxyhydroxide deposits at a slow-spreading centre with thickened oceanic crust:the Lilliput Hydrothermal Field(9°33′S, Mid-Atlantic Ridge)[J].Chemical Geology, 2010, 278(3-4):186-200.

[34]Humphris S E, Klein F. Progress in deciphering the controls on the geochemistry of fluids in seafloor hydrothermal systems[J]. Annual Review of Marine Science, 2018, 10:315-343.

[35]Gonzalez F J, Rincon-Tomas B, Somoza L, et al. Low-temperature,shallow-water hydrothermal vent mineralization following the recent submarine eruption of Tagoro Volcano(El Hierro, Canary Islands)[J].Marine Geology, 2020, 430:106333.

[36]Li B, Wang J, Li C, et al. An oceanic core complex and its associated weathered hydrothermal deposit on a ridge-transform intersection zone at 23°S, Southern Mid-Atlantic Ridge[J]. Marine Geology, 2024,475:107360.

[37]Jamieson J W, Gartman A. Defining active, inactive, and extinct seafloor massive sulfide deposits[J]. Marine Policy, 2020, 117:103926.

[38]Paikaray S. Environmental stability of schwertmannite:a review[J].Mine Water and the Environment, 2021, 40(3):570-586.

[39]Caraballo M A, Asta M P, Perez J P H, et al. Past, present and future global influence and technological applications of iron-bearing metastable nanominerals[J]. Gondwana Research, 2022, 110:283-304.

[40]Dekov V, Boycheva T, Halenius U, et al. Atacamite and paratacamite from the ultramafic-hosted Logatchev Seafloor Vent Field(14°45′N,Mid-Atlantic Ridge)[J]. Chemical Geology, 2011, 286:169-184.

[41]Hannington M. The formation of atacamite during weathering of sulfides on the modern seafloor[J]. Canadian Mineralogist, 1993, 31:945-956.

[42]Herzig P M, Hannington M D, Scott S D, et al. Gold-rich sea-floor gossans in the Troodos ophiolite and on the Mid-Atlantic Ridge[J].Economic Geology, 1991, 86(8):1747-1755.

[43]Lindsay M B J, Moncur M C, Bain J G, et al. Geochemical and mineralogical aspects of sulfide mine tailings[J]. Applied Geochemistry,2015, 57:157-177.

[44]Schwertmann U, Murad E. Effect of pH on the formation of goethite and hematite from ferrihydrite[J]. Clays and Clay Minerals, 1983,31(4):277-284.

[45]Dekov V M, Kamenov G D, Stummeyer J, et al. Hydrothermal nontronite formation at Eolo Seamount(Aeolian Volcanic Arc, Tyrrhenian Sea)[J]. Chemical Geology, 2007, 245(1-2):103-119.

[46]Grantcharova M M, FernAndez-Caliani J C. Soil acidification, mineral neoformation and heavy metal contamination driven by weathering of sulphide wastes in a Ramsar Wetland[J]. Applied Sciences, 2022,12(1):249.

[47]Eftekhari N, Kargar M, Zamin F, et al. A review on various aspects of jarosite and its utilization potentials[J]. Annales De Chimie-Science Des Materiaux, 2020, 44(1):43-52.

[48]Schoepfer V A, Burton E D. Schwertmannite:a review of its occurrence, formation, structure, stability and interactions with oxyanions[J].Earth-Science Reviews, 2021, 221:103811.

[49]Peretyazhko T, Zachara J M, Boily J F, et al. Mineralogical transformations controlling acid mine drainage chemistry[J]. Chemical Geology,2009, 262(3):169-178.

[50]Sun Z, Li J, Huang W, et al. Generation of hydrothermal Fe-Si oxyhydroxide deposit on the southwest Indian ridge and its implication for the origin of ancient banded iron formations[J]. Journal of Geophysical Research:Biogeosciences, 2015, 120(1):187-203.

[51]杨宝菊.东马努斯海盆PACMANUS热液区Si-Fe-Mn氧化物的形成机制及其对热液活动的指示[D].中国科学院大学, 2015.[YANG Baoju. The forming mechnism of Si-Fe-Mn oxides and implications for hydrothermal activity at the PACMANUS hydrothermal field, Eastern Manus Basin[D]. University of Chinese Academy of Sciences, 2015.]

[52]Yang B, Zeng Z, Wang X, et al. Pourbaix diagrams to decipher precipitation conditions of Si-Fe-Mn-oxyhydroxides at the PACMANUS Hydrothermal Field[J]. Acta Oceanologica Sinica, 2014, 33(12):58-66.

[53]Benjamin S B, Haymon R M. Hydrothermal mineral deposits and fossil biota from a young(0.1 Ma)abyssal hill on the flank of the fast spreading east pacific rise:evidence for pulsed hydrothermal flow and tectonic tapping of axial heat and fluids[J]. Geochemistry, Geophysics, Geosystems, 2006, 7(5):2005GC001011.

[54]Juniper S K, Fouquet Y. Filamentous iron-silica deposits from modern and ancient hydrothermal sites[J]. Canadian Mineralogis, 1988, 26:859-869.

