在南大洋的冰川酸度
Michael J Ellwood1, Martin Wille, William Maher
1Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia. michael.ellwood@anu.edu.au
概括
在最后一个冰川时期,南大洋的营养水平在太平洋地区更高. 这一基于同位素的发现支持了酸泄漏假设,并表明营养物质的再分配.
科学领域:
- 古海洋学是古海洋学.
- 海洋生物地质化学海洋生物地质化学
- 同位素地球化学 同位素地球化学
背景情况:
- 在最后一个冰川时期重建南大洋深处的营养度,产生了相互矛盾的数据.
- / (Cd/Ca) 记录表明营养变化最小,而碳同位素数据表明营养水平较高.
研究的目的:
- 解决在最后一个冰川时期南大洋中相互矛盾的营养重建问题.
- 为了研究酸度使用同位素组成的海绵螺纹.
主要方法:
- 在化石海绵中分析同位素组成 (δ30Si).
- 从南大洋的大西洋和太平洋部门抽取样本.
主要成果:
- 在最后一个冰川时期,太平洋地区发现了较高的酸度.
- 这些发现表明,藻类对酸相对于酸和酸盐的固态度吸收发生了变化.
结论:
- 在太平洋中观察到的酸度的增加可能促进了整个南大洋的营养物质再分配.
- 结果与全球Cd/Ca数据一致,并支持酸泄漏假说.
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