海洋中微量金属的生物地质化学循环
1Department of Geosciences, Princeton University, Princeton, NJ 08544, USA. morel@princeton.edu
概括
海水中的微生物使用高效的金属吸收系统,释放复合剂以控制微金属的生物可用性. 这一过程影响海洋光合作用和营养循环,表明金属的可用性和浮游生物之间的平衡.
科学领域:
- 海洋化学 海洋化学
- 生物地质化学循环是什么
- 海洋学 海洋学 海洋学
背景情况:
- 表面海水表现出极低度的基本微量金属.
- 微生物在封存和循环这些微量营养素方面发挥着至关重要的作用.
- 微金属的可用性显著影响海洋的初级生产力和营养物质的转化.
研究的目的:
- 研究浮游生物控制海水中微金属度的机制.
- 了解金属生物可用性对海洋光合作用和营养吸收的影响.
- 探索金属度,浮游生物吸收系统和生物化学功能中的金属替代之间的关系.
主要方法:
- 对浮游生物吸收必需金属的分析.
- 研究微生物释放复合剂的研究.
- 对影响微量金属生物利用性的氧化还原反应的研究.
- 评估海洋水柱上部金属循环的情况.
主要成果:
- 浮游生物的吸收导致地表水中的微量金属度极低.
- 微生物的策略包括释放复合剂和催化氧化还原反应.
- 低金属可用性控制光合作用率和营养素 (例如) 的转化和吸收.
- 超高效的浮游生物吸收系统和金属替代是其关键特征.
结论:
- 海洋微生物通过复杂的吸收和循环机制积极调节必需微量金属度.
- 这些生物过程是海洋生产力和营养动态的关键驱动因素.
- 观察到的金属度是生物需求和微生物调节的结果,突出显示了动态平衡.
相关概念视频
What are Biogeochemical Cycles?
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
Metabolism of Chemolithotrophs
Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation. However, because inorganic electron donors...
Microbes and Other Elemental Cycles
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
Marine Microbial Ecology
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Microbial Leaching
Microbial leaching, also known as bioleaching, is an environmentally favorable method for extracting metals from low-grade ores using specific microorganisms. This biotechnological approach is particularly valuable for mining operations targeting copper, gold, and uranium, where traditional extraction methods may be economically or environmentally impractical.Copper Leaching and Microbial CatalysisIn copper bioleaching, crushed ore is arranged into heaps and irrigated with a dilute sulfuric...
Microbial Wastewater Treatment
Microbial communities in aquatic ecosystems play a key role in the natural breakdown of contaminants introduced through domestic and industrial effluents. Acting as biological catalysts, these microbes change and mineralize a wide range of organic and inorganic pollutants under different redox conditions.In oxygen-rich surface waters, aerobic heterotrophs lead organic matter breakdown, using oxygen as the terminal electron acceptor to efficiently oxidize substrates to carbon dioxide and water.


