English: The Palaeoloxodon Skeleton.

Show in National Museum Of Nature Science.

During the Ice Age, the dramatic drop in sea levels caused the Taiwan Strait to disappear, creating a vast new landmass that became a frontier for the ancient diamond-toothed elephant to expand its territory. These elephants undertook a long migration from the Huai River region in North China, leaving behind numerous traces of their habitats and skeletal remains. As time passed and glaciers melted, the Taiwan Strait reemerged, and fossils of these ancient elephants, long buried beneath the seabed, were serendipitously dredged up by fishermen. Although fragmented and incomplete, these fossil remnants are invaluable treasures for paleontologists, serving as crucial evidence of the ancient diamond-toothed elephant's remarkable sea-crossing journey.