Abstract
Pliocene climate is known as global cooling. However, some study was showing a warm condition during Pliocene. During Pliocene in the tropics, the warm condition mechanisms are still in debate, whether it occurs due to the permanent El Niño or not. Indonesia is the prominent site to study climate from past to present. Several Pliocene climate studies have resulted from records surrounding Indonesia, but not many were found from inside the Indonesian sea. Pliocene records based on Pollen analysis content in Sajau Formation, Northeast Kalimantan, shows that the presence convinces the warm wet climate condition during the late Pliocene of arboreal pollen domination. However, the causing mechanism of warm wet Pliocene climate has remained a question.
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