Long-term dynamics of a collembolan community
Introduction
It is a major shortcoming of soil ecological research that it is not possible to relate alterations in the function of edaphic organisms caused by environmental change to changes in the structure of the soil community (IGBP, 1992). This may be a difficult task anyway for various reasons (Anderson, 1995). An indispensable prerequisite, however, would be a much better understanding of the response of selected soil organisms to long-term fluctuations in environmental conditions. As a contribution to achieving this aim the distribution and abundance of the Collembola and their relationship with macroclimate (temperature, precipitation) in a beech forest on calcareous soil (Göttingen, Germany) was studied over a period of ten consecutive years. It has been argued that changes in the community structure of this microarthropod group sensitively indicate environmental stress (Hågvar, 1994). The following questions should be answered:
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Do fluctuations in macroclimate (temperature, precipitation) affect the density and/or the structure of the investigated community?
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Are there any indications of mechanisms guaranteeing a certain level of interspecific synchronization and community constancy?
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Is the community regulated by density dependent mechanisms?
Section snippets
Material and methods
The study site (about 12 ha) is situated in the Treppenweg area of the Göttinger Wald (Lower Saxony, Germany) on a plateau 400 to 420 m above sea level and is covered by 100 to 130 yr-old beech trees (Fagus sylvatica L.). The bedrock is shell-lime, the humus form is mull. The mean annual precipitation is 720 mm, the mean annual temperature is 7.9°C (weather station Göttingen). According to the German classification system, the soil is classified as Terra fusca Rendzina [Chromo-Calcic Cambisol
Results
A total of 48 collembolan species was found (Table 1). Of these, 21 were regularly extracted from soil cores and further calculations are based on this group. The annual mean density varied between 18 600 and 46 800 ind. m−2 yr−1 (Fig. 1). Strong seasonal fluctuations in density occurred. The maximum average density was 74 900 ind. m−2 in July 1983, and the minimum density was 7 600 ind. m−2 in July 1987. Annual changes in the mean abundances of the different species were not significantly
Discussion
The species richness of the collembolan community in the Göttinger Wald is within the range normally reported for temperate forest ecosystems (Schaefer, 1991). Most species are myco- and/or micro-saprophagous (Wolters, 1987). Many authors have demonstrated a strong effect of ambient temperature conditions on Collembola (e.g. Ashraf, 1971; Hutson, 1978; Klein and Wolters, 1996). The significant correlation between collembolan density and temperature conditions in the previous year is
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Temperature modifies the magnitude of a plant response to Collembola presence
2021, Applied Soil EcologyCitation Excerpt :Collembola, ectothermic organisms, may exhibit greater activity and higher growth and reproductive rates with moderate warming, resulting in elevated metabolic demands (Gillooly et al., 2001; Mallard et al., 2020). A few studies focusing on the fate of the Collembola community have tried to disentangle the effects of temperature from those of soil moisture (Wolters, 1998; Xu et al., 2012; Santonja et al., 2018; Mallard et al., 2020). These studies generally reported an increase in the growth rate, abundance and diversity of Collembola in warmer soil conditions if soil humidity remained favourable.
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2017, Applied Soil EcologyCitation Excerpt :Under field conditions, the correlation between collembolans and temperature is usually hard to establish or is only weakly confirmed. But for example, Wolters (1998) and Bedano et al. (2006), found that Collembola density was negatively correlated with soil and/or air temperature. Our results showed a general increase in collembolan density and species richness with reduction of tillage intensity which is in accordance with a number of previous studies (Brennan et al., 2006; Petersen, 2002; Wardle, 1995) and confirms our first hypothesis.
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2016, Applied Soil EcologyCitation Excerpt :Indeed, a higher functional diversity in forests has resulted from the occurrence of both epigeous and edaphic collembolan species, while most species found in open habitats were fast-dispersal epigeous species. This finding can be explained by the fact that forested sites are generally more concealed habitats and with thicker litter layers, maintaining higher resource quality and more stable conditions in terms of temperature and moisture, which is a preferred environment to eu-edaphic species (Wolters, 1998; Parisi et al., 2005; Berg and Bengtsson, 2007; Heiniger et al., 2015). These are more sensitive to environmental stress and need more protection from desiccation, considering that soil dwelling species are less mobile and then more difficultly colonize the preferred habitat conditions in changing environments (Lindberg and Bengtsson, 2005; Ponge et al., 2006; Salmon and Ponge, 2012).
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