Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes?
International audience [1] The reconstruction of past changes in bottom water CO 3 = is central to evaluating competing oceanic scenarios that deal with long-term variations in atmospheric pCO 2. In search of a quantitative bottom water CO 3 = proxy, we analyzed the variations of calcite crystallini...
Published in: | Geochemistry, Geophysics, Geosystems |
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Format: | Article in Journal/Newspaper |
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Online Access: | https://hal.archives-ouvertes.fr/hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898/document https://hal.archives-ouvertes.fr/hal-02921898/file/2003GC000668.pdf https://doi.org/10.1029/2003GC000668 |
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ftccsdartic:oai:HAL:hal-02921898v1 2023-05-15T18:00:50+02:00 Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? Bassinot, Franck Mélières, Frédéric Gehlen, Marion Levi, Camille Labeyrie, Laurent Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Paléocéanographie (PALEOCEAN) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Muséum national d'Histoire naturelle (MNHN) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) 2004-08 https://hal.archives-ouvertes.fr/hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898/document https://hal.archives-ouvertes.fr/hal-02921898/file/2003GC000668.pdf https://doi.org/10.1029/2003GC000668 en eng HAL CCSD AGU and the Geochemical Society info:eu-repo/semantics/altIdentifier/doi/10.1029/2003GC000668 hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898/document https://hal.archives-ouvertes.fr/hal-02921898/file/2003GC000668.pdf doi:10.1029/2003GC000668 info:eu-repo/semantics/OpenAccess ISSN: 1525-2027 EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://hal.archives-ouvertes.fr/hal-02921898 Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2004, 5 (8), ⟨10.1029/2003GC000668⟩ carbonate dissolution foraminifers calcite crystallinity bottom water CO3 [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 2004 ftccsdartic https://doi.org/10.1029/2003GC000668 2021-12-19T00:52:16Z International audience [1] The reconstruction of past changes in bottom water CO 3 = is central to evaluating competing oceanic scenarios that deal with long-term variations in atmospheric pCO 2. In search of a quantitative bottom water CO 3 = proxy, we analyzed the variations of calcite crystallinity of planktonic foraminifera Globigerinoides ruber shells picked from core top samples along three depth transects: Ontong Java Plateau and the northeast margin of Irian Jaya, in the western equatorial Pacific, and the Sierra Leone Rise, in the eastern tropical Atlantic. The strong empirical relationship between calcite crystallinity (inferred from the full width at half maximum (FWHM) of calcite (104) X-ray diffraction peak) and bottom water saturation relative to calcite (DCO 3) shows that foraminifera calcite crystallinity could be a promising proxy for the reconstruction of upper Pleistocene bottom water carbonate ion concentration. Article in Journal/Newspaper Planktonic foraminifera Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Jaya ENVELOPE(11.688,11.688,-70.766,-70.766) Pacific Geochemistry, Geophysics, Geosystems 5 8 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
carbonate dissolution foraminifers calcite crystallinity bottom water CO3 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
carbonate dissolution foraminifers calcite crystallinity bottom water CO3 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Bassinot, Franck Mélières, Frédéric Gehlen, Marion Levi, Camille Labeyrie, Laurent Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? |
topic_facet |
carbonate dissolution foraminifers calcite crystallinity bottom water CO3 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience [1] The reconstruction of past changes in bottom water CO 3 = is central to evaluating competing oceanic scenarios that deal with long-term variations in atmospheric pCO 2. In search of a quantitative bottom water CO 3 = proxy, we analyzed the variations of calcite crystallinity of planktonic foraminifera Globigerinoides ruber shells picked from core top samples along three depth transects: Ontong Java Plateau and the northeast margin of Irian Jaya, in the western equatorial Pacific, and the Sierra Leone Rise, in the eastern tropical Atlantic. The strong empirical relationship between calcite crystallinity (inferred from the full width at half maximum (FWHM) of calcite (104) X-ray diffraction peak) and bottom water saturation relative to calcite (DCO 3) shows that foraminifera calcite crystallinity could be a promising proxy for the reconstruction of upper Pleistocene bottom water carbonate ion concentration. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Paléocéanographie (PALEOCEAN) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Muséum national d'Histoire naturelle (MNHN) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) |
format |
Article in Journal/Newspaper |
author |
Bassinot, Franck Mélières, Frédéric Gehlen, Marion Levi, Camille Labeyrie, Laurent |
author_facet |
Bassinot, Franck Mélières, Frédéric Gehlen, Marion Levi, Camille Labeyrie, Laurent |
author_sort |
Bassinot, Franck |
title |
Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? |
title_short |
Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? |
title_full |
Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? |
title_fullStr |
Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? |
title_full_unstemmed |
Crystallinity of foraminifera shells: A proxy to reconstruct past bottom water CO 3 = changes? |
title_sort |
crystallinity of foraminifera shells: a proxy to reconstruct past bottom water co 3 = changes? |
publisher |
HAL CCSD |
publishDate |
2004 |
url |
https://hal.archives-ouvertes.fr/hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898/document https://hal.archives-ouvertes.fr/hal-02921898/file/2003GC000668.pdf https://doi.org/10.1029/2003GC000668 |
long_lat |
ENVELOPE(11.688,11.688,-70.766,-70.766) |
geographic |
Jaya Pacific |
geographic_facet |
Jaya Pacific |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
ISSN: 1525-2027 EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://hal.archives-ouvertes.fr/hal-02921898 Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2004, 5 (8), ⟨10.1029/2003GC000668⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2003GC000668 hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898 https://hal.archives-ouvertes.fr/hal-02921898/document https://hal.archives-ouvertes.fr/hal-02921898/file/2003GC000668.pdf doi:10.1029/2003GC000668 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2003GC000668 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
5 |
container_issue |
8 |
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1766170087934394368 |