揭示新新生代碳循环的发现
D T Johnston1, F A Macdonald, B C Gill
1Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA. johnston@eps.harvard.edu
Nature
|March 6, 2012
概括
岩石中的新新生代碳同位素异常表明,地球表面的碳循环发生了主要变化,而不仅仅是深海过程. 这一发现影响了我们对早期动物进化和海洋氧化的理解.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 沉积物学的沉积物学
背景情况:
- 岩石中的稳定碳同位素 (δ(13) C(carb) 和 δ(13) C(org)) 是解释地球过去气候和生物学的关键.
- 新新生态纪录显示了巨大的负碳同位素异常,挑战了与有机碳埋葬和氧气水平相关的传统解释.
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