Elsevier

Applied Soil Ecology

Volume 9, Issues 1–3, 1 September 1998, Pages 221-227
Applied Soil Ecology

Long-term dynamics of a collembolan community

https://doi.org/10.1016/S0929-1393(98)00079-1Get rights and content

Abstract

The collembolan community of a beech forest on limestone (Göttingen, Germany) was studied for a period of ten consecutive years (1980–1989). A total of 48 species was found. The annual mean density varied between 18 600 and 46 800 ind. m−2 yr−1. Abundance dynamics of the different species were not significantly intercorrelated. Year-to-year changes in annual mean temperature were significantly correlated with alterations in collembolan density in the following year. Specific differences in response patterns to temperature alterations apparently buffered each other in such a way that the response of the whole community to temperature is more predictable than that of most individual species. No clear-cut trend in the abundance dynamics of the collembolan community were detected and the actual densities of the individual species were not correlated with the corresponding densities in the following year. On the other hand, indication of density dependent regulation was found for eight species. To explain this seeming contradiction it was hypothesized that at least part of the collembolan community is exposed to density dependent regulation and that strong year-to-year fluctuations in density are due to significant year-to-year changes in the carrying capacity of the soil environment caused by long-term effects of temperature on the quantity and quality of the litter layer.

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:

  • Do fluctuations in macroclimate (temperature, precipitation) affect the density and/or the structure of the investigated community?

  • Are there any indications of mechanisms guaranteeing a certain level of interspecific synchronization and community constancy?

  • 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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