Abstract
Purpose
Fire-induced changes in soil properties exert influence on soil processes, e.g., soil organic carbon (SOC) mineralization. The mineralization of organic substrates and soil priming effects in post-fire soils and the mechanisms involved remain elusive. This study aimed to investigate substrate mineralization with chemical recalcitrance gradient (sucrose, maize flour, and maize straw) and induced priming effects on forest soils after the fire.
Methods
Fire-burned forest soils (unburned as control) after 8 years were collected, and the physicochemical and biotic properties using high-throughput Illumina sequencing) were analyzed. Incubation of 42 days was conducted to investigate substrate decomposition and soil priming effects using the natural abundance 13C technique.
Results
The bacterial community in soil after the fire event had high diversity and was dominated by the phyla of Actinobacteria, Proteobacteria, and Acidobacteria. The addition of substrate to the burned soil had larger mineralization and caused higher soil priming effects than the control soil. Positive priming of SOC by substrate was most likely attributed to “co-metabolism,” indicated by the positive correlation between soil priming and sucrose mineralization.
Conclusion
The intensity of substrate mineralization and soil priming effects in the burned soil depended on fire shifting microbial community and substrate quality itself.
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Change history
27 July 2021
A Correction to this paper has been published: https://doi.org/10.1007/s11368-021-03029-3
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This study was supported by the National Natural Science Foundation of China (41761134095, 41671233).
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The original online version of this article was revised: In the original version of this article, the name of the 5th and 6th authors were incorrectly captured and should be changed to Peduruhewa H. Jeewani and Jianming Xu.
The original online version of this article was revised: In the original version of this article, the name of the 5th and 6th authors were incorrectly captured and should be changed to Peduruhewa H. Jeewani and Jianming Xu.
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Supplementary file1 Fig. S1 Cumulative Total CO2 (a), cumulative Substate derived CO2 (b) and Cumulative Primed soil CO2 (c) with the addition of three substrates during 42 days of incubation. B: burned soil, UB: unburned soil; S1: sucrose, S2: maize powder; S3: maize straw (DOCX 387 KB)
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Zhang, J., Ling, L., Singh, B.P. et al. Decomposition of substrates with recalcitrance gradient, primed CO2, and its relations with soil microbial diversity in post-fire forest soils. J Soils Sediments 21, 3007–3017 (2021). https://doi.org/10.1007/s11368-021-03003-z
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DOI: https://doi.org/10.1007/s11368-021-03003-z