OSTRACODA MIOSEN DARI FORMASI CIMANDIRI, SUKABUMI, JAWA BARAT

LILI FAUZIELLY, . Winantris, Lia Jurnaliah, . Solihin, Ria Fitriani

Abstrak


ABSTRAK
Lima belas spesies fosil ostracoda berumur Miosen dari Formasi Cimandiri telah dianalisis dari 6 conto sedimen yang berasal dari penampang stratigrafi lintasan S. Cimerang, Sukabumi. Analisis mikrofosil secara kuantitatif , memperlihatkan ostracoda Miosen tersebar pada litologi batulempung. Ostracoda yang melimpah pada lintasan ini adalah Hemicytheridea ornata, Cytherella hemipuncta, Hemicytheridea reticulata, Cytherelloidea excavata, Cyherella javaseanse, and Keijella carrirei.
Berdasarkan kumpulan ostracoda, diketahui bahwa lingkungan pengendapan daerah penelitian adalah laut dangkal.
Kata kunci: Ostracoda, Miosen, Cimandiri, Lingkungan Pengendapan, Batulempung.
ABSTRACT
Fifteen species of fossil Ostracoda are describe from six sediment samples from Middle Miocene Cimandiri Formation, Sukabumi, West Java define from geological measure section profile Cimerang River. Microfossil Analysis based on quantitatively method, the distribution of Miocene Ostracoda be discovered in claystone lithology. Abundant ostracods are Hemicytheridea ornata, Cytherella hemipuncta, Hemicytheridea reticulata, Cytherelloidea excavata, Cyherella javaseanse, and Keijella carrirei. Based on the distribution of Ostracoda, it is known that the depositional environment of the study area is shallow sea.
Keyword: Ostracoda, Miocene, Cimandiri, Depositional Environment, Claystone.


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Referensi


Brady, G.S. 1868. Description of Ostracoda. In: Les fonds de la mer, Vol. 1 (L. De Folin & L. Perier, eds.), pp. 49–112. Savy, Paris.

Brady, G. S. (1911). Notes on marine Ostracoda from Madeira. Proceedings of the Zoological Society of London. 595-601.

Kingma, J.T. 1948. Contributions to the knowledge of the young-Caenozoic Ostracoda from the Malayan region. Ph.D. thesis, University of Utrecht, Utretch, The Netherlands.

LeRoy, L. W. (1939). Some small foraminifers, ostracoda and otoliths from the Neogene ("Miocene") of the Rokan-Tapanoeli area Central Sumatra. Natuurkunde Tijdschrift voor Nederlandsch-Indië. 99: 214-296.

McKenzie, K. G. & Sudijono, 1981. Plio - Pleistocene Ostracoda from Sangiran, Jawa,

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Sukamto, Rab.1975. Peta Geologi Lembar Jampang dan Balekambang, Jawa. Bandung : Pusat Penelitian dan Pengembangan Geologi.

Yassini, I. and Jones, B. G., 1995. Foraminifera and Ostracoda from Estuarine and Shelf Environments on the Southern Coast of Australia, The University of Wollongong Press, Wollongong, 484 p.

Brady, G.S. 1868. Description of Ostracoda. In: Les fonds de la mer, Vol. 1 (L. De Folin & L. Perier, eds.), pp. 49–112. Savy, Paris.

Brady, G. S. (1911). Notes on marine Ostracoda from Madeira. Proceedings of the Zoological Society of London. 595-601.

Kingma, J.T. 1948. Contributions to the knowledge of the young-Caenozoic Ostracoda from the Malayan region. Ph.D. thesis, University of Utrecht, Utretch, The Netherlands.

LeRoy, L. W. (1939). Some small foraminifers, ostracoda and otoliths from the Neogene ("Miocene") of the Rokan-Tapanoeli area Central Sumatra. Natuurkunde Tijdschrift voor Nederlandsch-Indië. 99: 214-296.

McKenzie, K. G. & Sudijono, 1981. Plio - Pleistocene Ostracoda from Sangiran, Jawa,

Indonesian Paleontology Series 1.

Mostafawi, N., 1992. Rezente Ostracoden aus Dem Mittleren Sunda -Schelf, Zwischen der Malaiishen Pbinsel und Borneo (abstract in English), Senckenbergiana lethaea72, 129 -168.

Sukamto, Rab.1975. Peta Geologi Lembar Jampang dan Balekambang, Jawa. Bandung : Pusat Penelitian dan Pengembangan Geologi.

Yassini, I. and Jones, B. G., 1995. Foraminifera and Ostracoda from Estuarine and Shelf Environments on the Southern Coast of Australia, The University of Wollongong Press, Wollongong, 484 p.




DOI: https://doi.org/10.24198/bsc.v17i2.22735

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