Sains Malaysiana 42(5)(2013): 561–570

 

Aptian to Turonian Radiolarians from Chert Blocks in the Kuamut Melange, Sabah, Malaysia

(Aptian hingga Turonian Radiolaria daripada Blok Rijang dalam Melange Kuamut, Sabah, Malaysia)

 

 

Basir Jasin

Geology Program, School of Environment and Natural Resource Sciences

Faculty of Science and Technology, Universiti Kebangsaan Malaysia

43600 Bangi, Selangor, Malaysia

 

Junaidi Asis*

Geology Program, School of Science and Technology, Universiti Malaysia Sabah

88999 Kota Kinabalu, Sabah, Malaysia

 

Diserahkan: 26 Mei 2011/Diterima: 14 November 2012

 

ABSTRACT

The Kuamut Melange is located in the Kunak district, southeast Sabah. The mélange consists of clasts and blocks of broken Paleogene formations, and dismembered ophiolite blocks embedded in shale matrix. Fourteen samples were collected from sections S1 and S2 of the Kuamut Melange. A total of 45 species of radiolarians have been identified and only 36 selected species are used for age determination. Three assemblages (I-III) were identified. Assemblage I consists of Dictyomitra excellence, Crucella bossoensis, Hiscocapsa asseni, Hexapyramis precedis, Thanarla brouweri, Acanthocircus levis, Obeliscoites vinassai, Stichomitra communis, Staurosphaeretta longispina, Xitus spicularius, Triactoma cellulosa, and Dactyliosphaera maxima. This assemblage is marked by the occurrence of Crucella gavalai indicative of Aptian to Albian in age. Assemblage II was characterized by zonal maker Xitus mclaughlini. Other species in this assemblage are Xitus spinosus, Stichomitra tosaensis, Dictyomitra gracilis, Dictyomitra montisserei, Pseudodictyomitra pseudomacrocephala, Pessagnobrachia fabianii, Crucella messinae, Tuguriella pagoda, Dictyomitra obesa, Triactoma paronai, Rhopalosyringium euganeum, Acanthocircus venetus, Acaeniotyle rebelis, Dictyomitra formosa, Pseudodictyomitra tiara and Patellula helios. This assemblage ranges from Albian to Cenomanian. Assemblages III is represented by zonal maker Crucella cachensis and others species in this assemblage are Hemicryptocapsa polyhedra, Eostichomitra bonum, Pseudotheocampe tina, Ultranapora cretacea and Alievium superbum. Assemblage III is Turonian in age. The radiolarian assemblages suggest that the age of chert blocks ranges from Aptian to Turonian, Cretaceous. The cherts were originally deposited on an oceanic crust of a marginal basin during Cretaceous and were tectonically deformed to form melange in Miocene time.

 

Keywords: Aptian; Kuamut; Melange; radiolarians; Turonian

 

ABSTRAK

Melange Kuamut terletak di daerah Kunak, tenggara Sabah. Melange Kuamut terdiri daripada klasta dan blok batuan sedimen formasi Paleogen yang terpecah dan blok ofiolit yang terpisah, yang tertanam dalam matriks syal. Empat belas sampel diambil daripada singkapan S1 dan S2 dalam Melange Kuamut. Sebanyak 45 spesies telah dikenal pasti dan hanya 36 spesies pilihan digunakan untuk penentuan usia. Tiga himpunan (I-III) telah dikenal pasti. Himpunan I terdiri daripada Dictyomitra excellence, Crucella bossoensis, Hiscocapsa asseni, Hexapyramis precedis, Thanarla brouweri, Acanthocircus levis, Obeliscoites vinassai, Stichomitra communis, Staurosphaeretta longispina, Xitus spicularius, Triactoma cellulosa dan Dactyliosphaera maxima. Himpunan ini ditandai oleh kehadiran Crucella gavalai yang menunjukkan usia Aptian hingga Albian. Himpunan II dicirikan oleh penanda zon Xitus mclaughlini. Spesies lain dalam himpunan ini adalah Xitus spinosus, Stichomitra tosaensis, Dictyomitra gracilis, Dictyomitra montisserei, Pseudodictyomitra pseudomacrocephala, Pessagnobrachia fabianii, Crucella messinae, Tuguriella pagoda, Dictyomitra obesa, Triactoma paronai, Rhopalosyringium euganeum, Acanthocircus venetus, Acaeniotyle rebelis, Dictyomitra formosa, Pseudodictyomitra tiara dan Patelulla helios yang menunjukkan usia Albian hingga Cenomanian. Himpunan III diwakili oleh penanda zon Crucella cachensis dan spesies lain dalam himpunan ini ialah Hemicryptocapsa polyhedra, Eostichomitra bonum, Pseudotheocampe tina, Ultranapora cretacea dan Alievium superbum. Himpunan III ini berusia Turonian. Himpunan radiolarian ini membuktikan bahawa usia rijang ialah Aptian hingga Turonian, Kapur. Rijang diendapkan di kerak lautan iaitu di lembangan pingiran semasa Aptian-Turonian, seterusnya mengalami defomasi tektonik yang membentuk melange pada usia Miosen.

