Le Paléolithique supérieur dans la péninsule coréenne et l’archipel du Japon

Abstract

There is one decisive gate between the Asian continent and the archipelago of Japan which is the strait of Tsushima that exists between the Korean peninsula and the archipelago. The strait is very narrow; however, the depth is relatively deep. If the sea level did not fall down to at least 130 meters below the present level, the terrestrial bridge would not be formed there. We know the former case concerning the first human population of which crossed this maritime gate of human groups 50,000 years ago. One supposes that the men did not have any means to cross there without the terrestrial bridge previous to 50,000 years. According to the studies of the abyssal drills of the Sea of Japan that one noted several lowering of the sea level according to the marine isotopic stages (MIS): 2, 6, 10, 12, 16, 18 and 20. With regard to the marine isotopic stage 2 that correspond to the Maximum-coldness of the last glacial when the sea dropped in below 125 meters in relation to the present level. According to study of the seismic stratigraphy and according to the obtained ages of seabed sediments by the method of carbon 14 that one concluded the concerned strait remained always like a marine channel and narrow during the last glacial (Park et al., 2000). We notice the typological common points between the lithic industry of the Korean peninsula and the one of the Kyushu island during the marine isotopic stage 2 (MIS-2) which are the tanged point (flake point), the bifacial point to triangular section (point to three retouched faces), etc. However, there are some differences in the composition of tools and the fabrication technique. Regarding the cultural origin and the big human migration, we cannot prove them for now. Such situation showed that some obstacles existed between such two regions. There are no common features on the flaking technique and the typology before 50,000 years in these two regions since we do not have any affirmative overdraft.