Mustonen Kaisa-Riikka, Mykrä Heikki, Louhi Pauliina, Markkola Annamari, Tolkkinen Mikko, Huusko Ari, Alioravainen Nico, Lehtinen Sirkku, Muotka Timo
Thule Institute, University of Oulu, P.O. Box 7300, FI-90014, Oulu, Finland.
Department of Ecology, University of Oulu, P.O. Box 8000, FI-90014, Oulu, Finland.
Ecol Appl. 2016 Oct;26(7):2116-2129. doi: 10.1890/15-1841.1. Epub 2016 Sep 12.
Stream ecosystems are affected by multiple abiotic stressors, and species responses to simultaneous stressors may differ from those predicted based on single-stressor responses. Using 12 semi-natural stream channels, we examined the individual and interactive effects of flow level (low or high flow) and addition of fine sediments (grain size <2 mm) on key ecosystem processes (leaf breakdown, algal biomass accrual) and benthic macroinvertebrate and fungal communities. Both stressors had mostly independent effects on biological responses, with sand addition being the more influential of the two. Sand addition decreased algal biomass and microbe-mediated leaf breakdown significantly, whereas invertebrate shredder-mediated breakdown only responded to flow level. Macroinvertebrate community composition responded significantly to both stressors. Fungal biomass decreased and shredder abundance increased when sand was added; thus, organisms at different trophic levels can exhibit highly variable responses to the same stressor. Terrestrial endophytic fungi were abundant in low-flow flumes where leaf mass loss was also highest, indicating that terrestrial endophytes may contribute importantly to leaf decomposition in the aquatic environment. Leaf breakdown rates depended on the identity and abundance of the dominant decomposer species, suggesting that the effects of anthropogenic activities on ecosystem processes may be driven by changes in the abundance of a few key species. The few observed interactive effects were all antagonistic (i.e., less than the sum of the individual effects); for example, increased flow stimulated algal biomass accumulation but this effect was largely cancelled by sand. While our finding that sand and stream flow did not have strong synergistic effects can be considered reassuring for management, future experiments should manipulate these and other human stressors in experiments that run for much longer periods, thus focusing on the long-term impacts of multiple simultaneously operating stressors.
溪流生态系统受到多种非生物胁迫因素的影响,物种对同时存在的胁迫因素的反应可能与基于单一胁迫因素反应所预测的不同。我们使用12个半自然溪流渠道,研究了流量水平(低流量或高流量)和添加细颗粒沉积物(粒径<2毫米)对关键生态系统过程(树叶分解、藻类生物量积累)以及底栖大型无脊椎动物和真菌群落的单独和交互影响。这两种胁迫因素对生物学反应大多具有独立影响,其中添加沙子的影响更大。添加沙子显著降低了藻类生物量和微生物介导的树叶分解,而无脊椎动物碎食者介导的分解仅对流量水平有反应。大型无脊椎动物群落组成对这两种胁迫因素均有显著反应。添加沙子时,真菌生物量减少,碎食者丰度增加;因此,不同营养级的生物对同一胁迫因素可能表现出高度可变的反应。陆地内生真菌在低流量水槽中含量丰富,那里树叶质量损失也最高,这表明陆地内生菌可能对水生环境中的树叶分解有重要贡献。树叶分解速率取决于优势分解物种的身份和丰度,这表明人为活动对生态系统过程的影响可能由少数关键物种丰度的变化驱动。观察到的少数交互作用都是拮抗作用(即小于单独作用的总和);例如,流量增加刺激了藻类生物量积累,但这种影响在很大程度上被沙子抵消了。虽然我们发现沙子和溪流流量没有强烈的协同效应这一结果对于管理来说可能是令人安心的,但未来的实验应该在运行时间长得多的实验中操纵这些以及其他人为胁迫因素,从而关注多个同时作用的胁迫因素的长期影响。