| Project/Area Number |
01470053
|
|---|
| Research Category |
Grant-in-Aid for General Scientific Research (B)
|
| Allocation Type | Single-year Grants |
|---|
| Research Field |
地質学一般
|
|---|
| Research Institution | University of Tokyo |
|---|
Principal Investigator |
IIJIMA Azuma University of Tokyo Faculty of Science, Professor, 理学部, 教授 (90011501)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
KAKUWA Yoshitaka University of Tokyo College of General Education, Assistant, 教養学部, 助手 (70124667)
OGIHARA Shigenori University of Tokyo Faculty of Science, Assistant, 理學部, 助手 (50214044)
TADA Ryuji University of Tokyo Faculty of Science, Assistant, 理學部, 助手 (30143366)
MATSUMOTO Ryo University of Tokyo Faculty of Science, Associate Professor, 理學部, 助教授 (40011762)
|
|---|
| Project Period (FY) |
1989 – 1990
|
| Project Status |
Completed (Fiscal Year 1990)
|
| Budget Amount *help |
¥5,300,000 (Direct Cost: ¥5,300,000)
Fiscal Year 1990: ¥1,000,000 (Direct Cost: ¥1,000,000)
Fiscal Year 1989: ¥4,300,000 (Direct Cost: ¥4,300,000)
|
|---|
| Keywords | Paleoenvironmental analysis / Opening of the Japan Sea / Siliceous sediments / C / S ratio of sediments / Tertiary Sedimentary basins / 古環境解析 / 新第三紀 / 堆積岩中の硫黄 / 女川層 / 東北日本 |
|---|
| Research Abstract |
(1) We established analytical method to determine total sulfur content in marine sediments using a LECO-HF20 equipment. Measurements are seriously affected by a little amount of salts, particularly NaCl. It is, therefore, necessary to desalt the marine sediments before analyzing.
(2) Total sulfur content (S) and total organic carbon content (C) in Neogene sediments of the Japan Sea, collected during ODP Leg 127, were analzsed. The C/S ratio of sediments reflects oxygen level in bottom water and it is about 3 in normal seawater sediments. The Leg 12 Neogene sediments show a wide range of the C/S ratio from 0.10 to 20. Late Miocene dark gray mudrocks have the minimum value of the C/S ratio, which indicates an anoxic environment due to isolation of the Japan Sea.
(3) Quaternary sedimentary columns at sites 794, 795 and 797 is characterized by cyclic repetition of lighter-colored and darker-colored muddy sediments. The lighter-colored muds have larger values of the C/S ratio indicating oxyic environments. In contrast, the darker-colored muds show smaller values suggesting anoxyic conditions. This cyclicity accords with the cyclicity of Quaternary climatic change.
(4) Evolution of Tertiary sedimentary basins in the circum-Japan Sea region with reference to opening of the Japan Sea is clarified on the basis of paleogeographical and paleobathymetrical maps of each interval from Eocene to latest Pliocene in age. The phenomena of the above items (2) and (3) can be interpreted by the evolution of the basins.
|
