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在地中海中部的轨道和次轨道温度变化,跨越了普略纪/普纪过渡时期
Elena Zanola1, Teresa Rodrigues2,3, Sergio Bonomo4
1Dipartimento di Geoscienze, Università degli Studi di Padova, Padova, Italy.
PloS one
|December 26, 2024
概括
这项研究重建了地中海中部世-普世时期的海面温度,揭示了早期格拉西亚冰川时期的倾斜驱动周期和显著的亚轨道变化.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 地质地质地质地质地质地
背景情况:
- 重建过去的气候对于理解地球系统至关重要.
- 世/普世过渡期是研究冰川-冰川间动态的一个关键时期.
- 地中海中部地区是古气候研究的重要参考点.
研究的目的:
- 为了重建高分辨率的海面温度 (SSTs) 跨越纪/纪边界.
- 分析SST在地中海中部地区的周期性和变异性.
- 为了研究轨道和次轨道强迫对早期格拉西亚气候的影响.
主要方法:
- 从G. ruber.获得的利用的基UK'37指数和浮游体 δ18O值.
- 从西西里山圣尼古拉山 (Monte San Nicola) 重建的SSTs.
- 在古气候记录上进行了光谱分析.
主要成果:
- 确定了与斜度相关的 ~ 47 kyr 主导周期性.
- 在冰川时期检测到显著的次轨周期 (~5 kyr和~8 kyr).
- 在早期的格拉西亚时期观察到高频气候不稳定.
结论:
- 地中海中部地区为古气候研究提供了关键的参考.
- 亚轨道气候变化可能与大西洋南部翻转循环或 precessional 强迫的破坏有关.
- 需要进一步的研究才能充分理解这些气候不稳定的驱动机制.
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