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• W2474837458 abstract "The influence of ocean circulation changes on atmospheric CO2 hinges primarily on the ability to alter the ocean interior's respired nutrient inventory. Here we investigate the Atlantic overturning circulation at the Last Glacial Maximum and its impact on respired carbon storage using radiocarbon and stable carbon isotope data from the Brazil and Iberian Margins. The data demonstrate the existence of a shallow well-ventilated northern-sourced cell overlying a poorly ventilated, predominantly southern-sourced cell at the Last Glacial Maximum. We also find that organic carbon remineralization rates in the deep Atlantic remained broadly similar to modern, but that ventilation ages in the southern-sourced overturning cell were significantly increased. Respired carbon storage in the deep Atlantic was therefore enhanced during the last glacial period, primarily due to an increase in the residence time of carbon in the deep ocean, rather than an increase in biological carbon export." @default.
• W2474837458 created "2016-07-22" @default.
• W2474837458 creator A5000850017 @default.
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• W2474837458 date "2016-06-27" @default.
• W2474837458 modified "2023-10-13" @default.
• W2474837458 title "Radiocarbon evidence for enhanced respired carbon storage in the Atlantic at the Last Glacial Maximum" @default.
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• W2474837458 doi "https://doi.org/10.1038/ncomms11998" @default.
• W2474837458 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/4931225" @default.
• W2474837458 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/27346723" @default.
• W2474837458 hasPublicationYear "2016" @default.
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