Northern peatlands are an integral part of the global carbon cycle—a strong sink of atmospheric carbon dioxide and source of methane. Increasing anthropogenic carbon dioxide and methane in the atmosphere are thought to strongly impact these environments, and yet, peatlands are not routinely included in Earth system models. Here we present a quantification of the sink and stock of northern peat carbon from the last glacial period through the pre-industrial period. Additional data and new algorithms for reconstructing the history of peat carbon accumulation and the timing of peatland initiation increased the estimate of total northern peat carbon stocks from 545 Gt to 1,055 Gt of carbon. Further, the post-glacial increases in peatland initiation rate and carbon accumulation rate are more abrupt than previously reported. Peatlands have been a strong carbon sink throughout the Holocene, but the atmospheric partial pressure of carbon dioxide has been relatively stable over this period. While processes such as permafrost thaw and coral reef development probably contributed some additional carbon to the atmosphere, we suggest that deep ocean upwelling was the most important mechanism for balancing the peatland sink and maintaining the observed stability.
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All data for this investigation is publicly available. Radiocarbon dates and attendant metadata from the Neotoma Paleoecology Database13 were accessed via its API using the ‘neotoma’ package for the R statistical computing environment (https://www.r-project.org/). Radiocarbon dates and peat carbon density data used in the Loisel et al. compilation14 is available to download at https://peatlands.lehigh.edu. The Treat et al. compilation15 is available from the Pangaea databases at https://doi.org/10.1594/PANGAEA.864101 and https://doi.org/10.1594/PANGAEA.863697. Radiocarbon measurements on basal peat without depth information were accessed from the supplementary information included with refs. 10,11,17.
Gorham, E. Northern Peatlands: Role in the carbon cycle and probable responses to climatic warming. Ecol. Appl. 1, 182–195 (1991).
Charman, D. J. et al. Climate-related changes in peatland carbon accumulation during the last millennium. Biogeosciences 10, 929–944 (2013).
Bragazza, L. et al. Persistent high temperature and low precipitation reduce peat carbon accumulation. Glob. Change Biol. 22, 4114–4123 (2016).
Gallego-Sala, A. V. et al. Latitudinal limits to the predicted increase of the peatland carbon sink with warming. Nat. Clim. Change 8, 907–913 (2018).
Frolking, S., Roulet, N. & Lawrence, D. in Carbon Cycling in Northern Peatlands (eds Baird, A. J. et al.) 19–35 (American Geophysical Union, 2009).
Waddington, J. M. et al. Hydrological feedbacks in northern peatlands. Ecohydrology 8, 113–127 (2014).
Yu, Z., Loisel, J., Brosseau, D. P., Beilman, D. W. & Hunt, S. J. Global peatland dynamics since the Last Glacial Maximum. Geophys. Res. Lett. 37, L13402 (2010).
Yu, Z. Northern peatland carbon stocks and dynamics: a review. Biogeosciences 9, 4071–4085 (2012).
Turetsky, M. R. et al. Global vulnerability of peatlands to fire and carbon loss. Nat. Geosci. 8, 11–14 (2015).
Macdonald, G. M. et al. Rapid early development of circumarctic peatlands and atmospheric CH4 and CO2 variations. Science 314, 285–288 (2006).
Korhola, A. et al. The importance of northern peatland expansion to the late-Holocene rise of atmospheric methane. Quat. Sci. Rev. 29, 611–617 (2010).
Loisel, J. et al. Insights and issues with estimating northern peatland carbon stocks and fluxes since the Last Glacial Maximum. Earth Sci. Rev. 165, 59–80 (2017).
Williams, J. W. et al. The Neotoma Paleoecology Database, a multiproxy, international, community-curated data resource. Quat. Res. 89, 156–177 (2018).
Loisel, J. et al. A database and synthesis of northern peatland soil properties and Holocene carbon and nitrogen accumulation. Holocene 24, 1028–1042 (2014).
Treat, C. C. et al. Effects of permafrost aggradation on peat properties as determined from a pan‐Arctic synthesis of plant macrofossils. J. Geophys. Res. Biogeosci. 121, 78–94 (2016).
Holmquist, J. R. et al. Quaternary geochronology. Quat. Geochronol. 31, 53–61 (2016).
Gorham, E., Lehman, C., Dyke, A., Janssens, J. & Dyke, L. Temporal and spatial aspects of peatland initiation following deglaciation in North America. Quat. Sci. Rev. 26, 300–311 (2007).
Xu, J., Morris, P. J., Liu, J. & Holden, J. PEATMAP: Refining estimates of global peatland distribution based on a meta-analysis. Catena 160, 134–140 (2017).
Reyes, A. V. & Cooke, C. A. Northern peatland initiation lagged abrupt increases in deglacial atmospheric CH4. Proc. Natl Acad. Sci. USA 108, 4748–4753 (2011).
Yang, J.-W., Ahn, J., Brook, E. J. & Ryu, Y. Atmospheric methane control mechanisms during the early Holocene. Clim. Past 13, 1227–1242 (2017).
