Abstract
Soil organic carbon is crucial for climate mitigation and agroecosystem sustainability, yet its depletion is concerning and its response to long-term fertilization remains unclear. Here we leverage the Broadbalk Classical Experiment at Rothamsted (UK), the world’s longest-running continuous winter wheat fertilization trial, along with 14C labelling, metagenomics and metabolomics to determine how 180 years of nitrogen (N) and phosphorus (P) fertilization impact soil organic carbon dynamics. Compared with no fertilization, long-term P, N and combined NP fertilization increased the soil organic carbon content by 10%, 22% and 28%, respectively. P application alone disproportionately increased microbial respiration (37%) and biomass (20%), limiting stable carbon formation and slightly increasing labile carbon. N application alone increased microbial carbon use and necromass accumulation efficiency, increasing mineral-associated carbon build-up. Combined NP fertilization enhanced plant-derived carbon inputs and the transformation of labile carbon into stable carbon, increasing soil organic carbon quantity and stability. A meta-analysis of the effects of fertilization duration on soil organic carbon revealed that N and P fertilization globally increased cropland soil organic carbon by 21% and 13%, and these promoting effects decreased before increasing after 16 and 34 years, respectively. Overall, long-term mineral fertilization can effectively enhance soil carbon sequestration.
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Data availability
All data generated and analysed during this study are available via Figshare at https://doi.org/10.6084/m9.figshare.28792301 (ref. 64). Sequencing data have been archived and are publicly accessible via the National Center for Biotechnology Information (NCBI) database under project number PRJNA1071733. Source data are provided with this paper.
Code availability
All code used in this study has been archived and is available via Code Ocean https://codeocean.com/capsule/2397954/tree/v1 (ref. 65).
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Acknowledgements
This work was supported by the National Key R&D Program of China (2023YFD2302200, 2023YFD1900601), National Natural Science Foundation of China (32402680, 32172674, U24A20575), Zhejiang Provincial Natural Science Foundation (LZ23C150002), Smart Fertilization Project (05) and the Rothamsted Long-Term Experiments National Bioscience Research Infrastructure (RLTE-NBRI), supported by the UK Research and Innovation Biotechnology and Biological Sciences Research Council (UKRI-BBSRC) under award number BBS/E/RH/23NB0007 (2023–2028) and the Lawes Agricultural Trust. We also thank the curators of the Electronic Rothamsted Archive (e-RA) for providing access to data from the Rothamsted Long-Term Experiments.
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S.T., L.W. and Q.M. contributed to conceptualization, methodology, formal analysis and writing—original draft. Y.Y., Z.L. and G.L. contributed to writing—review and editing. W.W., K.A.M., Y.K. and D.L.J. contributed to writing—original draft. A.S.G., D.R.C., W.P. and D.L.J. contributed to investigation. K.A.M. and D.R.C. also contributed to methodology and conceptualization. Y.L. contributed to conceptualization and writing—review and editing. D.L.J. supervised the study and acquired funding.
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Nature Geoscience thanks Kate Lajtha and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editors: Camilla Brunello, Xujia Jiang and Carolina Ortiz Guerrero, in collaboration with the Nature Geoscience team.
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Extended data
Extended Data Fig. 1 Global trends in nitrogen (N) and phosphorus (P2O5) fertilizer consumption since 1961.
a-c, Annual consumption rates of N (a), P2O5 (b), and combined N + P2O5 (c) fertilizers in China, India, the United Kingdom, and the United States. Data source: FAOSTAT (Food and Agriculture Organization of the United Nations, https://www.fao.org/faostat/en/#data/RFN).
Extended Data Fig. 2 Effects of long-term N and P fertilization on soil organic matter, amino sugars, and microbial necromass contents.
a, Soil organic matter. b, Muramic acid (MurN). c, Galactosamine (GalN). d, Glucosamine (GluN). e, Bacterial necromass C. f, Fungal necromass C. g, The ratio of bacterial to fungal necromass C. Box plots represent first and third quartiles (box), medians (central horizontal line), largest value smaller than 1.5 times the interquartile range (upper vertical line) and smallest value larger than 1.5 times the interquartile range (lower vertical line). Different letters above boxes indicate statistically significant differences among treatments (n = 4), determined using one-way ANOVA followed by Tukey’s post hoc test (two-sided; p < 0.05). Nil, no fertilization; P, P-only fertilization; N, N-only fertilization; NP, combined fertilization with N and P.
