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大范围生物快速灭绝 (1ｋａ至 1Ｍａ时间尺度 )地质记录的样品可以用于全球碳循环的大波动和白垩纪及早第三纪时期 (即大洋缺氧事件 (ＯＡＥｓ)和晚第三纪盛温期 (ＬＰＴＭ ) )地球极端气候变化的研究。人们对地球历史中这些临界事件发生的根本原因及其影响所知甚少 ,主要原因
Geologically documented samples of rapid mass extinction (1ka to 1Ma time-scale) can be used for large fluctuations in the global carbon cycle and in the Cretaceous and Early Tertiary epochs (OAEs and LPTM )) Earth’s extreme climate change research. Little is known about the root causes of these critical events in Earth’s history and their effects, the main reason