同位素证据表明,在最后一次脱冰过程中,海洋二氧化碳泄漏
M A Martínez-Botí1, G Marino2, G L Foster1
1Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK.
Nature
|February 13, 2015
概括
大气中的二氧化碳 (CO2) 水平在冰川时期大幅波动. 这项研究表明,南大洋在脱冰过程中释放了二氧化碳,支持其在调节地球气候中的作用.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 了解大气二氧化碳的冰期-冰期间波动对于气候系统研究至关重要.
- 假设表明深海碳储存的变化,受南洋过程的影响,驱动这些二氧化碳变化.
- 由于有限的代理数据,重建过去的海洋碳酸盐系统变化是具有挑战性的.
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