由珊瑚化石模式揭示的晚期古生物学气候
Weijia Zhang1,2, Jiaju Li1, Xue Cheng1
1Department of Mathematics, Physics and Information Sciences, Shaoxing University, Shaoxing, Zhejiang, China.
PloS one
|August 15, 2023
概括
来自中国的化石珊瑚生长线揭示了晚炭时期的阳光模式. 这项研究更新了气候记录,显示了四季的变化和古老的气候条件,类似于现代的中国北方.
科学领域:
- 古气候学 古气候学
- 古生物学的古生物学
- 地质地质地质地质地质地
背景情况:
- 珊瑚生长线提供了对过去环境条件的洞察.
- 之前的气候重建在时间分辨率上有局限性.
研究的目的:
- 为了分析来自Shiqiantan形成 (310万年前) 的珊瑚化石生长线.
- 为了重建晚碳期气候和太阳照明模式.
- 更新现有的最古老的气候分析记录.
主要方法:
- 检查化石珊瑚的生长线增长.
- 分析每日增长步骤的双模曲线.
- 关联生长模式与阳光照射时间.
主要成果:
- 珊瑚生长线的增长与阳光照射时间直接相关.
- 观察到每日增长的异常双模曲线.
- 证据表明,在晚石灰岩时期有明显的四季变化.
结论:
- 石地区的晚期碳期气候类似于现代的北中国.
- 这项研究为古老时代晚期气候研究提供了关键数据.
- 这些发现有助于理解日食线的古代斜率.
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