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This paper presents the results of soil research in a mycological reserve   that is defined as a special nature reserve according to the IUCN   categorization. Ecologically, fungi are the most valuable element in the   biological diversity of protected reserves. Favorable climate and the   complexity of geology, soils and vegetation of Lisina Mountain caused the   development of extraordinarily rich mycoflora. The soil cover here is   characterized mainly by soils on acid siliceous parent rocks. Carbonate   sediments as a part of volcanic sediment formation, present with laminated   black limestone, complicate the structure of the soil cover. The protected   area is defined by five basic soil types: rendzina, ranker, dystric   cambisols, luvisol and podzol. Soil properties depend on pedogenetic   processes and the nature of the parent rock. Rendzina is the most common soil   type on limestone-dolomite substrate, where it creates elementary and complex   soil combinations, mainly because of its strong relief. The most common soil   type on acid silicate rocks is dystric cambisols

Soils of the mycological reserve on Lisina Mountain in the Republic of Srpska, Bosnia and Herzegovina