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Soils of the mycological reserve on Lisina Mountain in the Republic of Srpska, Bosnia and Herzegovina
Author(s) -
Saša Eremija,
Milan Knežević,
Marijana Kapović Solomun
Publication year - 2014
Publication title -
archives of biological sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.217
H-Index - 25
eISSN - 1821-4339
pISSN - 0354-4664
DOI - 10.2298/abs1401299e
Subject(s) - earth science , podzol , soil water , geology , soil morphology , revegetation , soil classification , environmental science , soil science , ecology , geochemistry , biology , land reclamation
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

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