Microhabitat and seasonal dynamics of soil fauna communities in upper Andean successional forests

IF 2 3区 农林科学 Q3 ECOLOGY
Dennis Castillo-Figueroa , Camilo Castillo-Avila
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引用次数: 0

Abstract

Soil fauna play a crucial role in supporting soil functions and their communities change along forest successional gradients. However, our understanding of their temporal dynamics is limited, particularly in tropical mountain ecosystems with pronounced seasonal precipitation patterns. Additionally, the impact of forest successional stage on the regulation of seasonal changes in soil fauna communities remains poorly understood. In this study, we examined the changes of soil fauna communities across climatic seasons and microhabitats in mature and secondary forests of upper Andean tropical forests (UATF). We collected 168 soil samples (30x30x5 cm) across four climatic seasons (two wet and two dry) from 14 permanent plots in four UATF sites during La Niña event. Microclimatic data (air, surface, and soil temperatures, and soil moisture) were recorded every 15 minutes for a year using TOMST dataloggers. Our findings reveal that soil fauna richness and abundance significantly increase during wet seasons, although species composition remained unchanged. This increase is mainly due to higher soil moisture levels, which control soil fauna attributes. We also observed an interaction between climatic season and microhabitat: during wet seasons, when soils are water-saturated, more species migrate to the litter layer, whereas during dry seasons, when water availability is reduced, species tend to aggregate in the soil. However, no interactions were detected between these factors and successional stages. Soil moisture directly influenced soil fauna richness and abundance in both mature and secondary forests. Overall, our study highlights that soil fauna in UATF exhibit clear climatic seasonality, shaping microhabitat variability independent of forest successional stage.
上安第斯演替林土壤动物群落的微生境和季节动态
土壤动物在支持土壤功能及其群落沿森林演替梯度变化中起着至关重要的作用。然而,我们对其时间动态的理解是有限的,特别是在具有明显季节性降水模式的热带山地生态系统中。此外,森林演替阶段对土壤动物群落季节变化调控的影响尚不清楚。研究了上安第斯热带森林(UATF)成熟森林和次生林土壤动物群落在气候季节和微生境上的变化。在La Niña事件期间,我们从四个UATF站点的14个永久地块收集了168个土壤样本(30x30x5 cm),跨越四个气候季节(两个湿季和两个干季)。使用TOMST数据记录器每15 分钟记录一次小气候数据(空气、地表和土壤温度以及土壤湿度),持续一年。结果表明,雨季土壤动物丰富度和丰度显著增加,但物种组成保持不变。这种增加主要是由于土壤湿度较高,这控制了土壤动物的属性。我们还观察到气候季节和微生境之间的相互作用:在湿润季节,当土壤水分饱和时,更多的物种迁移到凋落物层,而在干旱季节,当水分可用性降低时,物种倾向于在土壤中聚集。然而,这些因素与演替阶段之间没有相互作用。土壤湿度直接影响成熟森林和次生林土壤动物的丰富度和丰度。总体而言,我们的研究强调了UATF土壤动物具有明显的气候季节性,形成了独立于森林演替阶段的微栖息地变异性。
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来源期刊
Pedobiologia
Pedobiologia 环境科学-生态学
CiteScore
4.20
自引率
8.70%
发文量
38
审稿时长
64 days
期刊介绍: Pedobiologia publishes peer reviewed articles describing original work in the field of soil ecology, which includes the study of soil organisms and their interactions with factors in their biotic and abiotic environments. Analysis of biological structures, interactions, functions, and processes in soil is fundamental for understanding the dynamical nature of terrestrial ecosystems, a prerequisite for appropriate soil management. The scope of this journal consists of fundamental and applied aspects of soil ecology; key focal points include interactions among organisms in soil, organismal controls on soil processes, causes and consequences of soil biodiversity, and aboveground-belowground interactions. We publish: original research that tests clearly defined hypotheses addressing topics of current interest in soil ecology (including studies demonstrating nonsignificant effects); descriptions of novel methodological approaches, or evaluations of current approaches, that address a clear need in soil ecology research; innovative syntheses of the soil ecology literature, including metaanalyses, topical in depth reviews and short opinion/perspective pieces, and descriptions of original conceptual frameworks; and short notes reporting novel observations of ecological significance.
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