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地球轨道节奏将德坎陷火山阶段的时间与全球气候变化联系起来
Thomas Westerhold1, Edoardo Dallanave2,3, Donald Penman4
1MARUM - Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany.
Science advances
|March 7, 2025
概括
德坎陷 (DT) 火山爆发引发了全球气候变化. 新的同位素数据将主要喷发阶段与碳循环中断联系起来,揭示了各种气候影响.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 火山学 火山学是一门学科.
背景情况:
- 德坎陷 (DT) 喷发与白纪末期的气候变化有关.
- 准确的年龄模型对于理解火山活动和气候影响至关重要.
研究的目的:
- 为了建立DT火山活动和全球气候变化之间的地化学联系.
- 改进DT喷发阶段的时间及其气候影响.
主要方法:
- 对海洋同位素 (187Os/188Os) 的分析.
- 检查本土藻类的碳和氧同位素.
- 开发一个天文学校准的年龄模型.
主要成果:
- 在66.49和66.28百万年前确定了两个主要的海洋奥斯转移.
- 他将这些变化与Deccan Traps火山爆发阶段相关联.
- 观察到与火山活动相关的全球碳循环中出现的破坏.
结论:
- DT火山活动直接影响了全球气候和碳循环的破坏.
- 早期的DT阶段涉及大量的喷发量和高挥发性排放 (SO2,CO2).
- 奥斯转移表明各种挥发性排放具有不同的气候后果.
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