Institute of Geography and Geoecology, Karlsruhe Institute of Technology (KIT), Reinhard-Baumeister-Platz 1, 76131, Karlsruhe, Germany.
Institute of Biology, Leipzig University, Johannisallee 21, 04103, Leipzig, Germany.
Oecologia. 2020 Jul;193(3):731-748. doi: 10.1007/s00442-020-04717-6. Epub 2020 Jul 31.
Gross rates of nitrogen (N) turnover inform about the total N release and consumption. We investigated how plant diversity affects gross N mineralization, microbial ammonium (NH) consumption and gross inorganic N immobilization in grasslands via isotopic pool dilution. The field experiment included 74 plots with 1-16 plant species and 1-4 plant functional groups (legumes, grasses, tall herbs, small herbs). We determined soil pH, shoot height, root, shoot and microbial biomass, and C and N concentrations in soil, microbial biomass, roots and shoots. Structural equation modeling (SEM) showed that increasing plant species richness significantly decreased gross N mineralization and microbial NH consumption rates via increased root C:N ratios. Root C:N ratios increased because of the replacement of legumes (low C:N ratios) by small herbs (high C:N ratios) and an increasing shoot height, which was positively related with root C:N ratios, with increasing species richness. However, in our SEM remained an unexplained direct negative path from species richness to both N turnover rates. The presence of legumes increased gross N mineralization, microbial NH consumption and gross inorganic N immobilization rates likely because of improved N supply by N fixation. The positive effect of small herbs on microbial NH consumption and gross inorganic N immobilization could be attributed to their increased rhizodeposition, stimulating microbial growth. Our results demonstrate that increasing root C:N ratios with increasing species richness slow down the N cycle but also that there must be additional, still unidentified processes behind the species richness effect potentially including changed microbial community composition.
总氮周转率的速率可以反映氮的释放和消耗总量。我们通过同位素池稀释的方法,研究了植物多样性如何影响草原中的总氮矿化、微生物铵(NH)消耗和总无机氮固定。该田间实验包括 74 个样方,每个样方中含有 1-16 种植物和 1-4 种植物功能群(豆科植物、禾本科植物、高大草本植物、小型草本植物)。我们测定了土壤 pH 值、地上部分高度、根系、地上部分和微生物生物量,以及土壤、微生物生物量、根系和地上部分中的 C 和 N 浓度。结构方程模型(SEM)表明,随着植物物种丰富度的增加,根系 C:N 比增加,从而导致总氮矿化和微生物 NH 消耗速率显著降低。根系 C:N 比增加的原因是豆科植物(低 C:N 比)被小型草本植物(高 C:N 比)所取代,以及地上部分高度的增加,而地上部分高度与根系 C:N 比呈正相关,随着物种丰富度的增加而增加。然而,在我们的 SEM 中,仍然存在一个未解释的直接负路径,即物种丰富度与两个氮周转率直接相关。豆科植物的存在增加了总氮矿化、微生物 NH 消耗和总无机氮固定的速率,可能是因为氮固定改善了氮供应。小型草本植物对微生物 NH 消耗和总无机氮固定的积极影响可能归因于它们增加的根分泌物,刺激了微生物的生长。我们的研究结果表明,随着物种丰富度的增加,根系 C:N 比的增加会减缓氮循环,但在物种丰富度效应的背后,肯定还存在其他尚未确定的过程,包括微生物群落组成的变化。