概述了地史早期宏体植物化石的记录。从细胞群体到组织－ 器官构造有大约１１ 亿年的漫长进化史。蓝田植物群和庙河生物群标志着震旦晚期（大约７—５．４ 亿年间）发生了宏体植物演化史上的一次大辐射，非矿化、弱矿化、和矿化的高级藻类出现。寒武纪发生了另一次辐射。非矿化藻类是最有发展前途的类群，可能直接导致了维管植物的出现。 An overview of the records of early macro-plant fossils is provided. From cell populations to tissue-organ constructs, there is a long evolutionary history of about 1.1 billion years. The Lantian flora and the Miaohe biota signify the occurrence of a major radiation, non-mineralization, weak mineralization, and mineralization of high-grade algal blooms in the late Sinian period (about 7-5.4 billion years) . Another radiation occurred in the Cambrian. Non-mineralized algae are the most promising groups, which may directly lead to the emergence of vascular plants.