古气候学:古时的气氛和气候
1Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16801, USA. kasting@geosc.psu.edu
Nature
|December 8, 2004
概括
早期的地球地球.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 大气科学 大气科学
背景情况:
- 在古代岩石中发现的 siderite (FeCO3) 的重新分析表明,在阿基亚纪晚期和早期新生代大气中,有大量的二氧化碳 (CO2) 和稀缺的甲 (CH4).
- 这挑战了早期地球大气组成的现有模型.
相关概念视频
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Conditions on Early Earth
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.
Conditions on Early Earth
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.
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