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铜绿假单胞菌在以缬氨酸 - C14为碳源生长过程中丙氨酸和天冬氨酸的形成。

Alanine and aspartate formation during growth on valine-C14 by Pseudomonas aeruginosa.

作者信息

Sokatch J R

出版信息

J Bacteriol. 1966 Jul;92(1):72-5. doi: 10.1128/jb.92.1.72-75.1966.

DOI:10.1128/jb.92.1.72-75.1966
PMID:4957438
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC276197/
Abstract

Sokatch, J. R. (University of Oklahoma School of Medicine, Oklahoma City). Alanine and aspartate formation during growth on valine-C(14) by Pseudomonas aeruginosa. J. Bacteriol. 92:72-75. 1966.-Pseudomonas aeruginosa grown with dl-valine-4,4'-C(14) synthesized alanine labeled mainly in carbons 1 and 3, indicating that the isopropyl carbons of valine were the precursors of pyruvate for alanine formation by a pathway which did not involve randomization of isotope. Alanine from cells grown on valine-1-C(14) contained isotope only in the carboxyl carbon, suggesting another route to pyruvate from valine by carbon dioxide fixation. Oxidation of valine to propionyl-coenzyme A (CoA), as it occurs in animal tissues, followed by the oxidation of propionyl-CoA to acrylyl-CoA, lactyl-CoA, and pyruvate, would account for the isotope data. Cells grown on valine oxidized valine, isobutyrate, and propionate immediately, whereas cells grown on acetate did not oxidize valine or isobutyrate and required an induction period before propionate was oxidized. P. aeruginosa grown with propionate-1-C(14) or propionate-2-C(14) formed alanine-1-C(14) and alanine-2-C(14), respectively, which agrees with the contention that at least part of the propionate is oxidized via the acrylate pathway. Aspartate formed from valine-1-C(14) was labeled only in the carboxyl carbons, whereas that formed from valine-4,4'-C(14) was labeled in all four carbons, but most heavily in carbons 1 and 3. These data suggest that the main route for the formation of the carbon skeleton of aspartate was by a C(3) plus C(1) condensation, with the C(3) unit derived from the isopropyl carbons of valine and the C(1) unit probably from carbon dioxide.

摘要

索卡奇,J. R.(俄克拉荷马大学医学院,俄克拉荷马城)。铜绿假单胞菌在缬氨酸-C(14)上生长期间丙氨酸和天冬氨酸的形成。《细菌学杂志》92:72 - 75。1966年。——用dl-缬氨酸-4,4'-C(14)培养的铜绿假单胞菌合成的丙氨酸主要在碳1和碳3处标记,这表明缬氨酸的异丙基碳是通过一条不涉及同位素随机化的途径形成丙氨酸的丙酮酸前体。在缬氨酸-1-C(14)上生长的细胞产生的丙氨酸仅在羧基碳处含有同位素,这表明通过二氧化碳固定从缬氨酸到丙酮酸还有另一条途径。缬氨酸氧化为丙酰辅酶A(CoA),如同在动物组织中发生的那样,随后丙酰辅酶A氧化为丙烯酰辅酶A、乳酰辅酶A和丙酮酸,这可以解释同位素数据。在缬氨酸上生长的细胞立即氧化缬氨酸、异丁酸和丙酸,而在乙酸盐上生长的细胞不氧化缬氨酸或异丁酸,并且在丙酸被氧化之前需要一个诱导期。用丙酸盐-1-C(14)或丙酸盐-2-C(14)培养的铜绿假单胞菌分别形成丙氨酸-1-C(14)和丙氨酸-2-C(14),这与至少部分丙酸盐通过丙烯酸途径氧化的观点一致。由缬氨酸-1-C(14)形成的天冬氨酸仅在羧基碳处标记,而由缬氨酸-4,4'-C(14)形成的天冬氨酸在所有四个碳处都有标记,但在碳1和碳3处标记最重。这些数据表明,天冬氨酸碳骨架形成的主要途径是通过C(3)加C(1)缩合,其中C(3)单元来自缬氨酸的异丙基碳,C(1)单元可能来自二氧化碳。

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本文引用的文献

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The conversion of L-valine to glucose and glycogen in the rat.大鼠体内L-缬氨酸向葡萄糖和糖原的转化
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