A. Dave, PLANKTIC FORAMINIFERAL BIOSTRATIGRAPHY AND BIOCHRONOLOGY OF THE POST-MIOGYPSINA NEOGENE OF BOMBAY OFFSHORE BASIN, Journal of the Geological Society of India, 51(4), 1998, pp. 533-542
Neogene planktic foraminiferal events and biostratigraphy of four deep
well sections viz D1-A-1, SS-1, R-13-1 and D-4-1 in the Bombay Offsho
re Basin have been established A pronounced and regional unconformity
separates the post-Miogypsina (post Zone N10 or N12, Middle Miocene) c
lay/claystone succession from the underlying carbonates. In most of th
e studied wells the hiatus covers a time span of 6.5 Ma (or 9.7 Ma) in
volving part of Middle Miocene and entire Late Miocene except in well
D-4-1 where its span is greatly reduced. Three planktic foraminiferal
datums viz LAD of Globigerina nepenthes (3.78 Ma), LAD of Dentoglobige
rina altispira (2.6 Ma) and LAD of Globigerinoides fistulosus (1.6 Ma)
have been demarcated in the Pliocene. A comparison of these biochrono
logic datums with those recorded from the DSDP sites in northern India
n Ocean is made. The delayed Last Occurrence of Globoquadrina dehiscen
s in Bombay Offshore is attributed to its reworking in Pliocene.