通过对济宁唐阳井煤田晚古生代含煤岩系中的孢粉化石的研究，共鉴定出孢粉化石７１ 属１７７种。根据孢粉属种组成和含量在纵向上的变化，自上而下共建立了两个孢粉组合带，即：ⅡＧｕｌｉｓｐｏｒｉｔｅｓｃｏｃｈｌｅａｒｉｕｓ－ Ｓｉｎｕｌａｔｉｓｐｏｒｉｔｅｓｓｉｎｅｎｓｉｓ－ Ｇｒａｎｕｌａｔｉｓｐｏｒｉｔｅｓ ｐｉｒｏｆｏｒｍｉｓ 带和ⅠＬａｅｖｉｇａｔｏｓｐｏｒｉｔｅｓ ｖｕｌｇａｒｉｓ－ Ｔｈｙｍｏｓｐｏｒａｐｓｅｕｄｏｔｈｉｅｓｓｅｎｉｉ 带。以上两个孢粉组合如与华北部分地区石炭———二叠纪孢粉组合带对比，它们所代表的地质时代分别为晚石炭世晚期（ 太原组） 和早二叠世早期（ 山西组）。 Through the study of sporopollen fossils in Late Paleozoic coal-bearing rocks in Tangyangjing Coalfield, Jining, a total of 177 species of 71 genera of sporopollen fossils were identified. According to the changes of composition and content of pollen species in the vertical direction, two sporopollen assemblages were established from top to bottom, that is, ⅡGulisporitescochlearius-Sinulatisporitessinensis-Granulatisporites piroformis band andⅠLaevigatosporites vulgaris-Thymosporapseudothiessenii band. The above two sporopollen assemblages, as compared with the Carboniferous-Permian sporopollen assemblages in some areas of North China, represent the geological epochs of Late Late Carboniferous (Taiyuan Formation) and Early Permian (Shanxi Formation) .