构造学触发了法内罗纪的第一个重大灭绝:早期坎布里亚时期的辛斯克事件
Paul M Myrow1, John W Goodge2,3, Glenn A Brock4
1Department of Geology, Colorado College, Colorado Springs, CO 80903, USA.
Science advances
|March 29, 2024
概括
辛斯克事件是坎布里亚爆炸期间的一次重大灭绝,是由于冈德瓦纳的构造学变化造成的. 这导致息地丧失,火山活动和气候变化,影响海洋生态系统.
科学领域:
- 古生物学的古生物学
- 地质地质地质地质地质地
- 地球科学 地球科学 地球科学
背景情况:
- 坎布里亚爆炸,地球历史的一个关键时期,有两个阶段,由辛斯克事件分开.
- 辛斯克事件代表了法内罗纪纪第一个重大灭绝事件.
研究的目的:
- 分析来自南极洲和澳大利亚的三虫化石数据,以了解辛斯克事件.
- 调查辛斯克事件的地力学,古环境和生物后果.
主要方法:
- 分析来自Ross Orogen (南极洲) 和Delamerian Orogen (澳大利亚) 的系列2层的三虫化石数据.
- 构造沉积变迁与帕拉雷亚热内亚三生物区的相关性.
主要成果:
- 在南极洲和澳大利亚记录了相同和同步的构造沉积物移动,标志着辛斯克事件.
- 这些变化是Gondwana边缘沿着突然收缩的上形变的结果.
- 灭绝是由这种收缩引发的,导致息地丧失,火山活动 (Kalkarindji大型火山区),气体释放和气候变化.
结论:
- 辛斯克事件的灭绝是由沿着冈德瓦纳边缘的地收缩引发的.
- 这一事件造成了一连串的环境变化,包括海洋息地丧失,构造变化和生态系统崩.
- 这些发现提供了关于导致大规模灭绝的地质和环境因素复杂相互作用的见解.
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