[55]Rimstidt J D, Cole D R. Geothermal mineralization; I, the mechanism of formation of the Beowawe, Nevada, siliceous sinter deposit[J].American Journal of Science, 1983, 283(8):861-875.

[56]Janecky D R, Seyfried W E. Formation of massive sulfide deposits on oceanic ridge crests:incremental reaction models for mixing between hydrothermal solutions and seawater[J]. Geochimica et Cosmochimica Acta, 1984, 48(12):2723-2738.

[57]Halbach M, Halbach P, LUders V. Sulfide-impregnated and pure silica precipitates of hydrothermal origin from the Central Indian Ocean[J].Chemical Geology, 2002, 182(2-4):357-375.

[58]Yee N, Phoenix V R, Konhauser K O, et al. The effect of cyanobacteria on silica precipitation at neutral pH:implications for bacterial silicification in geothermal hot springs[J]. Chemical Geology, 2003,199:83-90.

[59]Jones B, Konhauser K O, Renaut R W, et al. Microbial silicification in Iodine Pool, Waimangu Geothermal Area, North Island, New Zealand:implications for recognition and identification of ancient silicified microbes[J]. Journal of the Geological Society, 2004, 161(6):983-993.

[60]Dekov V M, Lalonde S V, Kamenov G D, et al. Geochemistry and mineralogy of a silica chimney from an inactive seafloor hydrothermal field(East Pacific Rise, 18°S)[J]. Chemical Geology, 2015, 415:126-140.

[61]Sauro F, Cappelletti M, Ghezzi D, et al. Microbial diversity and biosignatures of amorphous silica deposits in orthoquartzite caves[J]. Scientific Reports, 2018, 8(1):17569.

[62]Dong A, Sun Z, Kendall B, et al. Insights from modern diffuse-flow hydrothermal systems into the origin of post-GOE deep-water Fe-Si precipitates[J]. Geochimica et Cosmochimica Acta, 2022, 317:1-17.

[63]Toner B M, BerquóT S, Michel F M, et al. Mineralogy of iron microbial mats from Loihi Seamount[J]. Frontiers in Microbiology, 2012,3:118.

[64]Campbell A S, Schwertmann U, Stanjek H, et al. Si incorporation into hematite by heating Si-ferrihydrite[J]. Langmuir, 2002, 18(21):7804-7809.

[65]Schwertmann U, Friedl J, Stanjek H, et al. Iron oxides and smectites in sediments from the Atlantis II Deep, Red Sea[J]. European Journal of Mineralogy, 1998:953-968.

[66]Severmann S, Mills R A, Palmer M R, et al. The origin of clay minerals in active and relict hydrothermal deposits[J]. Geochimica et Cosmochimica Acta, 2004, 68(1):73-88.

[67]Hrischeva E, Scott S D. Geochemistry and morphology of metalliferous sediments and oxyhydroxides from the Endeavour Segment, Juan de Fuca Ridge[J]. Geochimica et Cosmochimica Acta, 2007, 71(14):3476-3497.

[68]Carlson L, Schwertmann U. Natural ferrihydrites in surface deposits from Finland and their association with silica[J]. Geochimica Et Cosmochimica Acta, 1981, 45(3):421-429.

[69]Swedlund P J, Webster J G. Adsorption and polymerisation of silicic acid on ferrihydrite, and its effect on arsenic adsorption[J]. Water Research, 1999, 33(16):3413-3422.

[70]Pokrovski G S, Schott J, Fran?ois Farges, et al. Iron(III)-silica interactions in aqueous solution:insights from X-ray absorption fine structure spectroscopy[J]. Geochimica Et Cosmochimica Acta, 2003, 67(19):3559-3573.

[71]Cole T. The nature and origin of smectite in the Atlantis II Deep, Red Sea[J]. Canadian Mineralogist, 1988, 26:755-76.

[72]Kohler B, Singer A, Stoffers P. Biogenic nontronite from marine white smoker chimneys[J]. Clays and Clay Minerals, 1994, 42(6):689-701.

[73]Ueshima M, Tazaki K. Possible role of microbial polysaccharides in nontronite formation[J]. Clays and Clay Minerals, 2001, 49(4):292-299.

[74]Cuadros J, Dekov V M, Arroyo X, et al. Smectite formation in submarine hydrothermal sediments:samples from the HMS challenger expedition[J]. Clays and Clay Minerals, 2011, 59(2):147-164.

[75]Cuadros J, Segvic B, Dekov V, et al. Electron microscopy investigation of the genetic link between Fe oxides/oxyhydroxides and nontronite in submarine hydrothermal fields[J]. Marine Geology, 2018, 395:247-259.

[76]Edwards K J. Formation and degradation of seafloor hydrothermal sulfide deposits[M]. Geological Society of America, 2004.

[77]Emerson D, Moyer C L. Neutrophilic Fe-oxidizing bacteria are abundant at the Loihi Seamount hydrothermal vents and play a major role in Fe oxide deposition[J]. Applied and Environmental Microbiology,2002, 68(6):3085-3093.

