DIGITALNA ARHIVA ŠUMARSKOG LISTA
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S. Redžić, S. Barudanović: THE PETTERNS OF DYVERSITY OF FORESTVEGETATION OF THE CRVANJ ...Šumarski list br. 5–6, CXXXIV (2010), 261-274 (all stations). During the vegetation period climate isThe climate of lower parts of Crvanj Mt. is mainly semiarid, arid and semihumid (Redžić&al., 2000).submontane, with more or less distinct maritime influence. Kalinovik area is characterised by montane cli- Assessed thermic character of climate is temperate mate, with certain level of maritime influences.Toward warm for stations Gacko and Nevesinje, but temperate to the top of mountain, climate character is transformed cold for station Kalinovik.Assessed thermic character to typical mountain, and on highest peak has certain at- during the vegetation period is warm to teperate warm. tributes of mild alpine climate. Period of winter is tem- Relative air humidity varies between 75 to 80 % du perate cold, and summer temperate warm. ring the year. During the vegetation period it is between According to annual isothermic maps –The clima 58 to 76 %.The annual average of cloudiness is bet- tic atlas of ex-SFRJ (Ak,1967), and temperature gra ween 51 to 63 %.The lowest cloudiness is recorded dudient, it has been shown that the air temperature of the ring summer months. highest part of Crvanj is about 2 oC. According to Milosavljević(1973) investigated area is considered as moderate bright, i.e. moderate cloudy part of Bosnia and Herzegovina. 3. RESULTS AND DISCUSSION – Rezultati rada i diskusija Syntaxonomical review of forest vegetation– Sintaksonomski pregled šumske vegetacije QUERCO-FAGETEABr. – Bl. & Vlieger inVlieger 1937 QUERCETALIA PUBESCENTISKlika 1933 (=Quercetalia pubescentisBr. – Bl. /1931 n.nud./1932) Quercion petraeae – cerris[(Lakušić 1976) Lakušić & Jovanović 1980] Čarni et al. 2009 Quercetum petraeae – cerrisB. Jovanović (1960)1979seslerietosum autumnalissubas. nova hoc loco EUNIS code G1.7 FAGETALIA SYLVATICAEPawlowski in Pawłowski & al. 1928 Erythronio-Carpinion betuli(Horvat 1958) Marinček in Mucina et al. 1993 Querco – Carpinetum betuliHorvat 1938 emend. Blečić 1958 subas.quercetosum cerrisStefanović 1964 aposeriosum foetidaefacies nov hoc loco EUNIS code G1.A/P-41.24 Seslerio-Fagion sylvaticaenomen nov hoc loco (Syn.:Fagion moesiacae Blečić & Lakušić 1970; Incl.Fagenion moesiacae „montanum”B. Jovanović 1976) Lathyro verni-Fagetum sylvaticaeRedžić 2007 nom. nov (Syn.:Fagetum moesiacae montanumBlečić & Lakušić 1970) EUNIS code G1.6/P-41.1B Seslerio autumnalis-FagetumB. Jovanović 1976 EUNIS code G1.6/P-41.16 Phyteumo spicatae-FagetumBarudanović 2003 (Syn.:Aceri – Fagetum subalpinumFukarek & Stefanović 1958 emend. Fukarek1969) EUNIS code G1.6/P-41.15 Review of forest phytocoenoses – Pregled šumskih fitocenoza Class:QUERCO-FAGETEABr.-Bl. & Vlieger inVlieger 1937 Order: QUERCETALIA PUBESCENTISKlika 1933 Alliance:Quercion petraeae – cerris[(Lakušić 1976) Lakušić & Jovanović 1980]Čarni et al. 2009 Ass.:Quercetum petraeae – cerris B. Jovanović (1960) 1979seslerietosum autumnalis subas. nova (Nomenclature type: Releve 1,Tab.1; Diagnostic species: Sesleria autumnalis, Helleborus odorus, Lembotropis nigricans) The separate vegetation belt is formed by communi-of one of mentioned species are found on certain aspect ties of durmast andTurkey oak. It is found in the lowestand inclination. The species of High level of signifipart of Crvanj, from 670 m altitude going to the Lake,cance, as diagnostic species, have:Fraxinus ornus, Vi- at SE aspect with inclination cca 30°.burnum lantana, Sorbus torminalis, Quercus cerris, Geological foundation on sites is silicate stone andAcer monspessulanum, Lembotropis nigricans, Silene limestone in series with silicates. The soil is districnutans, Verbascum nigrum, Potentilla micrantha, Hellecambisol where eroded humus–accumulative horizontborus multifidus, Lychnis coronaria, Sesleria autumnais determined.lisand other (Tab. 1). In the tree stratum durmast and Turkey oaks are equally present.Although communities with domination |