Revealing the hidden carbon in forested wetland soils

Anthony J. Stewart (), Meghan Halabisky, Chad Babcock, David E. Butman, David V. D’Amore and L. Monika Moskal
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Anthony J. Stewart: University of Washington, Seattle
Meghan Halabisky: University of Washington, Seattle
Chad Babcock: University of Minnesota
David E. Butman: University of Washington, Seattle
David V. D’Amore: Pacific Northwest Research Station, U.S. Department of Agriculture Forest Service
L. Monika Moskal: University of Washington, Seattle

Nature Communications, 2024, vol. 15, issue 1, 1-13

Abstract: Abstract Inland wetlands are critical carbon reservoirs storing 30% of global soil organic carbon (SOC) within 6% of the land surface. However, forested regions contain SOC-rich wetlands that are not included in current maps, which we refer to as ‘cryptic carbon’. Here, to demonstrate the magnitude and distribution of cryptic carbon, we measure and map SOC stocks as a function of a continuous, upland-to-wetland gradient across the Hoh River Watershed (HRW) in the Pacific Northwest of the U.S., comprising 68,145 ha. Total catchment SOC at 30 cm depth (5.0 TgC) is between estimates from global SOC maps (GSOC: 3.9 TgC; SoilGrids: 7.8 TgC). For wetland SOC, our 1 m stock estimates are substantially higher (Mean: 259 MgC ha−1; Total: 1.7 TgC) compared to current wetland-specific SOC maps derived from a combination of U.S. national datasets (Mean: 184 MgC ha−1; Total: 0.3 TgC). We show that total unmapped or cryptic carbon is 1.5 TgC and when added to current estimates, increases the estimated wetland SOC stock to 1.8 TgC or by 482%, which highlights the vast stores of SOC that are not mapped and contained in unprotected and vulnerable wetlands.

Date: 2024
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DOI: 10.1038/s41467-024-44888-x

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