Nannoplankton Biostratigraphy from Banggai-Sula Basin, Central Sulawesi

Q4 Agricultural and Biological Sciences Journal of Tropical Biodiversity and Biotechnology Pub Date : 2024-03-11 DOI:10.22146/jtbb.85308
Efrilia Mahdilah Nurhidayah, A. Akmaluddin, D. Barianto, Salahuddin Husein, Asep Saripudin
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Abstract

The nannoplankton research was conducted in the MH-2 well, Banggai-Sula Basin, Central Sulawesi. Thirty-four ditch-cutting samples were utilized to observe the Minahaki, Kintom, and Biak Formations. Age determination was carried out using biostratigraphy method and standard procedure for first and last occurrence of nannoplankton biodatum and had an absolute age, widely known as a zone indicator.  This study aims to determine the age and nannoplankton biozonation of each geological formation in Banggai-Sula Basin. Based on the biostratigraphic analysis, 39 species from 14 genera with abundance frequencies ranging from rare to abundant were found in the MH-2 well. In this study, new results of the age of Banggai-Sula Basin areMiddle Miocene – Early Middle Pliocene (13,706 – 3,727 Ma), and can identify into six calcareous nannoplankton zones that are more detailed than previous researchers, Discoaster signus zone (NN5), Discoaster exilis zone (NN6-NN7), Discoaster berggrenii zone (NN11), Ceratolithus acustus zone (NN12), Helicosphaera sellii zone (NN13-NN15), and the Discoaster tamalis zone (NN16). Biostratigraphic data also shows new information for the first time, the absence of three zones from zone NN8 to zone NN10. This result indicates an unconformity in the Late Miocene age (10.606–8.20 Ma). 
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中苏拉威西邦盖-苏拉盆地的浮游动物生物地层学
浮游动物研究在中苏拉威西邦盖-苏拉盆地的 MH-2 井进行。利用 34 个沟切样本观察了 Minahaki、Kintom 和 Biak 地层。采用生物地层学方法和标准程序对首次和最后出现的浮游动物生物群进行了年龄测定,并得出了绝对年龄,即广为人知的区域指标。 本研究旨在确定邦盖-苏拉盆地各地质构造的年龄和浮游动物生物区系。根据生物地层分析,在 MH-2 井中发现了 14 个属的 39 个物种,丰度频率从罕见到丰富不等。这项研究的新结果表明,邦盖-苏拉盆地的年龄为中新世中期-中新世早期(13,706 - 3,727Ma),并可划分为六个钙质浮游动物区,比以往的研究更为详细、Discoaster signus 区(NN5)、Discoaster exilis 区(NN6-NN7)、Discoaster berggrenii 区(NN11)、Ceratolithus acustus 区(NN12)、Helicosphaera sellii 区(NN13-NN15)和 Discoaster tamalis 区(NN16)。生物地层数据还首次显示了新的信息,即从 NN8 区到 NN10 区没有三个区。这一结果表明在晚中新世(10.606-8.20Ma)出现了一个不整合。
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来源期刊
Journal of Tropical Biodiversity and Biotechnology
Journal of Tropical Biodiversity and Biotechnology Immunology and Microbiology-Applied Microbiology and Biotechnology
CiteScore
1.10
自引率
0.00%
发文量
40
审稿时长
12 weeks
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