Late Cenozoic Rise in Seawater δ11B Not Driven by Increasing Boron Adsorption
Abstract The boron isotopic value of ancient seawater (δ11Bsw) is a prerequisite for the reconstruction of seawater pH and atmospheric CO2 concentrations. Available models and some proxy records suggest that δ11Bsw underwent a large increase during the last 45 million years. This increase has been a...
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| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2025-05-01
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| Series: | Geochemistry, Geophysics, Geosystems |
| Online Access: | https://doi.org/10.1029/2024GC011911 |
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