Ocean Crust Alteration and the Deep Biosphere

洋壳变化与深层生物圈

• 批准号: 0752541
• 负责人: Everett Shock
• 金额: $ 28.39万
• 依托单位: Arizona State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-03-01 至 2012-02-29
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0752541&HistoricalAwards=false
• 关键词: Ocean; Crust; Alteration; Deep; Biosphere

ABSTRACT-0752541 (Shock)Intellectual Merit: This research provides the theoretical framework and tools needed to model and interpret the increasing evidence for the presence and actions of microbes in the deep biosphere in oceanic crust. It will also allow us to make predictions of microbial habitation and metabolic mechanisms which will ensure greater returns on the costly investments required to access the deep biosphere through seafloor exploration and drilling. This research uses existing data on diffuse fluids and altered rocks from subsurface basalt aquifers to quantify the supply of energy that can be used by microbes. Work to codify the interactions between essential biomolecules and enzymes and geological materials will permit the prediction of mechanisms of microbial metabolism as function of temperature, pressure, fluid composition, and extent of rock alteration. Justification for the work comes from the fact that the deep biosphere in the oceanic crust is sustained by the disequilibrium between seawater and igneous rocks. Recent work provides estimates of the supply of energy that supports the deep biosphere derived from observations of the extent of oxidative alteration of basalts and other crustal igneous rocks that suggest the portion of the deep biosphere hosted in altering igneous rocks may rival that in seafloor sediments. As a result, the deep biosphere has become a major target for Earth exploration, but lack of knowledge of the signatures of and metabolic needs of microbes in the subsurface have prevented us from adequately investigating their presence and importance. This research attacks this issue. Broader Impacts: Broader impacts of the work include development of a thermodynamic framework for microbiological processes that will be made publicly available on the Internet. Results of the work also cross over into biology and can be used by environmental scientists for the bioremediation of toxic waste and the downstream impacts of engineered nanoparticles. The work also supports the training of graduate and undergraduate students and the creation of a display for the Arizona State University Open House and Museum on the deep biosphere. Work will complement activities in both NSF's IODP and Ocean Observing Systems Programs.

摘要-0752541（震惊）智力价值：这项研究提供了建模和解释海洋地壳深层生物圈中微生物存在和活动的越来越多的证据所需的理论框架和工具。 它还将使我们能够预测微生物的栖息和代谢机制，这将确保通过海底勘探和钻探进入深层生物圈所需的昂贵投资获得更大的回报。 这项研究利用地下玄武岩含水层中扩散流体和蚀变岩石的现有数据来量化可供微生物使用的能量供应。 编纂基本生物分子和酶与地质材料之间的相互作用的工作将允许预测微生物代谢机制作为温度、压力、流体成分和岩石蚀变程度的函数。 这项工作的理由来自于海洋地壳中的深层生物圈是由海水和火成岩之间的不平衡维持的。最近的工作提供了支持深层生物圈的能量供应的估计，这些估计来自对玄武岩和其他地壳火成岩的氧化蚀变程度的观察，这表明深层生物圈中存在于蚀变火成岩中的部分可能与海底沉积物中的部分相媲美。因此，深层生物圈已成为地球探索的主要目标，但缺乏对地下微生物的特征和代谢需求的了解，使我们无法充分调查它们的存在和重要性。 这项研究攻击这个问题。更广泛的影响：这项工作的更广泛的影响包括为微生物过程制定一个热力学框架，该框架将在互联网上公布。 这项工作的结果也跨越到生物学领域，可以被环境科学家用于有毒废物的生物修复和工程纳米颗粒的下游影响。 这项工作还支持研究生和本科生的培训，并为亚利桑那州立大学开放日和博物馆举办关于深层生物圈的展览。 这项工作将补充NSF的IODP和海洋观测系统计划的活动。