Högberg Mona N, Bååth Erland, Nordgren Anders, Arnebrant Kristina, Högberg Peter
Section of Soil Science, Department of Forest Ecology, SLU, SE-901 83 Umeå, Sweden.
Department of Microbial Ecology, Lund University, SE-223 62 Lund, Sweden.
New Phytol. 2003 Oct;160(1):225-238. doi: 10.1046/j.1469-8137.2003.00867.x.
• Soil microorganisms are considered C-limited, while plant productivity is frequently N-limited. Large stores of organic C in boreal forest soils are attributed to negative effects of low temperature, soil acidity and plant residue recalcitrance upon microbial activity. • We examined microbial activity, biomass and community composition along a natural 90-m-long soil N supply gradient, where plant species composition varies profoundly, forest productivity three-fold and soil pH by three units. • There was, however, no significant variation in soil respiration in the field across the gradient. Neither did microbial biomass C determined by fumigation-extraction vary, while other estimates of activity and biomass showed a weak increase with increasing N supply and soil pH. Simultaneously, a phospholipid fatty acid attributed mainly to mycorrhizal fungi declined drastically, while bacterial biomass increased. • We hypothesize that low N supply and plant productivity, and hence low litter C supply to saprotrophs is associated with a high plant C supply to mycorrhizal fungi, while the reverse occurs under high N supply. This should mean that effects of N availability on C supply to these functional groups of microbes acts in opposing directions.
• 土壤微生物被认为受碳限制,而植物生产力通常受氮限制。北方森林土壤中大量的有机碳储存归因于低温、土壤酸度和植物残体难分解性对微生物活动的负面影响。
• 我们沿着一条90米长的天然土壤氮供应梯度研究了微生物活动、生物量和群落组成,在该梯度上植物物种组成有很大差异,森林生产力相差三倍,土壤pH值相差三个单位。
• 然而,该梯度上田间土壤呼吸没有显著变化。通过熏蒸提取法测定的微生物生物量碳也没有变化,而其他活性和生物量估计值随氮供应和土壤pH值增加略有增加。同时,主要归因于菌根真菌的一种磷脂脂肪酸急剧下降,而细菌生物量增加。
• 我们推测,低氮供应和植物生产力,以及由此导致的向腐生生物的凋落物碳供应低,与向菌根真菌的植物碳供应高有关,而在高氮供应下情况则相反。这意味着氮有效性对这些微生物功能组碳供应的影响作用方向相反。