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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Shifting zonal patterns of the southern boreal forest in eastern Canada associated with changing fire regime during the Holocene
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Shifting zonal patterns of the southern boreal forest in eastern Canada associated with changing fire regime during the Holocene

机译:全新世期间火势的变化与加拿大东部北方北方森林的带状变化

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摘要

This research aims at uncovering the stand-scale Holocene fire history of balsam fir forest stands from two bioclimatic zones of the boreal forest and assessing the existence of a sub-continental shift in past fire activity that could have triggered a change in the Holocene zonal pattern. In eastern Canada, the extant closed-crown boreal forest corresponds to two ecological regions separated along 49°N, the northern black spruce zone and the southern balsam fir zone. We sampled balsam fir stands from the southern fir zone (n=7) and among the northernmost patches of fir forest located far beyond the fir zone boundary, into the spruce zone (n=6). Macrofossil analysis of charcoal in mineral soils was used to reconstruct both the stand-scale and regional Holocene fire histories. Data were interpreted in the context of published palaeoecological evidence. Stands of the balsam fir zone were submitted to recurrent fire disturbances between c. 9000 and 5000. cal.yr. B.P. Local fire histories suggested that four sites within the fir zone escaped fire during the Holocene. Such fire protected sites allowed the continuous maintenance of the balsam fir forest in the southern boreal landscape. Stands of the spruce zone have been affected by recurrent fires from 5000. cal.yr. B.P. to present. Local fire histories indicated that no site escaped fire in this zone. Published palaeoecological data suggested that balsam fir migrated to its current northern limit sometime between 7300 and 6200. cal.yr. B.P. A change of the fire regime 5000 years ago caused the regional decline of an historical northern balsam fir forest and its replacement by black spruce forest. The consequence was a sub-continental reshuffling of the fir and spruce zones within the closed-crown boreal forest. The macrofossil analysis of charcoal in mineral soils was instrumental to the reconstruction of stand-scale Holocene fire history at sites where no other in situ fire proxies were available.
机译:这项研究的目的是从北方森林的两个生物气候带中发现苦瓜冷杉林分等级的全新世火史,并评估过去的火活动是否存在次大陆性变化,这可能触发了全新世地带格局的变化。 。在加拿大东部,现存的封闭式冠状北方森林对应于沿着49°N分开的两个生态区域,即北部的黑云杉带和南部的苦瓜冷杉带。我们从南部冷杉带(n = 7)和远在冷杉带边界之外的最北边的冷杉林片中抽取香脂冷杉林,进入云杉带(n = 6)。矿物土壤中木炭的宏观化石分析被用于重建林分规模和区域全新世的火史。在已发布的古生态证据的背景下解释了数据。苦瓜冷杉带的林分遭受了c。 9000和5000。 B.P.当地的火灾历史表明,在全新世期间,冷杉带内有四个地点逃脱了大火。这样的防火场所使南部寒带地区的香脂冷杉森林得以持续维护。从5000 cal.yr起,反复发生的火灾影响了云杉区域的林分。 B.P.展示。当地的火灾历史表明,该地区没有火灾发生。已发布的古生态数据表明,苦瓜冷杉在公元7300年至6200年之间迁移到了其当前的北限。 B.P. 5000年前火灾发生的变化导致了北部香脂冷杉森林的地区性衰退,并由黑云杉林代替。结果是封闭冠状北方森林内的冷杉和云杉区域发生了次大陆性改组。矿物土壤中木炭的宏观化石分析有助于在没有其他现场火灾代理的地点重建标准规模的全新世火灾历史。

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