Low atmospheric CO 2 levels during the Little Ice Age due to cooling-induced terrestrial uptake

• Published in: Nature Geoscience
• Main Authors: Rubino M., Etheridge D. M., Trudinger C. M., Allison C. E., Rayner P. J., Enting I., Mulvaney R., Steele L. P., Langenfelds R. L., Sturges W. T., Curran M. A. J., Smith A. M.
• Other Authors: Rubino, M., Etheridge, D. M., Trudinger, C. M., Allison, C. E., Rayner, P. J., Enting, I., Mulvaney, R., Steele, L. P., Langenfelds, R. L., Sturges, W. T., Curran, M. A. J., Smith, A. M.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2016
• Subjects: Dronning Maud Land; Antarc*; Antarctica; ice core
• Online Access: http://hdl.handle.net/11591/410552; https://doi.org/10.1038/ngeo2769; http://www.nature.com/ngeo/index.html

Low atmospheric carbon dioxide (CO 2) concentration during the Little Ice Age has been used to derive the global carbon cycle sensitivity to temperature. Recent evidence confirms earlier indications that the low CO 2 was caused by increased terrestrial carbon storage. It remains unknown whether the terrestrial biosphere responded to temperature variations, or there was vegetation re-growth on abandoned farmland. Here we present a global numerical simulation of atmospheric carbonyl sulfide concentrations in the pre-industrial period. Carbonyl sulfide concentration is linked to changes in gross primary production and shows a positive anomaly during the Little Ice Age. We show that a decrease in gross primary production and a larger decrease in ecosystem respiration is the most likely explanation for the decrease in atmospheric CO 2 and increase in atmospheric carbonyl sulfide concentrations. Therefore, temperature change, not vegetation re-growth, was the main cause of the increased terrestrial carbon storage. We address the inconsistency between ice-core CO 2 records from different sites measuring CO 2 and Í 13 CO 2 in ice from Dronning Maud Land (Antarctica). Our interpretation allows us to derive the temperature sensitivity of pre-industrial CO 2 fluxes for the terrestrial biosphere (I 3 L = â '10 to â '90 Pg C K â '1), implying a positive climate feedback and providing a benchmark to reduce model uncertainties.