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Dong Ye. PHOSPHORITES FORMED BY THE ACTION OF MICROORGANISM[J]. Acta Sedimentologica Sinica, 1985, 3(3): 1-6.
Citation: Dong Ye. PHOSPHORITES FORMED BY THE ACTION OF MICROORGANISM[J]. Acta Sedimentologica Sinica, 1985, 3(3): 1-6.

PHOSPHORITES FORMED BY THE ACTION OF MICROORGANISM

  • Received Date: 1984-04-07
  • Publish Date: 1985-09-10
  • According to their fabric features, Sinian-Cambrian Phosphorites in South China can be classified into three major basic types: micrograined, grained and crust-grained phosphorites, among which the textural component of the crust-grained phosphorite is predominately made up of phosphate crust-grains formed by microorganism. There are six forms of phosphate microorganism found in the phosphate crust-grains; ( 1 ) tube-shaped, ( 2 ) rod-shaped, ( 3 ) fibrous, ( 4 ) microglobal, ( 5 ) clumping, ( 6 ) tricuspid. All of them not only have distinct form features of microorganism,but also remain important organic components-amino acid and nucleic-acid-of organic tissues in their fossils. It is known that phosphorus, as a basic nutrient, is so necessary for the growth of all microorganism that none of them would not depend on it. Phosphorus is a structural element of enzymes, adenosine triphosphate, ribonucleic acid, desoxyri-bonucleic acid,nucleic acid and phospholipids,from which cell membranes are made. Microorganism plays a very important role in the circle of phosphorus on the earth. It is the microorganism action that is an important link in the circle of 'phosphorus in the ocean for the concentration of phosphorus to form ore deposits. Recent year studies on liquid crystal materials hane convinced the author that consideralle physiological behaviors of phosphorus-thirsty microorganism, i. e. the preferential extraction, accumulation and transportation of phosphates, may be attributed to the liquid crystal form of the tissues and cells of phosphorus-thirsty microorganism
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    (2)叶连俊,1959,中国磷块岩矿床的若干特点及找矿远景《中国磷块岩的形成特点矿石类型及远景评价》科学出版社。

    (3)南京大学地质系古生物地史教研室,1980,古生物学(下册),地质出版社。

    (4)朱为庆,1978,最古老的铁细菌,科学通报,第5期。

    (5)H.r·霍洛得尼,1953,铁细菌,1957中译本,科学出版社。

    (6)蔡浩然,1978,液晶态生物膜,科学通报,第4期。

    (7)武汉大学、复旦大学生物系微生物教研室,1979,微生物学,人民教育出版社。

    (8)薛廷耀编译,1962,海洋细菌学,科学出版社。

    (9)Cietrich Demus, 19810液晶的性质、理论与分子结构。《液晶的性质和应用》,上海科技出版社。

    (10)C· И ·库兹涅佐夫等,1966,地质微生物学引论(中译本)。地质出版社。

    (11)方宗熙、江乃曹,1981,生物学基础知识,中国青年出版社。

    (12)原田 馨(日),1978,生命起源的化学基础(中译本),上海科技出版社。

    (13)徐文玉、丁朝玉,1982,奥妙的物质循环。吉林人民出版社。

    (14) D·J·琼斯,微体化石概论(1959年中译本),科学出版社。

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    (16)E·D·Weinberg, 1977, Microoganisms anal minerals, EXXON Research and Eng-Engineering company, ANew york,

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  • Received:  1984-04-07
  • Published:  1985-09-10

PHOSPHORITES FORMED BY THE ACTION OF MICROORGANISM

Abstract: According to their fabric features, Sinian-Cambrian Phosphorites in South China can be classified into three major basic types: micrograined, grained and crust-grained phosphorites, among which the textural component of the crust-grained phosphorite is predominately made up of phosphate crust-grains formed by microorganism. There are six forms of phosphate microorganism found in the phosphate crust-grains; ( 1 ) tube-shaped, ( 2 ) rod-shaped, ( 3 ) fibrous, ( 4 ) microglobal, ( 5 ) clumping, ( 6 ) tricuspid. All of them not only have distinct form features of microorganism,but also remain important organic components-amino acid and nucleic-acid-of organic tissues in their fossils. It is known that phosphorus, as a basic nutrient, is so necessary for the growth of all microorganism that none of them would not depend on it. Phosphorus is a structural element of enzymes, adenosine triphosphate, ribonucleic acid, desoxyri-bonucleic acid,nucleic acid and phospholipids,from which cell membranes are made. Microorganism plays a very important role in the circle of phosphorus on the earth. It is the microorganism action that is an important link in the circle of 'phosphorus in the ocean for the concentration of phosphorus to form ore deposits. Recent year studies on liquid crystal materials hane convinced the author that consideralle physiological behaviors of phosphorus-thirsty microorganism, i. e. the preferential extraction, accumulation and transportation of phosphates, may be attributed to the liquid crystal form of the tissues and cells of phosphorus-thirsty microorganism

Dong Ye. PHOSPHORITES FORMED BY THE ACTION OF MICROORGANISM[J]. Acta Sedimentologica Sinica, 1985, 3(3): 1-6.
Citation: Dong Ye. PHOSPHORITES FORMED BY THE ACTION OF MICROORGANISM[J]. Acta Sedimentologica Sinica, 1985, 3(3): 1-6.
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