古海洋学:在罗纪早期的甲释放
Paul B Wignall1, John M McArthur, Crispin T S Little
1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK. wignall@earth.leeds.ac.uk
Nature
|June 2, 2006
概括
罗纪早期的变暖可能不是由甲释放引起的. 新的研究表明,快速的碳同位素转移可能源于当地的海洋条件,而不是从酸盐的全球甲释放.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
背景情况:
- 罗纪早期时期经历了显著的全球变暖,可能与酸盐释放的甲有关.
- 肯普和其他人. 确定了三次尖的delta13C(org) 突出,将它们归因于甲释放事件.
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