概括
在深海沉积物中,aloisoleucine与isoleucine的比例可靠地表明其年龄高达40万年. 这种氨基酸的种族化速率为沉积物年代和代遗传过程提供了洞察力.
科学领域:
- 地质化学 地质化学
- 古生物学的古生物学
- 氨基酸地化学 氨基酸地化学
背景情况:
- 氨基酸种族化是测定沉积物的关键地质年代学工具.
- 深海沉积物含有氨基酸,这些氨基酸在地质时间尺度上经历了种族化.
研究的目的:
- 为了研究深海沉积物中异黄素的种族化速率.
- 为了评估aloisoleucine与isoleucine比率的可靠性,作为一个地球时间学指标.
主要方法:
- 在日期的深海沉积物内核中分析异构素和异构素.
- 在各种基因条件下对氨基酸种族化的动力学研究.
主要成果:
- 随着沉积物年龄的增长,isoleucine的种族化逐渐增加.
- 沉积性氨基酸的种族化速度比自由氨基酸快得多.
- 素素/素素的比率是一个可靠的年龄指标,沉积物年龄高达40万年.
- 在大约1500万年以上的沉积物中,isoleucine会变成racemic.
结论:
- 素氨酸与素氨酸的比率为年轻深海沉积物的约会提供了一种有价值的方法.
- 代遗传过程影响沉积物中的氨基酸种族化动力学.
- 需要进一步的研究来完善老沉积物样本的年龄估计.
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