A new procedure for determining DL amino acid ratios in fossils using reverse phase liquid chromatography

被引:281
作者
Kaufman, DS [1 ]
Manley, WF
机构
[1] Utah State Univ, Dept Geol, Logan, UT 84322 USA
[2] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA
基金
美国国家科学基金会;
关键词
D O I
10.1016/S0277-3791(97)00086-3
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Amino acid geochronology is based largely on the extent of racemization in fossils, as measured by the ratio amounts of D- and L-isomers. Here we report a new, fully automated reverse phase HPLC procedure for simple and precise stereoisomeric separations. At least nine pairs of ar-amino acids are separated with baseline resolution in 75 min using commercially available reagents and equipment. By optimizing precolumn derivatization, we attained compound detectability in the sub-picomole range, sufficient for milligram-size molluscan samples. Analytical reproducibility for nine Dr ratios in four fossils spanning a broad range of ages averages 7% (n = 14-28). Asp and Glu Dr ratios are the most consistently well resolved and reproduced, with analytical variations of 2 and 3%, respectively. Ratios in three fossil mollusc samples analyzed by the new method and measured previously by GC-based laboratories overlap in 17 out of 18 cases, when considering the fl sd analytical errors and +/-1 sd inter-laboratory variation. To determine the hydrolysis procedure that minimizes induced racemization while maximizing amino acid recovery, nle hydrolyzed seven powdered molluscan fossils of different ages and genera for 0-48 h at 110 degrees C. Concentrations of most amino acids reached a stable plateau after 6-8 h. For young samples, in which faster-racemizing amino acids are targeted (especially Asp), a hydrolysis time of 6 h minimizes induced racemization while attaining nearly complete amino acid recovery. For older samples, 22 h at 110 degrees C is preferred. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:987 / 1000
页数:14
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