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IODP Expedition 337: Deep Coalbed Biosphere off Shimokita – Microbial processes and hydrocarbon system associated with deeply buried coalbed in the ocean

机译:IODP第337号探险:下北田以外的深层煤层生物圈–与海洋深层煤层相关的微生物过程和碳氢化合物系统

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pstrongAbstract./strong The Integrated Ocean Drilling Program (IODP) Expedition 337 was the first expedition dedicated to subseafloor microbiology that used riser-drilling technology with the drilling vessel iChikyu/i. The drilling Site C0020 is located in a forearc basin formed by the subduction of the Pacific Plate off the Shimokita Peninsula, Japan, at a water depth of 1180span class="thinspace"/spanm. Primary scientific objectives during Expedition 337 were to study the relationship between the deep microbial biosphere and a series of ?~?span class="thinspace"/span2span class="thinspace"/spankm deep subseafloor coalbeds and to explore the limits of life in the deepest horizons ever probed by scientific ocean drilling. To address these scientific objectives, we penetrated a 2.466span class="thinspace"/spankm deep sedimentary sequence with a series of lignite layers buried around 2span class="thinspace"/spankm below the seafloor. The cored sediments, as well as cuttings and logging data, showed a record of dynamically changing depositional environments in the former forearc basin off the Shimokita Peninsula during the late Oligocene and Miocene, ranging from warm-temperate coastal backswamps to a cool water continental shelf. The occurrence of small microbial populations and their methanogenic activity were confirmed down to the bottom of the hole by microbiological and biogeochemical analyses. The factors controlling the size and viability of ultra-deep microbial communities in those warm sedimentary habitats could be the increase in demand of energy and water expended on the enzymatic repair of biomolecules as a function of the burial depth. Expedition 337 provided a test ground for the use of riser-drilling technology to address geobiological and biogeochemical objectives and was therefore a crucial step toward the next phase of deep scientific ocean drilling./p.
机译:> >摘要。海洋综合钻探计划(IODP)337探险队是第一项专门用于海底微生物学的探险,该探险队使用了升船钻井技术和Chikyu 船。钻井地点C0020位于前太平洋盆地中,该太平洋盆地由日本下北田半岛附近的太平洋板块俯冲而成,水深为1180 class =“ thinspace”> m。 337号探险队的主要科学目标是研究深层微生物生物圈与一系列深达千米的?〜? class =“ thinspace”> 2 class =“ thinspace”> km之间的关系。海底煤层,并通过科学的海洋钻探探索最深层的生命极限。为了实现这些科学目标,我们穿透了2.466 class =“ thinspace”> km的深层沉积层序,在其下方2 class =“ thinspace”> km周围埋有一系列褐煤层。海底。岩心沉积物以及钻屑和测井数据显示,在渐新世和中新世末期,下积田半岛前前臂盆地的沉积环境动态变化,记录范围从温带沿海回潮到凉水大陆架。通过微生物学和生物地球化学分析,确认了小微生物种群的发生及其产甲烷活性,直至孔的底部。在这些温暖的沉积栖息地中,控制超深微生物群落规模和生存力的因素可能是生物分子的酶修复所消耗的能量和水的需求随埋葬深度的增加而增加。 337探险队提供了使用立管钻井技术解决地球生物学和生物地球化学目标的试验场,因此是迈向下一阶段的深海科学海洋钻探的关键一步。

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