氮气循环
古细菌
氮气
环境科学
土(古典元素)
营养物
早期地球
活性氮
生态学
温室气体
营养污染
水循环
生物
地球科学
天体生物学
化学
细菌
地质学
遗传学
数学物理
有机化学
物理
作者
Donald E. Canfield,Alexander N. Glazer,Paul G. Falkowski
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2010-10-08
卷期号:330 (6001): 192-196
被引量:1972
标识
DOI:10.1126/science.1186120
摘要
Nitrogen's Past and Future Microorganisms have been controlling Earth's nitrogen cycle since life originated. With life evolving around it, nitrogen became both an essential nutrient and a major regulator of climate. Canfield et al. (p. 192 ) review the major changes in the nitrogen cycle throughout Earth's history. Most of the time, perturbations typically coincided with the evolution of new metabolic pathways in various Bacteria or Archaea. The last century, however, has seen humans push the biological nitrogen cycle into a new stage altogether. The addition of large quantities of fixed nitrogen to crops in the form of fertilizer chokes out aquatic life that relies on runoff and adds significant amounts of N 2 O—a potent greenhouse gas—to the atmosphere. Although microorganisms may one day restore balance to the nitrogen cycle that they helped shape for billions of years, humans must modify their behavior or risk causing irreversible changes to life on Earth.
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