. . "CZ - \u010Cesk\u00E1 republika" . "DLOUHODOB\u00C9 SLEDOV\u00C1N\u00CD MAKROMYCET\u016E V KYSEL\u00C9 DOUBRAV\u011A A HODNOCEN\u00CD JEJICH V\u00DDZNAMU"@cs . "4" . "2"^^ . "1"^^ . . "DLOUHODOB\u00C9 SLEDOV\u00C1N\u00CD MAKROMYCET\u016E V KYSEL\u00C9 DOUBRAV\u011A A HODNOCEN\u00CD JEJICH V\u00DDZNAMU" . "LONG-TERM SURVEY OF MACROMYCETES IN THE ACID OAK-WOOD AND THEIR IMPORTANCE"@en . . "macromycetes, oak, mycologic monitoring, defoliation"@en . "DLOUHODOB\u00C9 SLEDOV\u00C1N\u00CD MAKROMYCET\u016E V KYSEL\u00C9 DOUBRAV\u011A A HODNOCEN\u00CD JEJICH V\u00DDZNAMU"@cs . . "RIV/60460709:41320/14:66066" . "Zpr\u00E1vy lesnick\u00E9ho v\u00FDzkumu" . "DLOUHODOB\u00C9 SLEDOV\u00C1N\u00CD MAKROMYCET\u016E V KYSEL\u00C9 DOUBRAV\u011A A HODNOCEN\u00CD JEJICH V\u00DDZNAMU" . "59" . . "11965" . . "RIV/60460709:41320/14:66066!RIV15-MSM-41320___" . "The occurrence of the macromycetes and their significance for the health state of the forest cover was monitored on the permanent research oak plot (Quercus petrae at the age of 160 years) in D\u0159ev\u00ED\u010D of the K\u0159ivokl\u00E1tsko region (Czech Republic) between 1993\u20132013. The observation of the macromycetes formed a part of more comprehensive evaluation of the forest ectotrophic stability with a simultaneous assessment of the mycorrhizae and defoliation of all the 50 trees occurring on the plot. The results of the research show an increased proportion of the ectomycorrhizal fungi species. This phenomenon is verified by an assessment of the species spectrum of the macromycetes and changes in their abundance and frequency. Altogether 253 species of macromycetes were ascertained, from which 111 were ectomycorrhizal ones. All identified species are listed in the enclosed table. The ectotrophic forest stability, even at a higher stand age occurs as slightly disturbed, only."@en . "P\u0159edlo\u017Een\u00E1 pr\u00E1ce se zab\u00FDv\u00E1 v\u00FDsledky dlouhodob\u00E9ho sledov\u00E1n\u00ED makromycet\u016F (1993\u20132013) na studijn\u00ED plo\u0161e v kysel\u00E9 doubrav\u011B (Quercus petraea) na lokalit\u011B D\u0159ev\u00ED\u010D (K\u0159ivokl\u00E1tsko). Plocha byla pe\u010Dliv\u011B zvolena jako homogenn\u00ED s jedinou d\u0159evinou ve st\u00E1\u0159\u00ED cca 160 let. Nach\u00E1z\u00ED se v Chr\u00E1n\u011Bn\u00E9 krajinn\u00E9 oblasti (CHKO) K\u0159ivokl\u00E1tsko, kter\u00E1 byla vyhl\u00E1\u0161ena za biosf\u00E9rickou rezervaci UNESCO a rozkl\u00E1d\u00E1 se na z\u00E1padn\u00EDm okraji st\u0159edn\u00EDch \u010Cech. K\u0159ivokl\u00E1tsk\u00E1 pahorkatina zahrnuje Zbiro\u017Esko \u2013 K\u0159ivokl\u00E1tskou vrchovinu s L\u00E1nskou a Kralovickou