{"id":192872,"date":"2024-07-12T19:44:32","date_gmt":"2024-07-13T00:44:32","guid":{"rendered":"https:\/\/lifeboat.com\/blog\/2024\/07\/the-nature-of-the-last-universal-common-ancestor-and-its-impact-on-the-early-earth-system"},"modified":"2024-07-12T19:44:32","modified_gmt":"2024-07-13T00:44:32","slug":"the-nature-of-the-last-universal-common-ancestor-and-its-impact-on-the-early-earth-system","status":"publish","type":"post","link":"https:\/\/lifeboat.com\/blog\/2024\/07\/the-nature-of-the-last-universal-common-ancestor-and-its-impact-on-the-early-earth-system","title":{"rendered":"The nature of the last universal common ancestor and its impact on the early Earth system"},"content":{"rendered":"<p style=\"padding-right: 20px\"><a class=\"aligncenter blog-photo\" href=\"https:\/\/lifeboat.com\/blog.images\/the-nature-of-the-last-universal-common-ancestor-and-its-impact-on-the-early-earth-system2.jpg\"><\/a><\/p>\n<p>Life\u2019s evolutionary timescale is typically calibrated to the oldest fossil occurrences. However, the veracity of fossil discoveries from the early Archaean period has been contested<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 11\" title=\"Javaux, E. J. Challenges in evidencing the earliest traces of life. Nature 572451&ndash;460 (2019).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR11\" id=\"ref-link-section-d40170551e898\">11<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 12\" title=\"Lepot, K. Signatures of early microbial life from the Archean (4 to 2.5 Ga) eon. Earth Sci. Rev. 209, 103296 (2020).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR12\" id=\"ref-link-section-d40170551e901\">12<\/a><\/sup>. Relaxed Bayesian node-calibrated molecular clock approaches provide a means of integrating the sparse fossil and geochemical record of early life with the information provided by molecular data; however, constraining LUCA\u2019s age is challenging due to limited prokaryote fossil calibrations and the uncertainty in their placement on the phylogeny. Molecular clock estimates of LUCA<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" title=\"Betts, H. C. et al. Integrated genomic and fossil evidence illuminates life\u2019s early evolution and eukaryote origin. Nat. Ecol. Evol. 2, 1556&ndash;1562 (2018).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR13\" id=\"ref-link-section-d40170551e905\">13<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" title=\"Zhu, Q. et al. Phylogenomics of 10,575 genomes reveals evolutionary proximity between domains Bacteria and Archaea. Nat. Commun. 10, 5477 (2019).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR14\" id=\"ref-link-section-d40170551e905_1\">14<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 15\" title=\"Moody, E. R. R. et al. An estimate of the deepest branches of the tree of life from ancient vertically evolving genes. eLife 11, e66695 (2022).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR15\" id=\"ref-link-section-d40170551e908\">15<\/a><\/sup> have relied on conserved universal single-copy marker genes within phylogenies for which LUCA represented the root. Dating the root of a tree is difficult because errors propagate from the tips to the root of the dated phylogeny and information is not available to estimate the rate of evolution for the branch incident on the root node. Therefore, we analysed genes that duplicated before LUCA with two (or more) copies in LUCA\u2019s genome<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 16\" title=\"Schwartz, R. M. & Dayhoff, M. O. Origins of prokaryotes, eukaryotes, mitochondria, and chloroplasts. Science 199395&ndash;403 (1978).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR16\" id=\"ref-link-section-d40170551e912\">16<\/a><\/sup>. The root in these gene trees represents this duplication preceding LUCA, whereas LUCA is represented by two descendant nodes. Use of these universal paralogues also has the advantage that the same calibrations can be applied at least twice. After duplication, the same species divergences are represented on both sides of the gene tree<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 17\" title=\"Shih, P. M. & Matzke, N. J. Primary endosymbiosis events date to the later Proterozoic 994 with cross-calibrated phylogenetic dating of duplicated ATPase proteins. Proc. Natl Acad. Sci. USA 110,996 (2013).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR17\" id=\"ref-link-section-d40170551e916\">17<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 18\" title=\"Mahendrarajah, T. A. et al. ATP synthase evolution on a cross-braced dated tree of life. Nat. Commun. 14, 7456 (2023).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR18\" id=\"ref-link-section-d40170551e919\">18<\/a><\/sup> and thus can be assumed to have the same age. This considerably reduces the uncertainty when genetic distance (branch length) is resolved into absolute time and rate. When a shared node is assigned a fossil calibration, such cross-bracing also serves to double the number of calibrations on the phylogeny, improving divergence time estimates. We calibrated our molecular clock analyses using 13 calibrations (see \u2018Fossil calibrations\u2019 in <a data-track=\"click\" data-track-label=\"link\" data-track-action=\"supplementary material anchor\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#MOESM1\">Supplementary Information<\/a>). The calibration on the root of the tree of life is of particular importance. Some previous studies have placed a younger maximum constraint on the age of LUCA based on the assumption that life could not have survived Late Heavy Bombardment (LHB) (~3.7\u20133.9 billion years ago (Ga))<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 19\" title=\"Bottke, W. F. & Norman, M. D. The Late Heavy Bombardment. Annu. Rev. Earth Planet. Sci. 45619&ndash;647 (2017).