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首页> 外文期刊>Quaternary geochronology >Isolation of the intra-crystalline proteins and kinetic studies in Struthio camelus (ostrich) eggshell for amino acid geochronology
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Isolation of the intra-crystalline proteins and kinetic studies in Struthio camelus (ostrich) eggshell for amino acid geochronology

机译:鸵鸟双峰(鸵鸟)蛋壳中晶体内蛋白的分离和动力学研究,用于氨基酸年代学

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摘要

Ostrich eggshell is a favoured substrate for amino acid geochronology, yielding consistent results and thought to approximate a closed system with respect to protein diagenesis. We found that the intra-crystalline fraction in ostrich eggshell is more challenging to isolate than that from mollusc shells, requiring 72 h oxidative treatment with NaOCl, resulting in a loss of up to half of the whole-shell protein. Through high temperature studies we have shown that under continuous leaching conditions approximately 99% of the intra-crystalline amino acids are resistant to leaching. Furthermore, high temperature experiments of the intra-crystalline proteins at pH 5, 7 and 9 have shown that this fraction is unaffected by pH changes over this range. This study confirms that the intra-crystalline protein fraction in OES may approximate a closed system. The intra-crystalline amino acids have been shown to follow predictable patterns of hydrolysis and racemization for all amino acids studied. Most amino acids showed some conformity to pseudo reversible first order reaction kinetics for racemization over limited D/L ranges, but hydrolysis was generally described poorly by first order kinetics. We therefore tried a new scaling method to determine relative reaction rates, estimated by applying scaling factors to overlap the observed rates of racemization (or hydrolysis) at the different temperatures, with the advantage of not forcing a linear relationship with respect to time. Using apparent first order kinetics, constrained power functions and scaling methods, we estimated the Arrhenius parameters (activation energy, EA and frequency factors, A) for both hydrolysis and racemization. The different methods for the estimation of reaction rates can give significantly different, but equally plausible, activation energies. This study reinforces previous work that indicates we need to understand the underlying mechanisms in order to estimate accurate kinetic parameters.
机译:鸵鸟蛋壳是氨基酸年代学的首选底物,可产生一致的结果,并被认为与蛋白质成岩作用近似为封闭系统。我们发现,与从软体动物壳中分离相比,鸵鸟蛋壳中的晶体内部分更具挑战性,需要用NaOCl进行72 h氧化处理,导致损失多达一半的全壳蛋白。通过高温研究,我们表明在连续浸提条件下,大约99%的晶内氨基酸对浸提具有抵抗力。此外,在pH 5、7和9下对晶体内蛋白进行的高温实验表明,该部分不受此范围内pH变化的影响。这项研究证实,OES中的晶体内蛋白部分可能接近一个封闭的系统。对于所有研究的氨基酸,结晶内氨基酸已显示出遵循可预测的水解和外消旋化模式。大多数氨基酸显示出在有限的D / L范围内外消旋的拟可逆一级反应动力学的某些一致性,但通常一级动力学对水解的描述很差。因此,我们尝试了一种新的标度方法来确定相对反应速率,该方法通过应用标度因子使在不同温度下观察到的外消旋化(或水解)速率重叠,从而避免了相对于时间的线性关系。使用表观的一阶动力学,受约束的幂函数和缩放方法,我们估算了水解和外消旋作用的Arrhenius参数(活化能,EA和频率因子,A)。估计反应速率的不同方法可能会产生明显不同但同样合理的活化能。这项研究加强了以前的工作,表明我们需要了解潜在的机制才能估算出准确的动力学参数。

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