The sources contributing to the deglacial rise in atmospheric CO2 concentrations are unclear. Climate model simulations suggest thawing permafrost soils were the initial source, highlighting the vulnerability of modern permafrost carbon stores.
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References
Denton, G. H., Broecker, W. S. & Alley, R. B. PAGES News 14, 14–16 (2006).
Schmitt, J. et al. Science 336, 711–714 (2012).
Broecker, W. & Barker, S. Earth Planet. Sci. Lett. 256, 90–99 (2007).
Lourantou, A. et al. Global Biogeochem. Cycles 24, GB2015 (2010).
Crichton, K., Bouttes, N., Roche, D., Chappellaz, J. & Krinner, G. Nat. Geosci. 9, 683–686 (2016).
Schuur, E. et al. Nature 520, 171–179 (2015).
Hugelius, G. et al. Earth Syst. Sci. Data 5, 3–13 (2013).
Ciais, P. et al. Nat. Geosci. 5, 74–79 (2012).
Lüthi, D. et al. EPICA Dome C Ice Core 800 kyr Carbon Dioxide Data (IGBP PAGES, World Data Center for Paleoclimatology Data Contribution Series 55, 2008).
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MacDougall, A. Catalyst for deglaciation. Nature Geosci 9, 648–649 (2016). https://doi.org/10.1038/ngeo2802
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DOI: https://doi.org/10.1038/ngeo2802