伊朗中始新世肺泡藻群的地层学:钙质纳米化石生物带的校正和肺泡藻的描述。

Mehdi Hadi , Lorenzo Consorti , Ali Bahrami , Mohammad Parandavar , Saeed Khorramdel
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摘要

本文在伊朗中部Sabzevar地区南部的Chah-Talkh剖面对伊朗中部中始新世Alveolina进行了精确的分类和年代地层定标。我们已经鉴定出kiolina, Alveolina stercusmuris和Alveolina nuttalli以及我们纳入Alveolina elliptica组的新物种Alveolina ozcani n.sp。我们还发现了Nummulites uroniensis, Nummulites obesus和Nummulites cf. verneuili以及相关的钙质纳米化石,这些化石看起来可靠,可以与浅底栖区(SBZ)建立深思熟虑的相关性。有孔虫生物地层学划分为SBZ13(中始新世)下卢腾统上部—中卢腾统下部,通过鉴定钙质纳米化石NP14b-NP15b或CNE8-CNE10生物带,进一步加强了与全球地层标准的相关性。
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Stratigraphy of the Alveolina elliptica group from the Middle Eocene of Iran: Calibration with calcareous nannofossils biozones and description of Alveolina ozcani n. sp.

Precise taxonomy and the chronostratigraphic calibration of the Middle Eocene Alveolina from Central Iran is here undertaken from the Chah-Talkh section of the southern Sabzevar region (Central Iran). We have identified Alveolina kieli, Alveolina stercusmuris and Alveolina nuttalli along with the new species Alveolina ozcani n. sp. that we include into the Alveolina elliptica group. We have also found Nummulites uroniensis, Nummulites obesus and Nummulites cf. verneuili and associated calcareous nannofossils that look reliable to make thoughtful correlations with the Shallow Benthic Zones (SBZ). The foraminiferal biostratigraphy suggests an assignment to the upper part of the lower Lutetian–lower part of the middle Lutetian, SBZ13 (Middle Eocene), further strengthened through the identification of the calcareous nannofossil NP14b–NP15b or CNE8–CNE10 biozones, providing a solid correlation with the global stratigraphic standards.

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