回应评论"在三叠纪早期温室期间致命的高温"的评论
Yadong Sun1, Michael M Joachimski, Paul B Wignall
1State Key laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, P.R. China.
概括
这项研究质疑了一个新的三纪早期生物层级图谱方案. 氨类动物和类动物之间的相关性是没有证据的,这导致了不准确的海水温度历史.
科学领域:
- 古生物学的古生物学
- 古海洋学是古海洋学.
- 在平流体学上,平流体学是平流体学.
背景情况:
- 准确的生物层级图区划对于重建过去的环境条件至关重要.
- 之前的研究已经建立了早期三叠纪的海水温度历史.
- 新的生物层级图形方案需要严格的验证.
研究的目的:
- 评估Goudemand等人提出的新特里亚斯纪早期生物层级图谱方案的有效性.
- 为了质疑氨类动物和类动物数据之间的相关性.
- 为了质疑由此产生的海水温度重建.
主要方法:
- 重新分析现有的,严格限制的古生物学数据.
- 批评拟议的氨基体区分和假设的氨基体-体相关性.
- 将新的温度历史与已确定的数据进行比较.
主要成果:
- 拟议的生物层级图表方案导致海水温度历史不那么明显.
- 氨类动物和类动物之间的相关性被认为是假设的,没有证据.
- 新的温度重建被认为是不可靠的.
结论:
- 新的特里亚斯纪早期生物层级图表方案及其拟议的相关性没有得到数据的支持.
- 据称从这个方案中得出的海水温度历史是可疑的.
- 在接受修订后的生物层级图谱框架之前,需要进一步验证.
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