Micropaleontology studies microfossils such as Large Benthic Foraminifera (LBF), nannofossils, and palynomorphs to reconstruct past environments. Our group primarily uses these microfossils for biostratigraphy, basin correlation, and paleoclimate reconstruction in Cenozoic carbonate-rich settings. LBF are key indicators of sea-level changes and shallow marine environments. Calcareous nannofossils provide high-resolution age control and help detect major climatic events like the PETM. Palynomorphs, including pollen, spores, and dinoflagellate cysts, aid in interpreting terrestrial inputs, salinity, and marine productivity. Combined, these proxies support detailed sequence stratigraphy, paleoclimate studies, and have applications in hydrocarbon exploration and basin analysis.