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Main Authors: Gottschalk, Julia, Michel, Elisabeth, Thöle, Lena M, Studer, Anja S, Hasenfratz, Adam P, Schmid, Nicole, Mazaud, Alain, Martínez-García, Alfredo, Szidat, Sönke, Jaccard, Samuel L
Format: Dataset Open Access
Language:en
Published: PANGAEA 2020
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Online Access:https://doi.org/10.1594/PANGAEA.912711
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author Gottschalk, Julia
Michel, Elisabeth
Thöle, Lena M
Studer, Anja S
Hasenfratz, Adam P
Schmid, Nicole
Mazaud, Alain
Martínez-García, Alfredo
Szidat, Sönke
Jaccard, Samuel L
author_facet Gottschalk, Julia
Michel, Elisabeth
Thöle, Lena M
Studer, Anja S
Hasenfratz, Adam P
Schmid, Nicole
Mazaud, Alain
Martínez-García, Alfredo
Szidat, Sönke
Jaccard, Samuel L
collection Datos científicos de ciencias marinas y ambientales
contents Past changes in ocean 14C disequilibria have been suggested to reflect the Southern Ocean control on global exogenic carbon cycling. Yet, the volumetric extent of the glacial carbon pool and the deglacial mechanisms contributing to release remineralized carbon, particularly from regions with enhanced mixing today, remain insufficiently constrained. Here, we reconstruct the deglacial ventilation history of the South Indian upwelling hotspot near Kerguelen Island, using high-resolution 14C-dating of smaller-than-conventional foraminiferal samples and multi-proxy deep-ocean oxygen estimates. We find marked regional differences in Southern Ocean overturning with distinct South Indian fingerprints on (early de-)glacial atmospheric CO2 change. The dissipation of this heterogeneity commenced 14.6 kyr ago, signaling the onset of modern-like, strong South Indian Ocean upwelling, likely promoted by rejuvenated Atlantic overturning. Our findings highlight the South Indian Ocean's capacity to influence atmospheric CO2 levels and amplify the impacts of inter-hemispheric climate variability on global carbon cycling within centuries and millennia.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_912711
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Radiocarbon and oxygen ventilation in the deep South Indian Ocean during the last deglaciation
Gottschalk, Julia
Michel, Elisabeth
Thöle, Lena M
Studer, Anja S
Hasenfratz, Adam P
Schmid, Nicole
Mazaud, Alain
Martínez-García, Alfredo
Szidat, Sönke
Jaccard, Samuel L
Deglaciation; ocean circulation; Radiocarbon; Termination; ventilation
Past changes in ocean 14C disequilibria have been suggested to reflect the Southern Ocean control on global exogenic carbon cycling. Yet, the volumetric extent of the glacial carbon pool and the deglacial mechanisms contributing to release remineralized carbon, particularly from regions with enhanced mixing today, remain insufficiently constrained. Here, we reconstruct the deglacial ventilation history of the South Indian upwelling hotspot near Kerguelen Island, using high-resolution 14C-dating of smaller-than-conventional foraminiferal samples and multi-proxy deep-ocean oxygen estimates. We find marked regional differences in Southern Ocean overturning with distinct South Indian fingerprints on (early de-)glacial atmospheric CO2 change. The dissipation of this heterogeneity commenced 14.6 kyr ago, signaling the onset of modern-like, strong South Indian Ocean upwelling, likely promoted by rejuvenated Atlantic overturning. Our findings highlight the South Indian Ocean's capacity to influence atmospheric CO2 levels and amplify the impacts of inter-hemispheric climate variability on global carbon cycling within centuries and millennia.
title Radiocarbon and oxygen ventilation in the deep South Indian Ocean during the last deglaciation
topic Deglaciation; ocean circulation; Radiocarbon; Termination; ventilation
url https://doi.org/10.1594/PANGAEA.912711