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- W3007124927 abstract "The timing of emergence of major organismal groups is consistent with the climatic temperature being equal to their upper temperature limit of growth ( T max ), implying a temperature constraint on the evolution of each group, with the climatic temperature inferred from the oxygen isotope record of marine cherts. Support for this constraint comes from the correlation of T max with the rRNA molecular phylogenetic distance from the last common ancestor (LCA) for both thermophilic Archaea and Bacteria. In particular, this correlation for hyperthermophilic Archaea suggests a climatic temperature of about 120°C at the time of the LCA, likely in the Hadean." @default.
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- W3007124927 date "2004-01-01" @default.
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- W3007124927 title "Precambrian Surface Temperatures and Molecular Phylogeny" @default.
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- W3007124927 doi "https://doi.org/10.1017/s0074180900193532" @default.
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