Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...

<!--!introduction!--> The last glacial period was punctuated by a number of transient events during which massive iceberg discharges profoundly perturbed the deep ocean circulation dynamics, causing widespread climate and environmental changes. Detailed analysis of polar ice cores demonstrated...

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Main Authors: Yang, Ji-Woong, Ladant, Jean-Baptiste, Landais, Amaëlle, Blunier, Thomas, Kageyama, Masa, Jaccard, Samuel, Duchamp-Alphonse, Stéphanie, Sánchez Goñi, María Fernanda, Prié, Frédéric
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
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Online Access:https://dx.doi.org/10.57757/iugg23-2465
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018287
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spelling ftdatacite:10.57757/iugg23-2465 2023-07-23T04:21:53+02:00 Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... Yang, Ji-Woong Ladant, Jean-Baptiste Landais, Amaëlle Blunier, Thomas Kageyama, Masa Jaccard, Samuel Duchamp-Alphonse, Stéphanie Sánchez Goñi, María Fernanda Prié, Frédéric 2023 https://dx.doi.org/10.57757/iugg23-2465 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018287 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-2465 2023-07-03T17:36:25Z <!--!introduction!--> The last glacial period was punctuated by a number of transient events during which massive iceberg discharges profoundly perturbed the deep ocean circulation dynamics, causing widespread climate and environmental changes. Detailed analysis of polar ice cores demonstrated millennial-scale atmospheric CO 2 variations characterized by rapid shifts between relatively cold (stadial) and warm (interstadial) stages and in particular, a gradual rising of CO 2 during Heinrich Stadials (HS). To date, the observed CO 2 increase during HS has been attributed to ventilation changes in Southern Ocean, and/or reduced biological uptake. However, understanding the respective contribution of ocean ventilation and changes in the efficiency of the biological carbon pump is challenging because of difficulties in estimating global biosphere productivity based on local reconstructions as they are often based on indirect geochemical tracers and exhibit spatial heterogeneities. To address this, we ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> The last glacial period was punctuated by a number of transient events during which massive iceberg discharges profoundly perturbed the deep ocean circulation dynamics, causing widespread climate and environmental changes. Detailed analysis of polar ice cores demonstrated millennial-scale atmospheric CO 2 variations characterized by rapid shifts between relatively cold (stadial) and warm (interstadial) stages and in particular, a gradual rising of CO 2 during Heinrich Stadials (HS). To date, the observed CO 2 increase during HS has been attributed to ventilation changes in Southern Ocean, and/or reduced biological uptake. However, understanding the respective contribution of ocean ventilation and changes in the efficiency of the biological carbon pump is challenging because of difficulties in estimating global biosphere productivity based on local reconstructions as they are often based on indirect geochemical tracers and exhibit spatial heterogeneities. To address this, we ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author Yang, Ji-Woong
Ladant, Jean-Baptiste
Landais, Amaëlle
Blunier, Thomas
Kageyama, Masa
Jaccard, Samuel
Duchamp-Alphonse, Stéphanie
Sánchez Goñi, María Fernanda
Prié, Frédéric
spellingShingle Yang, Ji-Woong
Ladant, Jean-Baptiste
Landais, Amaëlle
Blunier, Thomas
Kageyama, Masa
Jaccard, Samuel
Duchamp-Alphonse, Stéphanie
Sánchez Goñi, María Fernanda
Prié, Frédéric
Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
author_facet Yang, Ji-Woong
Ladant, Jean-Baptiste
Landais, Amaëlle
Blunier, Thomas
Kageyama, Masa
Jaccard, Samuel
Duchamp-Alphonse, Stéphanie
Sánchez Goñi, María Fernanda
Prié, Frédéric
author_sort Yang, Ji-Woong
title Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
title_short Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
title_full Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
title_fullStr Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
title_full_unstemmed Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
title_sort global biosphere productivity changes during heinrich stadial 4: preliminary results from the triple o2 isotopes and coupled climate model simulations ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-2465
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018287
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-2465
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