波罗地
劳伦蒂娅
冰期
冈瓦纳大陆
间冰期
句号(音乐)
优势(遗传学)
地质学
古生物学
泥盆纪
奥陶纪
生物
物理
构造盆地
基因
生物化学
声学
作者
Shie-Ming Peng,Loren E. Babcock,Per Ahlberg
出处
期刊:Elsevier eBooks
[Elsevier]
日期:2020-01-01
卷期号:: 565-629
被引量:29
标识
DOI:10.1016/b978-0-12-824360-2.00019-x
摘要
Appearance of metazoans with mineralized skeletons, “explosion” in biotic diversity and disparity, infaunalization of the substrate, occurrence of metazoan Konservat Fossil-lagerstätten, establishment of most invertebrate phyla, strong faunal provincialism, dominance of trilobites, generally warm climate but with possible glacial–interglacial cycles in the later part, opening of the Iapetus Ocean, progressive equatorial drift and separation of Laurentia, Baltica, Siberia, and Avalonia from Gondwana characterize the Cambrian Period.
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