Evolution of Earth’s oxygenation and temperature depends on surface carbonate accumulation

Lewis Alcott, Benjamin J. W. Mills

Research output: Contribution to journalArticle (Academic Journal)peer-review

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Abstract

There are no good models for the chemical evolution of the Earth’s surface over the planet’s lifetime, because models typically overlook the progressive build-up of carbonate rocks in the crust. A new model that includes this accumulation enables the reconstruction of major oxygen and temperature trends throughout Earth’s history.
Original languageEnglish
Pages (from-to)377-378
Number of pages2
JournalNature Geoscience
Volume17
Issue number5
Early online date11 Apr 2024
DOIs
Publication statusPublished - 1 May 2024

Bibliographical note

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© Springer Nature Limited 2024.

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