| Project/Area Number |
13440149
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Geology
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| Research Institution | Kyushu University |
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Principal Investigator |
SANO Hiroyoshi Kyushu University, Faculty of Science, Prof, 大学院・理学研究院, 教授 (80136423)
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| Co-Investigator(Kenkyū-buntansha) |
KAWAMURA Toshio Miyagi University of Education, Faculty of Education, Prof, 教育学部, 教授 (60186145)
MATSUMOTO Ryo University of Tokyo, Faculty of Science, Prof, 理学系研究科, 教授 (40011762)
IRYU Yasufimi Tohoku University, Faculty of Science, Assoc.Prof, 大学院・理学研究科, 助教授 (00250671)
KANO Akihiro Hiroshima University, Faculty of Science, Assoc.Prof, 大学院・理学研究科, 助教授 (60231263)
EZAKI Yoichi Osaka City University, Faculty of Science, Assoc.Prof, 大学院・理学研究科, 助教授 (60221115)
上野 勝美 福岡大学, 理学部, 助教授 (90241786)
すぎ山 哲男 福岡大学, 理学部, 教授 (50131826)
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| Project Period (FY) |
2001 – 2003
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| Project Status |
Completed (Fiscal Year 2003)
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| Budget Amount *help |
¥15,300,000 (Direct Cost: ¥15,300,000)
Fiscal Year 2003: ¥4,400,000 (Direct Cost: ¥4,400,000)
Fiscal Year 2002: ¥4,200,000 (Direct Cost: ¥4,200,000)
Fiscal Year 2001: ¥6,700,000 (Direct Cost: ¥6,700,000)
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| Keywords | calci-microbes / shallow-marine carbonates / paleoclimate / sea-level change / mass-extinction / metazoan reef-builders / シアノバクテリア / 炭酸塩堆積物 / 進化 / 大量絶滅 / 炭酸塩アトラス / 古環境変動 / 生物進化 / 海山型石灰岩 / 礁生態系 / パンサラッサ海 |
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| Research Abstract |
Part of results of this research program have been published in relevant journals and presented at many conferences and meetings. Major results are summarized as follows ;
1.Highly diverse calci-microbes, mainly of cyanobacteria, were recognized at many stratigraphic levels of shallow-marine carbonate units in Japan, but also in South China, western Canada, Ws confirmed their occurrence ranges in age from Silurian to Quaternary(Recent) through the field and microscopic examination.
2.Calci-microbes were recognized in a wide range of shallow-marine carbonate facies, and occurs as significant sediment-producer in varied environments and sediment-stabilizer and -binder of reefal fades.
3.Calci-microbes flourished especially in several geologic periods of decline and demise of metazoan reef-builders(e.g., Permo-Triassic boundary interval, Late Carboniferous prolonged and severe icehouse climate) and played a significant role as rock-forming biotas in these environment-devastated periods.
4.Various types of calci-microbial reefal facies and related organo-sedimentary structures were reported from shallow-marine carbonate sediments of many geologic ages. These microbial sediments are considered as having built up small-scale topographic highs of reefa facies, along with submarine cements.
Our results suggest that geochemical approaches needed in order to more thoroughly and quantitatively delineate temporal changes of environmental factors(temperatures, salinity, atmospheric CO_2 pressure, sea-level fluctuation, etc) in relation to flourish of calci-microbes. Some investigators of our research project have already begun hew researches with this aim.
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