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Grassland communities of areas with high levels of zinc and lead in the Olkusz region (southern Poland) were studied. They developed spontaneously on mine waste deposited at the beginning of the 20th century. Twenty phytosociological releves in two areas are presented, along with pH and the zinc and lead concentrations in the upper soil layer. The soils were shallow, pH-neutral or slightly alkaline, and with very high heavy metal content (Zn 3.3–10.4%, Pb 0.32–1.66%). The grasslands were generally short and rather dense, and floristically similar to the Armerietum halleri Libbert 1930 association described by many authors from metalliferous areas of Germany; they differed from German ones by the presence of Biscutella laevigata and by the constant and often abundant occurrence of some vascular plants and lichen species (e.g., Rumex thyrsifl orus, Cardaminopsis arenosa, Diploschistes muscorum, Verrucaria muralis). Difficulties in comparing phytosociological materials from various areas are discussed. The paper points to the need to conserve grassland islands in the monotonous, seriously degraded landscape of the area.
The post-mining (Zn, Pb) open pit under study (local name “Krążek”) is situated in the Silesian Upland (50°17’N, 19°27’E) in an area abounding in zinc-lead ores. The open pit, 7.5 ha in area and 30 m deep, was designated for reclamation. Reclamation work started in 1999 and consisted in filling the excavation with foreign (nonlocal) material, and planting pine and oak. It was completed in 2002. Studies of the vegetation colonizing the open pit were carried out in 20 permanent plots (25 m²) representing two types of imported soil substrate (sandy, clayey) in the years 2003–2005. They were based on 60 phytosociological relevés made according to Braun-Blanquet’s methods. In the studied open pit, 178 vascular plant species, spontaneously colonizing the newly created substrate, were found. Only 43 species were present in every year of the study. Most frequent were sporadic species (130), occurring in less than 20% of the relevés. The plants of the reclaimed area represented different ecological groups. Species associated with human-transformed sites (e.g. Solidago canadensis, Tussilago farfara) were the most numerous, but their number decreased with time during the study. Species connected with seminatural (meadow) sites (e.g. Achillea millefolium, Daucus carota) and natural (xerothermic and sandy grassland) sites (e.g. Hypericum perforatum, Poa compressa, Corynephorus canescens) were less frequent, but their number increased with time during the study. Six groups of species connected with the soil substrate type (sand – Rumex acetosella, Cardaminopsis arenosa; clay – Ranunculus repens, Medicago lupulina) and the colonization period (2003 – Atriplex patula, Polygonum lapathifolium, Polygonum hydropiper; 2004–2005 – Calamagrostis epigejos, Leontodon hispidus) were distinguished. Species composition changed over the study period. In the clayey plots these changes were more apparent than in the sandy ones. The numbers of species were lower, the diversity indexes slightly lower and the evenness indexes slightly higher in 2003 than in later years (2004–2005). The initial stages of colonization of the open pit were characterized by the presence of mostly nonlocal ruderal species (Melandrium album, Matricaria maritima, Atriplex patula) which originated from the bank of diaspores in the soil brought to the open pit and from seeds introduced during the reclamation work. Local plants contributed little to the colonization process. Ecological restoration methods in areas degraded by mining activity are discussed; the use of local soil material containing the local bank of diasporas and soil microorganism associations is recommended.
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