pahorkatinou. Oblast tvo\u0159\u00ED b\u00FDval\u00E9 dno starohorn\u00EDho mo\u0159e, kter\u00E9 bylo vyzdvi\u017Eeno vulkanickou \u010Dinnost\u00ED. \u00DAzem\u00ED je v\u00FDrazn\u011B modelov\u00E1no severn\u00ED \u010D\u00E1st\u00ED rovinat\u00FDm a\u017E m\u00EDrn\u011B zvln\u011Bn\u00FDm ter\u00E9nem s nejvy\u0161\u0161\u00ED k\u00F3tou Skalka (435 m n. m.) ze severu a sva\u017Eit\u00FDm ter\u00E9nem k \u00FAdol\u00ED \u0159eky Berounky spolu s ost\u0159e za\u0159\u00EDzl\u00FDmi poto\u010Di\u0161ti, zejm\u00E9na lev\u00FDm p\u0159\u00EDtokem Berounky potokem V\u016Fznice. V\u00FD\u0161kov\u00E9 rozp\u011Bt\u00ED lokality D\u0159ev\u00ED\u010D je 220 a\u017E 435 m n. m. V\u00FDzkumn\u00E1 plocha n\u00E1le\u017E\u00ED k lesn\u00ED spr\u00E1v\u011B (LS) Ni\u017Ebor a rev\u00EDru D\u0159ev\u00ED\u010D." . . . "8"^^ . "41320" . "Pe\u0161kov\u00E1, V\u00EDt\u011Bzslava" . "[0C845594AEFD]" . . . "S" . . "0" . "LONG-TERM SURVEY OF MACROMYCETES IN THE ACID OAK-WOOD AND THEIR IMPORTANCE"@en . "Landa, Jaroslav" . . "0322-9688" . . . "P\u0159edlo\u017Een\u00E1 pr\u00E1ce se zab\u00FDv\u00E1 v\u00FDsledky dlouhodob\u00E9ho sledov\u00E1n\u00ED makromycet\u016F (1993\u20132013) na studijn\u00ED plo\u0161e v kysel\u00E9 doubrav\u011B (Quercus petraea) na lokalit\u011B D\u0159ev\u00ED\u010D (K\u0159ivokl\u00E1tsko). Plocha byla pe\u010Dliv\u011B zvolena jako homogenn\u00ED s jedinou d\u0159evinou ve st\u00E1\u0159\u00ED cca 160 let. Nach\u00E1z\u00ED se v Chr\u00E1n\u011Bn\u00E9 krajinn\u00E9 oblasti (CHKO) K\u0159ivokl\u00E1tsko, kter\u00E1 byla vyhl\u00E1\u0161ena za biosf\u00E9rickou rezervaci UNESCO a rozkl\u00E1d\u00E1 se na z\u00E1padn\u00EDm okraji st\u0159edn\u00EDch \u010Cech. K\u0159ivokl\u00E1tsk\u00E1 pahorkatina zahrnuje Zbiro\u017Esko \u2013 K\u0159ivokl\u00E1tskou vrchovinu s L\u00E1nskou a Kralovickou pahorkatinou. Oblast tvo\u0159\u00ED b\u00FDval\u00E9 dno starohorn\u00EDho mo\u0159e, kter\u00E9 bylo vyzdvi\u017Eeno vulkanickou \u010Dinnost\u00ED. \u00DAzem\u00ED je v\u00FDrazn\u011B modelov\u00E1no severn\u00ED \u010D\u00E1st\u00ED rovinat\u00FDm a\u017E m\u00EDrn\u011B zvln\u011Bn\u00FDm ter\u00E9nem s nejvy\u0161\u0161\u00ED k\u00F3tou Skalka (435 m n. m.) ze severu a sva\u017Eit\u00FDm ter\u00E9nem k \u00FAdol\u00ED \u0159eky Berounky spolu s ost\u0159e za\u0159\u00EDzl\u00FDmi poto\u010Di\u0161ti, zejm\u00E9na lev\u00FDm p\u0159\u00EDtokem Berounky potokem V\u016Fznice. V\u00FD\u0161kov\u00E9 rozp\u011Bt\u00ED lokality D\u0159ev\u00ED\u010D je 220 a\u017E 435 m n. m. V\u00FDzkumn\u00E1 plocha n\u00E1le\u017E\u00ED k lesn\u00ED spr\u00E1v\u011B (LS) Ni\u017Ebor a rev\u00EDru D\u0159ev\u00ED\u010D."@cs .