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首页> 外文期刊>Oikos: A Journal of Ecology >Ungulate and topographic control of nitrogen: phosphorus stoichiometry in a temperate grassland; soils, plants and mineralization rates
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Ungulate and topographic control of nitrogen: phosphorus stoichiometry in a temperate grassland; soils, plants and mineralization rates

机译:氮的松散和地形控制:温带草原的磷化学计量;土壤,植物和矿化率

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Although the link between the nitrogen (N): phosphorus (P) stoichiometry of biota and availability has received considerable attention in aquatic systems, there has been relatively little effort to compare the elemental composition of biota and supply in terrestrial habitats. In this study, I explored the effects of a prominent topo-edaphic gradient, from dry hilltop to wet slope-base, and native ungulates on N and P of soils, plants, and rates of in situ net mineralization in grasslands of Yellowstone National Park. Nitrogen and P measurements were made May-September, 2000, in paired, grazed and 38-42 year fenced, ungrazed grassland at five topographically variable sites. Similar to findings from other grassland ecosystems, several site factors associated with organic activity, including soil moisture, C, and plant biomass, covaried with soil N concentration and/or net N mineralization. Soil P concentration and net P mineralization, however, were unrelated to those factors. Instead, net P mineralization was negatively related to soil pH, which is known to control the form of inorganic P and its availability, and soil P was uncorrelated with any soil or plant variable measured in the study. Because of being influenced by different soil properties, N and P net mineralization were unrelated among grasslands. Furthermore, supply and plant N:P ratios were uncorrelated in this grassland system. Based on critical N:P ratios reflecting nutritional limitation of plants, Yellowstone grassland vegetation ranged from being N limited to N-P co-limited. Grazers increased N-P co-limitation by enhancing plant N concentrations and the soil pH gradient across grassland sites regulated plant nutritional limitation by affecting plant-available P. These findings showed how ungulates and a landscape factor, i.e. soil pH, determined plant nutrient status among YNP grasslands differently by influencing plant N concentration versus plant P concentration, respectively.
机译:尽管生物系统的氮(N):磷(P)化学计量与可利用性之间的联系在水生系统中受到了相当大的关注,但在比较陆地生境中生物群和供应的元素组成方面的工作相对较少。在这项研究中,我探索了从干燥的山顶到湿坡基以及从有蹄类动物到土壤,植物的氮和磷以及黄石国家公园草地上原位净矿化速率的显着地形-坡度梯度的影响。 。氮和磷的测量是在2000年5月至9月期间,在五个地形变化的地点,成对,放牧和38-42年的围栏,未磨砂的未草原上进行的。与其他草地生态系统的发现相似,与有机活性相关的几个站点因子,包括土壤水分,碳和植物生物量,与土壤氮浓度和/或净氮矿化量有关。然而,土壤磷浓度和净磷矿化与这些因素无关。相反,净磷矿化与土壤pH负相关,已知该pH控制着无机磷的形态及其有效性,并且土壤P与研究中测得的任何土壤或植物变量均不相关。由于受到不同土壤特性的影响,草地之间的氮和磷净矿化作用无关。此外,在该草地系统中,供应与植物氮磷比不相关。根据反映植物营养限制的关键氮磷比,黄石草地植被的氮含量从N限制为N-P限制。 Grazers通过提高植物N的浓度来增加NP共限制,并且通过影响植物可获得的P来调节草原站点的土壤pH梯度来调节植物的营养限制。这些发现表明,有蹄类动物和景观因子(即土壤pH)如何决定了YNP中植物的营养状况分别通过影响植物N浓度和植物P浓度来影响草原。

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