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  • 1
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 1999-08-14
    Description: Molecular fossils of biological lipids are preserved in 2700-million-year-old shales from the Pilbara Craton, Australia. Sequential extraction of adjacent samples shows that these hydrocarbon biomarkers are indigenous and syngenetic to the Archean shales, greatly extending the known geological range of such molecules. The presence of abundant 2alpha-methylhopanes, which are characteristic of cyanobacteria, indicates that oxygenic photosynthesis evolved well before the atmosphere became oxidizing. The presence of steranes, particularly cholestane and its 28- to 30-carbon analogs, provides persuasive evidence for the existence of eukaryotes 500 million to 1 billion years before the extant fossil record indicates that the lineage arose.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Brocks, J J -- Logan, G A -- Buick, R -- Summons, R E -- New York, N.Y. -- Science. 1999 Aug 13;285(5430):1033-6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Geosciences, University of Sydney, Sydney, NSW 2006, Australia. jochen.brocks@agso.gov.au〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/10446042" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; Australia ; *Biological Evolution ; Biomarkers/analysis ; Cholestanes/analysis ; Cyanobacteria/physiology ; Eukaryotic Cells/*physiology ; Fossils ; Geologic Sediments/*chemistry ; Hydrocarbons/*analysis ; Lipids/*analysis ; Paleontology ; Photosynthesis ; Steroids/*analysis ; Triterpenes/*analysis
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 1992-01-03
    Description: The Tumbiana Formation, about 2700 million years old, was largely deposited in ephemeral saline lakes, as judged by the unusual evaporite paragenesis of carbonate and halite with no sulfate. Stromatolites of diverse morphology occur in the lacustrine sediments, some with palimpsest fabrics after erect filaments. These stromatolites were probably accreted by phototropic microbes that, from their habitat in shallow isolated basins with negligible sulfate concentrations, almost certainly metabolized by ozygenic photosynthesis.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Buick, R -- New York, N.Y. -- Science. 1992 Jan 3;255(5040):74-7.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Botanical Museum, Harvard University, Cambridge, MA 02138, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11536492" target="_blank"〉PubMed〈/a〉
    Keywords: Archaea ; Australia ; Bacteria ; *Biological Evolution ; Carbonates/analysis/chemistry/metabolism ; Earth (Planet) ; *Environmental Microbiology ; *Evolution, Planetary ; *Fossils ; Fresh Water ; Geologic Sediments/*analysis/microbiology ; Oxidation-Reduction ; Paleontology ; Photosynthesis/*physiology ; Sodium Chloride/analysis ; Sulfates/analysis
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2015-02-18
    Description: Nitrogen is an essential nutrient for all organisms that must have been available since the origin of life. Abiotic processes including hydrothermal reduction, photochemical reactions, or lightning discharge could have converted atmospheric N2 into assimilable NH4(+), HCN, or NOx species, collectively termed fixed nitrogen. But these sources may have been small on the early Earth, severely limiting the size of the primordial biosphere. The evolution of the nitrogen-fixing enzyme nitrogenase, which reduces atmospheric N2 to organic NH4(+), thus represented a major breakthrough in the radiation of life, but its timing is uncertain. Here we present nitrogen isotope ratios with a mean of 0.0 +/- 1.2 per thousand from marine and fluvial sedimentary rocks of prehnite-pumpellyite to greenschist metamorphic grade between 3.2 and 2.75 billion years ago. These data cannot readily be explained by abiotic processes and therefore suggest biological nitrogen fixation, most probably using molybdenum-based nitrogenase as opposed to other variants that impart significant negative fractionations. Our data place a minimum age constraint of 3.2 billion years on the origin of biological nitrogen fixation and suggest that molybdenum was bioavailable in the mid-Archaean ocean long before the Great Oxidation Event.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Stueken, Eva E -- Buick, Roger -- Guy, Bradley M -- Koehler, Matthew C -- England -- Nature. 2015 Apr 30;520(7549):666-9. doi: 10.1038/nature14180. Epub 2015 Feb 16.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth &Space Sciences and Astrobiology Program, University of Washington, Seattle, Washington 98195-1310, USA. ; Department of Geology, University of Johannesburg, Auckland Park 2006, South Africa.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25686600" target="_blank"〉PubMed〈/a〉
    Keywords: *Biological Evolution ; Evolution, Molecular ; Geologic Sediments/chemistry ; History, Ancient ; Molybdenum/*metabolism ; *Nitrogen Fixation ; Nitrogen Isotopes/*analysis ; Nitrogenase/*metabolism ; Oceans and Seas ; Oxidation-Reduction ; Time Factors
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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