The Surficial Basin Sediment Investigation and Its Concerned Vertebrate Fossils in Sirtwo Island, Western Part of Saguling Dam, West Java, Indonesia

Johan Budi Winarto, Wilda Aini Nurlathifah, Agustina Djafar, Andy Dharmedy Sipayung, Rahajeng Ayu Permana Sari, Halmi Insani
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Abstract

In October 2021, the depreciation of the water level of dam Saguling revealed the surficial sediment where was dam up Citarum river. Sirtwo island and surroundings are part of the body sediment were arisen which is part of the sedimentary facies in the western of Bandung Lake ancient. Several vertebrate fossils were found on Sirtwo island and Pasir Benteng island. The investigation of vertebrate fossils was carried out to understand where are deposited in Bandung lake. The geological survey lead to the recognition of types of lake deposits and was divided into 5 block observations i.e., Block A, Block B, Block C, Block D, and Block E. Geographic information system was used to determine the location points where the fossil was found and is correlated with other location. The fossils fragment is identified as vertebrate fossils i.e., Bovid sp., Rusa sp., and Elephas maximus. The detail of vertebrate fossils type and sediment petrology is under further analysis. The sedimentary facies are lake deposit and is distinguished into 3 sub-facies: 1) volcanic deposit with vertebrate fossil 2) sandstone tuff without vertebrate fossil and 3) sandstone tuff with vertebrate fossil. The age of lithology is estimated between 10.000 till >135.000 Years ago and the depositional environment is interpreted into fan lake, channel, and lake bottom. This study clearly determines lithofacies in the research area which contain vertebrate fossils.
印度尼西亚西爪哇萨古林大坝西部Sirtwo岛表层盆地沉积物调查及其相关脊椎动物化石
2021年10月,Saguling大坝水位下降,揭示了Citarum河上游大坝的地表沉积物。Sirtwo岛及其周围是万隆湖西部古沉积相的一部分,是体沉积的一部分。在Sirtwo岛和Pasir Benteng岛发现了一些脊椎动物化石。为了解万隆湖脊椎动物化石的沉积位置,开展了脊椎动物化石调查。通过地质调查对湖泊沉积类型进行了识别,并将其划分为A、B、C、D、e 5个区块观测,利用地理信息系统确定化石发现的位置点,并与其他位置进行对比。化石碎片被鉴定为脊椎动物化石,即Bovid sp., Rusa sp.和大象maximus。详细的脊椎动物化石类型和沉积物岩石学有待进一步分析。沉积相为湖泊沉积,可分为3个亚相:1)含脊椎动物化石的火山沉积;2)不含脊椎动物化石的砂岩凝灰岩;3)含脊椎动物化石的砂岩凝灰岩。岩石年龄估计在1万~ 13.5万年之间,沉积环境解释为扇湖、河道和湖底。本研究明确了研究区含脊椎动物化石的岩相。
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