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晚白时期的 precessional 周期在双倍的时间:一个温暖的地球 milankovitch 响应
概括
南大西洋的白纪晚期气候周期受到地球轨道前行的影响. 沉积物的磁性易感性显示出强大的周期性,表明阳光照射,赤道气候动态和沉积模式之间的联系.
科学领域:
- 古气候学 古气候学
- 地质物理学 地质物理学
- 沉积物学的沉积物学
背景情况:
- 晚白时期的气候周期对于理解地球过去的气候动态至关重要.
- 深海沉积物提供了关于过去环境条件的宝贵档案.
- 南大西洋深海钻井项目 (DSDP) 站点516F提供了对白纪古海洋学的见解.
研究的目的:
- 为了研究轨道周期对南大西洋晚白纪沉积物的影响.
- 分析碳酸盐沉积物的岩石学和磁性变化.
- 了解赤道气候动态在塑造沉积模式中的作用.
主要方法:
- 来自DSDP站点516F的石质学和磁性易感性数据的分析.
- 频谱分析以确定沉积物性质的周期性.
- 观察到的周期与天文周期的相关性,特别是等的前行.
主要成果:
- 识别了与 precessional 周期相关的磁感应周期 (20-60 cm).
- 在较低的坎帕尼亚区间内观察到强的周期性,包括高调光谱峰值.
- 在单个 precession 周期内检测到的二次敏感度最大值.
结论:
- 南大西洋的白纪晚期沉积是由 precessional 阳光照射周期调节的.
- 赤道气候动态可能发挥了重要作用,信号被周围的陆地质量放大.
- 沉积物的磁性易感性作为一个可靠的代理用于重建过去的轨道强迫和气候动态.
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