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Holocene variations of wildfire occurrence as a guide for sustainable management of the northeastern Canadian boreal forest

机译:野火发生的全新世变化作为加拿大东北北方森林可持续管理的指南

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Background: Cumulative impacts of wildfires and forest harvesting can cause shifts from closed-crown forest to open woodland in boreal ecosystems. To lower the probability of occurrence of such catastrophic regime shifts,forest logging must decrease when fire frequency increases, so that the combined disturbance rate does not exceed the Holocene maximum. Knowing how climate warming will affect fire regimes is thus crucial to sustainably manage the forest. This study aimed to provide a guide to determine sustainable forest harvesting levels, by reconstructing the Holocene fire history at the northern limit of commercial forestry in Quebec using charcoal particles preserved in lake sediments.Methods: Sediment cores were sampled from four lakes located close to the northern limit of commercial forestry in Quebec. The cores were sliced into consecutive 0.5 cm thick subsamples from which 1 cm3 was extracted to count and measure charcoal particles larger than 150 microns. Age-depth models were obtained for each core based on accelerator mass spectroscopy(AMS) radiocarbon dates. Holocene fire histories were reconstructed by combining charcoal counts and age-depth models to obtain charcoal accumulation rates and, after statistical treatment,long-term trends in fire occurrence(expressed as number of fires per 1000 years).Results: Fire occurrence varied between the four studied sites, but fires generally occurred more often during warm and dry periods of the Holocene, especially during the Holocene Thermal Maximum(7000–3500 cal. BP), when fire occurrence was twice as high as at present.Conclusions: The current fire regime in the study area is still within the natural range of variability observed over the Holocene. However, climatic conditions comparable to the Holocene Thermal Maximum could be reached within the next few decades, thus substantially reducing the amount of wood available to the forest industry.
机译:背景:野火和森林砍伐的累积影响可能导致北方生态系统中的封闭森林转变为开阔的林地。为了降低发生此类灾难性政权转移的可能性,当火灾频率增加时,必须减少森林采伐,以使综合干扰率不超过全新世最大值。因此,了解气候变暖将如何影响火势对于可持续管理森林至关重要。这项研究旨在通过使用沉积在湖中的木炭颗粒重建魁北克商业森林北部极限的全新世火灾历史,为确定可持续的森林采伐水平提供指导。魁北克商业林业的北限。将核心切成连续的0.5厘米厚的子样本,从中提取1立方厘米以计数和测量大于150微米的木炭颗粒。基于加速器质谱(AMS)放射性碳数据,获得了每个岩心的年龄深度模型。通过结合木炭计数和年龄深度模型重建全新世的火灾历史,以获得木炭积累率,并经过统计处理,得出火灾的长期趋势(以每1000年的火灾次数表示)。结果:有四个研究点,但是大火通常在全新世的温暖和干燥期间发生,特别是在全新世最高温度(7000–3500 cal。BP)期间,当时的火灾发生率是目前的两倍。研究区的气候变化仍然处于全新世观测到的自然变化范围之内。但是,在接下来的几十年内,将达到与全新世最高温度相当的气候条件,从而大大减少了可用于林业的木材数量。

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