岩石不混合性为 prebiotic 化学提供酸盐.
Daniel Weller1, Thomas Matreux2,3, Iris B A Smokers4
1Earth and Environmental Sciences, Ludwig Maximilians University, Munich, Germany.
Science advances
|November 19, 2025
概括
火山过程可能会丰富酸盐,这是生命的关键元素. 酸盐与酸盐在化物中的不混合性会产生富含酸盐的液滴,从而使早期地球上产生了前生物化学物质.
科学领域:
- 地质化学 地质化学
- 天体生物学 天体生物学
- 益生菌化学 益生菌化学
背景情况:
- 对于生命至关重要,但它的稀缺性和矿物不溶性阻碍了早期的地球化学.
- 益生菌化学需要可获得的化合物来源.
研究的目的:
- 为了研究酸盐-酸盐在火山融中的不混合性,作为酸盐丰富的机制.
- 评估火山过程的潜力,以供应用于前生物合成.
主要方法:
- 模拟具有高含量的古老火山融化.
- 诱导快速冷却以观察不混合性和滴滴形成.
- 对酸盐度进行滴滴成分分析和浸出实验.
- 从化酸盐中测试化剂的合成.
主要成果:
- 富含的溶液的快速冷却形成了不混合的玻璃状滴,含有高达21%的氧化.
- 这些水滴由火山发射到地表.
- 水性浸产生了毫米度的酸盐度.
- 聚酸盐和伊米达酸盐的成功合成,产量高达34%.
结论:
- 在火山融化中酸盐-酸盐不混合性是缩酸盐的可行机制.
- 火山过程可能为地球早期的前生物化学提供了必需的酸盐.
更多相关视频
11:50Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
12.9K
12:55Chemical Gardens as Flow-through Reactors Simulating Natural Hydrothermal Systems
Published on: November 18, 2015
14.9K
相关概念视频
Conditions on Early Earth
100.3K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
100.3K
The Phosphorus Cycle
43.5K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
43.5K
Diversity of Archaea IV
381
Hyperthermophilic archaea are a group of extremophiles thriving at temperatures above 80°C, often in hydrothermal vents and volcanic soils where conditions surpass the boiling point of water. At such temperatures, proteins, membranes, and DNA in most organisms degrade, but hyperthermophiles have evolved remarkable adaptations to maintain stability and function.Unique Cellular FeaturesHyperthermophilic membranes are composed of a monolayer of biphytanyl tetraether lipids, which resist...
381
Metabolism of Chemolithotrophs
733
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.
733
Diversity of Archaea I
518
Archaea, a domain of single-celled microorganisms, are classified into five major phyla based on genetic and biochemical characteristics: Euryarchaeota, Crenarchaeota, Thaumarchaeota, Korarchaeota, and Nanoarchaeota. Among these, the phylum Euryarchaeota is notable for its remarkable diversity in morphology, metabolism, and ecological adaptations.Morphological and Metabolic DiversityMembers of Euryarchaeota exhibit a variety of cellular shapes, including rods and cocci. Their metabolic pathways...
518
Biosynthesis of Lipids
499
Microbial membranes exhibit remarkable diversity in lipid composition, reflecting evolutionary adaptations to various environmental conditions. The three domains of life—Bacteria, Archaea, and Eukarya—synthesize membrane lipids through distinct biosynthetic pathways, leading to fundamental structural differences that impact membrane stability, function, and adaptability.Fatty Acid-Based Lipids in Bacteria and EukaryaBacteria and eukaryotes share a common fatty acid biosynthesis...
499
