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首页> 外文期刊>Ecological research >Variation in leaf nitrogen and phosphorus stoichiometry in the nitrogen-fixing Chinese sea-buckthorn (Hippophae rhamnoides L. subsp. sinensis Rousi) across northern China
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Variation in leaf nitrogen and phosphorus stoichiometry in the nitrogen-fixing Chinese sea-buckthorn (Hippophae rhamnoides L. subsp. sinensis Rousi) across northern China

机译:中国北方固氮沙棘(沙棘)中叶​​氮和磷化学计量的变化

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Nitrogen (N) and phosphorus (P) concentrations and N:P ratios in terrestrial plants and their patterns of change along environmental gradients are important traits for plant adaptation to changes. We determined the leaf N and P concentrations of Chinese sea-buckthorn (Hippophae rhamnoides L. subsp. sinensis Rousi), a non-legume species with symbiotic N fixation (SNF), at 37 sites across northern China and explored their geographical patterns in relation to climate and soil factors. (1) The mean leaf N, P, and N:P ratio were 36.5, 2.1 mg g~(-1), and 17.6, respectively, higher than the mean values of most shrub species in the region. (2) Leaf N was correlated with soil mineral N in cool areas (mean annual temperature MAT < 3 ℃) but with temperature in warm areas (MAT > 3 ℃). The high leaf N and divergent leaf N-soil N relationship suggested the importance of SNF in plant N uptake; SNF increases with temperature and is probably the major N source in warm areas. (3) Leaf P was positively related to mean annual precipitation. Leaf N:P ratio was primarily driven by changes in leaf P. The high leaf P reflected the greater requirements of the N-fixing species for P. Our results represent a major advance in understanding the elemental stoichiometry of non-legume N-fixing plants, indicating high P and N requirements and a shift in N source from SNF to soil as temperature declines. This knowledge will help in assessing the habitat suitability for the species and predicting the species dynamics under environmental changes.
机译:陆生植物中氮(N)和磷(P)的浓度以及N:P的比例及其沿环境梯度的变化模式是植物适应变化的重要特征。我们在中国北方的37个站点上确定了具有共生固氮(SNF)的非豆科植物沙棘(Sippoensis Rousi)的叶N和P浓度,并探讨了它们的地理分布受气候和土壤因素影响。 (1)平均叶片氮,磷和氮:磷比分别为36.5、2.1 mg g〜(-1)和17.6,高于该地区大多数灌木物种的平均值。 (2)在凉爽地区(平均气温MAT <3℃),叶片氮与土壤矿质氮相关,而在温暖地区(MAT> 3℃),叶片氮与土壤矿质氮相关。高叶氮和发散叶氮-土壤氮的关系表明SNF在植物吸收氮中的重要性。 SNF随温度升高而增加,可能是温暖地区的主要氮源。 (3)叶片P与年平均降水量呈正相关。叶片N:P的比例主要由叶片P的变化决定。较高的叶片P反映了固氮菌对磷的更高要求。我们的结果代表了对非豆科固氮植物元素化学计量的重大进步。 ,表明对磷和氮的需求较高,并且随着温度下降,氮源从SNF转移到土壤。这些知识将有助于评估物种对栖息地的适应性,并预测环境变化下物种的动态。

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