Lambeck, K., Rouby, H., Purcell, A., Sun, Y. & Sambridge, M. Sea level and global ice volumes from the Last Glacial Maximum to the Holocene. Proc. Natl Acad. Sci. USA 111, 15296–15303 (2014).
Peteet, D. M. et al. Delayed deglaciation or extreme Arctic conditions 21–16 cal. kyr at southeastern Laurentide Ice Sheet margin? Geophys. Res. Lett. 39, L11706 (2012).
Jones, M. C. & Yu, Z. Rapid deglacial and early Holocene expansion of peatlands in Alaska. Proc. Natl Acad. Sci. USA 107, 7347–7352 (2010).
Schmitt, J. et al. Carbon isotope constraints on the deglacial CO2 rise from ice cores. Science 336, 711–714 (2012).
Anderson, R. F. et al. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2. Science 323, 1443–1448 (2009).
Studer, A. S. et al. Antarctic Zone nutrient conditions during the last two glacial cycles. Paleoceanogr. Paleoclimatol. 30, 845–862 (2015).
Studer, A. S. et al. Increased nutrient supply to the Southern Ocean during the Holocene and its implications for the pre-industrial atmospheric CO2 rise. Nat. Geosci. 11, 756–760 (2018).
Wang, X. T. et al. Deep-sea coral evidence for lower Southern Ocean surface nitrate concentrations during the last ice age. Proc. Natl Acad. Sci. USA 114, 3352–3357 (2017).
Sarma, V. V. S. S. Monthly variability in surface pCO2 and net air-sea CO2 flux in the Arabian Sea. J. Geophys. Res. 108(C8), 3255 (2003).
Clemens, S. C. & Prell, W. L. A 350,000 year summer-monsoon multi-proxy stack from the Owen Ridge, Northern Arabian Sea. Mar. Geol. 201, 35–51 (2003).
Naidu, P. D. & Malmgren, B. A. Seasonal sea surface temperature contrast between the Holocene and last glacial period in the western Arabian Sea (Ocean Drilling Project Site 723A): Modulated by monsoon upwelling. Paleoceanogr. Paleoclimatol. 20, PA1004 (2005).
Koutavas, A. & Joanides, S. El Niño-Southern Oscillation extrema in the Holocene and Last Glacial Maximum. Paleoceanogr. Paleoclimatol. 27, PA4208 (2012).
Koutavas, A., deMenocal, P. B., Olive, G. C. & Lynch-Stieglitz, J. Mid-Holocene El Niño–Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments. Geology 34, 993–996 (2006).
Chazen, C. R., Altabet, M. A. & Herbert, T. D. Abrupt mid-Holocene onset of centennial-scale climate variability on the Peru-Chile Margin. Geophys. Res. Lett. 36, L18704 (2009).
Schmittner, A. & Somes, C. J. Complementary constraints from carbon (13C) and nitrogen (15N) isotopes on the glacial ocean’s soft-tissue biological pump. Paleoceanogr. Paleoclimatol. 31, 669–693 (2016).
Berger, W. H. Increase of carbon dioxide in the atmosphere during deglaciation: the coral reef hypothesis. Naturwissenschaften 69, 87–88 (1982).
Vecsei, A. & Berger, W. H. Increase of atmospheric CO2 during deglaciation: constraints on the coral reef hypothesis from patterns of deposition. Glob. Biogeochem. Cycles 18, GB1035 (2004).
Ciais, P. et al. Large inert carbon pool in the terrestrial biosphere during the Last Glacial Maximum. Nat. Geosci. 5, 74–79 (2011).
Köhler, P., Nehrbass-Ahles, C., Schmitt, J., Stocker, T. F. & Fischer, H. A 156 kyr smoothed history of the atmospheric greenhouse gases CO2, CH4, and N2O and their radiative forcing. Earth Syst. Sci. Data 9, 363–387 (2017).
Haslett, J. & Parnell, A. A simple monotone process with application to radiocarbon-dated depth chronologies. J. Roy. Stat. Soc. Ser. C 57, 399–418 (2008).
Reimer, P. J. et al. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 1869–1887 (2013).
Nichols, J. E., Peteet, D. M., Frolking, S. & Karavias, J. A probabilistic method of assessing carbon accumulation rate at Imnavait Creek Peatland, Arctic Long Term Ecological Research Station, Alaska. J. Quat. Sci. 32, 579–586 (2017).
We acknowledge L. Heusser for her comments on the manuscript and R. Anderson and D. Sigman for their helpful discussions. This work is supported by the National Science Foundation grants (nos. ARC-1022979 to D.M.P. and DEB-1557078 to J.E.N.).
The authors declare no competing interests.
Peer review information Primary Handling Editor(s): Xujia Jiang.
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Nichols, J.E., Peteet, D.M. Rapid expansion of northern peatlands and doubled estimate of carbon storage. Nat. Geosci. 12, 917–921 (2019). https://doi.org/10.1038/s41561-019-0454-z
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