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前言迭层石是由藻类和光合细菌构成的有机沉积构造。迭层石化石从太古代到现代一直都存在,但是只对元古界,特别是中、晚元古界地层具有一定的地层意义。对迭层石的研究,从Steel 1825年发表的第一篇有关迭层石的文章开始,已有150年的历史了,从Matthew在1890年出版的第一本描述前寒武纪迭层石的书“Archaezoon acadiense”(Matthew 1890a.P40)开始也有近90年的历史了。回顾研究迭层石的历史,从研究
Preface Laminates are organic deposits of algae and photosynthetic bacteria. The laminated fossils have been existed from the Archean to modern times, but have certain stratigraphic significance only to the Proterozoic, especially the Middle and Late Proterozoic strata. The study of laminated stone has been 150 years old since the first article on laminated stone published in 1825 by Steel, from Matthew’s first book, Pre-Cambrian, published in 1890 The book “Archaezoon acadiense” (Matthew 1890a.P40) has nearly 90 years of history. Review the history of the study of laminated stone