A forest that grows green leaves in warm summers and loses its leaves in cold winters. Summer-green high tree forests form a typical temperate zone, and are developed in Europe at latitudes 40° to 60° north, and in North America and Asia at latitudes 30° to 50° north. In Japan, they occur in areas at altitudes of 600 to 1700m in central Japan, and on the plains of Hokkaido. They are a mixture of chestnut, alder, Japanese oak, maple, hornbeam, elm, horse chestnut, and katsura, but are roughly divided into a chestnut zone in the lowlands, an oak zone in the middle areas, and a beech zone in the highlands. Shade-loving beech trees form climax forests. The most representative sun-loving tree is the silver birch. Before the leaves grow thick on the treetops from spring to early summer, spring plants such as Anemone (→ Anemone) and Viola (→ Violet) flower and produce fruit on the forest floor, and the seasonal changes of new green leaves, autumn leaves (yellow leaves), and fallen leaves are remarkable. Small-scale summer-green shrubs are commonly found near the tree line, and in the high mountains of Japan there are shrubs of Alnus alder, Betula ermanii, and Rowan alpine. (→ Community) Source: Encyclopaedia Britannica Concise Encyclopedia About Encyclopaedia Britannica Concise Encyclopedia Information |
温暖な夏に緑葉をつけて活動し,寒冷な冬に落葉する森林。夏緑高木林は温帯の代表的植物帯をつくり,ヨーロッパで北緯 40°~60°,北アメリカとアジアで北緯 30°~50°の地域に発達。日本では中部で標高 600~1700mの地域,北海道では平地に生じる。クリ,ハンノキ,ミズナラ,カエデ,シデ,ニレ,トチノキ,カツラなど混合するが,おおまかには低地のクリ帯,中間地のナラ帯,高地のブナ帯に区分される。陰樹のブナが極相林をつくる。陽樹の代表はシラカバ。春から初夏の樹冠の葉が茂る前に,林床にアネモネ属(→アネモネ),スミレ属(→スミレ)のような春植物が開花結実し,新緑,紅葉(黄葉),落葉の季節変化が著しい。夏緑低木林は,森林限界付近に小規模のものが普通にみられ,日本の高山にはミヤマハンノキ,ダケカンバ,タカネナナカマドの低木林がある。(→群系)
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