中始新世(Lutetian-Bartonian)来自Batman和Siirt(土耳其东南部新特提斯南部)的大型底栖有孔虫组合:一个新的评估

Pub Date : 2023-01-01 DOI:10.29041/strat.20.1.01
Derya Sinanoglu
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引用次数: 0

摘要

在阿拉伯地台(土耳其东南部)原生单元之一的Hoya组Kurtalan和Eruh地区露头灰岩中描述了底栖有孔虫组合。在两个测量剖面中,其中一个剖面(DH-Dodan剖面)由于白云化作用,化石含量较少,而另一个剖面(EH-Eruh剖面)化石含量相当显著。有孔虫组合以Asterigerina rotula (Kaufmann)、Operculina ex. g.g omezi Colom和Bauza、Victoriella conoidea Rutten、Amphistegina sp.、Elphidium sp.、Peneroplis sp.、Carpenteria sp.、Stomatorbina sp.、百虫和轮虫形态和棘皮动物、Dodan剖面的珊瑚碎片为代表。有孔虫组合以Nummulites biedai Schaub、Nummulites maximus d’archiac、Nummulites perforatus de Montfort、Nummulites postfossulatus Sirel and Deveciler、Nummulites praeaturicus Schaub、Assilina exponens (Sowerby)、Sphaerogypsina globulus (Reuss)、Asterigerina rotula (Kaufmann)、Lockhartia cfh . hunti Ovey、Neoratlia sp.、Operculina sp.、Discocyclina sp.、Asterocyclina sp.、Lockhartia sp.、Lenticulina sp.、埃鲁剖面的千万种轮状动物和棘皮动物。所描述的化石组合表明,灰岩属于勒特—巴尔顿系,表明其沉积环境为极浅海相。该研究提供了有助于重新评价该地区始新世地质演化的生物地层学和地层资料。古生物地理上,在土耳其东南部的碳酸盐台地上记录的大型底栖有孔虫组合显示出与阿拉伯和中东台地的亲缘关系。
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Middle Eocene (Lutetian-Bartonian) larger benthic foraminifera assemblages from Batman and Siirt (Southern Neotethys, SE Turkey): a new assessment
The benthic foraminifera assemblage has been described in the limestones outcropped in Kurtalan and Eruh district of Hoya formation which is one of autochthonous units of Arabian Platform (SE Turkey). From the two measured sections, one of them has rare fossil content due to dolomitization (DH-Dodan section),while the other is fairly remarkable in terms of fossil content (EH-Eruh section). The foraminiferal assemblages are represented by Asterigerina rotula (Kaufmann), Operculina ex. gr. gomezi Colom and Bauza, Victoriella conoidea Rutten, Amphistegina sp., Elphidium sp., Peneroplis sp., Carpenteria sp., Stomatorbina sp., miliolid and rotaliid forms and echinoderms, coral fragments in the Dodan section. The foraminiferal assemblages are represented by Nummulites biedai Schaub, Nummulites maximus d’Archiac, Nummulites perforatus de Montfort, Nummulites postfossulatus Sirel and Deveciler, Nummulites praeaturicus Schaub, Assilina exponens (Sowerby), Sphaerogypsina globulus (Reuss), Asterigerina rotula (Kaufmann), Lockhartia cf. hunti Ovey, Neoratlia sp., Operculina sp., Discocyclina sp., Asterocyclina sp., Lockhartia sp., Lenticulina sp., miliolid-rotaliid forms and echinoderms in the Eruh section. The fossil assemblage described shows that the limestones are of Lutetian-Bartonian and this assemblage indicates a very shallow marine deposition environment. This study provides biostratigraphic and stratigraphic data that help to reassess the Eocene geological evolution of the region. Paleobiogeographically, larger benthic foraminiferal assemblages recorded on carbonate platforms in southeastern Turkey show an affinity to Arabian and Middle Eastern platforms.
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