TY - JOUR
T1 - Fine root and soil carbon stocks are positively related in grasslands but not in forests
AU - Malhotra, Avni
AU - Moore, Jessica A.M.
AU - Weintraub-Leff, Samantha
AU - Georgiou, Katerina
AU - Berhe, Asmeret Asefaw
AU - Billings, Sharon A.
AU - de Graaff, Marie Anne
AU - Fraterrigo, Jennifer M.
AU - Grandy, A. Stuart
AU - Kyker-Snowman, Emily
AU - Lu, Mingzhen
AU - Meier, Courtney
AU - Pierson, Derek
AU - Tumber-Dávila, Shersingh Joseph
AU - Lajtha, Kate
AU - Wieder, William R.
AU - Jackson, Robert B.
N1 - Publisher Copyright:
© This is a U.S. Government work and not under copyright protection in the US; foreign copyright protection may apply 2025.
PY - 2025/12
Y1 - 2025/12
N2 - Increasing fine root carbon (FRC) inputs into soils has been proposed as a solution to increasing soil organic carbon (SOC). However, FRC inputs can also enhance SOC loss through priming. Here, we tested the broad-scale relationships between SOC and FRC at 43 sites across the US National Ecological Observatory Network. We found that SOC and FRC stocks were positively related with an across-ecosystem slope of 7 ± 3 kg SOC m−2 per kg FRC m−2, but this relationship was driven by grasslands. Grasslands had double the across-ecosystem slope while forest FRC and SOC were unrelated. Furthermore, deep grassland soils primarily showed net SOC accrual relative to FRC input. Conversely, forests had high variability in whether FRC inputs were related to net SOC priming or accrual. We conclude that while FRC increases could lead to increased SOC in grasslands, especially at depth, the FRC-SOC relationship remains difficult to characterize in forests.
AB - Increasing fine root carbon (FRC) inputs into soils has been proposed as a solution to increasing soil organic carbon (SOC). However, FRC inputs can also enhance SOC loss through priming. Here, we tested the broad-scale relationships between SOC and FRC at 43 sites across the US National Ecological Observatory Network. We found that SOC and FRC stocks were positively related with an across-ecosystem slope of 7 ± 3 kg SOC m−2 per kg FRC m−2, but this relationship was driven by grasslands. Grasslands had double the across-ecosystem slope while forest FRC and SOC were unrelated. Furthermore, deep grassland soils primarily showed net SOC accrual relative to FRC input. Conversely, forests had high variability in whether FRC inputs were related to net SOC priming or accrual. We conclude that while FRC increases could lead to increased SOC in grasslands, especially at depth, the FRC-SOC relationship remains difficult to characterize in forests.
UR - https://www.scopus.com/pages/publications/105010034631
U2 - 10.1038/s43247-025-02486-9
DO - 10.1038/s43247-025-02486-9
M3 - Article
AN - SCOPUS:105010034631
VL - 6
JO - Communications Earth and Environment
JF - Communications Earth and Environment
IS - 1
M1 - 497
ER -