【摘要】 淮北元古界金山寨组最近发现了一批毫米—厘米级宏体碳质压膜化石 ,这些带状化石具有明显的固着器和营养体的分化 ,部分标本保存了紧密排列的横纹构造。根据这些特点 ,可以确定这些碳质压膜是后生植物化石 ,它们是新元古代早期生命多细胞化的可靠证据。更多还原

【Abstract】 A megascopic fossil assemblage of carbonaceous compressions was found in the Neoproterozoic Jingshanzhai Formation in the Huaibei area, Anhui Province. Some ribbon like specimens differentiate into a basal rhizoidal or globose holdfast and an erect blade that does not branch. These remains are probably metaphytes that occurred in the Neoproterozoic Jingshanzhai Formation just before the Sinian System.更多还原