摘要
塔里木盆地中、晚奥陶世疑源类被划分为4个组合,自下而上分别为Peteinosphaeridium-Baltisphaeridium组合,Baltisphaerosum-Dichotisphaera组合,Navifusa-Ordovicidium组合及Dactylofusa-Leiosphaeridia组合。下部3个组合产于中奥陶统,代表台地—台缘斜坡相环境,最上部1个组合产于上奥陶统。
Four acritarch assemblages, namely in ascending order,
Peteinosphaeridium Baltisphaeridium, Baltisphaerosum Dichotisphaera, Navifusa
Ordoricidium, Dactylofusa Leiosphaeridia assemblages, covering the age from Middle to Late
Ordovician have been first documented from the Tarim Basin. The three assemblages from the
lower part are Middle Ordovician in age and represent platform to slope facies environment
while the assemblage from the upper part is Late Ordovician in age and represents littoral
facies or terrestrial facies enviroment.
出处
《地层学杂志》
CSCD
北大核心
1999年第2期124-129,共6页
Journal of Stratigraphy
基金
中国科学院古生物与古人类基础研究特别支持费资助
国家自然科学基金
关键词
疑源类
晚奥陶世
塔里木盆地
中奥陶世
地层
acritarch assemblages, Middle-Late
Ordovician, Tarim Basin, Xinjiang