THE PASSAGEWAY OF THE FLORA MIGRATION ON BOTH SIDES OF THE TAIWAN STRAIT IN PLEISTOCENEEPOCH

Taiwan is a part of the mainland of China. The Taiwan strait was formed as a result of faulting activity.The floras have closing relationship in both sides of the Taiwan strait with the mutual migration and distribution。Fujian- Taiwan land bridge is a part of the most shallow in the Taiwan strait.It was revealed on the sea surface for four times that is due to the regression in Pleistoeene glacial epoch,therefore Fujian-Taiwan land bridge turned into passageway of the flo-ras migration on both sides of the Taiwan strait in Pleistoeene Epoch.