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Permafrost

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territories have natural and anthropogenic origin.<br />

Eventually, all disturbed habitats with well drainage in the permafrost areas of strong<br />

continental climate with small precipitations (tundra, forest-tundra, taiga) are grown over by<br />

steppe plants (almost all Yakutia, Zabaikalie). The projective cover of these plants is small. Soil<br />

similar to steppe ones are also formed: humus is accumulated but not peat, soil reaction is about<br />

neutral, and the amount of exchangeable calcium and magnesium increases. The humus content<br />

accounts for 1 – 1,5 % in upper horizons of minor soils and about 3 - 8 % in fine earth from<br />

grass tussock. All investigated soils have neutral or close to neutral reaction. This process was<br />

not market in Tynda (Amur region) because of the influence of Far East monsoon climate on<br />

this region. This process was not market too in northern-western seaside part of Yakutia with<br />

frequent drizzling rains (Tiksi, Chokhurdakh, Khroma bay) where disturbed habitats are grown<br />

over by pioneer and apophyte vegetation. Such situation is near Vorkuta (tundra), Labytnangi<br />

and Salechard (Yamal, forest-tundra), Khatanga (tundra) where the climate is more humid then<br />

in north-east of Russia. We known from scientific publication that analogical situation exist in<br />

north of European part of Russia too.<br />

It is necessary to tell separately about pine forests. The pine forests are wide-spread in<br />

Zabaikalye and in neighbouring territories. They grow on sandy sediment in intermountain<br />

valleys. These forests penetrated into a steppe zone of Mongolia through high sandy ridge. They<br />

were investigated in Verhnyeangarskaya depression during 2004 year (around Novy Uoyan<br />

settlement, northwest of Buryatia).<br />

The area is located in Moscow latitude. True altitude is more than 500 m. These pine<br />

forests are "classical" types. Litter or lichen pine forests grow on high sandy ridge,<br />

grass-cowberry-lichen forests distributed on flat surface. Soils here are sandy weakly podzolic<br />

and podburs. The permafrost is deeply and does not affect the pedogenesis.<br />

Forests around of settlement are under strong anthropogenic stress: unpaved roads, groove,<br />

wood dumps and other. Light sands are formed here too. Disturbed sites slowly obliterate with<br />

pioneer plants, and then steppe ones: wormwoods, thyme, steppe grasses and etc. Lawns in<br />

settlement have steppe aspect also. Pioneer and steppe plants cover roadsides from railway<br />

station to northwest.<br />

The pine forests will be replaced by steppe as it takes place in south Buryatia without<br />

application of special security measures.<br />

Key words: Disturbed habitats, permafrost regions, pioneer plants, apophyte plants, steppe<br />

plants and soils<br />

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