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大型陨石撞击对早期进化——生命三域出现的影响。

The effects of heavy meteorite bombardment on the early evolution--the emergence of the three domains of life.

作者信息

Gogarten-Boekels M, Hilario E, Gogarten J P

机构信息

Dept. Molecular and Cell Biology, University of Connecticut, Storrs 06269-3044.

出版信息

Orig Life Evol Biosph. 1995 Jun;25(1-3):251-64. doi: 10.1007/BF01581588.

Abstract

A characteristic of many molecular phylogenies is that the three domains of life (Bacteria, Archaea, Eucarya) are clearly separated from each other. The analyses of ancient duplicated genes suggest that the last common ancestor of all presently known life forms already had been a sophisticated cellular prokaryote. These findings are in conflict with theories that have been proposed to explain the absence of deep branching lineages. In this paper we propose an alternative scenario, namely, a large meteorite impact that wiped out almost all life forms present on the early Earth. Following this nearly complete frustation of life on Earth, two surviving extreme thermophilic species gave rise to the now existing major groups of living organisms, the Bacteria and Archaea. [The latter also contributed the major portion to the nucleo-cytoplasmic component of the Eucarya]. An exact calibration of the molecular record with regard to time is not yet possible. The emergence of Eucarya in fossil and molecular records suggests that the proposed late impact should have occurred before 2100 million years before present (BP). If the 3500 million year old microfossils [Schopf, J. W. 1993: Science 260: 640-646] are interpreted as representatives of present day existing groups of bacteria (i.e., as cyanobacteria), then the impact is dated to around 3700 million years BP. The analysis of molecular sequences suggests that the separation between the Eucarya and the two prokaryotic domains is less deep then the separation between Bacteria and Archaea. The fundamental cell biological differences between Archaea and Eucarya were obtained over a comparatively short evolutionary distance (as measured in number of substitution events in biological macromolecules). Our interpretation of the molecular record suggests that life emerged early in Earth's history even before the time of the heavy bombardment was over. Early life forms already had colonized extreme habitats which allowed at least two prokaryotic species to survive a late nearly ocean boiling impact. The distribution of ecotypes on the rooted universal tree of life should not be interpreted as evidence that life originated in extremely hot environments.

摘要

许多分子系统发育的一个特点是生命的三个域(细菌、古菌、真核生物)彼此明显分离。对古老重复基因的分析表明,所有目前已知生命形式的最后一个共同祖先已经是一种复杂的细胞原核生物。这些发现与为解释缺乏深度分支谱系而提出的理论相冲突。在本文中,我们提出了另一种设想,即一次大型陨石撞击消灭了早期地球上几乎所有的生命形式。在地球上生命几乎完全灭绝之后,两个幸存的极端嗜热物种产生了现在现存的主要生物群体,即细菌和古菌。[后者也为真核生物的核质成分贡献了主要部分]。目前还无法对分子记录进行精确的时间校准。化石和分子记录中真核生物的出现表明,所提出的晚期撞击应该发生在距今21亿年前(BP)之前。如果将有35亿年历史的微化石[肖普夫,J. W. 1993:《科学》260:640 - 646]解释为当今现存细菌群体的代表(即蓝细菌),那么撞击的时间可追溯到距今约37亿年前。分子序列分析表明,真核生物与两个原核域之间的分离不如细菌和古菌之间的分离那么深。古菌和真核生物之间基本的细胞生物学差异是在相对较短的进化距离内产生的(以生物大分子中替代事件的数量来衡量)。我们对分子记录的解释表明,生命在地球历史早期就已出现,甚至在重轰炸期结束之前。早期生命形式已经在极端栖息地定殖,这使得至少两个原核生物物种能够在晚期几乎使海洋沸腾的撞击中幸存下来。在有根的生命通用树上生态型的分布不应被解释为生命起源于极端炎热环境的证据。

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