Extended Data Fig. 3 Variation in δ13C abundance and relationships between microbial necromass C and microbial C use efficiency and biomass C.
a, Linear relationship between microbial necromass C and microbial C use efficiency. b, Linear relationship between microbial necromass C and microbial biomass C. c, Box plots showing δ¹³C values of soil organic matter under four fertilization treatments: Nil (unfertilized control), N (nitrogen), P (phosphorus), and NP (combined N and P). Box plots represent first and third quartiles (box), medians (central horizontal line), largest value smaller than 1.5 times the interquartile range (upper vertical line) and smallest value larger than 1.5 times the interquartile range (lower vertical line). Different letters above boxes indicate statistically significant differences among treatments (n = 4), determined using one-way ANOVA followed by Tukey’s post hoc test (two-sided; p < 0.05). d, Linear relationship between soil δ13C and SOC content across all treatments. Solid line indicates the fitted linear regression; the shaded area represents the 95% confidence interval.
Extended Data Fig. 4 Metabolic responses to long-term N and P fertilization.
a, Heatmap of soil metabolite z-scores across fertilization regimes. Color gradient (red to blue) indicates metabolite concentrations standardized to the mean (scale bar: −2 to +2 standard deviations). b, Principal component analysis (PCA) of metabolite profiles, showing treatment-specific clustering (95% confidence ellipses). Treatment effects were tested by permutational multivariate analysis of variance (PERMANOVA) with multiple comparisons (p < 0.001, Benjamini–Hochberg corrected). Axes indicate percentage variance explained by each component. c, Comparative analysis of the abundances of differentially expressed metabolites under each fertilization treatment, with numbers in blue and red representing the number of significantly (two-sided t-test, FDR corrected, p < 0.05) decreased and increased metabolites between treatments, respectively. Nil, no fertilizer application; P, P-only fertilization; N, N-only fertilization; NP, combined fertilization with N and P.
Extended Data Fig. 5 Effects of long-term N and P fertilization on microbial community diversity, composition, and structure.
a, Archaeal α-diversity (Shannon index), community structure (non-metric multidimensional scaling, NMDS based on Bray–Curtis dissimilarities), and taxonomic composition under four fertilization treatments: Nil (no fertilizer), P (phosphorus fertilization), N (nitrogen fertilization), and NP (combined N and P fertilization). b, Bacterial community. c, Fungal community. Box plots represent first and third quartiles (box), medians (central horizontal line), largest value smaller than 1.5 times the interquartile range (upper vertical line) and smallest value larger than 1.5 times the interquartile range (lower vertical line). Different letters above boxes indicate statistically significant differences among treatments (n = 4), determined using one-way ANOVA followed by Tukey’s post hoc test (two-sided; p < 0.05). Different lowercase letters indicate significant differences (p < 0.05) between fertilization treatments. Asterisks in NMDS plots indicate significant differences in microbial community structure between treatments based on PERMANOVA, with p-values adjusted using the Benjamini–Hochberg method (FDR corrected, p < 0.05). Shaded areas in NMDS plots represent 95% confidence intervals for each treatment group.
Extended Data Fig. 6 Partial least squares path modelling (PLS-PM) of fertilization effects on SOC.
a, Pathways of fertilization effects on SOC. Arrow colors indicate effect direction (blue: positive, red: negative). Path coefficients are shown adjacent to arrows (standardized values). Significance was assessed via bootstrapping (1000 iterations). *p < 0.05, **p < 0.01, ***p < 0.001. b, Standardized total effects of factors on SOC.
Extended Data Fig. 7 Drivers of soil carbon pool variation: N and P contributions.
a, Random Forest analysis quantifying the relative importance of soil N and P fractions in explaining C pool variability. b, Pearson correlations combined with Random forest analysis between soil N, soil P and soil C contents. Colors indicate correlation direction (red: positive; blue: negative). Circle size represents variable importance in Random Forest analysis (larger circles = higher importance). *p < 0.05, **p < 0.01, ***p < 0.001. BN: bacterial necromass; FN: fungal necromass; TN: total necromass; POC: particulate organic C; MAOC: mineral-associated organic C; SOC: soil organic C; SOM: soil organic matter; DOC: dissolved organic C. c, Variation partitioning via redundancy analysis quantifying unique and shared explanatory power of N and P.
Extended Data Fig. 8 PRISMA-flowchart: observational meta-analysis.
a, Nitrogen fertilization. b, Phosphorus fertilization.
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Tang, S., Pan, W., Yang, Y. et al. Soil carbon sequestration enhanced by long-term nitrogen and phosphorus fertilization. Nat. Geosci. (2025). https://doi.org/10.1038/s41561-025-01789-y
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DOI: https://doi.org/10.1038/s41561-025-01789-y