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A multi-scale investigation of species richness, productivity and nutrient relationships in herbaceous plant communities of the grasslands of Southern Interior British Columbia

机译:不列颠哥伦比亚省南部内陆草原草本植物群落物种丰富度,生产力和养分关系的多尺度研究

摘要

Philip Grime's humped-back model predicts that species richness reaches a maximum at intermediate productivity and drops off at low and high productivities. Soil nutrient availability is known to influence primary productivity and plant species richness. In general, productivity increases with increasing soil nutrient availability, and experiments that increase soil nutrients often show increases in biomass with corresponding decreases in species richness; as such, certain patterns in soil nutrients are expected to coincide with the humped-back model. Scale is also an important factor, as the relationship between species richness and productivity may vary with scale. Objectives of this work were (1) to test the explicit humped-back model prediction that the relationship between species richness and productivity is unimodal; (2) to test implicit humped-back model predictions that species richness is related to nutrients that are tightly associated with productivity, such as carbon and nitrogen, by a unimodal relationship and identify patterns between soil nutrients, leaf nutrients, productivity and species richness; and (3) to evaluate the influence of increasing scales from 1 m2 to 64 m2 on relationships found between species richness, productivity and nutrients. This was done using biomass and litter collections and species richness counts from 14 multi-scale grids (8 m × 8 m grids containing 64, 1 m2 plots), soil samples from a subset of four of the 14 multi-scale grids, and leaf samples from a subset of nine adjacent plots in each of the four multi-scale grids that were sampled for soil nutrients. Total carbon and nitrogen contents in soil and leaf samples were analyzed with a CE-440 Elemental Analyzer. Total aluminum, boron, calcium, copper, iron, magnesium, manganese, sodium, phosphorus, potassium, sulphur, and zinc were quantified in soil samples prepared by very high-pressure closed vessel microwave acid digestion in a Milestone “Ultrawave” single reaction chamber followed by analysis with a Teledyne/Leeman Labs “Prodigy” dual view inductively coupled plasma-optical emission spectrometer. In principal component analyses of soil nutrient data, the first and second principal components appeared to represent productivity and species richness, respectively; and carbon, nitrogen, phosphorus, potassium, boron, iron, magnesium and manganese were identified as important soil nutrients. Bivariate regressions of the first principal component with total biomass (R2 = 0.76) and the second principal component with species richness (R2 = 0.35) returned strong R2 values. Species richness was related to total biomass (R2 = 0.11), soil carbon (R2 = 0.15), soil nitrogen (R2 = 0.14) and iron (R2 = 0.29) by concave down relationships, to boron (R2 = 0.17) and magnesium (R2 = 0.49) by concave up relationships, to phosphorus (R2 = 0.27) and manganese (R2 = 0.25) by positive linear relationships and to potassium (R2 = 0.14) by a negative linear relationship. Scaling results were inconclusive but suggested that patterns in the literature may be partly due to sample size. Results generally support the humped-back model and that nutrient availability is an important factor correlated with herbaceous plant productivity and species richness. Nutrient availability is likely an important driver of plant productivity and herbaceous plant diversity.
机译:菲利普·格里姆(Philip Grime)的驼峰模型预测,物种丰富度在中等生产力时达到最大,而在低生产力和高生产力时会下降。已知土壤养分的有效性会影响初级生产力和植物物种丰富度。一般而言,生产力随着土壤养分利用率的增加而增加,而增加土壤养分的实验通常表明生物量增加,物种丰富度相应降低。因此,土壤养分的某些模式有望与驼峰模型相吻合。规模也是一个重要因素,因为物种丰富度和生产力之间的关系可能随规模而变化。这项工作的目的是(1)检验显式驼峰模型预测,即物种丰富度与生产力之间的关系是单峰的; (2)通过单峰关系检验隐式驼峰模型预测,即物种丰富度与与生产力紧密相关的养分有关,例如碳和氮,并确定土壤养分,叶片养分,生产力和物种丰富度之间的关系; (3)评价从1平方米增加到64平方米的比例对物种丰富度,生产力和养分之间关系的影响。通过使用来自14个多尺度网格(包含64个1 m2地块的8 m×8 m网格),来自14个多尺度网格中的四个的子集的土壤样本和叶子的生物量和垫料收集以及物种丰富度计数来完成此操作在四个多尺度网格的每一个中,从九个相邻地块的子集中抽取样本,以获取土壤养分。用CE-440元素分析仪分析土壤和叶片样品中的总碳和氮含量。在里程碑“超波”单反应室中通过超高压封闭容器微波酸消解制备的土壤样品中,对铝,硼,钙,铜,铁,镁,锰,钠,磷,钾,硫和锌中的总铝,定量进行了定量然后用Teledyne / Leeman Labs的“ Prodigy”双视图电感耦合等离子体-光谱发射光谱仪进行分析。在土壤养分数据的主成分分析中,第一和第二主成分似乎分别代表了生产力和物种丰富度。碳,氮,磷,钾,硼,铁,镁和锰被确定为重要的土壤养分。具有总生物量(R2 = 0.76)的第一主成分和具有物种丰富度(R2 = 0.35)的第二主成分的双变量回归返回了很强的R2值。物种丰富度通过凹向下关系与总生物量(R2 = 0.11),土壤碳(R2 = 0.15),土壤氮(R2 = 0.14)和铁(R2 = 0.29)有关,与硼(R2 = 0.17)和镁( R2 = 0.49)通过凹向上关系,磷(R2 = 0.27)和锰(R2 = 0.25)通过正线性关系,钾(R2 = 0.14)通过负线性关系。缩放结果尚无定论,但表明文献中的模式可能部分归因于样本量。结果通常支持驼背模型,养分利用率是与草本植物生产力和物种丰富度相关的重要因素。营养物的供应可能是植物生产力和草本植物多样性的重要驱动力。

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