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 language | English |
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Pages (from-to) | 377-378 |
Number of pages | 2 |
Journal | Nature Geoscience |
Volume | 17 |
Issue number | 5 |
Early online date | 11 Apr 2024 |
DOIs | |
Publication status | Published - 1 May 2024 |
Bibliographical note
Publisher Copyright:© Springer Nature Limited 2024.