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Biological soil crusts modulate nitrogen availability in semi-arid ecosystems: insights from a Mediterranean grassland

机译:生物土壤结皮调节半干旱生态系统中的氮素利用率:来自地中海草原的见解

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Biological soil crusts (BSCs) greatly influence the N cycle of semi-arid ecosystems, as some organisms forming them are able to fix atmospheric N. However, BSCs are not always taken into account when studying biotic controls on N cycling and transformations. Our main objective was to understand how BSCs modulate the availability of N in a semi-arid Mediterranean ecosystem dominated by the tussock grass Stipa tenacissima. We selected the six most frequent soil cover types in the study area: S. tenacissima tussocks (ST), Retama sphaerocarpa shrubs (RS), and open areas with very low (BS), low (LC) medium (MC) and high (HC) cover of well developed and lichen-dominated BSCs. The temporal dynamics of available N dynamics followed changes in soil moisture. Available NH -N did not differ between microsites, while available NO -N was substantially higher in the RS than in any other microsite. No significant differences in the amount of available NO -N were found between ST and BS microsites, but these microsites had more NO -N than those dominated by BSCs (LC, MC and HC). Our results suggest that BSCs may be inhibiting nitrification, and highlight the importance of this biotic community as a modulator of the availability of N in semi-arid ecosystems.
机译:生物土壤结壳(BSC)极大地影响了半干旱生态系统的N循环,因为形成它们的某些生物能够固定大气中的N。但是,在研究有关N循环和转化的生物控制时,并不总是考虑BSC。我们的主要目标是了解BSC如何在以草丛草Stipa tenacissima为主的半干旱地中海生态系统中调节N的有效性。我们在研究区域中选择了六种最常见的土壤覆盖类型:S。tenacissima丛生草(ST),Retama sphaerocarpa灌木(RS)以及低(BS),低(LC)中(MC)和高( HC)涵盖了发达且以地衣为主的BSC。可利用的N动态的时间动态跟随土壤水分的变化。微型站点之间的可用NH -N没有差异,而RS中可用的NO -N显着高于其他任何微型站点。 ST和BS微站点之间的可用NO -N量没有显着差异,但是这些微站点的NO -N比BSC(LC,MC和HC)为主。我们的结果表明BSC可能正在抑制硝化作用,并突出了这种生物群落作为调节半干旱生态系统中N有效性的重要意义。

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