Changes in the structure of the soil nematode community over long-term secondary grassland succession in drained fen peat

• Published in: Applied soil ecology : a section of Agriculture, ecosystems & environment Vol. 32; no. 2; pp. 165 - 179
• Main Author: Wasilewska, Lucyna
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 01.06.2006; Elsevier
• Subjects: Agronomy. Soil science and plant productions; Biochemistry and biology; Biological and medical sciences; c-p Class structure; Chemical, physicochemical, biochemical and biological properties; community structure; drainage; Drained meadows; ecological succession; fens; Fundamental and applied biological sciences. Psychology; grassland soils; grasslands; life history; Natural fens; Nematode succession; peat; Physics, chemistry, biochemistry and biology of agricultural and forest soils; population density; soil nematodes; Soil science; Taxonomic structure; taxonomy; trophic relationships; Trophic structure; Zoology (interactions between soil fauna and agricultural or forest soils); Poland; Eastern Europe; Europe; Nematode succession; Drained meadows; c-p Class structure; Natural fens; Taxonomic structure; Trophic structure; Grassland; Fauna; Taxonomy; Bogs; Ecology; Long term; Peat; Drainage; Microfauna; Soil fauna; Animal community; Helmintha; Nemathelminthia; Soil science; Invertebrata; Wetland; Nematoda
• ISSN: 0929-1393; 1873-0272
• DOI: 10.1016/j.apsoil.2005.07.003

The different kind of soil nematode structures, based on the proportions of different orders, trophic groups and individuals belonging to groups with different life history strategies were studied in grasslands transformed by drainage of natural fens, situated at Biebrza Wetland in Poland. Natural fens were studied for comparison with drained meadows, which had a time span from 2 to 117 years after drainage. After conversion of fens into permanent managed meadows, the peat-forming process is replaced by a mucking process (mineralization and humification of peat), accompanied by physicochemical changes in the peat soil. When the nematofauna was classified into nine orders, the most abundant groups on drained meadows were tylenchids (36–84%) and rhabditids (12–39%), followed by araeolaimids, aphelenchids, dorylaimids, enoplids, mononchids, monhysterids and chromadorids. In terms of trophic categories, obligate plant feeders (19–64%) and bacterivores (13–55%) dominated, followed by facultative plant feeders, fungivores, omnivores and predators. Analysis of life history strategy expressed as percentage contribution of c-p classes to total nematodes indicated the dominance of the c-p 2 class, but its contribution decreased with time since drainage, as did the c-p 1 nematodes. The taxa in c-p 3 did not change, and the contribution of c-p 4 and c-p 5 increased with time. In natural fens, c-p 2 taxa also dominated, followed by c-p 1, c-p 3, c-p 4 and c-p 5 classes. As pulse-stabilized nutrient resources activated mainly by the peat mucking process still exist over succession, although the process rate declines over time, the achievement of a sub-climax state sensu Odum (1969) could be accepted for drained fen meadows. It is proposed that the point at which such a sub-climax state may start is not less than about 65 years after drainage, because it coincides with a point, when taxa c-p 4 and c-p 5 approach similar levels of dominance as in natural, undrained fens. The similarities between natural fens and drained sites after 117 years, measured by the Renkonen number, were 85.5, 72 and 77.1% corresponding to three kinds of structures. The maturity index ΣMI significantly increased in the course of succession ( P < 0.001). For considering the construction of ΣMI over time, individuals of the separate c-p classes were expressed in trophic terms. The temporal changes in abundance of some genera are presented.