冲绳海槽海底硫化物中微生物矿化研究
A study on the microbial mineralization in submarine black smoker chimneys from the Okinawa Trough
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摘要: 报道了冲绳海槽伊平屋海洼海底黑烟囱样品中保留完好的矿化微生物群,它们的形态完好。主要有四种不同类型的丝状体,这些丝状体可能是硫或者铁氧化化能自养细菌和真菌矿化而成。对这些微生物矿化过程的研究表明,它们主要经过了两个阶段的矿化:(1)生物控制矿化阶段;(2)生物诱导矿化阶段。早期以生物控制矿化为主,晚期以生物诱导矿化为主。形成的矿物与热液成分以及微生物种类有关。Abstract: Large amounts of microfossil records have been discovered in the seafloor black smoker chimney from the Okinawa Trough. They preserve good shapes,many of which can be divided into four kinds of filamentous microfossils. It suggested that the fossils may be derived from sulfur or iron oxidation chemolithotrophic prokar yotes and fungi. Two steps of biomineralization were hypot hesized based on the comparison studies of the microbial mineralization processes:(1)biology-controlled mineralization;(2)biology-induced mineralization. At the earlier stage the biology-controlled mineralization is as a main process,at the later stage biomineralizalion is dominated by the biology-induced mineralization.The composition of the fluids and the species of the microbes will decide the types of the minerals formed.
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Key words:
- micro fossils /
- biomineralization /
- black smoker /
- Okinawa Trough
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COOK T L,STAKES D S.Biogeological mineralization in deep-sea hydrothermal deposits[J].Science,1995,267:1975-1979. FOUQUET Y,STACKEBERG U,CHALOU J L,et al.Hydrothermal activity in the Lau back-are basin;sulfides and water chemistry[J].Geology,1991,19:303-306. FOUQUET Y,STACKEBERG U,CHALOU J L,et al.MetaUogenesis in back-arc environments:the Lau Basin example[J].Economic Geology,1993,88:2154-2181. HAYMON R M,KOSKI R A,ABRAMS M J.Hydrothermal discharge zones beneath massive sulfide deposits mapped in the Oman ophiolite[J].Geology,1989,17:531-535. SCOTT S D.Minerals on land,minerals in the sea[J].Geotimes,2002,47:1-8. 冯军,李江海,陈征,等.海底黑烟囱与生命起源综述[J].北京大学学报(自然科学版),2004,40(2):318-325. KIMURA M.Active hydrothermal mounds in the Okinawa Trough backarc basin,Japan[J].Tectonophysics,1988,145 (3-4):319-324. 高爱国,何丽娟.冲绳海槽伊是名海洼的热水活动特征[J].海洋科学,1996,1:26-29. 蒋富清.冲绳海槽现代海底热液活动研究概况[J].海洋科学,1998,6:25-28. 马军英,翟世奎.冲绳海槽伊平屋海底热液活动区的生物群[J].海洋科学,1996,2:30-34. 曾志刚,蒋富清,翟世奎,等.冲绳海槽中部Jade热液活动区中海底热液沉积物的硫同位素组成及其地质意义[J].海洋学报,2000,22(4):74-82. 冯军,李江海,牛向龙.冲绳海槽海底黑烟囱中微生物化石的发现及其意义[J].微体占生物学报,2006,23(1):57-61. HOFMANN B A,FARMER J D.Filamentous fabrics in low-temperature mineral assemblages;are they fossil biomarkers? Implications for the search for a subsurface fossil record on the early earth and mars[J].Planetary and Space Science.2000,48;1077-1086. WESTAL F,WIT M J,DANN J,et al.Early Archean fossil bacteria and biofilms in hydrothermally influenced sediments from the Barberton greenstoue belt,South Africa[J].Precambrian Research,2001,106:93-116. SOUTHAM G,DONALD R.A structural comparison of bacterial microfossils vs "nanobacteria" and nanofossils[J].Earth-cience Reviews,1999,48:251-264. 冯军,李江海,牛向龙.热泉微生物化石的识别研究及其科学意义[J].微体古生物学报,2005,22(2):136-142. BANFIELD J F,WELCH S A,ZHANG Heng-zhong,et al.Aggregation-based crystal growth and microstructure development in natural iron oxyhydroxide biomineralization products[J].Science,2000,289:751-754. JUNIPER S K,FOUQUET Y.Filamentous iron-silica deposits from modern and ancient hydrothermal sites[J].Canadian Mineralogist,1988,26.-859-869. TAYLOR C D,WlRSEN C O.Microbiology and ecology of filamentous sulfur formation[J,].Science,1997,277:1483-1485. LOWENSTAM H A.Minerals formed by organisms[J].Nature,1981,211:1126-1131. 田崎和江.微生物おつく鉱物[J].地質ニュ一ス,1995,489:17-30. FORTIN D,FERRIS G F,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. FORTIN D,SOUTHAM G,BEVERIDGE T J.An examination of iron sulfide,iron-nickel sulfide and nickel sulfide precipitation by a Desulfotomaculum species:and its nickel resistance mechanisms[J].FEMS Microbiol Ecol,1994,14;121-132. GORBY Y A,LOVLEY D A.Enzymatic uranium precipitation[J].Environ Sci Technol,1992,26,205-207. PRACEJUS B,HALBACH P.Do marine moulds influence Hg and Si precipitation in the hydrothermal JADE field (Okinawa Trough)?[J] Chemical Geology,1996,130:87-99. KONHAUSER K O.Diversity of bacterial iron mineralization[J].Earth-Science Reviews,1998,43:91-121. KONHAUSER K O,PHOENIX V R,BOTTRELL S H,et al.Microbial-silica interactions in Icelandic hot spring sinter:possible analogues for some Precambrian siliceous stromatolites[J].Sedimentology,2001,48,415-433. URRUTIA M,KEMPER M,DOYLE R,et al.The membrane-induced proton motive force influences the metal binding ability of Bacillus subtilis cell walls[J].Appl Environ Mierobiol,1992,58:3837-3844.
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