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Nature 456, 942-945 (18 December 2008) | doi:10.1038/nature07393; Received 5 March 2008; Accepted 1 September 2008; Published online 26 November 2008

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Parallel adaptations to high temperatures in the Archaean eon

Bastien Boussau1,3, Samuel Blanquart2,3, Anamaria Necsulea1, Nicolas Lartillot2,4 & Manolo Gouy1

  1. Laboratoire de Biométrie et Biologie Evolutive, CNRS, Université de Lyon, Université Lyon I, 43 Boulevard du 11 Novembre, 69622 Villeurbanne, France
  2. LIRMM, CNRS, 161 rue Ada, 34392 Montpellier, France
  3. These authors contributed equally to this work.
  4. Present address: Département de Biochimie, Université de Montréal, C.P. 6128, succursale Centre-Ville, Montréal QC H3C3J7, Canada.

Correspondence to: Manolo Gouy1 Correspondence and requests for materials should be addressed to M.G. (Email: mgouy@biomserv.univ-lyon1.fr).

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Fossils of organisms dating from the origin and diversification of cellular life are scant and difficult to interpret1, for this reason alternative means to investigate the ecology of the last universal common ancestor (LUCA) and of the ancestors of the three domains of life are of great scientific value. It was recently recognized that the effects of temperature on ancestral organisms left 'genetic footprints' that could be uncovered in extant genomes2, 3, 4. Accordingly, analyses of resurrected proteins predicted that the bacterial ancestor was thermophilic and that Bacteria subsequently adapted to lower temperatures3, 4. As the archaeal ancestor is also thought to have been thermophilic5, the LUCA was parsimoniously inferred as thermophilic too. However, an analysis of ribosomal RNAs supported the hypothesis of a non-hyperthermophilic LUCA2. Here we show that both rRNA and protein sequences analysed with advanced, realistic models of molecular evolution6, 7 provide independent support for two environmental-temperature-related phases during the evolutionary history of the tree of life. In the first period, thermotolerance increased from a mesophilic LUCA to thermophilic ancestors of Bacteria and of Archaea–Eukaryota; in the second period, it decreased. Therefore, the two lineages descending from the LUCA and leading to the ancestors of Bacteria and Archaea–Eukaryota convergently adapted to high temperatures, possibly in response to a climate change of the early Earth1, 8, 9, and/or aided by the transition from an RNA genome in the LUCA to organisms with more thermostable DNA genomes10, 11. This analysis unifies apparently contradictory results2, 3, 4 into a coherent depiction of the evolution of an ecological trait over the entire tree of life.

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