相关实验视频
Updated: Jan 20, 2026
08:55
Making a Geologic Cross Section
Published on: April 30, 2023
48.9K
太阳系的混乱和由地质学和天文学所限制的古世-新世边界年龄
Richard E Zeebe1, Lucas J Lourens2
1School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, 1000 Pope Road, MSB 629, Honolulu, HI 96822, USA. zeebe@soest.hawaii.edu.
概括
现在的天文数据使得天文年代学可以追溯到5000万年前. 新的发现揭示了古世-新世热量最大值
科学领域:
- 地质科学
- 天文学
- 古气候学
背景情况:
- 天文计算对于周期表学和天文年代学至关重要.
- 由于轨道计算的差异,目前的天文时间尺度仅限于过去5000万年.
- 扩展这个时间尺度为地球的古代气候和轨道动态提供了关键的见解.
研究的目的:
- 发展一个新的,绝对的天文时间尺度,
- 精确古世 - 世边界的年龄,并确定古世 - 世热极值 (PETM) 的持续时间.
- 调查PETM的轨道触发和持续时间.
主要方法:
- 将地质数据与新型天文解决方案 (ZB18a) 整合起来.
- 高分辨率的天文模型重建过去的轨道配置.
- 精确测定沉积物序列与天文周期的相关性.
主要成果:
- 地质数据与5800万年至5300万年前的ZB18a天文解决方案之间的异常一致.
- 建立一个新的绝对天文年代, 延伸到5800万年前.
- 在56.01 ±0.05万年前确定新的古世-新世边界年龄.
- 这次PETM的发作与405千年的离心率最大相吻合,
- 确定PETM的持续时间为170±3万年.
结论:
- 这种新的天文解决方案使得前所未有的长时间和精确的天文年代学.
- 轨道强迫可能在触发PETM方面发挥了重要作用.
- 太阳系在5000万年前经历了一次混乱的共振转变,
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