大气(单位)
天体生物学
地球大气中的二氧化碳
大气氧
环境科学
土(古典元素)
行星
温室气体
温室效应
大气科学
地球大气层
早期地球
地球科学
气候变化
全球变暖
氧气
地质学
气象学
地理
天文
化学
物理
海洋学
有机化学
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:1993-02-12
卷期号:259 (5097): 920-926
被引量:1314
标识
DOI:10.1126/science.11536547
摘要
Ideas about atmospheric composition and climate on the early Earth have evolved considerably over the last 30 years, but many uncertainties still remain. It is generally agreed that the atmosphere contained little or no free oxygen initially and that oxygen concentrations increased markedly near 2.0 billion years ago, but the precise timing of and reasons for its rise remain unexplained. Likewise, it is usually conceded that the atmospheric greenhouse effect must have been higher in the past to offset reduced solar luminosity, but the levels of atmospheric carbon dioxide and other greenhouse gases required remain speculative. A better understanding of past atmospheric evolution is important to understanding the evolution of life and to predicting whether Earth-like planets might exist elsewhere in the galaxy.
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