Vestige of The Ancient Estuarine of Cisaar Valley, Sumedang as One of the Pleistocene Fossil Bearing Site in West Jawa

U. Wibowo, Anton Ferdianto, Nur Laili, Dida Yurnaldi, R. Setiawan
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引用次数: 1

Abstract

Cisaar Valley is located on the east part of Sumedang Regency, West Jawa Province. It’s close to the boundary of Sumedang-Majalengka Regency. In this location the sandy and clay dominated sedimentary rocks are well exposed along the outcrops in the Cisaar Valley. These sedimentary rocks is inferred from Pliocene-Pleistocene deposits from Kaliwangu and Citalang Formation. Foraminifera microfossil that commonly used for interpretation of depositional environment is rarely found, whereas freshwater mollusk and vertebrate fossils often found in the sediment rocks of this area.  This condition raises a question, what is the environment of this valley in the past? Data obtained from measured stratigraphic sections along Cisaar river and its tributary rivers in Cibengkung and Cirendang hamlets, Jembarwangi village. There are at least three depositional paleoenvironments which from old to young are: shallow marine, estuarine and fluviatil braided channel depositional paleoenvironment.  Characteristics of the lower, middle and upper of the estuarine environment were found in this Cisaar Valley as the evidences of the oceanic regression processes was happened in the past in this area. 
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西爪哇更新世含化石遗址之一——苏梅当西萨尔河谷古河口遗迹
Cisaar Valley位于西爪哇省Sumedang Regency的东部。它靠近苏梅丹-马嘉伦卡摄政的边界。在这个位置,砂质和粘土为主的沉积岩沿着西萨尔山谷的露头很好地暴露出来。这些沉积岩来自卡里万古组和西塔朗组的上新世-更新世沉积岩。通常用于解释沉积环境的有孔虫微化石很少发现,而淡水软体动物和脊椎动物化石则经常在该地区的沉积岩中发现。这种情况提出了一个问题,这个山谷过去的环境是怎样的?数据来自Jembarwangi村Cibengkung村和Cirendang村沿Cisaar河及其支流河流测量的地层剖面。沉积古环境从古至今至少有三种沉积古环境:浅海沉积、河口沉积和河流辫状河道沉积古环境。西萨尔河谷的河口环境具有下、中、上游的特征,表明该地区过去曾发生过海洋退退过程。
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