Bulletin of the Geological Society of Malaysia, Volume 45, May 2002, pp. 179 – 184
Program Geologi, Pusat Pengajian Sains Sekitaran & Sumber Alam, Fakulti Sains & Teknologi Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor D.E., Malaysia
Abstract: The identified palynomorph assemblage from a rock sequence which is exposed at Felda Keratong 8, southeastern part of Pahang, resembles the Paradoxa Assemblage and it is suggested that its age is late Lower Cretaceous (Barremian-Albian). The occurrence of monosuIcate pollen of Clavatipollenites hughesii indicates that the emergence of angiosperms has taken place during the deposition of the sediments in this area.
Abstrak: Himpunan palinomorf yang dikenal pasti dari jujukan batuan yang tersingkap di Felda Keratong 8, bahagian tenggara Pahang, mempunyai persamaan dengan Himpunan Paradoxa dan dicadangkan usianya sebagai akhir Kapur Awal (Barremian-Albian). Kehadiran polen jenis monosulkat Clavatipo/lenites hughesii menunjukkan kemunculan angiosperma semasa pengendapan sedimen berlaku di kawasan ini.
https://doi.org/10.7186/bgsm45200227