Multiple prebiotic metals mediate translation.
basic_science · Level V
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- Record sourced from PubMed, PMID 30413624.
- Also identified by DOI 10.1073/pnas.1803636115 and PMC identifier 6275528.
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Abstract
Today, Mg<sup>2+</sup> is an essential cofactor with diverse structural and functional roles in life's oldest macromolecular machine, the translation system. We tested whether ancient Earth conditions (low O<sub>2</sub>, high Fe<sup>2+</sup>, and high Mn<sup>2+</sup>) can revert the ribosome to a functional ancestral state. First, SHAPE (selective 2'-hydroxyl acylation analyzed by primer extension) was used to compare the effect of Mg<sup>2+</sup>, Fe<sup>2+</sup>, and Mn<sup>2+</sup> on the tertiary structure of rRNA. Then, we used in vitro translation reactions to test whether Fe<sup>2+</sup> or Mn<sup>2+</sup> could mediate protein production, and quantified ribosomal metal content. We found that (<i>i</i>) Mg<sup>2+</sup>, Fe<sup>2+</sup>, and Mn<sup>2+</sup> had strikingly similar effects on rRNA folding; (<i>ii</i>) Fe<sup>2+</sup> and Mn<sup>2+</sup> can replace Mg<sup>2+</sup> as the dominant divalent cation during translation of mRNA to functional protein; and (<i>iii</i>) Fe and Mn associate extensively with the ribosome. Given that the translation system originated and matured when Fe<sup>2+</sup> and Mn<sup>2+</sup> were abundant, these findings suggest that Fe<sup>2+</sup> and Mn<sup>2+</sup> played a role in early ribosomal evolution.