Restoration of Wet Fen Meadows by Topsoil Removal: Vegetation Development and Germination Biology of Fen Species
By A. Patzelt, U. Wild, J. Pfadenhauer. 2001
122 citations recorded by the source corpus.
Subfields: Ecology, Nature and Landscape Conservation, Plant Science
View Paper: https://www.semanticscholar.org/paper/387aa79a021683dbc6e66eced65eab59b51c6951
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In Ecology
In Nature and Landscape Conservation
In Plant Science
Citations in the corpus
- Ecological significance of seed germination characteristics in flood-meadow species (2004, background): “Information on germination characteristics is also particularly relevant for habitat restoration, in which species-enrichment largely depends on re-establishment by artificially introduced or naturally dispersed seeds (e. g. Bakker & Berendse 1999; Patzelt et al. 2001).”
- Establishment and persistence of target species in newly created calcareous grasslands on former arable fields (2007, unknown): “…of target species on restoration sites have been tested e.g. sowing, planting (both reviewed in Walker et al. 2004) or transfer of diaspore containing autochthonous plant material such as fresh hay or clippings of seed-bearing shoots (Kirmer and Mahn 2001; Patzelt et al. 2001; Tränkle 2002).”
- Prospects for fen meadow restoration on severely degraded fens (2010, background): “, 2007), because it removes most of the plant-available phosphorus and has a greater rewetting effect (Patzelt et al., 2001; Smolders et al., 2008).”
- Effect of Hay Transfer on Long‐Term Establishment of Vegetation and Grasshoppers on Former Arable Fields (2006, methodology): “In the beginning of the twentieth century, most of the formerly extensive calcareous grasslands on pararendzina soils of the Munich gravel plain were converted by plowing and fertilization into arable land (Pfadenhauer 2001).”
- Evaluation of Initial Restoration Measures during the Restoration of Calcareous Grasslands on Former Arable Fields (2006, methodology): “Study Sites In 1993, a large-scale restoration project on former arable fields was started in the Northern Munich Gravel Plain (48 189 N, 11 399 E, 469 m above sea level) in the vicinity of ancient calcareous grasslands managed by mowing in the nature reserve ‘‘Garchinger Heide’’ (Pfadenhauer 2001).”