首页> 美国卫生研究院文献>Frontiers in Microbiology >Response of Biological Soil Crust Diazotrophs to Season Altered Summer Precipitation and Year-Round Increased Temperature in an Arid Grassland of the Colorado Plateau USA
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Response of Biological Soil Crust Diazotrophs to Season Altered Summer Precipitation and Year-Round Increased Temperature in an Arid Grassland of the Colorado Plateau USA

机译:美国科罗拉多高原干旱草原的生物土壤重氮细菌对季节夏季降水变化和全年升高的温度的响应

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摘要

Biological soil crusts (biocrusts), which supply significant amounts of fixed nitrogen into terrestrial ecosystems worldwide (∼33 Tg y−1), are likely to respond to changes in temperature and precipitation associated with climate change. Using nifH gene-based surveys, we explored variation in the diazotrophic community of biocrusts of the Colorado Plateau, USA in response to season (autumn vs. spring), as well as field manipulations that increased the frequency of small volume precipitation events and year-round soil temperature. Abundance of nifH genes in biocrusts ranged from 3 × 106 to 1 × 108 g−1 soil, and nifH from heterocystous cyanobacteria closely related to Scytonema hyalinum, Spirirestis rafaelensis, and Nostoc commune comprised >98% of the total. Although there was no apparent seasonal effect on total nifH gene abundance in the biocrusts, T-RFLP analysis revealed a strong seasonal pattern in nifH composition. Spirirestis nifH abundance was estimated to oscillate 1 to >2 orders of magnitude between autumn (low) and spring (high). A year-round increase of soil temperature (2–3°C) had little effect on the diazotroph community structure over 2 years. Altered summer precipitation had little impact on diazotroph community structure over the first 1.5 years of the study, when natural background patterns across years and seasons superseded any treatment effects. However, after the second summer of treatments, nifH abundance was 2.6-fold lower in biocrusts receiving altered precipitation. Heterocystous cyanobacteria were apparently more resilient to altered precipitation than other cyanobacteria. The results demonstrate that diazotrophic community composition of biocrusts in this semi-arid grassland undergoes strong seasonal shifts and that the abundance of its dominant members decreased in response to more frequent, small volume precipitation events.
机译:生物土壤结皮(生物结皮)可能为全球陆地生态系统提供大量的固定氮(〜33 Tg y -1 ),可能会响应与气候变化有关的温度和降水变化。使用基于nifH基因的调查,我们探索了美国科罗拉多高原生物重氮营养生物群落对季节(秋季对春季)的响应,以及田间操作增加了小量降水事件和年份的频率。圆形土壤温度。生物结皮中nifH基因的丰度范围从3×10 6 到1×10 8 g -1 土壤,与异囊蓝藻的nifH密切相关透明孢子虫,拉氏螺旋藻和诺斯托克公社占总数的98%以上。尽管对生物外壳中总的nifH基因丰度没有明显的季节性影响,但T-RFLP分析显示nifH组成具有很强的季节性模式。估计螺旋藻nifH的丰度在秋季(低)和春季(高)之间振荡1到> 2个数量级。全年土壤温度(2-3°C)的升高对重氮营养菌群落结构的影响不超过2年。在研究的前1.5年中,夏季降水的变化对重氮营养菌群落结构几乎没有影响,而跨年和跨季节的自然本底模式取代了任何治疗效果。然而,在第二个夏季的治疗后,接受沉淀变化的生物结皮中的nifH丰度降低了2.6倍。异质性蓝藻细菌显然比其他蓝藻细菌更能适应降水变化。结果表明,该半干旱草原生物结皮的重营养生物群落组成经历了强烈的季节性变化,其主要成员的丰度随着更频繁,更小数量的降水事件而下降。

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