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Genomic methylation patterns in archaeological barley show de-methylation as a time-dependent diagenetic process

机译:考古大麦中的基因组甲基化模式显示脱甲基化是时间依赖性的成岩过程

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摘要

Genomic methylation is variable under biotic and abiotic stresses in plants. In particular, viral infection is thought to significantly increase genomic methylation with particularly high activity around transposable elements. Here we present the genomic methylation profiles of grains of archaeological barley (Hordeum vulgare) from several strata from a site in southern Egypt, from the Napatan to the Islamic periods (800 BCE – 1812 CE). One sample tested positive for viral infection and exhibits an unusually high degree of genomic methylation compared to the rest. A decreasing trend in global methylation levels according to deposition date shows in-situ de-methylation of 5-methylcytosine, which can be described as a diagenetic process. This is most likely a deamination mediated de-methylation process and is expected to lead to 5 mC > T base modifications in addition to the C > U modifications due to cytosine deamination, so represents a time-dependent process of DNA diagenesis in ancient DNA.
机译:基因组甲基化在植物的生物和非生物胁迫下是可变的。特别地,病毒感染被认为以转座因子周围特别高的活性显着增加了基因组甲基化。在这里,我们介绍了从埃及南部某个地方,从纳帕坦到伊斯兰时期(公元前800年–公元1812年)几个地层的考古大麦(Hordeum vulgare)谷物的基因组甲基化分布。一个样品检测出病毒感染呈阳性,与其他样品相比,显示出异常高的基因组甲基化程度。根据沉积日期,总体甲基化水平的下降趋势显示了5-甲基胞嘧啶的原位脱甲基化,这可以描述为成岩过程。这很可能是脱氨介导的脱甲基过程,除由于胞嘧啶脱氨引起的C> U修饰外,预期还会导致5 mC> T碱基修饰,因此代表了古代DNA中DNA成岩的时间依赖性过程。

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