Phytogeographical relationships of plant communities of the upper part of the Taisetsu mountain range, central Hokkaido, northern Japan, to plant communities of the northern boreal subzone of Far East Russia is discussed. Three major plant communities exist on the upper part of the Taisetsu mountain range. These are in the vertical order from the lower part of the mountain the
Betula ermanii forest, the
Pinus pumila thickets, and the wind-exposed dwarf shrubs. However, the fact is these three plant communities co-exist within a potential
Betula ermanii forest zone. Those three plant communities all have their phytogeographically corresponding plant communities within the same northern boreal subzone of Far East Russia, which has different continental-oceanic sectors (C1, OC, O1, and O2 sectors from the continental to oceanic). The
Betula ermanii forest corresponds to the
Betula ermanii forest in the Kamchatka Peninsula of O1 sector associated with an oceanic climate, the
Pinus pumila thickets to the
Larix gmelinii -
Pinus pumila, forest in the Kolyma and Koryak Hills of C1 and OC sector associated with a relatively continental climate, and the wind exposed dwarf shrubs to the treeless heaths in the Kurile Islands of O2 sector associated with a extremely oceanic climate. Apparent vertical arrangement of these three plant communities on the upper part of the Taisetsu mountain range was inconsistent with the horizontal arrangement in the northern boreal subzone of Far East Russia that consists of, from the continental to extremely oceanic sector, the
Larix gmelinii -
Pinus pumila forest, the
Betula ermanii forest, and the treeless heath community. Strong winds and heavy snowfalls in winter in the Taisetsu mountain range promoted such vertical plant community arrangement of the mountain that is inconsistent with the horizontal sector distribution in the northern boreal subzone of Far East Russia.
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