新疆准噶尔盆地中侏罗统西山窑组费尔干杉属表皮构造研究  

STUDY ON THE EPIGENETIC STRUCTURE OF Ferganiella FROM MIDDLE JURASSIC XISHANYAO FORMATION IN JUNGGAR BASIN,XINJIANG

作　　者：杨涛[1] 张渝金[2] 鄂婧雯 YANG Tao, ZHANG Yu-jin, E Jing-wen(1. College of paleontology, Shenyang Normal University, Shenyang 110034, China; 2. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, Chin)

机构地区：[1]沈阳师范大学古生物学院,辽宁沈阳110034 [2]中国地质调查局沈阳地质调查中心,辽宁沈阳110034

出　　处：《地质与资源》2018年第2期124-129,共6页Geology and Resources

基　　金：科技部基础性工作专项项目"中国标准地层建立-中国地层表的完善"(2015FY310100);国家自然科学青年基金项目"大兴安岭中段龙江盆地中侏罗统地层新研究"(41702032)

摘　　要：选择新疆准噶尔盆地白杨河地区中侏罗统西山窑组费尔干杉为研究对象,通过扫描电子显微镜观察,认为费尔干杉以气孔排列不定向为特征,与苏铁杉、林德勒枝等有较大区别.当前研究补充了费尔干杉属的资料,提高了松柏类植物化石的分类研究程度,增加了对中侏罗世松柏类植物的认识,同时为恢复新疆白杨河地区古地理及古环境的补充提供了新的数据.The Ferganiella sp. from Middle Jurassic Xishanyao Formation in Baiyanghe area of Juggar Basin,Xinjiang is observed through scanning electron microscope（SEM）. The fossil is characterized by non-orientated stomatal aperture which can distinguish it from Podozamites and Lindleycladus. The current study can supplement the data for Ferganiella and restoration of paleo-geography and environment in Baiyanghe area,and improve understanding of Coniferales plants in Middle Jurassic and classification study of fossils.

关 键 词：费尔干杉属 表皮构造 松柏类 白杨河地区 新疆 

分 类 号：Q914.87[天文地球—古生物学与地层学]