摘要
淮北煤田早二叠世晚期下石盒子组树蕨类茎干印痕化石丰富,计有40余块。分属于蹄痕茎属(Caulopteris)、大痕木属(Megaphyton)及皱痕茎属(PtychoPteris),共3属9种;其中蹄痕茎属4种(包括2个新种,Cauloptrisyangzhuangensissp.nov.和Caulopterispsilocicatrixsp.nov.);大痕木属在国内尚属首次报道,仅见1种;皱痕茎属在国内亦属首次发现,鉴定有4个未定种。该类化石在本区以极大的丰度和良好的保存为特征,其发育显示该区早二叠世晚期热带雨林气候盛行。其次,说明树蕨类在其晚期发育中心已由欧美区移至华夏区。此外,该类在本区的发育是华夏植物地理区分化渐趋强烈的直接证据。
he tree-fern compression fossils in Huaibei coal-field are very abundant during the lower Shi-He-Zi formation of Early Permian.There are 40 specimens or more in this area.The fossils belong to 3 genera and 9 species, i.e. Cauloptelis, Megaphyton and Ptychopteris. Caulopteris consists of 4 species (including 2 new species, i. e. Caulopteris yangzhuangensis sp. nov. and Caulopteris psilocicatlix sp.nov.).Megaphyton is discovered in China for the first time. The genus only has a species. Ptychopteris is also found in our country firstly. We have diagnosed 4 underdetermined species of the genus. These genera have an excellent conservation and a deep abundance in this region.lts development demonstrates the tropical rainforest climates of this area in the late time of Early Permian, the growing center of the tree-ferns in its late period having migrated into Cathaysian flora from Eurrope-America flora. It is a direct evidence of the strong differentiation in Cathaysian floral province.
出处
《西安矿业学院学报》
北大核心
1994年第3期239-244,共6页
Journal of Xi'an University of Science & Technology
关键词
树蕨类
煤田地质
化石
Huai Bei coal-field
lower Shi-He-Zi formation
tree-ferns
tropical rainforest