 

Kata kunci: Aptian; Kuamut; Melange; radiolaria; Turonian

RUJUKAN

Aitchison, J.C. 1994. Early Cretaceous (pre-Albian) radiolarian from bloks in Ayer Complex mélange, eastern Sabah, Malaysia, with comments on their regional tectonic significance and the origins of enveloping mélanges. Journal SE Asian Earth Sci. 9(3): 255-262.

Bak, M. 1999. Cretaceous radiolarian zonation in the Polish part of the Pienny Klippen belt (Western Carpathians). Geologica Carpathica 50(1): 21-31.

Basir Jasin. 1991. The Sabah Complex - a lithodemic unit (a new name for the Chert Spilite Formation and its ultramafic association). Warta Geologi 17(6): 253-259.

Basir Jasin. 1992. Significance of radiolarian chert from the Chert-Spilite Formation, Telupid, Sabah. Bulletin Geological Society of Malaysia 31: 67-83.

Basir Jasin. 2000. Geological significance of radiolarians chert in Sabah. Bulletin Geological Society of Malaysia 44: 35-43.

Basir Jasin. 2000a. Geological significance of radiolarian chert in Sabah. Bulletin of Geological Society Malaysia 44: 35-43.

Basir Jasin. 2000b. Significance of Mesozoic Radiolarian Chert in Sabah and Sarawak. Proceedings of Annual Geological Conference, pp. 123-130.

Basir Jasin. 2002. Middle Miocene planktonic foraminifera and their implications in the geology of Sabah. Bulletin of Geological Society Malaysia 45: 157-162.

Basir Jasin & Sanudin Tahir. 1988. Barremian radiolaria from the Chert-spilit formation, Kudat, Sabah. Sains Malaysiana 17(1): 67-79.

Basir Jasin, Ahmad Jantan, Lim Peng Seng & Mat Niza Abd. Rahman. 1989. Some microfossils from the Wariu formation. Sains Malaysiana 18(1): 57-75.

Basir Jasin & Sanatulsalwa Hasan. 1992. Some early Cretaceos radiolaria from chert sequence in the Mandurian area, Sabah. Sains Malaysiana 21(1): 55-67.

Basir Jasin, Sanudin Tahir & Zaidi Harun. 1995. Some Miocene planktonic foraminifera from Bidu-Bidu area, Sabah. Warta Geologi 21(4): 241-246.

Basir Jasin & Tongkul F. 2000. Fosil radiolaria daripada Jujukan Ofiolit Lembah Baliojong, Tandek, Sabah. Warisan Geologi Malaysia 3: 219-230.

Clennell, B. 1991. The origin and tectonic significance of mélange of Eastern Sabah, Malaysia. Journal of the Southeast Asian Earth Science 6: 407-425.

Clennell, B. 1992. The Melange of Sabah, Malaysia. PhD thesis. University of London. (unpublished).

Collenette, P. 1965. The geology and mineral resources of the Pensiangan and upper Kinabatangan Area, Sabah. Malaysia Geological Survey Borneo Region, Memoir 12.

