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首页> 外文期刊>Frontiers of earth science >Moisture and temperature controls on nitrification differ among ammonia oxidizer communities from three alpine soil habitats
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Moisture and temperature controls on nitrification differ among ammonia oxidizer communities from three alpine soil habitats

机译:来自三个高山土壤生境的氨氧化剂群落之间的硝化水分和温度控制有所不同

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摘要

Climate change is altering the timing and magnitude of biogeochemical fluxes in many high-elevation ecosystems. The consequent changes in alpine nitrification rates have the potential to influence ecosystem scale responses. In order to better understand how changing temperature and moisture conditions may influence ammonia oxidizers and nitrification activity, we conducted laboratory incubations on soils collected in a Colorado watershed from three alpine habitats (glacial outwash, talus, and meadow). We found that bacteria, not archaea, dominated all ammonia oxidizer communities. Nitrification increased with moisture in all soils and under all temperature treatments. However, temperature was not correlated with nitrification rates in all soils. Site-specific temperature trends suggest the development of generalist ammonia oxidzer communities in soils with greater in situ temperature fluctuations and specialists in soils with more steady temperature regimes. Rapidly increasing temperatures and changing soil moisture conditions could explain recent observations of increased nitrate production in some alpine soils.
机译:气候变化正在改变许多高海拔生态系统中生物地球化学通量的时间和大小。高山硝化速率的随之变化可能会影响生态系统规模的响应。为了更好地了解不断变化的温度和湿度条件可能如何影响氨氧化剂和硝化活性,我们在科罗拉多流域从三个高山生境(冰川冲积,距骨和草甸)收集的土壤上进行了实验室培养。我们发现细菌而不是古细菌占主导地位的所有氨氧化剂社区。在所有土壤和所有温度处理下,硝化作用都随着水分的增加而增加。但是,温度与所有土壤的硝化率均不相关。特定地点的温度趋势表明,在原位温度波动较大的土壤中发展了多用途氨氧化器群落,而在温度制度更为稳定的土壤中则发展了专家。温度的快速升高和土壤湿度条件的变化可能解释了最近在某些高山土壤中硝酸盐产量增加的观察结果。

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