中国科学院南京地质古生物研究所机构知识库

Well-preserved megaspores are described for the first time from Pennsylvanian to Late Permian strata of the Baode region in Shanxi province, North China. A total of 20 species in 13 genera are described, amongst which one species Biharisporites grosstriletus sp. nov. is new. The other 19 are previously known from the Euramerican and Gondwanan floral provinces, but are described here for first time from the Cathaysian Province. Using first appearances of selected megaspore species and changes in species abundance in the succession, four assemblage zones can be recognised. In ascending order these are the Auritolagenicula renaulti-Setosisporites brevispinosus (RB, Moscovian), the Bentzisiporites margaritatus-Spencerisporites striatus (MS. Kasimovian-Roadian), the Biharisporites grosstriletus (G. Wordian-Capitanian) and the Biharisporites cf. foskettensis (F. Wuchiapingian) assemblage zones. Comparison with already known in situ megaspores indicates that the parent plants of the dispersed megaspores were mainly lycopods and this in turn indicates their likely palaeoenvironmental significance. Selaginella-like herbs and subarborescent lycopods which were low in abundance compared with arborescent lycopods in the early Pennsylvanian appeared to have become prevalent from the Late Pennsylvanian in northern China. However, some arborescent lycopods (mainly sigillarians) still played an important role in the Permian coal forming plants of the region. Several Carboniferous megaspores characteristic of Euramerica persist into the Mid Permian in North China, indicating that a warm and humid climate prevailed in this area during Pennsylvanian to Roadian, whereas the climate of Euramerica had already become arid by the end of the Carboniferous. This warm and humid climate in northern China made it a refuge for some typically Euramerican Carboniferous plants. From Roadian, with the disappearance of coal and marine sediments together with the appearance of red beds, the MS megaspore zone progressively changed to the G zone. This probably reflects the adaptation of the parent plants to a more and more arid climate. (C) 2011 Elsevier B.V. All rights reserved.