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首页> 外文期刊>Global change biology >Soil-nutrient availability under a global-change scenario in a Mediterranean mountain ecosystem.
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Soil-nutrient availability under a global-change scenario in a Mediterranean mountain ecosystem.

机译:地中海山区生态系统在全球变化情况下的土壤养分有效性。

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Changes in rainfall availability will alter soil-nutrient availability under a climate-change scenario. However, studies have usually analyzed the effect of either drier or wetter soil conditions, despite the fact that both possibilities will coexist in many climatic regions of the world. Furthermore, its effect may vary across the different habitats of the ecosystem. We experimentally investigated the effect of three contrasting climatic scenarios on different carbon (C), nitrogen (N), and phosphorus (P) fractions in soil and microbial compartments among three characteristic habitats in a Mediterranean-type ecosystem: forest, shrubland, and open areas. The climatic scenarios were dry summers, according to the 30% summer rainfall reduction projected in the Mediterranean; wet summer, simulating summer storms to reach the maximum historical records in the study area; and current climatic conditions (control). Sampling was replicated during two seasons (spring and summer) and 2 years. The climatic scenario did not affect the nutrient content in the litter layer. However, soil and microbial nutrients varied among seasons, habitats, and climatic scenarios. Soil-nutrient fractions increased with lower soil-moisture conditions (dry scenario and summer), whereas microbial nutrients increased under the wet summer scenario and spring. This pattern was consistent both studied years, although it was modulated by habitat, differences being lower with denser plant cover. Holm oak seedlings, used as live control of the experiment, tended to increase their N and P content (although not significantly) with water availability. Thus, the results support the idea that higher rainfall boosts microbial and plant-nutrient uptake, and hence nutrient cycling. By contrast, a rainfall reduction leads to an accumulation of nutrients in the soil, increasing the risk of nutrient loss by leaching or erosion. These results show that the projected climate change will have significant effects on nutrient cycles, and therefore will have important implications on the ecosystem functioning.
机译:在气候变化的情况下,降雨供应的变化将改变土壤养分的供应。然而,尽管事实上这两种可能性将在世界许多气候地区共存,但研究通常分析了干燥或潮湿土壤条件的影响。此外,其影响可能在生态系统的不同生境中有所不同。我们通过实验研究了三种不同气候情景对地中海型生态系统(森林,灌木丛和开阔地域)三个特征生境之间土壤和微生物区隔中不同碳(C),氮(N)和磷(P)部分的影响。地区。根据地中海地区预计的夏季降雨量减少30%的预测,气候情景是夏季干燥。夏季潮湿,模拟夏季风暴达到研究区域的最大历史记录;和当前的气候条件(控制)。在两个季节(春季和夏季)和两年中重复采样。气候情况不影响垫料层中的养分含量。但是,土壤和微生物养分随季节,生境和气候情景而变化。土壤养分含量随土壤湿度降低(干旱和夏季)而增加,而微生物养分在夏季潮湿和春季时增加。尽管受栖息地的影响,但这种模式在两个研究年中都是一致的,但随着植物覆盖的增加,差异变小。霍尔姆橡树幼苗用作实验的现场对照,随着水的可用性,它们的N和P含量趋于增加(尽管不显着)。因此,结果支持这样的想法,即较高的降雨会促进微生物和植物养分的吸收,从而促进养分循环。相反,减少降雨会导致土壤中养分的积累,从而增加因淋溶或侵蚀造成养分流失的风险。这些结果表明,预计的气候变化将对养分循环产生重大影响,因此将对生态系统功能产生重要影响。

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