Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th

International audience There is compelling evidence that millennial climate variability of the last glacial period was associated with significant changes in the Atlantic Meridional Overturning Circulation (AMOC). Several North Atlantic sedimentary Pa/Th records indicate a consistent and large Pa/Th...

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Published in:Quaternary Science Reviews
Main Authors: Missiaen, Lise, Menviel, Laurie C., Meissner, Katrin J., Roche, Didier M., Dutay, Jean-Claude, Bouttes, Nathaëlle, Lhardy, Fanny, Quiquet, Aurélien, Pichat, Sylvain, Waelbroeck, Claire
Other Authors: Climate Change Research Centre, ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney 2052, Australia, University of New South Wales Sydney (UNSW), Mark Wainwright Analytical Centre Sydney (UNSW ), 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), Modélisation du climat (CLIM), 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)), Institut Louis Bachelier, Université Claude Bernard Lyon 1 (UCBL), Université de Lyon, Max Planck Institute for Chemistry (MPIC), Max-Planck-Gesellschaft, Processus et interactions de fine échelle océanique (PROTEO), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Australian Research Council, ARC: FT180100606, DP180100048, KJM, LCM and LM acknowledge funding from the Australian Research Council grant DP180100048 awarded to KJM and LCM and grant FT180100606 awarded to LCM., European Project: 339108,EC:FP7:ERC,ERC-2013-ADG,ACCLIMATE(2014)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.science/hal-02883163
https://doi.org/10.1016/j.quascirev.2020.106394
id ftunivlyon:oai:HAL:hal-02883163v1
record_format openpolar
institution Open Polar
collection Université de Lyon: HAL
op_collection_id ftunivlyon
language English
topic Ocean circulation
Pa/Th
Particle fluxes
Abrupt climate events
iLOVECLIM
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle Ocean circulation
Pa/Th
Particle fluxes
Abrupt climate events
iLOVECLIM
[SDE.MCG]Environmental Sciences/Global Changes
Missiaen, Lise
Menviel, Laurie C.
Meissner, Katrin J.
Roche, Didier M.
Dutay, Jean-Claude
Bouttes, Nathaëlle
Lhardy, Fanny
Quiquet, Aurélien
Pichat, Sylvain
Waelbroeck, Claire
Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th
topic_facet Ocean circulation
Pa/Th
Particle fluxes
Abrupt climate events
iLOVECLIM
[SDE.MCG]Environmental Sciences/Global Changes
description International audience There is compelling evidence that millennial climate variability of the last glacial period was associated with significant changes in the Atlantic Meridional Overturning Circulation (AMOC). Several North Atlantic sedimentary Pa/Th records indicate a consistent and large Pa/Th increase across millennial-scale events, which has been interpreted as considerable reduction in North Atlantic Deep Water (NADW) formation. However, the use of sedimentary Pa/Th as a pure kinematic circulation proxy is challenging because Pa and Th are also highly sensitive to changes in particulate flux intensity and composition that might have occurred across these millennial scale events. In this study, we use the Pa/Th enabled iLOVECLIM Earth System Model of intermediate complexity to evaluate the impact of changes in biogenic particle flux intensity and composition on the Atlantic Pa/Th. We find that in our model, changes in Particulate Organic Carbon (POC), and to a lesser extent biogenic opal production, can significantly affect the sedimentary Pa/Th, possibly explaining up to 30% of the observed North Atlantic Pa/Th increase across Heinrich stadial 1. The sedimentary Pa/Th response is also likely sensitive to shifts in the geographical distribution of the particles, especially in high scavenging regions. Our study suggests that a decrease in opal production in the northwest Atlantic can induce a far field Pa/Th increase in a large part of the North Atlantic basin. Therefore, local monitoring of particle fluxes may not be sufficient to rule out any influence of changing particle fluxes on sedimentary Pa/Th records.
author2 Climate Change Research Centre, ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney 2052, Australia
University of New South Wales Sydney (UNSW)
Mark Wainwright Analytical Centre Sydney (UNSW )
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)
Modélisation du climat (CLIM)
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))
Institut Louis Bachelier
Université Claude Bernard Lyon 1 (UCBL)
Université de Lyon
Max Planck Institute for Chemistry (MPIC)
Max-Planck-Gesellschaft
Processus et interactions de fine échelle océanique (PROTEO)
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
Australian Research Council, ARC: FT180100606, DP180100048
KJM, LCM and LM acknowledge funding from the Australian Research Council grant DP180100048 awarded to KJM and LCM and grant FT180100606 awarded to LCM.
European Project: 339108,EC:FP7:ERC,ERC-2013-ADG,ACCLIMATE(2014)
format Article in Journal/Newspaper
author Missiaen, Lise
Menviel, Laurie C.
Meissner, Katrin J.
Roche, Didier M.
Dutay, Jean-Claude
Bouttes, Nathaëlle
Lhardy, Fanny
Quiquet, Aurélien
Pichat, Sylvain
Waelbroeck, Claire
author_facet Missiaen, Lise
Menviel, Laurie C.
Meissner, Katrin J.
