海洋氧化物中的海洋氧同位素的地质历史
Nir Galili1, Aldo Shemesh2, Ruth Yam2
1Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot, Israel. nir.galili@weizmann.ac.il itay.halevy@weizmann.ac.il.
概括
在数十亿年的海洋沉积物中,氧同位素 (δ18O) 显著增加. 新的铁氧化物数据表明海水升, 而不是温度, 推动了这一长期趋势.
科学领域:
- 地质化学
- 古代海洋学
- 同位素地化学
背景情况:
- 自古以来,海洋沉积岩的氧同位素组成 (δ18O) 增加了10-15.
- 由于温度和流体 δ18O 对岩石同位素组成的联合影响,解释这一趋势是复杂的.
研究的目的:
- 在海洋铁氧化物中建立一个新的 δ18O记录,
- 研究海洋沉物长期趋势的主要驱动因素.
主要方法:
- 在海洋氧化物中分析氧同位素组成 (δ18O).
- 铁氧化物沉的实验室实验以确定氧同位素与水的分离.
- 与现有的海洋沉积岩数据比较铁氧化物 δ18O记录
主要成果:
- 在过去的2000万年中,海洋氧化铁的长期上升反映了沉积岩的趋势.
- 铁氧化物-水氧同位素分离被发现是微弱的温度依赖.
- 长期观察到的海洋 δ18值的增加主要归因于随着时间的推移而增加的海水 δ18O.
结论:
- 海水升是解释海洋沉量长期上升的主要因素.
- 海水缩的潜在原因包括陆地沉积物覆盖的增加或地变化过程的变化.
- 需要进一步研究以充分阐明导致海水长期变化的机制.
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