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首页> 外文期刊>Biology and Fertility of Soils >Seasonal patterns of root-surface phosphatase activities in a Mediterranean shrubland. Responses to experimental warming and drought
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Seasonal patterns of root-surface phosphatase activities in a Mediterranean shrubland. Responses to experimental warming and drought

机译:地中海灌木丛中根表面磷酸酶活性的季节性模式。对实验性变暖和干旱的反应

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摘要

Mediterranean ecosystems are water limited and the current general circulation Models (GCM) and ecophysiological models forecast a warming and a further increase of drought in the next decades. A stronger water stress can decrease the capacity for nutrient absorption by plants. We conducted a field experiment to simulate forecasted drought and warming in a Mediterranean calcareous shrubland to assess the performance of root-surface phosphatase activities of the dominant shrub Globularia alypum. These enzyme activities were higher in autumn and spring, when the climate conditions were optimal for plant activity, than in summer or winter, when there was either lack of water or cold temperatures. A decrease in soil moisture in drought plots decreased root-surface phosphatase activity (29% in summer and 25% in autumn). The decrease in root-surface phosphatase activity in drought plots coincided with a decrease in P leaf concentrations and P accumulation in aboveground biomass and loss of photosynthetic capacity of some dominant shrub species of this ecosystem, and with a tendency to increase total soil-P. These results suggest that the expected drier conditions in this Mediterranean shrubland in the next decades will slow down the P uptake by plants, thereby, diminishing the P contents in biomass and increasing total P contents in soil in non-available forms and that this can be, in part, attributable to a result of the decrease in root-surface phosphatase activity.
机译:地中海生态系统缺水,目前的一般循环模型(GCM)和生态生理模型预测,未来几十年气候变暖,干旱进一步加剧。较强的水分胁迫会降低植物吸收养分的能力。我们进行了野外实验,以模拟地中海钙质灌木丛中的预测干旱和变暖,以评估优势灌木globularia alypum根表面磷酸酶活性的表现。在气候条件最适合植物活动的秋季和春季,这些酶的活性高于缺水或低温的夏季或冬季。干旱区土壤水分的减少会降低根表面磷酸酶的活性(夏季为29%,秋季为25%)。干旱区根表面磷酸酶活性的下降与该生态系统中一些主要灌木物种的磷叶浓度和磷累积下降,地上生物量磷积累下降以及光合能力丧失以及土壤总磷增加的趋势相吻合。这些结果表明,在未来几十年中,该地中海灌木丛中预期的较干燥条件将减缓植物对P的吸收,从而减少生物量中的P含量并增加土壤中非有效形式的P总量,这可能是,部分归因于根表面磷酸酶活性降低的结果。

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