14亿年前,地球表面环境的广泛全球氧化
Hao Yan1, Zheng Qin2, Lingang Xu3
1School of Earth Sciences and Resources, China University of Geosciences, Beijing, China.
Nature communications
|November 26, 2025
概括
中原生态时代的全球氧化程度比以前想象的要高. 来自古代岩石的新证据表明,大约14亿年前,氧气水平普遍存在.
科学领域:
- 地质化学 地质化学
- 古海洋学是古海洋学.
- 地球科学 地球科学 地球科学
背景情况:
- 人们认为中原生态时代 (1.61.0亿年前) 是生物地化学停滞的时期.
- 短暂的,局部氧气增加的证据挑战了这一观点,但全球范围仍在争论中.
研究的目的:
- 为了研究在中原生态时期全球氧化程度.
- 为了评估氧气水平在14亿年前是否在全球范围内上升.
主要方法:
- 从约145亿年前的Tieling形成,中国北部的 (Mn) 和铁 (Fe) 丰富的化学沉积岩中分析 (Mo) 同位素值.
- 质量平衡建模用于估计海底氧化水平.
主要成果:
- 检测到全球海水Mo同位素值升高,超过了中原生态时期的基线.
- 质量平衡建模表明,全球海底高达80%的海洋可能被氧化.
- 研究结果表明,一个重要的全球氧化事件发生在14亿年前左右.
结论:
- 中原生态时期并不是一个完全生物地化学静止的时期.
- 大约14亿年前,一个比以前认为的更广泛,更长时间的全球氧化事件发生了.
更多相关视频
09:38Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures
Published on: January 7, 2019
9.1K
08:28Creating Rapid Oxygen Oscillations in Microbial Single-cell Growth Analysis using a Microfluidic Double-layer Device
Published on: July 18, 2025
491
相关概念视频
Oxygen Transport in the Blood
5.9K
Hemoglobin (Hb) is a crucial molecule in the human body, consisting of four polypeptide chains, each bound to an iron-containing heme group. This unique structure enables hemoglobin to bind to oxygen, with each molecule capable of combining with four molecules of oxygen, leading to rapid and reversible oxygen loading. When fully loaded with oxygen, it is called oxyhemoglobin, while hemoglobin that has released oxygen is called reduced hemoglobin or deoxyhemoglobin. As hemoglobin binds oxygen,...
5.9K
Oxygenic Photosynthesis
683
Oxygenic photosynthesis is a fundamental process in which light energy is harnessed to drive the oxidation of water, leading to the production of molecular oxygen (O₂), adenosine triphosphate (ATP), and nicotinamide adenine dinucleotide phosphate (NADPH). This process is essential for sustaining aerobic life on Earth and is primarily carried out by cyanobacteria, algae, and plants. The core of oxygenic photosynthesis lies in the thylakoid membranes, where chlorophyll pigments facilitate...
683
Gas Exchange and Transport
76.4K
Gas exchange, the intake of molecular oxygen (O2) from the environment and the outflow of carbon dioxide (CO2) into the environment, is necessary for cellular function. Gas exchange during respiration occurs largely via the movement of gas molecules along pressure gradients. Gas travels from areas of higher partial pressure to areas of lower partial pressure. In mammals, gas exchange occurs in the alveoli of the lungs, which are adjacent to capillaries and share a membrane with them.
76.4K
Oxygen Requirements and Growth Patterns
1.1K
Microorganisms exhibit diverse oxygen requirements and growth patterns driven by their metabolic strategies and environmental adaptations. Oxygen, while essential for many organisms, can also be toxic under certain conditions, shaping how microorganisms grow and survive.Oxygen Requirements of MicroorganismsMicroorganisms are classified based on their ability to use or tolerate oxygen:● Obligate aerobes like Mycobacterium tuberculosis need oxygen for energy production, as it serves as the...
1.1K
Respiration and Gaseous Exchange
3.0K
The intricate interplay between the cardiovascular and respiratory systems is crucial for efficiently transporting respiratory gases throughout the body. Let us explore the cardiovascular system's multifaceted functions, emphasizing its pivotal role in gas exchange.
Respiration involves the exchange of gases, especially oxygen (O2) and carbon dioxide (CO2), between the alveoli and body cells, a process facilitated by blood circulation. As a result, the cardiovascular system, which involves...
Respiration involves the exchange of gases, especially oxygen (O2) and carbon dioxide (CO2), between the alveoli and body cells, a process facilitated by blood circulation. As a result, the cardiovascular system, which involves...
3.0K
The Colonization of Land
37.0K
Changes in the environment of the early Earth drove the evolution of organisms. As prokaryotic organisms in the oceans began to photosynthesize, they produced oxygen. Eventually, oxygen saturated the oceans and entered the air, resulting in an increase in atmospheric oxygen concentration, known as the oxygen revolution approximately 2.3 billion years ago. Therefore, organisms that could use oxygen for cellular respiration had an advantage. More than 1.5 years ago, eukaryotic cells and...
37.0K
