Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH
International audience [1] Using the CRPG-CNRS Cameca 1270 ion microprobe facility, we have measured boron isotopic compositions (11 B/ 10 B) in different ultrastructural components of the deep-sea aragonitic scleractinian coral Lophelia pertusa. We observe a systematic difference in B isotopic comp...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2007
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Online Access: | https://hal.science/hal-02956092 https://hal.science/hal-02956092/document https://hal.science/hal-02956092/file/2007GC001686.pdf https://doi.org/10.1029/2007GC001686 |
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HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) |
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language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Blamart, D. Rollion-Bard, C. Meibom, A. Cuif, J.-P. Juillet-Leclerc, A. Dauphin, Y. Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience [1] Using the CRPG-CNRS Cameca 1270 ion microprobe facility, we have measured boron isotopic compositions (11 B/ 10 B) in different ultrastructural components of the deep-sea aragonitic scleractinian coral Lophelia pertusa. We observe a systematic difference in B isotopic composition between the Early Mineralization Zone (EMZ) and adjacent fibrous skeleton. In EMZ the measured d 11 B values are consistently low. Fibrous aragonite is characterized by systematically higher d 11 B values but also displays B isotopic heterogeneity associated with specific growth bands in the calyx wall. The magnitude of the observed B isotopic variations cannot be explained by changes in environmental conditions and is likely caused by biological processes involved in the biomineralization of new skeleton, i.e., ''vital'' effects. The observed B isotopic variations are opposite to the predictions of geochemical models for vital effects. These models are based on the idea that stable isotopic fractionations (including C and O) in coral skeleton are driven by changes in pH of the fluid from which the skeleton is presumed to precipitate. Our data indicate that pH variations are not responsible for the observed stable isotopic fractionations. Geochemical models therefore do not provide an adequate framework within which to understand coral skeletal formation. Without a better understanding of these processes the use of B isotopic composition to reconstruct paleo-pH variations in the oceans must be considered problematic, at least as far as Lophelia pertusa is concerned. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Paléocéanographie (PALEOCEAN) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Centre de Recherches Pétrographiques et Géochimiques (CRPG) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'Etude de la Matière Extraterrestre / UMS Nano-analyses (LEME / UNA) Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS) Interactions et dynamique des environnements de surface (IDES) Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Blamart, D. Rollion-Bard, C. Meibom, A. Cuif, J.-P. Juillet-Leclerc, A. Dauphin, Y. |
author_facet |
Blamart, D. Rollion-Bard, C. Meibom, A. Cuif, J.-P. Juillet-Leclerc, A. Dauphin, Y. |
author_sort |
Blamart, D. |
title |
Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH |
title_short |
Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH |
title_full |
Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH |
title_fullStr |
Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH |
title_full_unstemmed |
Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH |
title_sort |
correlation of boron isotopic composition with ultrastructure in the deep-sea coral lophelia pertusa : implications for biomineralization and paleo-ph |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.science/hal-02956092 https://hal.science/hal-02956092/document https://hal.science/hal-02956092/file/2007GC001686.pdf https://doi.org/10.1029/2007GC001686 |
genre |
Lophelia pertusa |
genre_facet |
Lophelia pertusa |
op_source |
EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://hal.science/hal-02956092 Geochemistry, Geophysics, Geosystems, 2007, 8 (12), pp.Q12001. ⟨10.1029/2007GC001686⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1029/2007GC001686 hal-02956092 https://hal.science/hal-02956092 https://hal.science/hal-02956092/document https://hal.science/hal-02956092/file/2007GC001686.pdf doi:10.1029/2007GC001686 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2007GC001686 |
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Geochemistry, Geophysics, Geosystems |
container_volume |
8 |
container_issue |
12 |
container_start_page |
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ftceafr:oai:HAL:hal-02956092v1 2024-09-15T18:18:00+00:00 Correlation of boron isotopic composition with ultrastructure in the deep-sea coral Lophelia pertusa : Implications for biomineralization and paleo-pH Blamart, D. Rollion-Bard, C. Meibom, A. Cuif, J.-P. Juillet-Leclerc, A. Dauphin, Y. Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Paléocéanographie (PALEOCEAN) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Centre de Recherches Pétrographiques et Géochimiques (CRPG) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'Etude de la Matière Extraterrestre / UMS Nano-analyses (LEME / UNA) Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS) Interactions et dynamique des environnements de surface (IDES) Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2007-12 https://hal.science/hal-02956092 https://hal.science/hal-02956092/document https://hal.science/hal-02956092/file/2007GC001686.pdf https://doi.org/10.1029/2007GC001686 en eng HAL CCSD AGU and the Geochemical Society info:eu-repo/semantics/altIdentifier/doi/10.1029/2007GC001686 hal-02956092 https://hal.science/hal-02956092 https://hal.science/hal-02956092/document https://hal.science/hal-02956092/file/2007GC001686.pdf doi:10.1029/2007GC001686 info:eu-repo/semantics/OpenAccess EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://hal.science/hal-02956092 Geochemistry, Geophysics, Geosystems, 2007, 8 (12), pp.Q12001. ⟨10.1029/2007GC001686⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2007 ftceafr https://doi.org/10.1029/2007GC001686 2024-07-22T13:17:55Z International audience [1] Using the CRPG-CNRS Cameca 1270 ion microprobe facility, we have measured boron isotopic compositions (11 B/ 10 B) in different ultrastructural components of the deep-sea aragonitic scleractinian coral Lophelia pertusa. We observe a systematic difference in B isotopic composition between the Early Mineralization Zone (EMZ) and adjacent fibrous skeleton. In EMZ the measured d 11 B values are consistently low. Fibrous aragonite is characterized by systematically higher d 11 B values but also displays B isotopic heterogeneity associated with specific growth bands in the calyx wall. The magnitude of the observed B isotopic variations cannot be explained by changes in environmental conditions and is likely caused by biological processes involved in the biomineralization of new skeleton, i.e., ''vital'' effects. The observed B isotopic variations are opposite to the predictions of geochemical models for vital effects. These models are based on the idea that stable isotopic fractionations (including C and O) in coral skeleton are driven by changes in pH of the fluid from which the skeleton is presumed to precipitate. Our data indicate that pH variations are not responsible for the observed stable isotopic fractionations. Geochemical models therefore do not provide an adequate framework within which to understand coral skeletal formation. Without a better understanding of these processes the use of B isotopic composition to reconstruct paleo-pH variations in the oceans must be considered problematic, at least as far as Lophelia pertusa is concerned. Article in Journal/Newspaper Lophelia pertusa HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Geochemistry, Geophysics, Geosystems 8 12 n/a n/a |