profittis Ilias单元(Rhodes, Greece)新修订的生物年代地层约束的古海洋学意义

T. Danelian, M. Bonneau, J. Cadet, A. Poisson, Β. Vrielynck
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引用次数: 3

摘要

从Profitis Ilias单元(Rhodes island)放射斑岩顶部提取的中牛津—早kimimmeridian放射斑岩表明,后者的年龄基本为中侏罗世,而其上的硅质页岩则为晚侏罗世。以前在Profitis Ilias硅质泥灰岩顶部发现的Calpionellid层现在被认为是早期的Valanginian。根据上述年代地层限制,可以在profittis Ilias和Pindos-Olonos沉积单元之间进行初步对比。最后,讨论了罗得岛研究序列和土耳其马尔马里斯地区可能类似的上层层序的古海洋学意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Palaeoceanographic implications of new and revised bio-chronostratigraphic constraints from the Profitis Ilias Unit (Rhodes, Greece)
Middle Oxfordian-early Kimmeridgian radiolaria, extracted from the top of radiolarites of Profitis Ilias unit (Rhodes island), suggest that the latter are essentially Middle Jurassic in age and the overlying siliceous shales Late Jurassic. The previously identified Calpionellid horizon at the top of Profitis Ilias siliceous marls is now regarded as early Valanginian in age. The above chronostratigraphic constraints allow tentative correlations to be made between Profitis Ilias and Pindos-Olonos sedimentary units. Finally, the palaeoceanographic significance of the studied series in Rhodes and potentially similar pelagic sequences in the Marmaris area of Turkey are discussed.
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