Basin, was selected for this purpose. Lithologically, the Patala Formation is composed of shale and limestone interbeds. Three different fossil groupssmaller benthic foraminifera, planktic foraminifera, and calcareous nanno-planktonsare used to establish a biostratigraphic framework for the Patala Formation. The biozones recognized in this study include: (a) bathyal benthic biozones, BB1 and BB2 of the Late Palaeocene and Early Eocene, respectively; (b) planktic biozones, P4 and P5 of the Late Palaeocene, while E1 and E2 of the Early Eocene; and (c) Calcareous Nannoplanktons biozones: the NP9, which is further divided into NP9a and NP9b of the Late Palaeocene and Early Eocene, respectively. These biozones have been integrated to identify the Palaeocene-Eocene (P-E) boundary interval by applying widely used biostratigraphic criteria (i.e., Rhomboaster-Discoaster [RD]-assemblage of calcareous nanno-planktons). In this study, we have considered the lithological interval between ChN/TP-16 and ChN/TP-17 as a marker horizon for the P-E boundary