Ekelund Flemming, Frederiksen Helle B, Rønn Regin
Department of Terrestrial Ecology, Zoological Institute, University of Copenhagen, Universitetsparken 15, DK-2100 Copenhagen Ø, Denmark.
Appl Environ Microbiol. 2002 Mar;68(3):1096-101. doi: 10.1128/AEM.68.3.1096-1101.2002.
Soil protozoa are characterized by their ability to produce cysts, which allows them to survive unfavorable conditions (e.g., desiccation) for extended periods. Under favorable conditions, they may rapidly excyst and begin feeding, but even under optimal conditions, a large proportion of the population may be encysted. The factors governing the dynamics of active and encysted cells in the soil are not well understood. Our objective was to determine the dynamics of active and encysted populations of ciliates during the decomposition of freshly added organic material. We monitored, in soil microcosms, the active and total populations of ciliates, their potential prey (bacteria and small protozoa), their potential competitors (amoebae, flagellates, and nematodes), and their potential predators (nematodes). We sampled with short time intervals (2 to 6 days) and generated a data set, suitable for mathematical modeling. Following the addition of fresh organic material, bacterial numbers increased more than 1,400-fold. There was a temporary increase in the number of active ciliates, followed by a rapid decline, although the size of the bacterial prey populations remained high. During this initial burst of ciliate growth, the population of cystic ciliates increased 100-fold. We suggest that internal population regulation is the major factor governing ciliate encystment and that the rate of encystment depends on ciliate density. This model provides a quantitative explanation of ciliatostasis and can explain why protozoan growth in soil is less than that in aquatic systems. Internally governed encystment may be an essential adaptation to an unpredictable environment in which individual protozoa cannot predict when the soil will dry out and will survive desiccation only if they have encysted in time.
土壤原生动物的特点是能够产生包囊,这使它们能够在不利条件(如干燥)下长期存活。在有利条件下,它们可能迅速脱囊并开始摄食,但即使在最佳条件下,也有很大一部分群体可能处于包囊状态。控制土壤中活跃细胞和包囊细胞动态的因素尚不清楚。我们的目标是确定新添加有机物质分解过程中纤毛虫活跃群体和包囊群体的动态。我们在土壤微观系统中监测了纤毛虫的活跃群体和总群体、它们潜在的猎物(细菌和小型原生动物)、潜在的竞争者(变形虫、鞭毛虫和线虫)以及潜在的捕食者(线虫)。我们以短时间间隔(2至6天)进行采样,并生成了一个适合数学建模的数据集。添加新鲜有机物质后,细菌数量增加了1400多倍。活跃纤毛虫的数量暂时增加,随后迅速下降,尽管细菌猎物种群的规模仍然很高。在纤毛虫生长的最初爆发期间,包囊纤毛虫的数量增加了100倍。我们认为内部种群调节是控制纤毛虫形成包囊的主要因素,包囊形成的速率取决于纤毛虫的密度。该模型对纤毛虫静止状态提供了定量解释,并可以解释为什么土壤中原生动物的生长低于水生系统。内部控制的包囊形成可能是对不可预测环境的一种重要适应,在这种环境中,单个原生动物无法预测土壤何时会干涸,只有及时形成包囊才能在干燥中存活。