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Tree ring evidence of rapid development of drunken forest induced by permafrost warming

机译:多年冻土增温诱发醉林快速发育的树木年轮证据

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Abstract Black spruce trees growing on warming permafrost lean in all directions due to soil movement, forming a “drunken” forest. Two hypothetical drivers of drunken forest development are (i) loosening of the soil foundation induced by permafrost degradation in warm summers and (ii) mound rising induced by freezing soil in winter. However, no evidence has previously clarified whether recent tree leaning is related to climate warming or is part of a natural hummock formation process. Here, we provide evidence that tree leaning and soil hummock formation have accelerated due to climate warming. We find that trees’ leaning events synchronize with the development of soil hummocks as recorded in tree rings with lignin‐rich cells. Tree leaning is caused by mound rising in winter due to refreezing of soil following deep thaws in summer, rather than by loosening of the soil foundation in summer. Hummock formation shifted from periodic events before 1960 to continuous mound rising in the warmer succeeding 50 years. Although soil change is generally a slow process, recent permafrost warming has induced rapid hummock formation, which threatens the stability of drunken forests and organic carbon in soil hummocks based on shallow permafrost table.
机译:摘要 生长在变暖的永久冻土层上的黑云杉树因土壤运动而向四面八方倾斜,形成“醉”林。醉林发育的两个假设驱动因素是:(i)夏季多年冻土退化引起的土壤基础松动和(ii)冬季冻土引起的土丘上升。然而,以前没有证据表明最近的树木倾斜是否与气候变暖有关,或者是自然丘陵形成过程的一部分。在这里,我们提供了证据表明,由于气候变暖,树木倾斜和土壤丘陵的形成加速了。我们发现树木的倾斜事件与土壤丘陵的发育同步,如富含木质素细胞的树木年轮所记录的那样。树木倾斜是由于冬季土丘上升,由于夏季深度解冻后土壤重新冻结,而不是夏季土壤基础松动引起的。丘陵的形成从1960年之前的周期性事件转变为随后50年温暖的丘陵的持续上升。虽然土壤变化总体上是一个缓慢的过程,但近年来多年冻土变暖导致了快速的丘陵形成,威胁着醉林的稳定性和基于浅层永久冻土表的土壤丘陵中的有机碳。

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