δ11B as monitor of calcification site pH in divergent marine calcifying organisms
WOS:000426917500003 International audience The boron isotope composition (delta B-11) 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 thermodyn...
Published in: | Biogeosciences |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2018
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Online Access: | https://hal.science/hal-02651007 https://hal.science/hal-02651007/document https://hal.science/hal-02651007/file/Sutton_etal_calcification_Biogeosciences_2018.pdf https://doi.org/10.5194/bg-15-1447-2018 |
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Portail HAL-ANR (Agence Nationale de la Recherche) |
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English |
topic |
ACL great-barrier-reef planktonic-foraminifera b-11 mas nmr boron isotopic composition carbon-dioxide concentrations co2-induced ocean acidification mc-icp-ms paleo-ph seawater ph tissue-skeleton interface [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
spellingShingle |
ACL great-barrier-reef planktonic-foraminifera b-11 mas nmr boron isotopic composition carbon-dioxide concentrations co2-induced ocean acidification mc-icp-ms paleo-ph seawater ph tissue-skeleton interface [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Sutton, Jill Liu, Yi-Wei Ries, Justin B. Guillermic, Maxence Ponzevera, Emmanuel Eagle, Robert A. δ11B as monitor of calcification site pH in divergent marine calcifying organisms |
topic_facet |
ACL great-barrier-reef planktonic-foraminifera b-11 mas nmr boron isotopic composition carbon-dioxide concentrations co2-induced ocean acidification mc-icp-ms paleo-ph seawater ph tissue-skeleton interface [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
WOS:000426917500003 International audience The boron isotope composition (delta B-11) 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 reactions are required to derive seawater pH from delta B-11 biogenic carbonates. It is also probable that delta B-11 of biogenic carbonate reflects seawater pH at the organism's site of calcification, which may or may not reflect seawater pH. Here, we report the development of methodology for measuring the delta B-11 of biogenic carbonate samples at the multicollector inductively coupled mass spectrometry facility at Ifremer (Plouzane, France) and the evaluation of delta(BCaCO3)-B-11 in a diverse range of marine calcifying organisms reared for 60 days in isothermal seawater (25 degrees C) equilibrated with an atmospheric pCO(2) of ca. 409 mu atm. Average delta(BCaCO3)-B-11 composition for all species evaluated in this study range from 16.27 to 35.09 %, including, in decreasing order, coralline red alga Neogoniolithion sp. (35.89 +/- 3.71 %), temperate coral Oculina arbuscula (24.12 +/- 0.19 %), serpulid worm Hydroides crucigera (19.26 +/- 0.16 %), tropical urchin Eucidaris tribuloides (18.71 +/- 0.26 %), temperate urchin Arbacia punctulata (16.28 +/- 0.86 %), and temperate oyster Crassostrea virginica (16.03 %). These results are discussed in the context of each species' proposed mechanism of biocalcification and other factors that could influence skeletal and shell delta B-11, including calcifying site pH, the proposed direct incorporation of isotopically enriched boric acid (instead of borate) into biogenic calcium carbonate, and differences in shell/skeleton polymorph mineralogy. We conclude that the large inter-species variability in delta(BCaCO3)-B-11 (ca. 20%) and significant discrepancies between measured delta(BCaCO3)-B-11 and delta(BCaCO3)-B-11 expected from established ... |
author2 |
Laboratoire des Sciences de l'Environnement Marin (LEMAR) (LEMAR) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire Géosciences Océan (LGO) Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) Northeastern University Boston Géosciences Marines (GM) Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) University of California Los Angeles (UCLA) University of California (UC) Department of Atmospheric and Oceanic Sciences Los Angeles (AOS) University of California (UC)-University of California (UC) ANR-10-LABX-0019,LabexMER,LabexMER Marine Excellence Research: a changing ocean(2010) |
format |
Article in Journal/Newspaper |
author |
Sutton, Jill Liu, Yi-Wei Ries, Justin B. Guillermic, Maxence Ponzevera, Emmanuel Eagle, Robert A. |
author_facet |
Sutton, Jill Liu, Yi-Wei Ries, Justin B. Guillermic, Maxence Ponzevera, Emmanuel Eagle, Robert A. |
author_sort |
Sutton, Jill |
title |
δ11B as monitor of calcification site pH in divergent marine calcifying organisms |
title_short |
δ11B as monitor of calcification site pH in divergent marine calcifying organisms |
title_full |
δ11B as monitor of calcification site pH in divergent marine calcifying organisms |
title_fullStr |
δ11B as monitor of calcification site pH in divergent marine calcifying organisms |
title_full_unstemmed |
δ11B as monitor of calcification site pH in divergent marine calcifying organisms |
