大气中的二氧化碳度在22亿年前之前
1Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA.
Nature
|December 7, 1995
概括
早期的地球地球.
科学领域:
- 地质科学 地质科学
- 古气候学 古气候学
- 大气科学 大气科学
背景情况:
- 地球早期大气层的组成仍在争论中.
- 由于太阳亮度较低,可能需要更高的二氧化碳 (CO2) 来提供热量.
- 古提供了早期大气氧 (pO2) 的限制.
研究的目的:
- 约束大气中的二氧化碳 (pCO2) 水平在275亿至22亿年前之间.
- 研究二氧化碳在调节早期地球气候中的作用.
- 重新评估Archaean晚期和Proterozoic早期时代的气候模型.
主要方法:
- 对经过充分研究的古岩的分析 (化石气候变化概况).
- 检查铁沉模式在古的配置文件.
- 使用铁酸盐和铁碳酸盐的形成来推断pCO2水平.
主要成果:
- 大气中的pCO2小于10~-1.4) atm (约. 目前水平的100倍).
- 这一水平明显低于早期地球气候模型预测的水平.
- 铁作为酸盐而不是碳酸盐的沉积表明有限的CO2.
结论:
- 早期地球对二氧化碳的气候敏感性可能高于以前的假设.
- 其他温室气体可能在调节古代气候方面发挥了重要作用.
- 这些发现挑战了现有的阿古时代和原生时代大气组成和气候模型.
更多相关视频
相关概念视频
The Carbon Cycle
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
The Sulfur Cycle
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
Standard Enthalpy of Formation
Enthalpy changes are typically tabulated for reactions in which both the reactants and products are at the same conditions. A standard state is a commonly accepted set of conditions used as a reference point for the determination of properties under other different conditions. For chemists, the IUPAC standard state refers to materials under a pressure of 1 bar and solutions at 1 M and does not specify a temperature. Many thermochemical tables list values with a standard state of 1 atm. Because...
Carbon Dioxide Transport in the Blood
Carbon dioxide (CO2) transport in the blood is critical to human physiology. On average, our body cells produce around 200 mL of CO2 per minute, precisely the quantity expelled by the lungs. This process involves the transportation of CO2 from the tissue cells to the lungs in three primary forms.
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
Origin of Photosynthesis
Photosynthesis represents a fundamental biological process that transformed Earth's atmosphere and paved the way for complex life. Emerging roughly 3.4–3.8 billion years ago, the earliest photosynthetic organisms harnessed light energy to produce organic compounds. These anoxygenic phototrophs used electron donors like hydrogen sulfide (H₂S) or ferrous iron (Fe²⁺), rather than water, and did not release molecular oxygen (O₂) as a byproduct. Various groups, including green sulfur and purple...
Microbes and the Carbon Cycle
The carbon cycle is a fundamental Earth process involving the transfer of carbon among the biosphere, lithosphere, atmosphere, and hydrosphere. It plays a critical role in regulating the planet’s climate and supporting life by cycling carbon through various chemical forms and reservoirs. Carbon primarily circulates as carbon dioxide (CO₂), representing its oxidized form, while reduced forms such as methane (CH₄) and organic compounds also play essential roles.Microbial activity is central to...


