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The microbial community size, structure, and process rates along natural gradients of soil salinity

机译:沿土壤盐度自然梯度的微生物群体规模,结构和工艺率

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Over 840 M ha of arable land is affected by salinization, and the area is predicted to increase due to global change. Assessments of the status of the microbial community in saline soils have frequently been based on microbial biomass estimates, which might not accurately reflect microbial process rates in soil. Moreover, assessments of how the relative importance of major decomposer groups bacteria and fungi are affected by salinity remain inconclusive. In this study we set out to assess the soil microbial community size, structure and process rates along two salinity gradients. To distinguish between the direct effects of high salinity and indirect effects resulting from reduced soil organic matter (OM) concentrations in saline soils we also assessed the gradients following plant litter amendments to compensate for differences in OM content between soils and isolate the effect of salinity. The research aims were to (i) investigate the microbial biomass responses to salinity as estimated based on both PLFA concentrations and qPCR measurements and to compare these responses to those of respiration and microbial growth, (ii) compare the responses of bacteria and fungi to increased salinity and (iii) assess the responses of these microbial variables to the alleviation of OM scarcity expected in saline soils. Microbial biomass estimates generally were less negatively affected by salinity than bacterial growth and respiration, and were not correlated to rates of microbial growth or respiration rates. While bacterial growth was strongly inhibited by salinity, fungal growth was similar in soils of all salinities, indicating a higher fungal tolerance to salinity. OM additions increased process rates in saline soils and alleviated some of the negative impact of salinity on respiration and growth. In conclusion, this study demonstrates differential responses of saprotrophic fungi and bacteria to increasing salinity and that bacteria are directly impacted by soil salinity while fungi are responding to the indirect effect by salinity related to reduced plant C input.
机译:超过840米HA的耕地受到盐渍化的影响,而且由于全球变化,该地区预计将增加。盐渍土壤中微生物群落状态的评估通常是基于微生物生物量估计,这可能无法准确反映土壤中的微生物过程率。此外,对主要分解组细菌和真菌的相对重要性的评估受盐度的影响仍然不确定。在这项研究中,我们开始评估土壤微生物群落规模,结构和工艺速率沿两个盐度梯度。区分盐水土壤中减少的土壤有机物质(OM)浓度导致的高盐度和间接效应的直接效应,我们还评估了植物凋落物修正后的梯度,以补偿土壤之间的OM含量的差异,并分离盐度的影响。研究目标是(i)研究微生物生物质对盐度的抑制,估计基于PLFA浓度和QPCR测量,并比较这些反应与呼吸和微生物生长,(ii)比较细菌和真菌的反应增加盐度和(iii)评估这些微生物变量对盐渍土壤中预期的呼应的反应。微生物生物量估计通常含有的盐度较小,而不是细菌生长和呼吸,并且与微生物生长或呼吸速率的速率无关。虽然通过盐度强烈抑制细菌生长,但所有薪水的土壤中的真菌生长相似,表明对盐度的更高的真菌耐受性。 OM添加了盐水土壤中的加​​工速率,并减轻了盐度对呼吸和生长的一些负面影响。总之,本研究证明了嗜血毛刺真菌和细菌对余处的差异反应,并且细菌直接受到土壤盐度的影响,而真菌正在响应与降低植物C输入的盐度的间接效果。

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