[78]Emerson D, Fleming E J, McBeth J M. Iron-oxidizing bacteria:an environmental and genomic perspective[J]. Annual Review of Microbiology, 2010, 64(1):561-583.

[79]Kikuchi S, Makita H, Mitsunobu S, et al. Application of synchrotronμ-XRF-XAFS to the speciation of Fe on a single stalk in bacteriogenic iron oxides(BIOS)[J]. Chemistry Letters, 2011, 40(7):680-681.

[80]McAllister S M, Moore R M, Gartman A, et al. The Fe(II)-oxidizing Zetaproteobacteria historical, ecological and genomic perspectives[J].FEMS Microbiology Ecology, 2019, 95(4):fiz015.

[81]Makita H, Kikuchi S, Mitsunobu S, et al. Comparative analysis of microbial communities in iron-dominated flocculent mats in deep-sea hydrothermal environments[J]. Applied and Environmental Microbiology, 2016, 82(19):5741-5755.

[82]Anderson C R, James R E, Fru E C, et al. In situ ecological development of a bacteriogenic iron oxide-producing microbial community from a subsurface granitic rock environment[J]. Geobiology, 2006,4(1):29-42.

[83]Maisch M, Lueder U, Laufer K, et al. Contribution of microaerophilic iron(II)-oxidizers to iron(III)mineral formation[J]. Environmental Science&Technology, 2019, 53(14):8197-8204.

[84]Druschel G K, Emerson D, Sutka R, et al. Low-oxygen and chemical kinetic constraints on the geochemical niche of neutrophilic iron(II)oxidizing microorganisms[J]. Geochimica et Cosmochimica Acta, 2008,72(14):3358-3370.

[85]Kasama T, Murakami T. The effect of microorganisms on Fe precipitation rates at neutral pH[J]. Chemical Geology, 2001, 180(1):117-128.

[86]Emerson D. Biogeochemistry and microbiology of microaerobic Fe(II)oxidation[J]. Biochemical Society Transactions, 2012, 40(6):1211-1216.

[87]Chan C S, McAllister S M, Leavitt A H, et al. The architecture of iron microbial mats reflects the adaptation of chemolithotrophic iron oxidation in freshwater and marine environments[J]. Frontiers in Microbiology, 2016, 7:796.

[88]Posth N R, Canfield D E, Kappler A. Biogenic Fe(III)minerals:from formation to diagenesis and preservation in the rock record[J]. EarthScience Reviews, 2014, 135:103-121.

[89]Fleming E J, Langdon A E, Martinez-Garcia M, et al. What’s new is old:resolving the identity of Leptothrix ochracea using single cell genomics, pyrosequencing and FISH[J]. PLOS One, 2011, 6(3):e17769.

[90]Emerson D, Rentz J A, Lilburn T G, et al. A novel lineage of proteobacteria involved in formation of marine Fe-oxidizing microbial mat communities[J]. PLOS One, 2007, 2(8):e667.

[91]Chan C S, Fakra S C, Emerson D, et al. Lithotrophic iron-oxidizing bacteria produce organic stalks to control mineral growth:implications for biosignature formation[J]. ISME Journal, 2011, 5(4):717-727.

[92]Hallberg R, Ferris F G. Biomineralization by Gallionella[J]. Geomicrobiology Journal, 2004, 21(5):325-330.

[93]Suzuki T, Hashimoto H, Matsumoto N, et al. Nanometer-scale visualization and structural analysis of the inorganic/organic hybrid structure of Gallionella ferruginea twisted stalks[J]. Applied and Environmental Microbiology, 2011, 77(9):2877-2881.

[94]Langley S, Igric P, Takahashi Y, et al. Preliminary characterization and biological reduction of putative biogenic iron oxides(BIOS)from the Tonga-Kermadec Arc, Southwest Pacific Ocean[J]. Geobiology, 2009,7:35-49.

[95]Makita H. Iron-oxidizing bacteria in marine environments:recent progresses and future directions[J]. World Journal of Microbiology and Biotechnology, 2018, 34:110.

[96]Aubineau J, Chi Fru E, Destrigneville C, et al. Iron-rich microband formation in marine sediments by hydrothermal iron cycling bacteria at Lucky Strike[J]. Communications Earth&Environment, 2025, 6:338.

[97]Chan C S, Emerson D, Luther G W. The role of microaerophilic Fe-oxidizing micro-organisms in producing banded iron formations[J]. Geobiology, 2016, 14:509-528.

[98]Moeller K, Schoenberg R, Grenne T, et al. Comparison of iron isotope variations in modern and ordovician siliceous Fe oxyhydroxide deposits[J]. Geochimica et Cosmochimica Acta, 2014, 126:422-440.

[99]Planavsky N, Rouxel O, Bekker A, et al. Iron-oxidizing microbial ecosystems thrived in late Paleoproterozoic redox-stratified oceans[J],Earth and Planetary Science Letters, 2009, 286:230-242.