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Park Tundra Park tundra was a plant community that occurred in northwestern Europe after the last ice age ended. The community was similar to that found today at the boundary between tundra and taiga in Siberia: species included the dwarf birch and the least willow. Park tundra stretched as far south as the Alps and the Pyrenees.〔 Park tundra was common during the colder post-glacial periods, such as the Older Dryas (12,000-10,000 BCE) and the Younger Dryas (8800-8300 BCE).〔 ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Park Tundra」の詳細全文を読む
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