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ZDRUŽBA BUKVE IN TRILISTNE VETRNICE
Anemono trifoliae–Fagetum Tregubov 1962
Združba bukve in trilistne vetrnice je conalna združba predalpsko-alpskega fitogeografskega območja ilirske florne province. Gozdove te asociacije uvrščamo med altimontansko-subalpinske, saj uspevajo nad nadmorsko višino 900 metrov do zgornje gozdne meje 1500 metrov. Prevladuje zmerno subpolarna klima, vlažna in hladna z obilo snega. Vegetacijsko obdobje je relativno kratko, od junija do oktobra, povprečno pade preko 2000 mm padavin letno, večina v dobi rasti. Prevladujejo strma do zelo strma bolj ali manj gladka pobočja. Zakrasele planote so redkejše. Osnovna geološka podlaga so večinoma dolomiti, apnenci so redkejši. Tla pod alpskimi bukovimi gozdovi so navadno slabo razvita; prevladujejo plitve do srednje globoke rendzine. Globlja rjava tla so le na apnčasti matični podlagi. Diagnostična kombinacija rastlinskih vrst Alpski bukov gozd ima stabilno biocenotsko zgradbo. Zaraščanje pašnikov na potencialno naravnem rastišču združbe se zaraščajo s smreko, v višjih legah se ji pridruži tudi macesen. Alpski bukovi gozdovi so večinoma enodobni, pogosto dvoplastni s prevladujočo smreko oziroma macesnom v zgornji plasti in podstojno bukvijo. Posebno gozdovi z obilno primesjo macesna so gospodarsko zelo pomembni. Del gozdov te združbe v bolj ekstremnih ekoloških razmerah ima varovalno vlogo. Združbo bukve in trilistne vetrnice uvrščamo v zvezo Aremonio-Fagion. |
The Anemono trifoliae–Fagetum is a zonal association of the prealpine-alpine phytogeographical territory of the Illyrian flora province. The forests of this association are altimontane-subalpine forests growing at an altitude of 900 meters to the upper forest boundary of 1,500 meters. A moderate subpolar, humid, and cold climate with plenty of snow is characteristic of this region. The vegetation period is relatively short, lasting from June to October, with a mean precipitation of more than 2,000 mm annually, mostly during the growth period. There are steep to very steep, more or less smooth slopes, and karst plateaus are more seldom. The basic geological material consists mostly of dolomite while limestone is more rare. The soils under the beech forests are not well developed, and shallow to medium deep rendzic Leptosols predominate. Deeper Cambisol is found only on limestone bedrock. Diagnostic combination of plant species The alpine beech forest has a stable biocenotic structure. The reforestation process on meadows on a potentially natural site of this association develops through Norway spruce (Picea abies) and at higher locations through European larch (Larix decidua). The alpine beech forests are mostly even-aged and often in two layers with predominantly spruce and larch in the upper layer and beech in the lower layer. In particular, the forests with abundant mixture of larch play an important economic role. Parts of the forests of this association play a protective role in more extreme ecological conditions. The Anemono trifoliae–Fagetum is classified in the alliance Aremonio–Fagion. |
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