摘要
<正>Diverse Ordovician marine ecosystems were abruptly terminated by the Late Ordovician mass extinction (LOME), when around 85%of species were eliminated. Previous studies thought early Silurian (~443–433 Ma) recovery of biotic diversity and ecosystem complexity [1] occurred relatively rapidly, in the first few million years of the Silurian [2].
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单位地质过程与矿产资源国家重点实验室; 中国科学技术大学