Nicholas School of the Environment, Duke University, P.O. Box 90328, Durham, North Carolina 27705, USA.
Ecol Appl. 2010 Apr;20(3):609-19. doi: 10.1890/09-0283.1.
Wetlands are valuable for buffering waterways from excess nitrogen, yet these habitats are often dominated by invasive plant species. There is little understanding as to how various invasive species alter ecosystem nitrogen cycling, especially if one invasive overtakes an entire community of plants. Microstegium vimineum is a nonnative annual grass from Asia that is dominating riparian wetlands in the southeastern United States. To evaluate M. vimineum impacts on the N cycle, we used six paired plots, one invaded by M. vimineum and the other carefully weeded of M. vimineum; removal allowed the establishment of a diverse plant community consisting of Polygonum, Juncus, and Carex species. In the paired plots, we estimated (1) N uptake and accumulation in vegetation biomass, (2) rates of decomposition and N release from plant detritus, (3) mineral soil N mineralization and nitrification, (4) root zone redox potential, and (5) soil water concentrations of inorganic N. The M. vimineum community accumulated approximately half the annual N biomass of the diverse community, 5.04 vs. 9.36 g N x m(-2) x yr(-1), respectively (P = 0.05). Decomposition and release of N from M. vimineum detritus was much less than in the diverse community, 1.19 vs. 5.24 g N x m(-2) x yr(-1). Significantly higher inorganic soil N persisted beneath M. vimineum during the dormant season, although rates of soil N mineralization estimated by in situ incubations were relatively similar in all plots. Microstegium vimineum invasion thus appears to greatly diminish within-ecosystem circulation of N through the understory plants of these wetlands, whereas invasion effects on ecosystem N losses may derive more from enhanced denitrification (due to lower redox potential under M. vimineum plots) than due to leaching. Microstegium vimineum's dominance and yet slower internal cycling of N are counterintuitive to conventional thinking that ecosystems with high N contain vegetation that quickly uptake and release N.
湿地在缓冲河道过量氮素方面具有重要价值,但这些栖息地常常被入侵植物物种所主导。目前对于各种入侵物种如何改变生态系统氮循环知之甚少,特别是如果一种入侵物种完全取代了整个植物群落。薇甘菊是一种来自亚洲的非本地一年生草本植物,正在主导美国东南部的河岸湿地。为了评估薇甘菊对氮循环的影响,我们使用了 6 个配对样地,其中一个样地被薇甘菊入侵,另一个样地则经过精心除草,以清除薇甘菊;清除薇甘菊后,建立了一个由Polygonum、Juncus 和 Carex 等物种组成的多样化植物群落。在配对样地中,我们估计了(1)植被生物量中的氮吸收和积累,(2)植物凋落物的分解和氮释放速率,(3)矿物土壤氮矿化和硝化作用,(4)根区氧化还原电位,以及(5)土壤无机氮的浓度。薇甘菊群落每年积累的氮生物量约为多样化群落的一半,分别为 5.04 和 9.36 g N x m(-2) x yr(-1)(P = 0.05)。薇甘菊凋落物的分解和氮释放量远低于多样化群落,分别为 1.19 和 5.24 g N x m(-2) x yr(-1)。尽管原位培养法估计的土壤氮矿化速率在所有样地中都相对相似,但薇甘菊下的无机土壤氮在休眠季节仍保持较高水平。因此,薇甘菊的入侵似乎极大地减少了这些湿地下层植被的生态系统内部氮循环,而生态系统氮损失的入侵效应可能更多地来自于增强的反硝化作用(由于薇甘菊下的氧化还原电位较低),而不是淋失。薇甘菊的优势地位和较慢的内部氮循环与传统观念相悖,传统观念认为,高氮含量的生态系统含有能迅速吸收和释放氮的植被。