Articles | Volume 17, issue 13
https://doi.org/10.5194/bg-17-3487-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-3487-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Jul 2020
Research article |
| 08 Jul 2020
| 08 Jul 2020
Seawater pH reconstruction using boron isotopes in multiple planktonic foraminifera species with different depth habitats and their potential to constrain pH and pCO2 gradients
Maxence Guillermic
CORRESPONDING AUTHOR
Department of Earth, Planetary, and Space Sciences, Department of
Atmospheric and Oceanic Sciences, Institute of the Environment and
Sustainability, UCLA, University of California – Los Angeles, Los Angeles,
CA 90095, USA
Laboratoire Géosciences Océan UMR6538, UBO, Institut
Universitaire Européen de la Mer, Rue Dumont d'Urville, 29280
Plouzané, France
Sambuddha Misra
Indian Institute of Science, Centre for Earth Sciences, Bengaluru,
Karnataka 560012, India
The Godwin Laboratory for Palaeoclimate Research, Department of
Earth Sciences, University of Cambridge, Cambridge, UK
Robert Eagle
Department of Earth, Planetary, and Space Sciences, Department of
Atmospheric and Oceanic Sciences, Institute of the Environment and
Sustainability, UCLA, University of California – Los Angeles, Los Angeles,
CA 90095, USA
Laboratoire Géosciences Océan UMR6538, UBO, Institut
Universitaire Européen de la Mer, Rue Dumont d'Urville, 29280
Plouzané, France
Alexandra Villa
Department of Earth, Planetary, and Space Sciences, Department of
Atmospheric and Oceanic Sciences, Institute of the Environment and
Sustainability, UCLA, University of California – Los Angeles, Los Angeles,
CA 90095, USA
Department of Geoscience, University of Wisconsin, Madison, WI
53706, USA
Fengming Chang
Key Laboratory of Marine Geology and Environment, Institute of
Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
Aradhna Tripati
CORRESPONDING AUTHOR
Department of Earth, Planetary, and Space Sciences, Department of
Atmospheric and Oceanic Sciences, Institute of the Environment and
Sustainability, UCLA, University of California – Los Angeles, Los Angeles,
CA 90095, USA
Laboratoire Géosciences Océan UMR6538, UBO, Institut
Universitaire Européen de la Mer, Rue Dumont d'Urville, 29280
Plouzané, France
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Cited
11 citations as recorded by crossref.
- Sea surface acidification events in the Andaman Sea associated with the last Toba volcanic activity A. Alves et al. 10.1016/j.gloplacha.2024.104460
- Recent advancements in marine micropaleontological and paleoceanographic research from India A. Singh & P. Naidu 10.1007/s43538-024-00307-9
- Non-traditional stable metal and metalloid isotopes and their potential applications in earth, ocean, and environmental sciences W. Rahaman 10.1016/j.geogeo.2024.100307
- Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
- Patterns of Element Incorporation in Calcium Carbonate Biominerals Recapitulate Phylogeny for a Diverse Range of Marine Calcifiers R. Ulrich et al. 10.3389/feart.2021.641760
- IN SITU STABLE ISOTOPE MEASUREMENTS IN FORAMINIFERAL TESTS BY SIMS R. Kozdon 10.61551/gsjfr.54.4.332
- Fossil Corals With Various Degrees of Preservation Can Retain Information About Biomineralization-Related Organic Material J. Drake et al. 10.3389/feart.2021.643864
- Atmospheric CO<sub>2</sub> estimates for the Miocene to Pleistocene based on foraminiferal <i>δ</i><sup>11</sup>B at Ocean Drilling Program Sites 806 and 807 in the Western Equatorial Pacific M. Guillermic et al. 10.5194/cp-18-183-2022
- Thermal stress reduces pocilloporid coral resilience to ocean acidification by impairing control over calcifying fluid chemistry M. Guillermic et al. 10.1126/sciadv.aba9958
- Physicochemical Control of Caribbean Coral Calcification Linked to Host and Symbiont Responses to Varying pCO2 and Temperature R. Eagle et al. 10.3390/jmse10081075
- Pliocene decoupling of equatorial Pacific temperature and pH gradients M. Shankle et al. 10.1038/s41586-021-03884-7
11 citations as recorded by crossref.
- Sea surface acidification events in the Andaman Sea associated with the last Toba volcanic activity A. Alves et al. 10.1016/j.gloplacha.2024.104460
- Recent advancements in marine micropaleontological and paleoceanographic research from India A. Singh & P. Naidu 10.1007/s43538-024-00307-9
- Non-traditional stable metal and metalloid isotopes and their potential applications in earth, ocean, and environmental sciences W. Rahaman 10.1016/j.geogeo.2024.100307
- Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
- Patterns of Element Incorporation in Calcium Carbonate Biominerals Recapitulate Phylogeny for a Diverse Range of Marine Calcifiers R. Ulrich et al. 10.3389/feart.2021.641760
- IN SITU STABLE ISOTOPE MEASUREMENTS IN FORAMINIFERAL TESTS BY SIMS R. Kozdon 10.61551/gsjfr.54.4.332
- Fossil Corals With Various Degrees of Preservation Can Retain Information About Biomineralization-Related Organic Material J. Drake et al. 10.3389/feart.2021.643864
- Atmospheric CO<sub>2</sub> estimates for the Miocene to Pleistocene based on foraminiferal <i>δ</i><sup>11</sup>B at Ocean Drilling Program Sites 806 and 807 in the Western Equatorial Pacific M. Guillermic et al. 10.5194/cp-18-183-2022
- Thermal stress reduces pocilloporid coral resilience to ocean acidification by impairing control over calcifying fluid chemistry M. Guillermic et al. 10.1126/sciadv.aba9958
- Physicochemical Control of Caribbean Coral Calcification Linked to Host and Symbiont Responses to Varying pCO2 and Temperature R. Eagle et al. 10.3390/jmse10081075
- Pliocene decoupling of equatorial Pacific temperature and pH gradients M. Shankle et al. 10.1038/s41586-021-03884-7
Latest update: 01 Nov 2024
Short summary
Boron isotope ratios (δ11B) of foraminifera are a promising proxy for seawater pH and can be used to constrain pCO2. In this study, we derived calibrations for new foraminiferal taxa which extend the application of the boron isotope proxy. We discuss the origin of different δ11B signatures in species and also discuss the potential of using multispecies δ11B analyses to constrain vertical pH and pCO2 gradients in ancient water columns to shed light on biogeochemical carbon cycling in the past.
Boron isotope ratios (δ11B) of foraminifera are a promising proxy for seawater pH and can be...
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