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Titlebook: Origin, Evolution, and Modern Aspects of Biomineralization in Plants and Animals; Rex E. Crick Book 1989 Springer Science+Business Media N

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書(shū)目名稱(chēng)Origin, Evolution, and Modern Aspects of Biomineralization in Plants and Animals
編輯Rex E. Crick
視頻videohttp://file.papertrans.cn/705/704616/704616.mp4
圖書(shū)封面Titlebook: Origin, Evolution, and Modern Aspects of Biomineralization in Plants and Animals;  Rex E. Crick Book 1989 Springer Science+Business Media N
描述The Fifth International Biomineralization Symposium was held in May 1986 at The University of Texas at Arlington, Arlington, Texas. The chosen theme was the origin, evolution and modern aspects of biomineralization in plants and animals. Thus, the symposium was designed to bring together experts in ocean and atmospheric chemistry, geochemistry, paleontology, biology, medicine and related fields to share accumulated knowledge and to broaden research horizons. The contents of this volume reflect the diversified interests and views of contributors from these fields. Topics range from contrasting views of the origin of ocean chemistry, the cause or causes for the biomineralization among plants and animals, the evolution of style and structure of biomineralization, and the role of inorganic and organic compounds in biomineraliza- tion. It was clear from those gathered in Arlington that the efforts of all researchers in any aspect of biomineralization can be strengthened and extended by greater exposure to the work of others in allied fields. At the time of this printing, several collaborative efforts have grown from interest and contacts developed during the symposium. Rex E. Crick viii
出版日期Book 1989
關(guān)鍵詞Lamarck; amino acid; biology; evolution; ontogeny; phosphorus; phylogeny; plants; the origin
版次1
doihttps://doi.org/10.1007/978-1-4757-6114-6
isbn_softcover978-1-4757-6116-0
isbn_ebook978-1-4757-6114-6
copyrightSpringer Science+Business Media New York 1989
The information of publication is updating

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Tidally Deposited Bands in Shells of Barnacles and Molluscsusly and uniformly, despite the ubiquity of calcium and the relevant anions in the surrounding seawater. Yearly growth interruptions, ascribed to annual temperature changes or other climatic variables, have long been observed and understood (Orton, 1923).
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The Evolution of Mineral Skeletonss after that time. Recent work on the earliest skeletal fossils provides little support for the view that phosphatic skeletons were more common than carbonate skeletons when hard parts first developed.
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Calcium Binding Substance in the Hermatypic Coral, , (Dana)e aqueous or organic extracting solutions. The major component of the calcium-binding substances in the skeleton is phospholipid, but not the other lipids such as neutral lipid or glycolipid. A high-performance TLC revealed that the skeletal calcium-binding phospholipids consisted mainly of acidic phosphatidylserine.
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The Soda Ocean Concept and Its Bearing on Biotic Evolutionlcium physiology of living cells implicate that the stepwisebuildup of calcium in the ancient ocean was of primary importance for the generation of multicellular life and the onset of biocalcification.
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