<i>δ</i><sup>11</sup>B as monitor of calcification site pH in divergent marine calcifying organisms
The boron isotope composition (<i>δ</i><sup>11</sup>B) of marine biogenic carbonates has been predominantly studied as a proxy for monitoring past changes in seawater pH and carbonate chemistry. However, a number of assumptions regarding chemical kinetics and thermodynamic isotope exchange reacti...
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| Autors principals: | , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Copernicus Publications
2018-03-01
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| Col·lecció: | Biogeosciences |
| Accés en línia: | https://www.biogeosciences.net/15/1447/2018/bg-15-1447-2018.pdf |
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