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Seasonal microbial and nutrient responses during a 5-year reduction in the daily temperature range of soil in a Chihuahuan Desert ecosystem
- van Gestel, Natasja C., Dhungana, Nirmala, Tissue, David T., Zak, John C.
- Oecologia 2016 v.180 no.1 pp. 265-277
- ammonium nitrogen, biomass production, carbon, dissolved organic carbon, ecosystems, field experimentation, heat, microbial biomass, nitrate nitrogen, nitrogen, nitrogen fixation, soil microorganisms, soil organic matter, soil respiration, soil temperature, soil water, spring, summer, Chihuahuan Desert
- High daily temperature range of soil (DTRₛₒᵢₗ) negatively affects soil microbial biomass and activity, but its interaction with seasonal soil moisture in regulating ecosystem function remains unclear. For our 5-year field study in the Chihuahuan Desert, we suspended shade cloth 15 cm above the soil surface to reduce daytime temperature and increase nighttime soil temperature compared to unshaded plots, thereby reducing DTRₛₒᵢₗ (by 5 ºC at 0.2 cm depth) without altering mean temperatures. Microbial biomass production was primarily regulated by seasonal precipitation with the magnitude of the response dependent on DTRₛₒᵢₗ. Reduced DTRₛₒᵢₗ more consistently increased microbial biomass nitrogen (MBN; +38 %) than microbial biomass carbon (MBC) with treatment responses being similar in spring and summer. Soil respiration depended primarily on soil moisture with responses to reduced DTRₛₒᵢₗ evident only in wetter summer soils (+53 %) and not in dry spring soils. Reduced DTRₛₒᵢₗ had no effect on concentrations of dissolved organic C, soil organic matter (SOM), nor soil inorganic N (extractable NO₃ ⁻–N + NH₄ ⁺–N). Higher MBN without changes in soil inorganic N suggests faster N cycling rates or alternate sources of N. If N cycling rates increased without a change to external N inputs (atmospheric N deposition or N fixation), then productivity in this desert system, which is N-poor and low in SOM, could be negatively impacted with continued decreases in daily temperature range. Thus, the future N balance in arid ecosystems, under conditions of lower DTR, seems linked to future precipitation regimes through N deposition and regulation of soil heat load dynamics.