首页> 外文期刊>The holocene >Long-term fire and forest history of subalpine balsam fir (Abies balsamea) and white spruce (Picea glauca) stands in eastern Canada inferred from soil charcoal analysis
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Long-term fire and forest history of subalpine balsam fir (Abies balsamea) and white spruce (Picea glauca) stands in eastern Canada inferred from soil charcoal analysis

机译:根据土壤木炭分析推断,加拿大东部的亚高山香脂冷杉(Abies balsamea)和白云杉(Picea glauca)的长期火灾和森林历史

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The northernmost balsam fir forest in eastern Canada forms disjunct stands far beyond the extensive balsam fir forest zone of southern Canada. The northern balsam fir stands are distributed in the subalpine belt of high plateaus and coexist locally with white spruce stands. These subalpine stands contrast greatly with black spruce forest stands located in lowlands. Given that subalpine stands are remnants of an earlier northern expansion of the balsam fir forest, the main objective of this study is to assess whether white spruce stands are distinct communities having diverged from the balsam fir forest community earlier in the Holocene or if they rather correspond to a different stage of the chronosequence within the subalpine belt. Macrofossil analysis of charcoal in mineral soils was used to compare the stand-scale fire histories and taxonomic fossil composition of subalpine, old-growth balsam fir stands and white spruce stands. No significant differences of mean number of observed fires (mean = 6.35 fires per site), Holocene fire recurrence at the landscape scale and mean fire-return interval (mean = 580 years) were found between white spruce stands and balsam fir stands.The botanical composition of charcoal fragments from mineral soils showed that Abies, Betula and Picea were present throughout the fire period from 5600 cal. BP to present, and no difference was found in the fossil composition of the balsam fir and white spruce stands. No historical change in the botanical composition of charcoal from soils of both stand types was observed indicating that the initial floristic composition remained through the period of recurrent fires. Charcoal data suggest that white spruce stands are not divergent community types. Rather, the two community types are arranged along a chronosequence of different successional stages within the subalpine relict flora.
机译:加拿大东部最北端的苦瓜冷杉林形成了分离的立地,远远超出了加拿大南部广阔的苦瓜冷杉林区。北部的苦瓜冷杉林分分布在高原的亚高山带,并与白色云杉林共存。这些亚高山林地与位于低地的黑云杉林林地形成鲜明对比。鉴于亚高山林是香脂冷杉森林早期向北扩展的残余物,因此本研究的主要目的是评估白云杉林是否是全新世早期与香脂冷杉森林群落不同的独特群落,或者它们是否对应到亚高山带内时间序列的不同阶段。用矿物化石中的木炭进行宏观化石分析,以比较林分规模的火史和亚高山,老生长的苦瓜冷杉林和白云杉林的分类学化石成分。白云杉林与苦瓜冷杉林分之间没有观察到平均火势平均数(平均= 6.35火势),景观规模上的全新世火情复发和平均火归还间隔(平均= 580年)的显着差异。矿物土壤中木炭碎片的组成表明,在整个5600 cal的火灾期间,都存在Abies,Betula和Picea。 BP到现在为止,香脂冷杉和白色云杉林的化石组成没有发现差异。在两种林分类型的土壤中,未观察到木炭的植物成分的历史变化,这表明在反复发生的火灾期间,初始植物区系成分仍然存在。木炭数据表明,白云杉林分并不是不同的群落类型。相反,这两种群落类型是沿着亚高山遗迹群内不同演替阶段的时间顺序排列的。

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