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The study, which was conducted in the Baturaja location, South Sumatra, Particularly along the Air Rambangnia river, is geared toward finding out the planktonic and bentonic foraminifera fossils that are available in the study space so the relative age and depositional surroundings within the examine spot is often attained. Relative age and depositional atmosphere ended up attained depending on the presence of moderate to plentiful planktonic and bentonic foraminifera fossils. The investigate system utilized is descriptive-interpretative. This technique describes the info found in the field for interpretation utilizing pre-present theories. Planktonic foraminifera fossils present in abundance are Orbulina universa, Praeorbulina transitoria, Globigerina praebulloides, Orbulina bilobata.
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Meanwhile, planktonic foraminifera fossils having a reasonable amount are Globigerinoides conglobata, Globigerina boweri, Globigerina yeguaensis. While using the existence of such planktonic foraminifera fossils, it can be witnessed the relative age from the Baturaja Development in which these fossils were uncovered is Kala Miocene. Bentonic foraminifera fossils located in abundance within the study space are Tubinella funalis, Quinqueloculina seminulum, Pileolina wiesneri, Ammonia beccari. Even though the bentonic foraminifera fossils which are current in moderate figures are Anomalina colligera. Determined by the presence of such bentonic foraminifera fossils, it may be viewed which the depositional surroundings inside the examine space will be the Shallow Maritime (Neritic).
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