Geographical changes in the vegetation pattern of raised bogs in the Bay of Fundy region of Maine and New Brunswick
Geographical changes in the vegetation pattern of raised bogs in the Bay of Fundy region of Maine and New Brunswick
复制标题
缅因州和新不伦瑞克芬迪湾地区凸起沼泽植被格局的地理变化
DOI：
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发表时间：
1977
期刊：
影响因子：
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通讯作者：
A. W. Damman
中科院分区：
文献类型：
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作者：
A. W. Damman
在北美东部，隆起的沼泽大致出现在连接站的线的北部和东部，根据10 cm的土壤蓄水量，平均每年缺水（Thornthwaite 1948）（图1）。在其分布区的南部，它们在芬迪湾附近的一个地区特别丰富，该地区或多或少与哥伦比亚森林区的芬迪海岸部分（Rowe 1972）和戴维斯（Davis 1966）绘制的云杉冷杉林区域相对应。
In eastern North America raised bogs occur roughly north and east of a line connecting stations with an average annual water deficiency (Thornthwaite 1948) based on a soil storage capacity of 10 cm (Figure 1). In the southern part of their range they are particularly abundant in an area near the Bay of Fundy which corresponds more or less with the Fundy Coast Section of the Acadian Forest Region (Rowe 1972) and the area mapped as spruce fir forest by Davis (1966).