Abstract
Fourteen major and trace elements in marine sediment core samples collected from the coasts along eastern Japan, i. e. Tokyo Bay (II)(the recess), Tokyo Bay (IV)(the mouth), Mutsu Bay and Funka Bay and the Northwest Pacific basin as a comparative subject were determined by the instrumental neutron activation analysis (INAA). The sedimentation rates and sedimentary ages were calculated for the coastal sediment cores by the 210Pb method.
The results obtained in this study are summarized as follows:
(1) Lanthanoid abundance patterns suggested that the major origin of the sediments was terrigenous material. La*/Lu* and Ce*/La* ratios revealed that the sediments from Tokyo Bay (II) and Mutsu Bay more directly reflected the contribution from river than those of other regions.
In addition, the Th/Sc ratio indicated that the coastal sedime n ts mainly originated in the materials from the volcanic island-arcs, Japanese islands, whereas those from the Northwest Pacific mainly from the continent.
(2) The correlation between the Ce/U and Th/U ratios with high correlation coefficients of 0.920 to 0.991 indicated that all the sediments from Tokyo Bay (II) and Funka Bay were in reducing conditions while at least the upper sediments from Tokyo Bay (IV) and Mutsu Bay were in oxidizing conditions.
(3) It became quite obvious that the sedimentation mechanism and the s edimentation environment at Tokyo Bay (II) was different from those at Tokyo Bay (N), since the sedimentation rate at Tokyo Bay (II) was approximately twice as large as that at Tokyo Bay (N).
The sedimentary age of the 5th layer (8-10 cm in depth) from Funka Bay was calculated at approximately 1940-50, which agreed with the time, 1943-45 when Showa-shinzan was formed by the eruption of the Usu volcano.
