Roles of Hydrothermal Processes in Biological Evolution
Roles of Hydrothermal Processes in Biological Evolution
批准号:
07041081
负责人:
OHMOTO Hiroshi
金额:
$15.23万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for international Scientific Research
财政年份:
1995
资助国家:
日本
项目状态:
已结题
起止时间:
1995 至 1996
中文摘要
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英文摘要
The main objective of this research project was to understand the causes for major biological events in the early Earth, especially the first appearances of eukaryotes around 2 billion years ago and of large marine fauna around 550 million years ago. This objective was mostly pursued from systematic geochemical investigations of organic matter, minerals and rocks in about 1000 rock specimens that were collected during our field surveys in 4 areas : (A) the southern Ontario district, Canada (2.8-1.8 Ga sequence), (B) the Burin Peninsula, Newfoundland, Canada (570-520 Ma sequence), (C) the Normandy district, France (600-500Ma sequence), and (D) the Kaapvaal Craton, South Africa (3.0-2.0 Ga sequence).Our investigations have resulted in the following major findings :(1). According to a currently popular theory, the first major division of biological species (Eukaryotes, Bacteria, and Eubacteria) were caused by a dramatic rise of the atmosphericO_2 around 2.0 billion years ago. However, we … More have discovered various lines of geochemical evidence suggesting that the major division of biological species and the development of an oxic atmosphere had already taken place by 3.0 billion years ago.(2). "The great biological explosion" of around 550 million years ago was probably caused by the global changes in the ocean water chemistry (e.g., an increase in the phosphate flux) and climate.(3). The major changes in the ocean water chemistyr that affected the biological activity in ocean through geologic time were probably caused by the changes in the geographical configuration of continents (e.g., breaking of super continents) and in submarine hydrothermal activity in mid ocean ridges. These changes were in turn caused by changes in the convective patterns in the mantle.Some of the results from our investigations have already been presented at national and international scientific meetings (about 25 presentations). Five papers have been published (or in press) in major international journals, and about 20 more papers related to this project are in preparation. Less
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Kakegawa,T.,Haruna.,M.,Hayashi.,K.,and Ohmoto,H.: "Behavior of elements during diagenesis and hedrothermal alteration of shales : IV. Formational mechanism of pyrite nodules" J. of the Soc. of Resource Geol.45. 258 (1995)
Kakekawa,T.,Haruna.,M.,Hayashi.,K.,and Ohmoto,H.:“页岩成岩作用和热液蚀变过程中元素的行为:IV.黄铁矿结核的形成机制”J. of the Soc。
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Ohmoto,H.: "Genetic relationships between black shales and submarine hedrothermal ore deposits" J. of the Soc. of Resource Geol.45. 259 (1995)
Ohmoto,H.:“黑色页岩与海底热液矿床之间的成因关系”J. of the Soc。
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Watanabe, Y., Liu, Y., Naraoka, H., and Ohmoto, H.: "Behavior of elements during diagenesis and hydrothermal alteration of shales : III.C,N,S,and P" J.of the Soc.of Resource Geol.45. 258 (1995)
Watanabe, Y.、Liu, Y.、Naraoka, H. 和 Ohmoto, H.:“页岩成岩作用和热液蚀变过程中元素的行为:III.C、N、S 和 P”J.of the Soc。
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Kakegawa, T., Haruna, M., Hayashi, K., and Ohmoto, H.: "Behavior of elements during diagenesis and hydrothermal alteration of shales : IV.Formational mechanisms of pyrite nodules" J.of the Soc.of Resource Geol.45. 258 (1995)
Kakekawa, T.、Haruna, M.、Hayashi, K. 和 Ohmoto, H.:“页岩成岩作用和热液蚀变过程中元素的行为:IV. 黄铁矿结核的形成机制” J.of the Soc.of Resource Geol
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Ohmoto, H.: John Welley & Sons, New York.Sulfur and Carbon isotopes : in Barnes, H.L.ed.Geochemistry of Hydrothermal Ore Deposits, III., (1996)
Ohmoto, H.:约翰·韦利
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Kinetic Study on the Chemical and Isotope Exchange Reactions Between Aqueous Solutions and Solid Compounds.
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批准号:63420019
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项目类别:Grant-in-Aid for General Scientific Research (A)
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资助金额:$17.15万
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财政年份:1988
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负责人:OHMOTO Hiroshi
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依托单位:
海外基金