Middle Miocene planktonic foraminifera and their implications in the geology of Sabah

Author : Basir Jasin
Publication : Bulletin of the Geological Society of Malaysia
Page : 157-162
Volume Number : 45
Year : 2002
DOI : https://doi.org/10.7186/bgsm45200224

Bulletin of the Geological Society of Malaysia, Volume 45, May 2002, pp. 157 – 162


Middle Miocene planktonic foraminifera and their implications in the geology of Sabah

Basir Jasin

Program Geologi, Pusat Pengajian Sains Sekitaran & Sumber Alam, Fakulti Sains & Teknologi, Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor D.E., Malaysia


Abstract: Planktonic foraminifera flourished during Middle Miocene. They were recorded from the Ayer, Kuamut, Garinono mélanges, the Libong Tuffite, Tungku Formation, Tabanak Conglomerate, and Setap Shale Formation. Three assemblages of planktonic foraminifera were identified from the Libong Tuffite, the Garinono mélanges, and the Setap Shale Formation. The assemblages indicate an age ranging from the early Middle Miocene Globigerinoides sicanus-Globigerinatella insueta Zone (N 8) to the middle Middle Miocene Globorotaliafohsifohsi Zone (NI2). The occurrence of the planktonic foraminifera suggests that a transgressive event caused the influx of the nutrient-rich water mass into the area. This event was probably related to the rifting of the Sulu Sea and the development of the eastern Sabah deep marine environment where the mélanges were deposited. The occurrence of tuff and tuffite indicates volcanic activity in the region. The age of the volcanic tuff is middle Middle Miocene as dated by planktonic foraminifera.