Mapping global distributions, environmental controls, and uncertainties of apparent topsoil and subsoil organic carbon turnover times

Abstract. The turnover time (τ) of global soil organic carbon is central to the functioning of terrestrial ecosystems. Yet our spatially explicit understanding of the depth-dependent variations and environmental controls of τ at a global scale remains incomplete. In this study, we combine multiple state-of-the-art observation-based datasets, including over 90 000 geo-referenced soil profiles, the latest root observations distributed globally, and large numbers of satellite-derived environmental variables, to generate global maps of apparent τ in topsoil (0–0.3 m) and subsoil (0.3–1 m) layers, with a spatial resolution of 30 arcsec (∼1 km at the Equator). We show that subsoil τ (385203485 years (mean, with a variation range from the 2.5th to 97.5th percentile)) is over 8 times longer than topsoil τ (1511137 years). The cross-validation shows that the fitted machine learning models effectively captured the variabilities in τ, with R2 values of 0.87 and 0.70 for topsoil and subsoil τ mapping, respectively. The prediction uncertainties of the τ maps were quantified for better user applications. The environmental controls on topsoil and subsoil τ were investigated at global, biome, and local scales. Our analyses illustrate the ways in which temperature, water availability, physio-chemical properties, and depth jointly exert impacts on τ. The data-driven approaches allow us to identify their interactions, thereby enriching our comprehension of mechanisms driving nonlinear τ–environment relationships at global to local scales. The distributions of dominating factors of τ at local scales were mapped for purposes of identifying context-dependent controls on τ across different regions. We further reveal that the current Earth system models may underestimate τ by comparing model-derived maps with our observation-derived τ maps. The resulting maps, with new insights, as demonstrated in this study, will facilitate future modelling efforts relating to carbon cycle–climate feedbacks and support effective carbon management. The dataset is archived and freely available at https://doi.org/10.5281/zenodo.14560239 (Zhang, 2025a).

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Publication Details

Journal
Earth system science data
Published
2025-06-16
DOI
https://doi.org/10.5194/essd-17-2605-2025
Citations
3
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
3.90

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article

Mapping global distributions, environmental controls, and uncertainties of apparent topsoil and subsoil organic carbon turnover times

G.B.M. Heuvelink, Lin Yang, Sebastian Döetterl, Lei Zhang et al.
3 citations
Earth system science data
Climate change and permafrost
3.90
article

Mapping global distributions, environmental controls, and uncertainties of apparent topsoil and subsoil organic carbon turnover times

G.B.M. Heuvelink, Lin Yang, Sebastian Döetterl, Lei Zhang, Yibiao Zou, Chenghu Zhou, Constantin M. Zohner, A‐Xing Zhu, Feixue Shen, Thomas Ward Crowther, Haozhi Ma, Alexandre M.J.‐C. Wadoux, Yue Pu
article en
3 citations

Abstract

Abstract. The turnover time (τ) of global soil organic carbon is central to the functioning of terrestrial ecosystems. Yet our spatially explicit understanding of the depth-dependent variations and environmental controls of τ at a global scale remains incomplete. In this study, we combine multiple state-of-the-art observation-based datasets, including over 90 000 geo-referenced soil profiles, the latest root observations distributed globally, and large numbers of satellite-derived environmental variables, to generate global maps of apparent τ in topsoil (0–0.3 m) and subsoil (0.3–1 m) layers, with a spatial resolution of 30 arcsec (∼1 km at the Equator). We show that subsoil τ (385203485 years (mean, with a variation range from the 2.5th to 97.5th percentile)) is over 8 times longer than topsoil τ (1511137 years). The cross-validation shows that the fitted machine learning models effectively captured the variabilities in τ, with R2 values of 0.87 and 0.70 for topsoil and subsoil τ mapping, respectively. The prediction uncertainties of the τ maps were quantified for better user applications. The environmental controls on topsoil and subsoil τ were investigated at global, biome, and local scales. Our analyses illustrate the ways in which temperature, water availability, physio-chemical properties, and depth jointly exert impacts on τ. The data-driven approaches allow us to identify their interactions, thereby enriching our comprehension of mechanisms driving nonlinear τ–environment relationships at global to local scales. The distributions of dominating factors of τ at local scales were mapped for purposes of identifying context-dependent controls on τ across different regions. We further reveal that the current Earth system models may underestimate τ by comparing model-derived maps with our observation-derived τ maps. The resulting maps, with new insights, as demonstrated in this study, will facilitate future modelling efforts relating to carbon cycle–climate feedbacks and support effective carbon management. The dataset is archived and freely available at https://doi.org/10.5281/zenodo.14560239 (Zhang, 2025a).

Earth system science dataVol. 17(6)
University of Wisconsin–Madison (US), Lawrence Berkeley National Laboratory (US), Chinese Academy of Sciences (CN), AgroParisTech (FR), Swiss Federal Institute for Forest, Snow and Landscape Research (CH), ISRIC - World Soil Information (NL), ETH Zurich (CH), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Institut Agro Montpelier (FR), Institute of Geographic Sciences and Natural Resources Research (CN), Institut de Recherche pour le Développement (FR), Nanjing University (CN), Wageningen University & Research (NL)
U.S. Department of Energy, National Natural Science Foundation of China, Nanjing University, Wageningen University and Research, Fundamental Research Funds for the Central Universities
Openalex Percentile: Top 7%
Climate change and permafrost
3.90
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