Roche, Didier M.
Dutay, Jean-Claude
Bouttes, Nathaëlle
Lhardy, Fanny
Quiquet, Aurélien
Pichat, Sylvain
Waelbroeck, Claire
author_sort Missiaen, Lise
title Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th
title_short Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th
title_full Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th
title_fullStr Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th
title_full_unstemmed Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th
title_sort modelling the impact of biogenic particle flux intensity and composition on sedimentary pa/th
publisher HAL CCSD
publishDate 2020
url https://hal.science/hal-02883163
https://doi.org/10.1016/j.quascirev.2020.106394
genre NADW
North Atlantic Deep Water
North Atlantic
Northwest Atlantic
genre_facet NADW
North Atlantic Deep Water
North Atlantic
Northwest Atlantic
op_source ISSN: 0277-3791
EISSN: 1873-457X
Quaternary Science Reviews
https://hal.science/hal-02883163
Quaternary Science Reviews, 2020, 240, ⟨10.1016/j.quascirev.2020.106394⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2020.106394
info:eu-repo/grantAgreement/EC/FP7/339108/EU/Elucidating the Causes and Effects of Atlantic Circulation Changes through Model-Data Integration/ACCLIMATE
hal-02883163
https://hal.science/hal-02883163
doi:10.1016/j.quascirev.2020.106394
WOS: 000546906200018
op_doi https://doi.org/10.1016/j.quascirev.2020.106394
container_title Quaternary Science Reviews
container_volume 240
container_start_page 106394
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spelling ftunivlyon:oai:HAL:hal-02883163v1 2024-06-23T07:54:40+00:00 Modelling the impact of biogenic particle flux intensity and composition on sedimentary Pa/Th Missiaen, Lise Menviel, Laurie C. Meissner, Katrin J. Roche, Didier M. Dutay, Jean-Claude Bouttes, Nathaëlle Lhardy, Fanny Quiquet, Aurélien Pichat, Sylvain Waelbroeck, Claire Climate Change Research Centre, ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney 2052, Australia University of New South Wales Sydney (UNSW) Mark Wainwright Analytical Centre Sydney (UNSW ) 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) Modélisation du climat (CLIM) 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)) Institut Louis Bachelier Université Claude Bernard Lyon 1 (UCBL) Université de Lyon Max Planck Institute for Chemistry (MPIC) Max-Planck-Gesellschaft Processus et interactions de fine échelle océanique (PROTEO) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Australian Research Council, ARC: FT180100606, DP180100048 KJM, LCM and LM acknowledge funding from the Australian Research Council grant DP180100048 awarded to KJM and LCM and grant FT180100606 awarded to LCM. European Project: 339108,EC:FP7:ERC,ERC-2013-ADG,ACCLIMATE(2014) 2020 https://hal.science/hal-02883163 https://doi.org/10.1016/j.quascirev.2020.106394 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2020.106394 info:eu-repo/grantAgreement/EC/FP7/339108/EU/Elucidating the Causes and Effects of Atlantic Circulation Changes through Model-Data Integration/ACCLIMATE hal-02883163 https://hal.science/hal-02883163 doi:10.1016/j.quascirev.2020.106394 WOS: 000546906200018 ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-02883163 Quaternary Science Reviews, 2020, 240, ⟨10.1016/j.quascirev.2020.106394⟩ Ocean circulation Pa/Th Particle fluxes Abrupt climate events iLOVECLIM [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2020 ftunivlyon https://doi.org/10.1016/j.quascirev.2020.106394 2024-05-27T14:45:40Z International audience There is compelling evidence that millennial climate variability of the last glacial period was associated with significant changes in the Atlantic Meridional Overturning Circulation (AMOC). Several North Atlantic sedimentary Pa/Th records indicate a consistent and large Pa/Th increase across millennial-scale events, which has been interpreted as considerable reduction in North Atlantic Deep Water (NADW) formation. However, the use of sedimentary Pa/Th as a pure kinematic circulation proxy is challenging because Pa and Th are also highly sensitive to changes in particulate flux intensity and composition that might have occurred across these millennial scale events. In this study, we use the Pa/Th enabled iLOVECLIM Earth System Model of intermediate complexity to evaluate the impact of changes in biogenic particle flux intensity and composition on the Atlantic Pa/Th. We find that in our model, changes in Particulate Organic Carbon (POC), and to a lesser extent biogenic opal production, can significantly affect the sedimentary Pa/Th, possibly explaining up to 30% of the observed North Atlantic Pa/Th increase across Heinrich stadial 1. The sedimentary Pa/Th response is also likely sensitive to shifts in the geographical distribution of the particles, especially in high scavenging regions. Our study suggests that a decrease in opal production in the northwest Atlantic can induce a far field Pa/Th increase in a large part of the North Atlantic basin. Therefore, local monitoring of particle fluxes may not be sufficient to rule out any influence of changing particle fluxes on sedimentary Pa/Th records. Article in Journal/Newspaper NADW North Atlantic Deep Water North Atlantic Northwest Atlantic Université de Lyon: HAL Quaternary Science Reviews 240 106394