title_sort |
δ11b as monitor of calcification site ph in divergent marine calcifying organisms |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://hal.science/hal-02651007 https://hal.science/hal-02651007/document https://hal.science/hal-02651007/file/Sutton_etal_calcification_Biogeosciences_2018.pdf https://doi.org/10.5194/bg-15-1447-2018 |
genre |
Ocean acidification Planktonic foraminifera |
genre_facet |
Ocean acidification Planktonic foraminifera |
op_source |
ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-02651007 Biogeosciences, 2018, 15 (5), pp.1447-1467. ⟨10.5194/bg-15-1447-2018⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-15-1447-2018 hal-02651007 https://hal.science/hal-02651007 https://hal.science/hal-02651007/document https://hal.science/hal-02651007/file/Sutton_etal_calcification_Biogeosciences_2018.pdf doi:10.5194/bg-15-1447-2018 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/bg-15-1447-2018 |
container_title |
Biogeosciences |
container_volume |
15 |
container_issue |
5 |
container_start_page |
1447 |
op_container_end_page |
1467 |
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1785572199674937344 |
spelling |
ftanrparis:oai:HAL:hal-02651007v1 2023-12-17T10:48:07+01:00 δ11B as monitor of calcification site pH in divergent marine calcifying organisms Sutton, Jill Liu, Yi-Wei Ries, Justin B. Guillermic, Maxence Ponzevera, Emmanuel Eagle, Robert A. Laboratoire des Sciences de l'Environnement Marin (LEMAR) (LEMAR) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire Géosciences Océan (LGO) Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) Northeastern University Boston Géosciences Marines (GM) Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) University of California Los Angeles (UCLA) University of California (UC) Department of Atmospheric and Oceanic Sciences Los Angeles (AOS) University of California (UC)-University of California (UC) ANR-10-LABX-0019,LabexMER,LabexMER Marine Excellence Research: a changing ocean(2010) 2018 https://hal.science/hal-02651007 https://hal.science/hal-02651007/document https://hal.science/hal-02651007/file/Sutton_etal_calcification_Biogeosciences_2018.pdf https://doi.org/10.5194/bg-15-1447-2018 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-15-1447-2018 hal-02651007 https://hal.science/hal-02651007 https://hal.science/hal-02651007/document https://hal.science/hal-02651007/file/Sutton_etal_calcification_Biogeosciences_2018.pdf doi:10.5194/bg-15-1447-2018 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-02651007 Biogeosciences, 2018, 15 (5), pp.1447-1467. ⟨10.5194/bg-15-1447-2018⟩ ACL great-barrier-reef planktonic-foraminifera b-11 mas nmr boron isotopic composition carbon-dioxide concentrations co2-induced ocean acidification mc-icp-ms paleo-ph seawater ph tissue-skeleton interface [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2018 ftanrparis https://doi.org/10.5194/bg-15-1447-2018 2023-11-18T22:35:07Z WOS:000426917500003 International audience The boron isotope composition (delta B-11) 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 reactions are required to derive seawater pH from delta B-11 biogenic carbonates. It is also probable that delta B-11 of biogenic carbonate reflects seawater pH at the organism's site of calcification, which may or may not reflect seawater pH. Here, we report the development of methodology for measuring the delta B-11 of biogenic carbonate samples at the multicollector inductively coupled mass spectrometry facility at Ifremer (Plouzane, France) and the evaluation of delta(BCaCO3)-B-11 in a diverse range of marine calcifying organisms reared for 60 days in isothermal seawater (25 degrees C) equilibrated with an atmospheric pCO(2) of ca. 409 mu atm. Average delta(BCaCO3)-B-11 composition for all species evaluated in this study range from 16.27 to 35.09 %, including, in decreasing order, coralline red alga Neogoniolithion sp. (35.89 +/- 3.71 %), temperate coral Oculina arbuscula (24.12 +/- 0.19 %), serpulid worm Hydroides crucigera (19.26 +/- 0.16 %), tropical urchin Eucidaris tribuloides (18.71 +/- 0.26 %), temperate urchin Arbacia punctulata (16.28 +/- 0.86 %), and temperate oyster Crassostrea virginica (16.03 %). These results are discussed in the context of each species' proposed mechanism of biocalcification and other factors that could influence skeletal and shell delta B-11, including calcifying site pH, the proposed direct incorporation of isotopically enriched boric acid (instead of borate) into biogenic calcium carbonate, and differences in shell/skeleton polymorph mineralogy. We conclude that the large inter-species variability in delta(BCaCO3)-B-11 (ca. 20%) and significant discrepancies between measured delta(BCaCO3)-B-11 and delta(BCaCO3)-B-11 expected from established ... Article in Journal/Newspaper Ocean acidification Planktonic foraminifera Portail HAL-ANR (Agence Nationale de la Recherche) Biogeosciences 15 5 1447 1467 |