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Structure, composition, and diversity of old-growth black spruce boreal forest of the Clay Belt region in Quebec and Ontario

机译:魁北克和安大略省粘土带地区的老龄黑云杉北方森林的结构,组成和多样性

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Old-growth black spruce (Picea mariana) boreal forest in the Clay Belt region of Ontario and Quebec is an open forest with a low canopy, quite different from what many consider to be "old growth". Here, we provide an overview of the characteristicsof old-growth black spruce forest for three different site types on organic, clay, and coarse deposits. Our objectives were (1) to identify the extent of older forests; (2) to describe the structure, composition, and diversity in different age classes; and (3) to identify key processes in old-growth black spruce forest. We sampled canopy composition, deadwood abundance, understorey composition, and nonvascular plant species in 91 forest stands along a chronosequence that extended from 20 to more than 250years after fire. We used a peak in tree basal area, which occurred at 100 years on clay and coarse sites and at 200 years on organic sites, as a process-based means of defining the start of old-growth forest. Old-growth forests are extensive in the Clay Belt, covering 30-50 percent of the forested landscape. Black spruce was dominant on all organic sites, and in all older stands. Although there were fewer understorey species and none exclusive to old-growth, these forests were structurally diverse andhad greater abundance of Sphagnum, epiphytic lichens, and ericaceous species. Paludification, a process characteristic of old-growth forest stands on clay deposits in this region, causes decreases in tree and deadwood abundance. Old-growth black spruceforests, therefore, lack the large trees and stags that are characteristic of other old-growth forests. Small-scale disturbances such as spruce budworm and windthrow are common, creating numerous gaps. Landscape and stand level management strategies couldminimize structural changes caused by harvesting, but unmanaged forest in all stages of development must be preserved in order to conserve all the attributes of old-growth black spruce forest.
机译:安大略和魁北克粘土带地区的老龄黑云杉(Picea mariana)寒带林是一个开放的森林,树冠较低,与许多人认为的“老龄化”完全不同。在这里,我们提供了针对有机,黏土和粗沉积物上三种不同站点类型的老式黑云杉林特征的概述。我们的目标是(1)确定较老的森林的范围; (2)描述不同年龄段的结构,组成和多样性; (3)确定老龄黑云杉林的关键过程。我们对91个林分中的冠层组成,枯木丰度,下层组成和非维管植物物种进行了采样,其时间顺序从火灾后20年延长到250年以上。我们使用了树木基部区域的峰值,该峰值发生在粘土和粗地上的100年,有机区域上的200年,作为基于过程的方法来定义旧林的开始。粘土带的原始森林茂盛,覆盖了30%至50%的森林景观。在所有有机地点和所有较旧的林分中,黑云杉均占主导地位。尽管下层物种较少,而且没有仅旧树种,但是这些森林的结构多样,并且有大量的泥炭藓,附生地衣和毛果树种。龟裂化是该地区老龄森林的一个过程特征,它位于粘土沉积物上,导致树木和枯木的丰度下降。因此,古老的黑云杉林缺少其他古老的森林所特有的大树和雄鹿。小规模的干扰,例如云杉芽虫和风疹,很常见,造成了许多空白。景观和林分水平管理策略可以最大程度地减少因采伐引起的结构变化,但是必须保护处于开发各个阶段的未经管理的森林,以保护老龄黑云杉林的所有属性。

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