在依赖和铁的海洋甲氧化过程中
Emily J Beal1, Christopher H House, Victoria J Orphan
1Department of Geosciences and Penn State Astrobiology Research Center, Pennsylvania State University, University Park, PA 16802, USA. ejbeal@gmail.com
概括
厌氧甲氧化 (AOM) 可以使用铁和,而不仅仅是硫酸盐. 这一发现扩大了我们对甲循环及其在地球气候调节中的作用的理解.
科学领域:
- 环境微生物学环境微生物学
- 生物地质化学循环 生物地质化学循环
- 气候科学是气候科学.
背景情况:
- 厌氧甲类植物对于调节地球气候至关重要.
- 甲的无氧氧化 (AOM) 通常被认为是硫酸盐依赖的.
- 其他电子受体在能量方面对AOM比硫酸盐更有利.
研究的目的:
- 研究海洋环境中无氧甲氧化的替代电子受体.
- 为了确定和铁是否可以在海洋沉积物中支持AOM.
主要方法:
- 从加利福尼亚州的鱼河流域收集的海洋甲入沉积物.
- 富含的微生物群落能够无氧化甲氧化.
- 评估了 (birnessite) 和铁 (ferrihydrite) 作为甲氧化过程中的电子受体的利用.
主要成果:
- 来自海洋甲入沉积物的微生物可以使用和铁氧化甲.
- 这表明,海洋AOM与比以前认可的更广泛的氧化剂相结合.
- 和铁由河流向海洋供应,这表明潜在的全球意义.
结论:
- 甲的海洋无氧氧化不仅限于作为电子受体的硫酸盐.
- 依赖和铁的AOM有可能成为全球重要的工艺.
- 这扩大了影响甲循环和气候调节的已知微生物通路.
相关概念视频
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...
Microbes and the Sulfur Cycle
Sulfur is a vital element in Earth's biogeochemical systems. It transitions through various inorganic states, including sulfate (SO₄²⁻), elemental sulfur (S⁰), and sulfide (S²⁻). Abiotic and biological mechanisms across oxic and anoxic environments intricately mediate these transformations. Sulfate, the most oxidized form of sulfur, is predominantly stored in rocks, marine sediments, and oceanic waters, acting as a long-term reservoir in the global sulfur cycle.In oxic environments,...
Microbes and Methanogenesis
Methanogenesis is a critical microbial process in anaerobic ecosystems responsible for the biological production of methane, a potent greenhouse gas and valuable biofuel. This metabolic pathway is primarily facilitated by methanogenic archaea, which thrive in anoxic environments such as wetlands, sediments, and animal gastrointestinal tracts. The absence of oxygen in these habitats prevents aerobic respiration, thereby favoring alternative biochemical pathways for organic matter degradation.In...
Microbial Corrosion
Microbiologically Influenced Corrosion (MIC) is a significant form of material degradation caused by the metabolic activities of microorganisms. This phenomenon poses substantial challenges across various industries, including oil and gas, maritime, and water treatment sectors.MIC occurs when microorganisms, such as bacteria, archaea, and fungi, colonize metal surfaces, forming biofilms that alter the local electrochemical environment. These biofilms can lead to the production of corrosive...
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...
Radical Oxidation of Allylic and Benzylic Alcohols
Activated manganese(IV) oxide can selectively oxidize allylic and benzylic alcohols via a radical intermediate mechanism. Primary allylic alcohols are oxidized to aldehydes, while secondary allylic alcohols yield ketones. The redox reaction of potassium permanganate with an Mn(II) salt such as manganese sulfate (under either alkaline or acidic conditions), followed by thorough drying, yields the oxidizing agent: activated MnO2. While MnO2 is insoluble in the solvents used for the reaction, the...


