首页> 外文期刊>Canadian Journal of Forest Research >Pre- and post-European settlement fire history of red pine dominated forest ecosystems of Seney National Wildlife Refuge, Upper Michigan
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Pre- and post-European settlement fire history of red pine dominated forest ecosystems of Seney National Wildlife Refuge, Upper Michigan

机译:上密歇根州塞尼国家野生动物保护区欧洲红松为主的森林生态系统在欧洲之前和之后的火灾历史

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摘要

To understand the dynamics of fire in red pine (Pinus resinosa Ait.) forest ecosystems that once dominated areas of the northern Lake States, we dendrochronologically reconstructed the fire regime prior to European settlement (pre-1860), after European settlement (1860-1935), and postrefuge establishment (post-1935) for different portions (wilderness and nonwilderness) and landforms (sand ridges and outwash channels) of the Seney National Wildlife Refuge (SNWR) in eastern Upper Michigan. Using data from 50 sites, we found that the cumulative number of fires showed a slow rate of accumulation from the 1700s to 1859, a steeper pattern suggesting higher fire occurrence from 1860 to 1935, and a return to fewer fires after 1935. Prior to European settlement, the fire cycle (FC) of sand ridge landforms interspersed within a poorly drained lacustrine plain in the Seney Wilderness Area was 91-144 years. This was longer than on glacial outwash channel landforms (53 years) and on sand ridge landforms interspersed within lacustrine plains located outside of the wilderness (47 years). The FC was also shorter (30 years) during this period and has subsequently increased (149-1090 years) after SNWR establishment. Differences in fire regimes among landform types were minor relative to the temporal variation in fire regimes among the three time periods.
机译:为了了解曾经主导北部湖州地区的赤松(Pinus resinosa Ait。)森林生态系统中的火灾动态,我们在欧洲人定居(1860-1935年)之后,欧洲定居之前(1860年之前)以树丛时间顺序重建了火情。 ),以及位于上密歇根州东部的塞尼国家野生动物保护区(SNWR)的不同部分(荒野和非荒野)和地形(沙脊和冲积通道)的避难所建立(1935年后)。使用来自50个站点的数据,我们发现从1700年代到1859年的累积火灾数量显示出缓慢的积累速度,更陡峭的格局表明从1860年到1935年发生的火灾次数更多,并且在1935年之后又减少了火灾次数。在塞尼荒野地区一个排水不畅的湖平原上散布的沙脊地貌的火循环(FC)为91-144年。这比在冰川冲刷河道地貌(53年)和散布在荒野外的湖平原上的沙脊地貌(47年)要长。在此期间,FC也较短(30年),随后在SNWR建立之后又增加了(149-1090年)。相对于三个时间间隔内火灾状况的时间变化,地貌类型之间的火灾状况差异较小。

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