1. S-Isovaline contained in meteorites, induces enantiomeric excess in D,L-glutamic acid during recrystallization
1. S-Isovaline contained in meteorites, induces enantiomeric excess in D,L-glutamic acid during recrystallization
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1. 陨石中含有的S-异缬氨酸,在重结晶过程中引起D,L-谷氨酸对映体过量
DOI:
10.1007/s11084-015-9407-8
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发表时间:
2015
期刊:
影响因子:
--
通讯作者:
S. Kojo
中科院分区:
文献类型:
--
作者:
宮永真澄;藤井将彦;酒井宏和;森本恵子;須藤元喜;仁木佳文;時光一郎;S. Kojo
S-Isovaline (S-Iva: 6.7 mmol) and D,L-glutamic acid (Glu: 2 mmol) were dissolved in 10 ml of hot water, and the resulting solution was divided in 5 vessels. After recrystallization, the crystals were collected from each vessel, and the enantiomeric excess (ee) of Glu was determined with chemical derivatization using 1-fluoro-2,4-dinitrophenyl- 5-L-leucinamide followed by high-performance liquid chromatography. Ten crystallizations provided all D-rich Glu with ee values of 2.69 % ± 0.81 % (mean ± standard deviation), and those using R-Iva provided all L-rich Glu with ee values of 6.24 % ± 2.20 %. Five recrystallizations of D,L-Glu alone provided ee values of 0.474 % ± 0.33 %. The differences among these three ee values were statistically significant, showing that S-Iva, which was present in meteorites caused a significant induction of ee in this physiological amino acid. This is the first outcome that S-Iva induced ee changes in a physiological amino acid. S-Iva did not induce any ee changes in D,L-asparagine, leucine, valine, methionine, phenylalanine, tryptophan, glutamine, tyrosine, aspartic acid, or histidine under similar recrystallizations.