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This led to inaccuracies in the surveying and over time it was no longer possible to identify individual clumps.Ībseiling technique during Alpine bells monitoring. This method was insufficient for obtaining more detailed data because of the large distance between the observer and the sites, and the acute angle at which the plants were observed. Monitoring of Alpine bells was begun by staff of the Czech Nature Conservation Institute (NCA since 1995) in 1992 by counting them with a stationary telescope from the upper rim and floor of the abyss (Řičánek 1994). It is almost certain that the experts who were studying Alpine bells never visited all the sites high on the rock face, but only investigated the localities on the debris cone, and possibly above the upper pool, which can be seen from the floor of the abyss. However, data on the size of the local population differ significantly. The first reports of the occurrence of Alpine bells at Macocha come from the years 1918–1921, with other authors mentioning this species later. The site is without direct sunlight all year round, and it is under the constant influence of cold air from the caves on the Punkva River, which are located below it. The long-term existence of this montane species is possible thanks to the cold and humid climate under rocky overhangs.
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It is a small, isolated population the closest localities of this species are in the Strážov Mountains and Malá Fatra Mountains in Slovakia and in the Alps. However, only three specimens now survive here.Īlpine bells is a glacial relict which occurs in the Czech Republic in only one place on the northern face of the Macocha Abyss. Previously, part of the Alpine bells population also occurred on the debris cone at the bottom of the Abyss, from where it was first described. Access to the habitat is very difficult and only possible with the help of ropes and for physically fit people with the necessary experience. This is because it grows in the Macocha Abyss, high on the vertical rock walls. moravica Soják) is undoubtedly one of the most famous plants of the Moravian Karst, even though very few people have ever seen it.
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