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR19\" id=\"ref-link-section-d40170551e927\">19<\/a><\/sup>. However, the LHB hypothesis is extrapolated and scaled from the Moon\u2019s impact record, the interpretation of which has been questioned in terms of the intensity, duration and even the veracity of an LHB episode<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" title=\"Reimink, J. et al. Quantifying the effect of late bombardment on terrestrial zircons. Earth Planet. Sci. Lett. 604, 118007 (2023).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR20\" id=\"ref-link-section-d40170551e931\">20<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" title=\"Boehnke, P. & Harrison, T. M. Illusory Late Heavy Bombardments. Proc. Natl Acad. Sci. USA 113, 10802&ndash;10806 (2016).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR21\" id=\"ref-link-section-d40170551e931_1\">21<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" title=\"Ryder, G. Mass flux in the ancient Earth&ndash;Moon system and benign implications for the origin of life on Earth. J. Geophys. Res. 107, 6-1&ndash;6-13 (2002).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR22\" id=\"ref-link-section-d40170551e931_2\">22<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 23\" title=\"Hartmann, W. K. History of the terminal cataclysm paradigm: epistemology of a planetary bombardment that never (?) happened. Geosciences 9,285 (2019).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR23\" id=\"ref-link-section-d40170551e934\">23<\/a><\/sup>. Thus, the LHB hypothesis should not be considered a credible maximum constraint on the age of LUCA. We used soft-uniform bounds, with the maximum-age bound based on the time of the Moon-forming impact (4,510 million years ago (Ma) \u00b1 10 Myr), which would have effectively sterilized Earth\u2019s precursors, Tellus and Theia<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 13\" title=\"Betts, H. C. et al. Integrated genomic and fossil evidence illuminates life\u2019s early evolution and eukaryote origin. Nat. Ecol. Evol. 2, 1556&ndash;1562 (2018).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR13\" id=\"ref-link-section-d40170551e938\">13<\/a><\/sup>. Our minimum bound on the age of LUCA is based on low \u03b4<sup>98 <\/sup>Mo isotope values indicative of Mn oxidation compatible with oxygenic photosynthesis and, therefore, total-group Oxyphotobacteria in the Mozaan Group, Pongola Supergroup, South Africa<sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 24\" title=\"Planavsky, N. J. et al. Evidence for oxygenic photosynthesis half a billion years before the great oxidation event. Nat. Geosci. 7283&ndash;286 (2014).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR24\" id=\"ref-link-section-d40170551e944\">24<\/a>,<a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 25\" title=\"Ossa, F. O. et al. Limited oxygen production in the Mesoarchean ocean. Proc. Natl Acad. Sci. USA 116, 6647&ndash;6652 (2019).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR25\" id=\"ref-link-section-d40170551e947\">25<\/a><\/sup>, dated minimally to 2,954 Ma \u00b1 9 Myr (ref. <sup><a data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 26\" title=\"Mukasa, S. B., Wilson, A. H. & Young, K. R. Geochronological constraints on the magmatic and tectonic development of the Pongola Supergroup (Central Region), South Africa. Precambrian Res. 224268&ndash;286 (2013).\" href=\"https:\/\/www.nature.com\/articles\/s41559-024-02461-1#ref-CR26\" id=\"ref-link-section-d40170551e951\">26<\/a><\/sup>).<\/p>\n<p>Our estimates for the age of LUCA are inferred with a concatenated and a partitioned dataset, both consisting of five pre-LUCA paralogues: catalytic and non-catalytic subunits from ATP synthases, elongation factor Tu and G, signal recognition protein and signal recognition particle receptor, tyrosyl-tRNA and tryptophanyl-tRNA synthetases, and leucyl-and valyl-tRNA synthetases<sup>27<\/sup>. Marginal densities (commonly referred to as effective priors) fall within calibration densities (that is, user-specified priors) when topologically adjacent calibrations do not overlap temporally, but may differ when they overlap, to ensure the relative age relationships between ancestor-descendant nodes. We consider the marginal densities a reasonable interpretation of the calibration evidence given the phylogeny; we are not attempting to test the hypothesis that the fossil record is an accurate temporal archive of evolutionary history because it is not<sup>28<\/sup>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Life\u2019s evolutionary timescale is typically calibrated to the oldest fossil occurrences. However, the veracity of fossil discoveries from the early Archaean period has been contested11,12. Relaxed Bayesian node-calibrated molecular clock approaches provide a means of integrating the sparse fossil and geochemical record of early life with the information provided by molecular data; however, constraining LUCA\u2019s [\u2026]<\/p>\n","protected":false},"author":661,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[19,385,412,48,8],"tags":[],"class_list":["post-192872","post","type-post","status-publish","format-standard","hentry","category-chemistry","category-evolution","category-genetics","category-particle-physics","category-space"],"_links":{"self":[{"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/posts\/192872","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/users\/661"}],"replies":[{"embeddable":true,"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/comments?post=192872"}],"version-history":[{"count":0,"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/posts\/192872\/revisions"}],"wp:attachment":[{"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/media?parent=192872"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/categories?post=192872"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/lifeboat.com\/blog\/wp-json\/wp\/v2\/tags?post=192872"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}