Maher I. El-Soughier
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引用次数: 0

摘要

本文对埃及西南沙漠Bir Abu Minqar剖面的Dakhla组矿床进行了研究。马斯特里赫特/丹麦的孢粉植物已经从上Dakhla组的微古生物(有孔虫-纳米浮游生物)和大型古生物(双壳类-菊石)沉积物中恢复。还发现了蕨类植物和苔类植物的孢子、裸子植物和被子植物的花粉以及鞭毛囊。被子植物花粉包括晚白垩世棕榈科的典型成员,如棘棘虫。棕榈花粉和水生蕨类植物孢子的存在表明,在研究剖面沉积期间,潮湿的热带环境普遍存在,在阿布明卡尔地区与晚白垩纪浅海接壤的潮间带沼泽中,Nypa棕榈红树林茁壮成长。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PALEOECOLOGICAL SIGNIFICANCE OF PALYNOMORPHS FROM PALEONTOLOGICALY-DATED MAASTRICHTIAN–DANIAN DEPOSITS, BIR ABU MINQAR AREA, SOUTH WESTERN DESERT, EGYPT
This study is carried out on the Dakhla Formation deposits at the Bir Abu Minqar section, South Western Desert, Egypt. Maastrichtian/Danian palynofloras have been recovered from the micropaleontology (foraminifera–nannoplankton)and macropaleontology (bivalvia-ammonites)dated deposits of the upper Dakhla Formation. Pteridophytic and liverworts spores, pollen of gymanosperms and angiosperms as well as dinoflagellate cysts have been identified. Angiosperm pollen includes typical members of the Late Cretaceous Palmae Province such as Spinizonocolpites echinatus. Presence of palm pollen and hygrophylic pteridophytic spores suggest a prevalence of humid tropical conditions during the deposition of the studied section, with Nypa palm mangroves thriving in the intertidal swamps that bordered the Late Cretaceous shallow sea at the area of the Abu Minqar.
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