Study on migration, disappearance and evolution of Ostatcoda with relation to the opening and clostire of the Tsushima and Korean Straits during the late Cenozoic
| Project/Area Number |
17540442
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| Research Category |
Grant-in-Aid for Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Stratigraphy/Paleontology
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| Research Institution | Shimane University |
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Principal Investigator |
IRIZUKI Toshiaki Shimane University, Interdisciplinary FacuIty of Science and Engineering, Associate Professor (60262937)
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| Project Period (FY) |
2005 – 2007
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| Project Status |
Completed (Fiscal Year 2007)
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| Budget Amount *help |
¥3,710,000 (Direct Cost: ¥3,500,000、Indirect Cost: ¥210,000)
Fiscal Year 2007: ¥910,000 (Direct Cost: ¥700,000、Indirect Cost: ¥210,000)
Fiscal Year 2006: ¥1,100,000 (Direct Cost: ¥1,100,000)
Fiscal Year 2005: ¥1,700,000 (Direct Cost: ¥1,700,000)
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| Keywords | Ostracoda / Tsushima Strait / Korean Strait / Javan Sea / Pliocene / Pleistocene / Miocene / 鍬江層 / 対馬 / 大村湾 / 宮崎層群 |
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| Research Abstract |
The aim of this study is to clarify the relationships between the opening and closure of the Thushima and Korean Straits and migration, disappearance and evolution of Ostracoda during the late Cenozoic. Surface sediment samples for the analysis of recent Ostracoda were collected from enclosed bays along the Tsushima Island. (Shush, Aso and Miura Bays) and Omura Bay. Concerning fossil. Ostracoda, I collected samples from the upper Pliocene Kuwae Formation, Niigata Prefecture, the Miyazaki Group, Miocene deposits in the Chugoku Mountains and so on. Based on these results and taking account of earlier studies, I led to the four conclusions as follows;
The Korean Strait has been a geographic bather far embayment ostracodes alter the middle Pleistocene. Namely dominant species in Japanese enclosed bays are different from those in Korean and Chinese enclosed bays
Warm water ostracode species living in marine areas shallower than 50 m in water depth were recognized in the interglacial deposits of the middle Pliocene Kuwae Formation. Especially, warm water inflows occurred certainly at about 2.9 Ma. However, there are only a few ostracode species which lived dominantly in shallow seas under the influence of the Kuroshio Current at that time. Thus warm water currents having flowed into the Japan Sea were weaker and thinner than today.
Temperate intermediate waters warmer than today (more than 6 ℃) were developed in each interglacial period of the Middle Pliocene. However, inflow routes of the waters were not clarified in this study.
Tropical to subtropical ostracode species were flourished through the northern to southern Japan during the Miocene climatic optimum (ca. 16 Ma) because the southern strait opened widely and strong warm water currents flowed into the Japan Sea. These ostracode assemblages were somewhat different from those in the late Early Miocene (ca. 17-18 Ma).
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Report
(4 results)
Research Products
(86 results)
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[Journal Article] Sea-level changes and water structures between ca. 3.5 to 2.8 Ma in the central part of the Japan Sea Borderland : analyses of fossil Ostracoda from the Pliocene Kuwae Formation, central Japan2007
Author(s)
Irizuki, T., Kusumoto, M., Ishida, K., Tanaka, Y.
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Journal Title
Palaeogcography, Palacoecology, Palacoclimatology vol.245
Pages: 421-443
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