Middle Eocene calcareous Nannofossil Biostratigraphy and Taxonomy of onland Kutch Basin, western India

J. Rai
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Abstract

Rich and diversified nannofossil assemblage comprising 110 species (13 new species and 8 new taxonomic combinations) and 4 calcareous dinoflagellates species are described from the type locality of Harudi Formation and Fulra Limestone Fonnation of Kutch Basin. The assemblage is dominated by the families Braarudosphaeraceae, Rhabdosphaeraceae and Calyptrosphaeraceae. All holococcolith genera except genus Peritrachelina are recorded in the assemblage. The assemblage is typically indicative of low-latitude, nearshore, shallow water environment and can be assigned to zone NP 17 Discoaster saipanensis Zone (Martini, 1971a emend. Rai, 1988). It also correlated with parts of both P 13 Orbulinoides beckmanni and P 14 Truncorotaloides rohri planktonic foraminifera Zones (Blow, 1969) and a part of D11 Dinoflagellate Zone (Costa & Manum in Vinken, 1988) of Bartonian age. Critical reappraisal of published fossil records including age diagnostic planktonic and larger foraminifera species and nannofossil data along with field observations of supratrappeans indicate, three discrete lithounits in ascending order viz., shale-marl-limestone upto terminal Fulra Limestone Formation.The proposed model questions the presence of marine sediments of Palaeocene, Lower Eocene and Lutetian age in onland Kutch Basin (Biswas & Raju, 1973; Biswas, 1992).
印度西部库奇盆地陆上始新世中钙质纳米化石生物地层学与分类
在Kutch盆地Harudi组和Fulra石灰岩Fonnation的模式区域,描述了丰富多样的纳米化石组合,包括110种(13种新种和8种新分类组合)和4种钙质鞭毛类。该组合以Braarudosphaeraceae、Rhabdosphaeraceae和Calyptrosphaeraceae为主。组合中除Peritrachelina属外,其余全球藻属均有记录。该组合具有典型的低纬度、近岸、浅水环境特征,可划分为NP - 17 disaster saipanensis zone (Martini, 1971a修订版)。意大利广播电视公司,1988)。它还与Bartonian时代的部分p13 Orbulinoides beckmanni和p14 Truncorotaloides rohri浮游有孔虫带(Blow, 1969)和部分D11 Dinoflagellate带(Costa & Manum in Vinken, 1988)相关。对已发表的化石记录(包括浮游生物和大型有孔虫物种的年龄诊断)和纳米化石数据以及对超超虫的实地观察进行了批判性的重新评估,表明三个独立的岩石单元按升序排列,即页岩-泥灰岩至富拉灰岩组。提出的模型质疑古新世、下始新世和鲁特世时代的海相沉积物在陆地Kutch盆地的存在(Biswas & Raju, 1973;Biswas, 1992)。
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