Planktic foraminifera, calcareous nannofossils and radiolaria were examined
from Early Neogene sequence of John Lawrence Island, Andaman Sea in order
to compare and contrast the stratigraphic ranges of various microfossil gro
ups to achieve a better biostratigraphic resolution. Based on stratigraphic
ranges of planktic foraminifera, the examined samples from the South Point
section of John Lawrence Island are referable to the upper part of the Glo
bigerinatella insueta Zone and lower part of Praeorbulina glomerosa Zone of
Srinivasan (1988). These zones also correspond to Globigerinoides bispheri
cus (M4b) Zone and Praeorbulina sicana-Praeorbulina glomerosa (M5a) Zone of
Berggren et al. (1995) delineating the Early / Middle Miocene boundary. Th
e boundary between these two zones demarcates the Jarawaian / Inglisian Sta
ge (Early / Middle Miocene) boundary. The calcareous nannofossil assemblage
recovered from the examined samples is assigned to Helicosphaera ampliaper
ta (NN4) Zone of Martini (1971), whereas radiolarian studies reveal the sam
ples to be referable to Calocycletta costata Zone of Reidel and Sanfilippo
(1970).
Berggren et al. (1995b) estimated an age range of 16.7-16.1 Ma for planktic
foraminiferal zones (M4b-M5a) and 18.3-15.6 Ma for the calcareous nannofos
sil zone (NN4). According to Nigrini (1985) the radiolarian Calocycletta co
stata Zone ranges in age from 17.3-15.7 Ma. A comparison of above estimated
ages reveals the age data based on planktic foraminifera to be more precis
e than the calcareous nannofossils and radiolaria. Thus, based on comparati
ve age data the sequence examined at John Lawrence Island represents the up
per part of calcareous nannofossil Helicosphaera ampliaperta (NN4) Zone and
also the upper part of the radiolaria Calocycletta costata Zone.
The inconsistency in the distribution and abundance of any single microfoss
il group throughout the examined section shows the need for employing multi
ple microfossil biostratigraphic approach. The study reveals that various m
icrofossil groups serve as complimentary to each other for attaining enhanc
ed biostratigraphic resolution.