<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Chen G</submitter><funding>National Natural Science Foundation of China (National Science Foundation of China)</funding><pagination>5862</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9532422</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>13(1)</volume><pubmed_abstract>Reconstructing historical atmospheric oxygen (O&lt;sub>2&lt;/sub>) levels at finer temporal resolution is a top priority for exploring the evolution of life on Earth. This goal, however, is challenged by gaps in traditionally employed sediment-hosted geochemical proxy data. Here, we propose an independent strategy-machine learning with global mafic igneous geochemistry big data to explore atmospheric oxygenation over the last 4.0 billion years. We observe an overall two-step rise of atmospheric O&lt;sub>2&lt;/sub> similar to the published curves derived from independent sediment-hosted paleo-oxybarometers but with a more detailed fabric of O&lt;sub>2&lt;/sub> fluctuations superimposed. These additional, shorter-term fluctuations are also consistent with previous but less well-established suggestions of O&lt;su</pubmed_abstract><journal>Nature communications</journal><pubmed_title>Reconstructing Earth's atmospheric oxygenation history using machine learning.</pubmed_title><pmcid>PMC9532422</pmcid><funding_grant_id>42050103</funding_grant_id><pubmed_authors>Zhao M</pubmed_authors><pubmed_authors>Shen J</pubmed_authors><pubmed_authors>Lyons TW</pubmed_authors><pubmed_authors>Agterberg F</pubmed_authors><pubmed_authors>Cheng Q</pubmed_authors><pubmed_authors>Chen G</pubmed_authors><pubmed_authors>Huang N</pubmed_authors></additional><is_claimable>false</is_claimable><name>Reconstructing Earth's atmospheric oxygenation history using machine learning.</name><description>Reconstructing historical atmospheric oxygen (O&lt;sub>2&lt;/sub>) levels at finer temporal resolution is a top priority for exploring the evolution of life on Earth. This goal, however, is challenged by gaps in traditionally employed sediment-hosted geochemical proxy data. Here, we propose an independent strategy-machine learning with global mafic igneous geochemistry big data to explore atmospheric oxygenation over the last 4.0 billion years. We observe an overall two-step rise of atmospheric O&lt;sub>2&lt;/sub> similar to the published curves derived from independent sediment-hosted paleo-oxybarometers but with a more detailed fabric of O&lt;sub>2&lt;/sub> fluctuations superimposed. These additional, shorter-term fluctuations are also consistent with previous but less well-established suggestions of O&lt;su</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022 Oct</publication><modification>2025-04-04T09:24:24.404Z</modification><creation>2025-04-04T09:24:24.404Z</creation></dates><accession>S-EPMC9532422</accession><cross_references><pubmed>36195593</pubmed><doi>10.1038/s41467-022-33388-5</doi></cross_references></HashMap>