気候を横断する土壌微生物ネクロマスの持続性における施肥と乾燥遺産の決定要因
Li-Xin Xu1, Guang-Hui Yu1, Cong-Qiang Liu1
1Institute of Surface-Earth System Science, School of Earth System Science, Tianjin Key Laboratory of Earth Critical Zone Science and Sustainable Development in Bohai Rim, Tianjin University, Tianjin, China.
Abstract:
Microbial necromass-mineral interactions are vital for soil organic carbon (C) persistence, but their response to concurrent climate and fertilization legacies in croplands remains unclear. Using six long-term field sites (27-38 years) across a pronounced aridity gradient, we show that stabilization of microbial necromass is coupled with short-range ordered (SRO) minerals in humid zones (aridity index, AI < 1.3). In arid zones (AI > 1.3), this correlation strongly weakens, challenging the universality of SRO-associated C paradigms. While aridity controls mineral weathering and SRO abundance, we showed that long-term fertilization can supersede aridity-driven constraints on necromass C accrual. Spatial mapping of 6060 in situ μ-FTIR spectra revealed reduced organic C transformation in outer aggregate rims under aridity, aligning with diminished microbial processing and a consequent weakening of necromass-SRO associations. Our findings establish soil moisture as a critical regulator of fertilization-induced ecological memory in mineral-necromass interactions, urging climate-tailored practices to sustain soil C resilience in water-limited ecosystems under global aridification.
さらに関連する動画
17:39A Lipid Extraction and Analysis Method for Characterizing Soil Microbes in Experiments with Many Samples
Published on: July 16, 2017
07:42Temperature Response of Soil Organic Matter Decomposition Rates: Construction and Applications of a Temperature Gradient Block
Published on: January 30, 2026
関連する概念動画
The Soil Ecosystem
Factors Influencing Microbial Growth: Temperature
The Roles of Bacteria and Fungi in Plant Nutrition
Diversity of Archaea III
Environmental Applications of Microorganisms
Diversity of Archaea I
