| Project/Area Number |
09041114
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| Research Category |
Grant-in-Aid for international Scientific Research
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| Allocation Type | Single-year Grants |
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| Section | Field Research |
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| Research Field |
Stratigraphy/Paleontology
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| Research Institution | National Science Museum |
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Principal Investigator |
UEMURA K Nath.Sci.Mus., Dept.Geol., Div.Head, 地学研究部, 室長 (50000138)
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| Co-Investigator(Kenkyū-buntansha) |
HASEGAWA T Kanazawa Univ., Fac.Sci., Assistant, 理学部, 助手 (50272943)
FUTAKAMI M Kawamura-Gakuen Woom.Univ., Prof., 一般教育学部, 助教授 (50211529)
KODAMA K Kochi Univ., Fac.Sci., Prof., 理学部, 教授 (00153560)
SHIGETA Y Nath.Sci.Mus., Dept.Geol., Curator, 地学研究部, 研究官 (30270408)
YOKOYAMA K Nath.Sci.Mus., Dept.Geol., Div.Head, 地学研究部, 室長 (40126628)
岡本 隆 愛媛大学, 理学部, 助教授 (30201990)
前田 晴良 京都大学, 理学部, 助教授 (10181588)
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| Project Period (FY) |
1997 – 1998
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| Project Status |
Completed (Fiscal Year 1998)
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| Budget Amount *help |
¥15,100,000 (Direct Cost: ¥15,100,000)
Fiscal Year 1998: ¥7,600,000 (Direct Cost: ¥7,600,000)
Fiscal Year 1997: ¥7,500,000 (Direct Cost: ¥7,500,000)
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| Keywords | Cretaceous / Russia / Sakhalin / biostratigraphy / Paleontology / magnetostratigraphy / Cretaceous events / K / T境界 |
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| Research Abstract |
The Cretaceous System in the southern part of Sakhalin, Russian Far East, was studied biostratigraphically, combined with matnetostratigraphic and carbon isotope stratigraphic surveys in 1997 and 1998. to establish a more precise bic- and chronostratigraphy for the Cretaceous System and to interpretate various aspects in biotic and physical evolution during the Cretaceous in the North Pacific regions, At the sections along the Naiba and Makarov rivers, we obtained the most reliable bio- and chronosratigraphic scheme in the North Pacific regions for the Santonian, Campanian and most part of Maastrichtian. The results, together with the middle and upper parts of the Cretaceous along the Ai River section, provide a sound basis for the biostratigraphic correlation based on marine invertebrates such as ammonites and inoceramids, and for our understandings of marine faunal characteristics in time and space. Carbon isotope changes from terrestrial organic carbon were examined to show globally recognized events and o prove its utility as a stratigraphic tool. Mineral composition and monazite ages in the Cretaceous sandstones indicate the same provenance as those in central Hokkaido. Although not conclusive, we collected additional data on the marine K/T boundary at the Naiba River section. The "Danian" part is still needed further investigations, and only its uppermost part is characterized by plant megafossils of Tertiary type.
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