Hutchison, C.S. 1992. The Southeast Sulu Sea, a Neogene marginal basin with outcropping extensions in Sabah. Bulletin of the Geological Society Malaysia 32: 69-88.

Hutchison, C.S. 2005. Geology of North-West Borneo (Sarawak, Brunei and Sabah). Amsterdam: Elsevier.

Guex, J. 1991. Biochronological Correlations. Berlin: Springer Verlag.

Jones, D.L. & Murchey, B. 1986. Geologic significance of Paleozoic and Mesozoic radiolarian chert. Ann. Rev. Earth Planet. Sci. 14: 455-492.

Leong, K.M. 1974. The geology and mineral resources of the upper Segama Valley and Darvel Bay area Sabah Malaysia. Geological Survey of Malaysia. Memoir 4: 104-134.

Leong, K.M. 1977. New age from radiolarian cherts of the Chert-Spilite Fomation, Sabah. Bulletin Geological Society of Malaysia 8: 109-111.

Liechti, P., Roe, F.W. & Haile, N.S. 1960. The geology of Sarawak, Brunei and eastern part of North Borneo. British Borneo Geol. Survey Bull. 3.

Mc Manus, J. & Tate, R.B. 1986. Mud volcanoes and the origin of certain chaotic deposits in Sabah. Bull. Geol. Soc. Malaysia 19: 193-205.

O’Dogherty, L., Carter, E.S., Dumitrica, P., Gorican, S., De Wever, P., Bandini, A.N., Baumgartner, P.O. & Matsuoka, A. 2009. Catalogue of Mesozoic radiolarian genera. Part 2: Jurassic-Cretaceous. Geodiversitas 31(2): 271-356.

O’Dogherty, L. 1994. Biochronology and plaeontology of mid-cretaceous radiolarians from Northern Apennines (Italy) and Betic Cordillera (Spain). Memoires de Geologie (Lausanne) 21: 1-413.

Pessagno, E.A. & Newport, R.L. 1972. A technique for extracting Radiolaria from Radiolarian chert. Micropaleontology 18(2): 231-234.

Rangin, C., Bellon, H., Bernard, F., Letouzey, J., Muller, C. & Sanudin Tahir. 1990. Neogene arc-continent collision in Sabah, Northern Borneo (Malaysia). Tectonophysics 183: 305-319.

Sanfilippo, A. & Riedel, W. R. 1985. Cretaceous Radiolaria. In Plankton Stratigraphy, edited by Bolli, H.M. Saunders, J.B. & Perch-Nielsen, K. New York: Cambridge University Press. pp. 573-712.

Sanudin Tahir & Baba Musta. 2007. Pengenalan kepada Stratigrafi. Kota Kinabalu: Penerbit Universiti Malaysia Sabah.

Schaaf, A. 1981. Late early cretaceous radiolaria from deep Ssea drilling Pproject Leg 62. In Deep Sea Drilling Project Reports and Publication, edited by Thiede, J., Vallier, T.L. & Adelseck, C.G. Washington D.C.: U.S. Government Printing Office. 62: 419-470.

Schaaf, A. 1985. Un nouveau canevas biocronologique du Cretace inferieur et moyen: les biozones a radiolares. Sci. geol. (Strasbourg) Bull. 38(3): 227-267.

Thurow, J. 1988. Cretaceous radiolarians of the North Atlantic Ocean: ODP Leg 103 (Site 638, 640 and 641) and DSDP Legs 93 (Site 603) and 47B (Site 398). In. Boillot, G., Winterer, E.L. et al. (Ed.). Proceedings of the Ocean Drilling Program, Scientific Result 103, p. 379-418. Texas, College Station.

Vishnevskaya, V.S. 1993. Jurassic and Cretaceous radiolarian biostratigraphy in Russia. In. Radiolarian of giant and subgiant fields in Asia, edited by Blueford, J. & Murchey, B. Micropaleontology special publ. 6: 175-200.

 

 

*Pengarang untuk surat-menyurat; email: junaidiasis@gmail.com

 

 

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