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Updated: Mar 12, 2026

06:10
Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
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评论"魔鬼洞气候记录与轨道强迫的和解"
1Emeritus, U.S. Geological Survey.
概括
魔鬼洞的地热水流挑战了终结II时代的同位素解释. 二次石沉积提供了一个更有可能的替代方法,用于测定洞穴形成中的年龄差异.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 洞穴学是一门洞穴学.
背景情况:
- 莫斯利和其他人莫斯利等人. 建议增加溶解的-230 (230Th) 与深度解释不同的终结II年龄.
- 终结II代表了地球气候历史上一个重要的冰川 - 冰川间过渡.
- 魔鬼洞洞穴系统为古气候研究提供了独特的地质记录.
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