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Paleoenvironmental and Biostratigraphic Significance of Uvigerinids and Other Foraminifera from the Bhuban Formation, Assam-Arakan Basin, Mizoram


Affiliations
1 Wadia Institute of Himalayan Geology, 33 GMS Road, Dehra Dun - 248 001, India
2 MSR Residency, Pragathi Marg, JN Road, Rajahmundry - 53 3103, India
     

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Planktic and benthic foraminifera including uvigerinids are documented from the Upper Bhuban Formation, exposed at Thingdawl village, Kolasib district, Mizoram. The foraminiferal assemblage is poorly preserved and consists of index fossils useful for precise biochronology and interpretation of the depositional environment. A total of ten benthic and six planktic foraminiferal species are described. Six species belong to the genus Uvigerina, four to Ammonia, one species each of Globorotalia, Globigerinoides, Clavatorella, Praeorbulina and two species of the genus Orbulina. Based on lithological and foraminiferal assemblage, middle neritic to upper part of outer neritic paleobathymetry is inferred for the deposition of this part of the Upper Bhuban Formation. The foraminiferal assemblage suggests late Early Miocene to early Middle Miocene, (∼16 Ma) equivalent to planktic foraminiferal zones N8-N9 for the Upper Bhuban Formation.

Keywords

Bhuban Formation, Miocene, Uvigerinids, Foraminifera, Assam-Arakan Basin, Mizoram.
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  • Paleoenvironmental and Biostratigraphic Significance of Uvigerinids and Other Foraminifera from the Bhuban Formation, Assam-Arakan Basin, Mizoram

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Authors

Kapesa Lokho
Wadia Institute of Himalayan Geology, 33 GMS Road, Dehra Dun - 248 001, India
D. S. N. Raju
MSR Residency, Pragathi Marg, JN Road, Rajahmundry - 53 3103, India
R. J. Azmi
Wadia Institute of Himalayan Geology, 33 GMS Road, Dehra Dun - 248 001, India

Abstract


Planktic and benthic foraminifera including uvigerinids are documented from the Upper Bhuban Formation, exposed at Thingdawl village, Kolasib district, Mizoram. The foraminiferal assemblage is poorly preserved and consists of index fossils useful for precise biochronology and interpretation of the depositional environment. A total of ten benthic and six planktic foraminiferal species are described. Six species belong to the genus Uvigerina, four to Ammonia, one species each of Globorotalia, Globigerinoides, Clavatorella, Praeorbulina and two species of the genus Orbulina. Based on lithological and foraminiferal assemblage, middle neritic to upper part of outer neritic paleobathymetry is inferred for the deposition of this part of the Upper Bhuban Formation. The foraminiferal assemblage suggests late Early Miocene to early Middle Miocene, (∼16 Ma) equivalent to planktic foraminiferal zones N8-N9 for the Upper Bhuban Formation.

Keywords


Bhuban Formation, Miocene, Uvigerinids, Foraminifera, Assam-Arakan Basin, Mizoram.