LATE MIOCENE–PLIOCENE PALEOCLIMATE AND PALEOCEANOGRAPHY OF HALANG AND TAPAK FORMATION IN PATIKRAJA, BANYUMAS BASIN
The Late Miocene–Pliocene represents a key interval of global climate reorganization marked by cooling trends, monsoon intensification, and major changes in Indo-Pacific ocean circulation. This study aims to reconstruct paleoceanographic and paleoclimatic evolution across the Halang–Tapak Formation transition in the Ba...