使用碳酸盐∆47/∆48分析,解决和纠正甲入古温度上的动力偏差
Philip Staudigel1, Dong Feng2, Jörn Peckmann3
1Goethe-Universität Frankfurt, Institut für Geowissenschaften, Frankfurt am Main 60438, Germany.
Science advances
|May 29, 2024
概括
对甲透碳酸盐的双同位素分析揭示了准确的形成温度. 这种方法纠正了石和石的动力偏差,改善了古气温和海水重建.
科学领域:
- 地质化学 地质化学
- 古海洋学是古海洋学.
- 同位素地球化学 同位素地球化学
背景情况:
- 来自甲的甲基碳酸盐对于了解过去的甲泄漏至关重要.
- 透碳酸盐中的聚合和氧同位素通常由于动力效应和水合水改性而提供不准确的温度数据.
研究的目的:
- 分析来自现代甲泄漏的authigenic碳酸盐的双结合同位素 (∆47/∆48) 组成.
- 证明双结合的同位素分析对纠正动力偏差和重建古温度和海水 δ18O 的实用性.
主要方法:
- 在authigenic碳酸盐中分析双结合同位素 (∆47/∆48) 组成.
- 数值建模以了解脱水/脱和扩散的同位素偏差.
主要成果:
- 阿拉戈尼特在接近同位素平衡的状态下形成,通过∆47.0产生准确的形成温度.
- 石因动态同位素效应而显著偏差.
- 双聚合同位素分析量化并纠正透碳酸盐中的动态偏差.
结论:
- 双结合的同位素分析是一种强大的工具,可以从透的碳酸盐中准确地重建古气温和海水 δ18O.
- 这种方法克服了在甲透环境中传统单块同位素分析的局限性.
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