论文部分内容阅读
化石是古代动植物遗体或遗述经过长期的地质作用而形成的,它们是保存在岩层中各个地史时期的生物遗体和遗迹。我国古代劳动人民很早就开始认识和研究化石了。公元770年间,唐朝大思想家颜真卿在“沧海变桑田”思想的启发下,提出了产化石的岩层与后来上升为山峰的地层间的联系,以及它们之间的形成关系。这可能不但是研究沉积岩地层的早期思想萌芽,而且是研究化石与地层间形成关系的较早记载。
Fossils are the result of long-term geological processes of the remains or remnants of ancient fauna and flora. They are the remains and relics of living preserved in various periods of the rock formations. The ancient working people in our country started to understand and study fossils very early. In the year 770 AD, Yan Zhenqing, a great thinker in the Tang Dynasty, raised the connection between fossil-bearing rock formations and strata that later rose to mountain peaks and the formation of the relationship between them. This may not only be the study of the early thought budding of sedimentary strata, but also an earlier record of the relationship between the formation of fossils and strata.