非编码 DNA 在寒武纪大爆发中的可能作用

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引用次数: 0

摘要

“寒武纪大爆发”(Cambrian explosion, CE)是指寒武纪(Cambrian period, CP)沉积物中生物化石数量的急剧增加,这一时期开始于5.388±20万年前,结束于4.854±190万年前。正是在CP时期,生物圈发生了巨大的变化:如果在此之前,几乎所有的生命都是简单的单细胞生物,那么在CE之后,复杂的多细胞生物的数量急剧增加。然而,这些剧烈变化的原因仍然未知。人们提出了各种各样的假设:气候急剧变化;有性生殖的出现;双侧性或氧浓度的增加使多细胞生物得以发展。显然,问题的实质是澄清生物圈根本变化的机制和物质基础。要实现这样的大爆发,基因组的根本改变是必要的。这表明,CE与真核生物DNA基因组中最可移动部分的进化有关,而不是与先前存在或新出现的基因数量的增加有关。从我们的观点来看,非编码DNA的进化构成了真核生物基因组中绝大多数DNA,可能在CE的出现中发挥了重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Possible Role of Non-coding DNAs in the Cambrian Explosion
The "Cambrian explosion" (CE) refers to a sharp increase in the number of fossils of living beings in the sediments of the Cambrian period (CP), which began 538.8 ± 0.2 million years ago and ended 485.4 ± 1.9 million years ago. It was in the CP that drastic changes took place in the biosphere: if before that almost all life was simple and unicellular, then after the CE there was a sharp increase in the number of complex multicellular organisms. However, the reason(s) for these drastic changes remains unknown. Various hypotheses were put forward: a sharp change in climate; the appearance of sexual reproduction; bilaterality or an increase in oxygen concentration that allowed the development of multicellularity. Apparently, the essence of the problem is to clarify the mechanisms and material basis of fundamental changes in the biosphere. For such an explosion, radical changes in the genome are necessary. It is suggested that the CE is associated with the evolution of the most mobile part of the eukaryotic DNA genome, rather than an increase in the number of previously existing or newly emerged genes. From our point of view, the evolution of non-coding DNAs, which make up the vast majority of DNA in the eukaryotic genome, could play an important role in the emergence of CE.
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