是否真的发生了古代酸盐危机?
Kurt O Konhauser1, Stefan V Lalonde, Larry Amskold
1Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada. kurtk@ualberta.ca
概括
古代海洋可能含有比以前想象的更多的酸盐. 实验表明,当时丰富的二氧化与酸盐在铁颗粒上竞争,减少了酸盐的去除,并提高了海洋的生产力.
科学领域:
- 地质化学 地质化学
- 古代海洋学 古代海洋学 古代海洋学
- 生物地质化学生物地质化学
背景情况:
- 带状的铁形形成表明大规模的阿尔开纪铁沉积.
- 以前的模型表明,氧化氧化铁颗粒去除了海洋酸盐,限制了植物浮游生物.
- 这些模型忽略了高的古时溶解的度.
研究的目的:
- 为了调查二氧化在古代海洋酸盐可用性中的作用.
- 实验测试二氧化和酸盐之间的竞争对铁颗粒的吸附.
主要方法:
- 实验室实验模拟阿克海水条件.
- 铁酸盐颗粒的合成和表征.
- 在铁酸盐上测量酸盐和二氧化吸附.
主要成果:
- 石在铁上对吸附点与酸盐进行了有效的竞争.
- 与铁酸盐的共沉降降低了粒子对酸盐的反应性.
- 这些发现表明,铁颗粒在古代减少了酸盐的去除.
结论:
- 古代海洋可能保留了比以前估计的高得多的酸盐度.
- 在早期海洋中调节酸盐的可用性方面发挥了关键作用.
- 由铁颗粒剥离酸盐的拟议模型需要修订,以包括的影响.
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