Treat, Claire C. , Kleinen, Thomas , Broothaerts, Nils, Dalton, April S., Dommain, René, Douglas, Thomas A. , Drexler, Judith Z., Finkelstein, Sarah A., Grosse, Guido, Hope, Geoffrey, Hutchings, Jack, Jones, Miriam C. , Kuhry, Peter, Lacourse, Terri, Lähteenoja, Outi, Loisel, Julie, Notebaert, Bastiaan, Payne, Richard J., Peteet, Dorothy M. , Sannel, A. Britta K. , Stelling, Jonathan M., Strauss, Jens, Swindles, Graeme T., Talbot, Julie, Tarnocai, Charles, Verstraeten, Gert, Williams, Christopher J., Xia, Zhengyu, Yu, Zicheng , Väliranta, Minna, Hättestrand, Martina, Alexanderson, Helena and Brovkin, Victor (2019) Widespread global peatland establishment and persistence over the last 130,000 y. Proceedings of the National Academy of Sciences of the United States of America (PNAS), 116 (11). pp. 4822-4827. DOI 10.1073/pnas.1813305116.

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Abstract

Significance

During the Holocene (11,600 y ago to present), northern peatlands accumulated significant C stocks over millennia. However, virtually nothing is known about peatlands that are no longer in the landscape, including ones formed prior to the Holocene: Where were they, when did they form, and why did they disappear? We used records of peatlands buried by mineral sediments for a reconstruction of peat-forming wetlands for the past 130,000 y. Northern peatlands expanded across high latitudes during warm periods and were buried during periods of glacial advance in northern latitudes. Thus, peat accumulation and burial represent a key long-term C storage mechanism in the Earth system.
Abstract

Glacial−interglacial variations in CO2 and methane in polar ice cores have been attributed, in part, to changes in global wetland extent, but the wetland distribution before the Last Glacial Maximum (LGM, 21 ka to 18 ka) remains virtually unknown. We present a study of global peatland extent and carbon (C) stocks through the last glacial cycle (130 ka to present) using a newly compiled database of 1,063 detailed stratigraphic records of peat deposits buried by mineral sediments, as well as a global peatland model. Quantitative agreement between modeling and observations shows extensive peat accumulation before the LGM in northern latitudes (>40°N), particularly during warmer periods including the last interglacial (130 ka to 116 ka, MIS 5e) and the interstadial (57 ka to 29 ka, MIS 3). During cooling periods of glacial advance and permafrost formation, the burial of northern peatlands by glaciers and mineral sediments decreased active peatland extent, thickness, and modeled C stocks by 70 to 90% from warmer times. Tropical peatland extent and C stocks show little temporal variation throughout the study period. While the increased burial of northern peats was correlated with cooling periods, the burial of tropical peat was predominately driven by changes in sea level and regional hydrology. Peat burial by mineral sediments represents a mechanism for long-term terrestrial C storage in the Earth system. These results show that northern peatlands accumulate significant C stocks during warmer times, indicating their potential for C sequestration during the warming Anthropocene.

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