这为研究河口区氧化还原敏感元素的生物地球化学过程提供了天然的实验场所。
As a natural laboratory, studies of the Yangtze Estuary maybe provide insight into for examining biogeochemical processes of redox sensitive elements in hypoxia environments.
海底缺氧带甲烷氧化作用是一个重要的甲烷生物地球化学过程，已被许多地球化学现象所证实。
Anaerobic methane oxidation (AMO) is a globally important biogeochemistry process, which has been identified by sufficient geochemical evidence.
矿物-水-微生物体系在分子级别上之相互作用的定量研究，对于理解低温地球化学和生物地球化学过程将是重要的。
Quantitative study of the interactions in the system of mineral-water-micro be at the molecular level will be important for understanding low-temperature geochemical and biogeochemical processes.
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