Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy
Boron isotopes in planktonic foraminifera are a widely used proxy to determine ancient surface seawater pH, and by extension atmospheric CO 2 concentration and climate forcing on geological time scales. Yet, to reconstruct absolute values for pH and CO 2 , we require a δ 11 B foram-borate to pH cali...
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ftcopernicus:oai:publications.copernicus.org:cpd108385 2023-05-15T16:38:49+02:00 Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy Vega, Elwyn Chalk, Thomas B. Hain, Mathis P. Wilding, Megan R. Casey, Daniel Gledhill, Robin Luo, Chongguang Wilson, Paul A. Foster, Gavin L. 2023-01-05 application/pdf https://doi.org/10.5194/cp-2022-93 https://cp.copernicus.org/preprints/cp-2022-93/ eng eng doi:10.5194/cp-2022-93 https://cp.copernicus.org/preprints/cp-2022-93/ eISSN: 1814-9332 Text 2023 ftcopernicus https://doi.org/10.5194/cp-2022-93 2023-01-09T17:22:42Z Boron isotopes in planktonic foraminifera are a widely used proxy to determine ancient surface seawater pH, and by extension atmospheric CO 2 concentration and climate forcing on geological time scales. Yet, to reconstruct absolute values for pH and CO 2 , we require a δ 11 B foram-borate to pH calibration and independent determinations of ocean temperature, salinity, a second carbonate parameter, and the boron isotope composition of seawater. Although δ 11 B-derived records of atmospheric CO 2 have been shown to perform well against ice core-based CO 2 reconstructions, these tests have been performed at only a few locations and with limited temporal resolution. Here we present two highly resolved CO 2 records for the late Pleistocene from ODP Sites 999 and 871. Our δ 11 B-derived CO 2 record shows a very good agreement with the ice core CO 2 record with an average offset of 4.6 ± 49 (2σ) ppm, and a RMSE of 25 ppm, with minor short-lived overestimations of CO 2 (of up to ~50 ppm) occurring during some glacial onsets. We explore potential drivers of this disagreement and conclude that partial dissolution of foraminifera has a minimal effect on the CO 2 offset. We also observe that the general agreement between δ 11 B -derived and ice core CO 2 is improved by optimising the δ 11 B foram-borate calibration. Despite these minor issues a strong linear relationship between relative change in climate forcing from CO 2 (from ice core data) and pH change (from δ 11 B) exists over the late Pleistocene, confirming that pH change is a robust proxy of climate forcing over relatively short (<1 million year) intervals. Overall, these findings demonstrate that the boron isotope proxy is a reliable indicator of CO 2 beyond the reach of the ice cores and can help improve determinations of climate sensitivity for ancient time intervals. Text ice core Planktonic foraminifera Copernicus Publications: E-Journals |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Boron isotopes in planktonic foraminifera are a widely used proxy to determine ancient surface seawater pH, and by extension atmospheric CO 2 concentration and climate forcing on geological time scales. Yet, to reconstruct absolute values for pH and CO 2 , we require a δ 11 B foram-borate to pH calibration and independent determinations of ocean temperature, salinity, a second carbonate parameter, and the boron isotope composition of seawater. Although δ 11 B-derived records of atmospheric CO 2 have been shown to perform well against ice core-based CO 2 reconstructions, these tests have been performed at only a few locations and with limited temporal resolution. Here we present two highly resolved CO 2 records for the late Pleistocene from ODP Sites 999 and 871. Our δ 11 B-derived CO 2 record shows a very good agreement with the ice core CO 2 record with an average offset of 4.6 ± 49 (2σ) ppm, and a RMSE of 25 ppm, with minor short-lived overestimations of CO 2 (of up to ~50 ppm) occurring during some glacial onsets. We explore potential drivers of this disagreement and conclude that partial dissolution of foraminifera has a minimal effect on the CO 2 offset. We also observe that the general agreement between δ 11 B -derived and ice core CO 2 is improved by optimising the δ 11 B foram-borate calibration. Despite these minor issues a strong linear relationship between relative change in climate forcing from CO 2 (from ice core data) and pH change (from δ 11 B) exists over the late Pleistocene, confirming that pH change is a robust proxy of climate forcing over relatively short (<1 million year) intervals. Overall, these findings demonstrate that the boron isotope proxy is a reliable indicator of CO 2 beyond the reach of the ice cores and can help improve determinations of climate sensitivity for ancient time intervals. |
format |
Text |
author |
Vega, Elwyn Chalk, Thomas B. Hain, Mathis P. Wilding, Megan R. Casey, Daniel Gledhill, Robin Luo, Chongguang Wilson, Paul A. Foster, Gavin L. |
spellingShingle |
Vega, Elwyn Chalk, Thomas B. Hain, Mathis P. Wilding, Megan R. Casey, Daniel Gledhill, Robin Luo, Chongguang Wilson, Paul A. Foster, Gavin L. Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy |
author_facet |
Vega, Elwyn Chalk, Thomas B. Hain, Mathis P. Wilding, Megan R. Casey, Daniel Gledhill, Robin Luo, Chongguang Wilson, Paul A. Foster, Gavin L. |
author_sort |
Vega, Elwyn |
title |
Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy |
title_short |
Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy |
title_full |
Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy |
title_fullStr |
Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy |
title_full_unstemmed |
Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy |
title_sort |
orbital co2 reconstruction using boron isotopes during the late pleistocene, an assessment of accuracy |
publishDate |
2023 |
url |
https://doi.org/10.5194/cp-2022-93 https://cp.copernicus.org/preprints/cp-2022-93/ |
genre |
ice core Planktonic foraminifera |
genre_facet |
ice core Planktonic foraminifera |
op_source |
eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-2022-93 https://cp.copernicus.org/preprints/cp-2022-93/ |
op_doi |
https://doi.org/10.5194/cp-2022-93 |
_version_ |
1766029151766052864 |