A record of Neogene seawater <i>δ</i><sup>11</sup>B reconstructed from paired <i>δ</i><sup>11</sup>B analyses on benthic and planktic foraminifera
The boron isotope composition (<i>δ</i><sup>11</sup>B) of foraminiferal calcite reflects the pH and the boron isotope composition of the seawater the foraminifer grew in. For pH reconstructions, the <i>δ</i><sup>11</sup>B of seawater must therefore be...
| Main Authors: | , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2017-02-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/13/149/2017/cp-13-149-2017.pdf |