ArticleNature communications2021
The kaolinite shuttle links the Great Oxidation and Lomagundi events.
Article in Nature communications, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
5 citing papers in PubMed.
- Silicate-bound iron drives abiotic solar energy conversion in terrestrial environments.Nature communications · 2026Article
- Evolutionary trajectory of microbial sulfur oxidation pathways recapitulates Earth's oxygenation history.Nature communications · 2026Article
- Phyllosilicate adsorption limited phosphorus bioavailability in early ferruginous oceans.Nature communications · 2026Article
- Volcanic forcing of the Lomagundi-Jatuli carbon isotope excursion.Proceedings of the National Academy of Sciences of the United States of America · 2025Article
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Authors and funding
11 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The ~2.22-2.06 Ga Lomagundi Event was the longest positive carbon isotope excursion in Earth's history and is commonly interpreted to reflect perturbations in continental weathering and the phosphorous cycle. Previous models have focused on mechanisms of increasing phosphorous solubilization during weathering without focusing on transport to the oceans and its dispersion in seawater. Building from new experimental results, here we report kaolinite readily absorbs phosphorous under acidic freshwater conditions, but quantitatively releases phosphorous under seawater conditions where it becomes bioavailable to phytoplankton. The strong likelihood of high weathering intensities and associated high kaolinite content in post-Great-Oxidation-Event paleosols suggests there would have been enhanced phosphorus shuttling from the continents into marine environments. A kaolinite phosphorous shuttle introduces the potential for nonlinearity in the fluxes of phosphorous to the oceans with increases in chemical weathering intensity.
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Registered trials
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