Biotic Enhancement of Weathering over the Past 3.7 Billion Years
Bibliographic Data
| ID | 23198117 |
|---|---|
| Authors | Gregory J Retallack (0000-0003-4356-9240, University of Oregon, corresponding author), Gregory Retallack |
| Year | 2022 |
| Volume | 32 |
| Issue | 12 |
| Pages | 4-9 |
| Publication date | 2022-12-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | GSA Today (JOURNAL) |
| Journal identifiers | ISSN: 1052-5173 |
| Publisher | Geological Society of America (PUBLISHER • US) |
| DOI | 10.1130/gsatg543a.1 |
| OpenAlex | W4285412637 |
| Language | EN |
| References cited | 1 |
Over the past four billion years, our sun became 30% brighter, yet Earth's water has neither completely frozen nor boiled off during that time. A theoretical solution to this paradox is a carbon dioxide greenhouse planetary thermostat regulated by evolutionary advances in biologically mediated silicate and apatite weathering. This carbon sequestration history can now be quantified using paleosols. Calculations of precipitation-normalized nutrient depletion rates (mol mm -1 a -1 ) in paleosols ranging in age back to 3.7 Ga show discrete order of magnitude increases in carbon consumption by silicate and apatite weathering due to evolutionary advances in life on land at around the Great Oxidation Event (2.45 Ga) and Neoproterozoic Oxidation Event (0.8 Ga). This biological weathering countered increased solar luminosity and continued emission of volcanic greenhouse gases.
Earth science · Geochemistry · Weathering · Geology · Historical and Archaeological Studies
| Highly cited | No |
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