A I Miller1

  • 1Department of Geology, University of Cincinnati, OH 45221-0013, USA. arnold.miller@uc.edu

Science (New York, N.Y.)
|August 26, 1998
PubMed
概括

在法内罗纪时期,海洋生物组成的变化是由物理干扰驱动的,而不仅仅是生物相互作用或大规模灭绝. 宏观进化过程在整个地质时间尺度上始终保持一致.

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