Important role of Fe oxides in global soil carbon stabilization and stocks

Iron (Fe) oxides can interact with soil organic carbon (SOC) to form Fe-bound organic carbon (OC-Fe), which strongly promotes SOC protection, mitigating global climate change. However, the global patterns and factors controlling OC-Fe are unclear. Here, we conducted a meta-analysis of 3,395 globally distributed soil profiles to reveal the role of Fe-Al oxides in global soil carbon stabilization and stocks. The global OC-Fe stock in topsoil is 233 PgC, accounting for 33 ± 15% of the total SOC stock. A substantial OC-Fe deficit (difference between OC-Fe and OC-Fe<sub>max</sub>) was observed at the equator and at mid-latitudes. Our findings suggest that mineral factors should be incorporated into soil carbon models to improve model predictions. Although there are uncertainties in current OC-Fe extraction method, the global distribution of OC-Fe and OC-Fe<sub>max</sub> constitutes a vital resource for future research targeting carbon cycling issues and offers innovative strategies for global soil carbon sequestration initiatives.

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Publication Details

Journal
Nature Communications
Published
2024-11-28
DOI
https://doi.org/10.1038/s41467-024-54832-8
Citations
99
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
33.04

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article

Important role of Fe oxides in global soil carbon stabilization and stocks

Mingyu Xie, Lei Li, Nan Jia, Hui Guo
99 citations
Nature Communications
Soil Carbon and Nitrogen Dynamics
33.04
article

Important role of Fe oxides in global soil carbon stabilization and stocks

Mingyu Xie, Lei Li, Nan Jia, Hui Guo
article en
99 citations

Abstract

Iron (Fe) oxides can interact with soil organic carbon (SOC) to form Fe-bound organic carbon (OC-Fe), which strongly promotes SOC protection, mitigating global climate change. However, the global patterns and factors controlling OC-Fe are unclear. Here, we conducted a meta-analysis of 3,395 globally distributed soil profiles to reveal the role of Fe-Al oxides in global soil carbon stabilization and stocks. The global OC-Fe stock in topsoil is 233 PgC, accounting for 33 ± 15% of the total SOC stock. A substantial OC-Fe deficit (difference between OC-Fe and OC-Fe<sub>max</sub>) was observed at the equator and at mid-latitudes. Our findings suggest that mineral factors should be incorporated into soil carbon models to improve model predictions. Although there are uncertainties in current OC-Fe extraction method, the global distribution of OC-Fe and OC-Fe<sub>max</sub> constitutes a vital resource for future research targeting carbon cycling issues and offers innovative strategies for global soil carbon sequestration initiatives.

Nature CommunicationsVol. 15(1)
Chinese Academy of Sciences (CN), North China University of Water Resources and Electric Power (CN), Institute of Ecology and Geography (MD), Xinjiang Institute of Ecology and Geography (CN), University of Chinese Academy of Sciences (CN), Bristol-Myers Squibb (Switzerland) (CH)
Natural Science Foundation of Xinjiang Province, National Natural Science Foundation of China, Chinese Academy of Sciences, Youth Innovation Promotion Association of the Chinese Academy of Sciences, Natural Science Foundation of Xinjiang, Youth Innovation Promotion Association
Zero hunger
Openalex Percentile: Top 0%
Soil Carbon and Nitrogen Dynamics
33.04
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