COMMENTS ON “BIOSTRATIGRAPHIC INVESTIGATION AND DEPOSITIONAL MODEL OF THE LATE THANETIAN RANIKOT AND THE YPRESIAN LAKI FORMATIONS IN THE SUBSURFACE OF THE SOUTHERN INDUS BASIN, PAKISTAN”

Maqsood ur Rahman
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Abstract

This note aims to criticize the identification of key larger benthic foraminifera (LBF) at species or genus rankand the biostratigraphic interpretations. The species figured in the under-discussion paper are largely misidentified. The authors did not follow the fundamental principles for the identification of the LBF. Usingthe misidenti fied species led to the incorrect establishment of the shallow benthic zones (SBZ). Consequently,pro vided the wrong biostratigraphic age to the Lower Eocene succession of the Southern Indus Basin. Themicropaleontological analysis coupled with microfacies description that suffers from the misidentification of most key-index taxa is useful for the definition of a precise depositional environment. The stratigraphic nomenclature is also wrong throughout the article where the authors confused the Group and Formation. The italic and non-italic protocols for the species and genus rank are also wrong throughout the article. Therefore, this note highlights the errors which have been made regarding the age, depositional model, and nomenclature of the Lower Eocene succession of the Southern Indus Basin.
《巴基斯坦南印度河盆地地下晚thanetian ranikot和ypresian laki组生物地层调查与沉积模式》述评
本文旨在对大型底栖有孔虫(LBF)的种属鉴定和生物地层学解释提出批评。在讨论中的论文中所提到的物种在很大程度上是被错误识别的。作者没有遵循识别LBF的基本原则。使用错误识别的物种导致了浅层底栖区(SBZ)的错误建立。从而为南印度河盆地下始新世的演替提供了错误的生物地层年龄。微古生物学分析与微相描述相结合对精确的沉积环境的定义是有用的,而微相描述受大多数关键指数分类群的错误识别的影响。整篇文章的地层命名法也是错误的,作者混淆了群和组。在整个文章中,种和属等级的斜体和非斜体协议也是错误的。因此,本文强调了在南印度河盆地下始新世序列的年代、沉积模式和命名方面的错误。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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