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首页> 外文期刊>Palynology >Lower and Middle Miocene biostratigraphy, Gulf of Suez, Egypt based on dinoflagellate cysts and calcareous nannofossils
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Lower and Middle Miocene biostratigraphy, Gulf of Suez, Egypt based on dinoflagellate cysts and calcareous nannofossils

机译:埃及苏伊士湾中下新世生物地层,基于鞭毛藻囊和钙质纳米化石

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摘要

This is the first detailed stratigraphic correlation of Lower and Middle Miocene deposits in the Gulf of Suez, Egypt using dinoflagellate cysts. The correlation is based on 273 ditch-cutting samples from five onshore boreholes located along the southwestern margin of the Gulf of Suez. The interval studied is represented by the Nukhul, Rudeis and Kareem formations of the Gharandal Group, and the lower part of the Belayim Formation of the Ras Malaab Group. These Miocene deposits unconformably overlie the Lower or lower Middle Eocene. The dinoflagellate cyst record is more diverse than previously reported and many taxa are documented for the first time in Egypt. Five biozones are established and tied to a chronostratigraphic framework by calibration to calcareous nannofossils (NN biozones) obtained from the same set of samples: (1) Lingulodinium machaerophorum Assemblage Biozone (GOSI), Aquitanian through mid-Burdigalian; (2) Exochosphaeridium insigne Taxon-range Biozone (GOS2), lower through mid-Burdigalian; (3) Apteodinium spiridoides Interval Biozone (GOS3), mid-Burdigalian through lower Langhian; (4) Cleistosphaeridium placacanthum Interval Biozone (GOS4), upper Burdigalian, Langhian, and lower Serravallian?); and (5) Polysphaeridium zoharyi Assemblage Biozone (GOSS), upper Langhian and Serravallian?Comparison with other Miocene biozonations from the Mediterranean, Central Paratethys, North Atlantic region, and eastern USA indicate that the highest occurrences of Apteodinium spiridoides, Cordosphaeridium cantharellus, Distatodinium paradoxum, Exochosphaeridium insigne and Cleistosphaeridium placacanthum, and the lowest occurrences of Exochosphaeridium insigne and Sumatradinium soucouyantiae are important datums, whereas the lowest occurrences of Hystrichosphaeropsis obscura, Labyrinthodinium truncatum, and Operculodinium? borgerholtense provide useful supporting age control.
机译:这是埃及的苏伊士湾中中新世沉积的第一个详细的地层相关性,使用的是鞭毛藻囊肿。相关性基于来自位于苏伊士湾西南边缘的五个陆上钻孔的273个沟渠切割样品。研究的间隔以Gharandal组的Nukhul,Rudeis和Kareem组以及Ras Malaab组的Belayim组下部表示。这些中新世沉积不整合地覆盖下中新世或下中新世。鞭毛藻囊肿的记录比以前报道的更为多样化,埃及首次记录了许多分类单元。通过校准从同一组样品中获得的钙质纳米化石(NN生物区),建立了五个生物区并将其与年代地层学框架联系在一起:(1)阿基坦至布尔迪加利中期的马齿Ling属生物群落组合生物区(GOSI); (2)外圆角线虫标志的紫杉范围生物区(GOS2),从下至中布尔迪加里安; (3)棉铃虫Aptoodinium spiridoides Interval Biozone(GOS3),从中布尔迪加里到下朗厄安; (4)十字花君子菌间隔生物区(GOS4),上布尔迪加利安,朗根和下塞拉瓦利安?); (5)多球藻类zoharyi组合生物区(GOSS),上朗吉安和塞拉瓦利安?与来自地中海,中Paratethys,北大西洋地区和美国东部的其他中新世生物区带的比较表明,最高发生率的是Apteodinium spiridoides,Cordosphaeridium cantharellus,Distatodidium paradoxum ,外圆球菌和桔梗菌以及最低的外圆球菌和Sumatradinium soucouyantiae都是重要的数据,而最低的是隐孢子虫,圆角迷宫和圆孔菌? borgerholtense提供有用的年龄控制支持。

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