Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism

The 3.45-billion-year-old Strelley Pool Formation of Western Australia preserves stromatolites that are considered among the oldest evidence for life on Earth. In places of exceptional preservation, these stromatolites contain laminae rich in organic carbon, interpreted as the fossil remains of anci...

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Main Authors: Bontognali, Tomaso R. R., Sessions, Alex L., Allwood, Abigail C., Fischer, Woodward W., Grotzinger, John P., Eiler, John M., Summons, Roger E
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: National Academy of Sciences (U.S.) 2013
Online Access:http://hdl.handle.net/1721.1/76730
https://orcid.org/0000-0002-7144-8537
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author Bontognali, Tomaso R. R.
Sessions, Alex L.
Allwood, Abigail C.
Fischer, Woodward W.
Grotzinger, John P.
Eiler, John M.
Summons, Roger E
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Bontognali, Tomaso R. R.
Sessions, Alex L.
Allwood, Abigail C.
Fischer, Woodward W.
Grotzinger, John P.
Eiler, John M.
Summons, Roger E
author_sort Bontognali, Tomaso R. R.
collection MIT
description The 3.45-billion-year-old Strelley Pool Formation of Western Australia preserves stromatolites that are considered among the oldest evidence for life on Earth. In places of exceptional preservation, these stromatolites contain laminae rich in organic carbon, interpreted as the fossil remains of ancient microbial mats. To better understand the biogeochemistry of these rocks, we performed microscale in situ sulfur isotope measurements of the preserved organic sulfur, including both Δ[superscript 33]S and δ[superscript 34]S[subscript CDT]. This approach allows us to tie physiological inference from isotope ratios directly to fossil biomass, providing a means to understand sulfur metabolism that is complimentary to, and independent from, inorganic proxies (e.g., pyrite). Δ33S values of the kerogen reveal mass-anomalous fractionations expected of the Archean sulfur cycle, whereas δ[superscript 34]S[subscript CDT] values show large fractionations at very small spatial scales, including values below -15‰. We interpret these isotopic patterns as recording the process of sulfurization of organic matter by H[subscript 2]S in heterogeneous mat pore-waters influenced by respiratory S metabolism. Positive Δ[superscript 33]S anomalies suggest that disproportionation of elemental sulfur would have been a prominent microbial process in these communities.
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spelling mit-1721.1/767302024-05-15T03:14:28Z Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism Bontognali, Tomaso R. R. Sessions, Alex L. Allwood, Abigail C. Fischer, Woodward W. Grotzinger, John P. Eiler, John M. Summons, Roger E Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Summons, Roger Everett The 3.45-billion-year-old Strelley Pool Formation of Western Australia preserves stromatolites that are considered among the oldest evidence for life on Earth. In places of exceptional preservation, these stromatolites contain laminae rich in organic carbon, interpreted as the fossil remains of ancient microbial mats. To better understand the biogeochemistry of these rocks, we performed microscale in situ sulfur isotope measurements of the preserved organic sulfur, including both Δ[superscript 33]S and δ[superscript 34]S[subscript CDT]. This approach allows us to tie physiological inference from isotope ratios directly to fossil biomass, providing a means to understand sulfur metabolism that is complimentary to, and independent from, inorganic proxies (e.g., pyrite). Δ33S values of the kerogen reveal mass-anomalous fractionations expected of the Archean sulfur cycle, whereas δ[superscript 34]S[subscript CDT] values show large fractionations at very small spatial scales, including values below -15‰. We interpret these isotopic patterns as recording the process of sulfurization of organic matter by H[subscript 2]S in heterogeneous mat pore-waters influenced by respiratory S metabolism. Positive Δ[superscript 33]S anomalies suggest that disproportionation of elemental sulfur would have been a prominent microbial process in these communities. 2013-02-05T19:17:41Z 2013-02-05T19:17:41Z 2012-09 2012-05 Article http://purl.org/eprint/type/JournalArticle 0027-8424 1091-6490 http://hdl.handle.net/1721.1/76730 Bontognali, T. R. R. et al. “Sulfur Isotopes of Organic Matter Preserved in 3.45-billion-year-old Stromatolites Reveal Microbial Metabolism.” Proceedings of the National Academy of Sciences 109.38 (2012): 15146–15151. © 2013 National Academy of Sciences https://orcid.org/0000-0002-7144-8537 en_US http://dx.doi.org/10.1073/pnas.1207491109 Proceedings of the National Academy of Sciences of the United States of America Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf National Academy of Sciences (U.S.) PNAS
spellingShingle Bontognali, Tomaso R. R.
Sessions, Alex L.
Allwood, Abigail C.
Fischer, Woodward W.
Grotzinger, John P.
Eiler, John M.
Summons, Roger E
Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism
title Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism
title_full Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism
title_fullStr Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism
title_full_unstemmed Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism
title_short Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism
title_sort sulfur isotopes of organic matter preserved in 3 45 gyr old stromatolites reveal microbial metabolism
url http://hdl.handle.net/1721.1/76730
https://orcid.org/0000-0002-7144-8537
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