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Synchrotron XFM data of Pages_12382 (Oct 2017)

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DataCite Commons2024-03-30 更新2025-04-09 收录
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https://data.csiro.au/collection/csiro%3A61939v1
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The ~3.5 Ga old barite-chert-hosted stromatolites of the Dresser Formation, Pilbara Craton (Australia), are among the oldest known fossiliferous rocks on the Earth. At least some of the stromatolites are interpreted to have formed by chemoautotrophic archaea or bacteria that grew in proximity to, and locally within, shallow hydrothermal seafloor vents or surficial hot spring systems. We aim to employ synchrotron-XFM element mapping to unravel the chemical signature of the Dresser Formation stromatolites, specifically with respect to hydrothermally-sourced transition (e.g., Fe, Ni and Zn) and post-transition (e.g., As) metals that are known to be vital for microbial metabolism
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CSIRO
创建时间:
2024-03-30
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