Search

Paddy soil experiences repeated anaerobic and aerobic changes during rice growth, the dramatic dynamics of soil water status accompanied by changes in redox condition and O availability. However, the effect of rapid water status change on soil microbial biomass and community composition is not well explored. Here, we present a comprehensive study focusing on the short-term water status change in 13 Chinese paddy soils. In order to gain a reliable way to determine soil microbial biomass carbon (MBC) in flooded or water-saturated soils, we also evaluated two different procedures (nitrogen bubbled and 100 °C water bath) to remove chloroform in extracts during the fumigation process. Compared to non-flooded paddy soils, the flooded paddy soils tended to have a lower microbial biomass, and this was much clearer using adenosine 5′-triphosphate (ATP) and phospholipid fatty acid (PLFA) analysis compared to biomass measured by the fumigation method. Fungal biomass, which was indicated by both ergosterol and the PLFA 18:2ω6,9c, also decreased after short-term flooding. Changes in soil microbial community composition (determined by PLFA biomarkers) were observed after short-term flooding, but the extent varied between soils. This study indicates that the dynamics of short-term water status altered the soil microbial biomass (ATP, MBC, and total PLFA) and community composition. Finally, our results suggested that liquid fumigation combined with the nitrogen-bubbled method is the best choice for analyzing MBC concentrations in water-saturated soils. [ABSTRACT FROM AUTHOR]

• Temperature and ferrihydrite jointly influence soil methanogenesis. • Raising temperature had a significant ability to enhance Fe reduction. • Fe reduction mediates the coexistence patterns of methanogens. • Temperate paddy soil exhibit higher Q 10 than subtropical paddy soil. Microbial methanogenesis in paddy soils contributes approximately one-fifth of global anthropogenic methane (CH 4) release, creating severe negative climate feedback. The dynamics of iron oxides in flooded paddy fields, as well as temperature changes, have an impact on CH 4 production. However, the relationship between the two, as well as their interactive mechanisms in influencing CH 4 production and microbial communities in paddy soils, is not yet clear. Therefore, we investigated the interactive effects of temperature (15, 25 and 35 °C) and iron oxide (ferrihydrite) on CH 4 production and methanogenic community structure in two Chinese paddy soils, one subtropical and one temperate. We characterized shifts in microbial communities using high-throughput sequencing of bacteria, archaea and methanogenic mcrA genes following an anaerobic incubation for 90 days. Our results showed that temperature significantly promoted Fe reduction in paddy soils, and both together regulated CH 4 production by reducing the number of methanogens. Additionally, the temperature sensitivity of methanogenesis was higher in the temperate than in the subtropical paddy soil. We also demonstrated that ferrihydrite can inhibit methanogenesis by reducing the relative abundance of Methanosarcinales and altering the community patterns of methanogens in these paddy soils. Likewise, increases in temperature changes the relative abundance of Methanosarcinales and Methanobacteriales, promoting methanogenesis. Overall, our results provide new insights into the role of iron oxides and temperature in regulating greenhouse gas emissions from paddy soils. [ABSTRACT FROM AUTHOR]