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        <identifier>oai:figshare.com:article/33990844</identifier>
        <datestamp>2026-09-24T20:16:29Z</datestamp>
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          <dc:title>Table 2_A 20% nitrogen reduction threshold optimizes soil carbon stability and microbial functional resilience under long-term straw return in a rice–wheat rotation.docx</dc:title>
          <dc:creator>Guohan Si (21684608)</dc:creator>
          <dc:creator>Huanqi Jiang (24868384)</dc:creator>
          <dc:creator>Chenglin Peng (21684605)</dc:creator>
          <dc:creator>Dabing Xu (18961138)</dc:creator>
          <dc:creator>Shujun Zhao (6541163)</dc:creator>
          <dc:subject>Microbiology</dc:subject>
          <dc:subject>aggregate stability</dc:subject>
          <dc:subject>carbon management index</dc:subject>
          <dc:subject>carbon sequestration</dc:subject>
          <dc:subject>metagenomics</dc:subject>
          <dc:subject>microbial carbon pump</dc:subject>
          <dc:subject>nitrogen reduction</dc:subject>
          <dc:subject>rice–wheat rotation</dc:subject>
          <dc:subject>soil organic carbon</dc:subject>
          <dc:description>&lt;p&gt;Reducing synthetic nitrogen (N) fertilizer while maintaining soil fertility and crop productivity is a major challenge for sustainable rice production. Straw return has been widely adopted to enhance soil organic carbon (SOC) sequestration; however, the mechanisms by which reduced N input interacts with straw return to regulate SOC stabilization remain poorly understood. Here we evaluated graded N reduction (0, 20, and 30%) under continuous straw return in a nine-year rice-wheat double-cropping experiment in central China. Soil carbon pools, aggregate stability, organic carbon functional groups, and microbial community structure and function were assessed using carbon fractionation, wet-sieving, FTIR spectroscopy, and metagenomic analyses. We found that 20% N reduction (80%NR) maintained grain yield comparable to conventional N fertilization while significantly increasing readily oxidizable organic carbon (ROOC, +18–26%), water-soluble organic carbon (WSOC, +12–21%), microbial biomass carbon (MBC, +15–24%), and carbon management index (CMI, +42–58% relative to NR). Moderate N reduction also enhanced macroaggregate-associated SOC and the relative abundance of aliphatic and aromatic carbon functional groups. Metagenomic analyses revealed that 80%NR enriched Firmicutes (+26%), Actinobacteria (+50%), and Nitrospira, reduced methanogenic archaea, and triggered a metabolic shift from CO oxidation (coxL/cutL, −15 to −22%) toward reductive carbon fixation via the Wood–Ljungdahl pathway (hdrA2, +6 to +19%). In contrast, 30% N reduction (70%NR) undermined subsurface aggregate stability and eroded microbial functional diversity, identifying 20% N reduction as an optimal threshold within the tested gradients. These findings provide a mechanistic basis for optimizing nitrogen management in sustainable rice production systems.&lt;/p&gt;</dc:description>
          <dc:date>2026-09-24T20:16:29Z</dc:date>
          <dc:type>Dataset</dc:type>
          <dc:type>Dataset</dc:type>
          <dc:identifier>10.3389/fmicb.2026.1928083.s002</dc:identifier>
          <dc:relation>https://figshare.com/articles/dataset/Table_2_A_20_nitrogen_reduction_threshold_optimizes_soil_carbon_stability_and_microbial_functional_resilience_under_long-term_straw_return_in_a_rice_wheat_rotation_docx/33990844</dc:relation>
          <dc:rights>CC BY 4.0</dc:rights>
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