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首页> 外文期刊>Frontiers in Plant Science >15N in tree rings as a bio-indicator of changing nitrogen cycling in tropical forests: an evaluation at three sites using two sampling methods
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15N in tree rings as a bio-indicator of changing nitrogen cycling in tropical forests: an evaluation at three sites using two sampling methods

机译:年轮中的 15 N是热带森林中氮循环变化的生物指标:使用两种采样方法在三个地点进行的评估

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Anthropogenic nitrogen deposition is currently causing a more than twofold increase of reactive nitrogen input over large areas in the tropics. Elevated~(15)N abundance (δ~(15)N) in the growth rings of some tropical trees has been hypothesized to reflect an increased leaching of~(15)N-depleted nitrate from the soil, following anthropogenic nitrogen deposition over the last decades. To find further evidence for altered nitrogen cycling in tropical forests, we measured long-term δ~(15)N values in trees from Bolivia, Cameroon, and Thailand. We used two different sampling methods. In the first, wood samples were taken in a conventional way: from the pith to the bark across the stem of 28 large trees (the “radial” method). In the second, δ~(15)N values were compared across a fixed diameter (the “fixed-diameter” method). We sampled 400 trees that differed widely in size, but measured δ~(15)N in the stem around the same diameter (20 cm dbh) in all trees. As a result, the growth rings formed around this diameter differed in age and allowed a comparison of δ~(15)N values over time with an explicit control for potential size-effects on δ~(15)N values. We found a significant increase of tree-ring δ~(15)N across the stem radius of large trees from Bolivia and Cameroon, but no change in tree-ring δ~(15)N values over time was found in any of the study sites when controlling for tree size. This suggests that radial trends of δ~(15)N values within trees reflect tree ontogeny (size development). However, for the trees from Cameroon and Thailand, a low statistical power in the fixed-diameter method prevents to conclude this with high certainty. For the trees from Bolivia, statistical power in the fixed-diameter method was high, showing that the temporal trend in tree-ring δ~(15)N values in the radial method is primarily caused by tree ontogeny and unlikely by a change in nitrogen cycling. We therefore stress to account for tree size before tree-ring δ~(15)N values can be properly interpreted.
机译:目前,人为氮的沉积使热带地区大面积的反应性氮输入增加了两倍以上。据推测,某些热带树木年轮中〜(15)N丰度(δ〜(15)N)升高,反映出人为氮沉积在土壤上之后,〜(15)N贫化硝酸盐从土壤中的淋失增加。最后几十年。为了找到热带森林中氮循环变化的进一步证据,我们测量了玻利维亚,喀麦隆和泰国树木的长期δ〜(15)N值。我们使用了两种不同的采样方法。首先,以常规方式采集木材样品:从髓到树皮,横穿28棵大树的茎(“径向”方法)。第二,比较固定直径下的δ〜(15)N值(“固定直径”方法)。我们对400棵大小不同的树木进行了采样,但在所有树木中,相同直径(20 cm dbh)的茎中测得的δ〜(15)N。结果,在该直径附近形成的生长环的年龄不同,并且可以随时间比较δ〜(15)N值,并明确控制δ〜(15)N值的潜在大小效应。我们发现,来自玻利维亚和喀麦隆的大树的茎径上的树木年轮δ〜(15)N显着增加,但是在任何一项研究中都没有发现树木年轮的δ〜(15)N值随时间变化控制树大小时的站点。这表明树木中δ〜(15)N值的径向趋势反映了树木的个体发育(大小发展)。但是,对于来自喀麦隆和泰国的树木,固定直径方法的统计功效较低,因此无法高度肯定地得出结论。对于来自玻利维亚的树木,固定直径方法的统计功效很高,这表明径向方法中树木年轮δ〜(15)N值的时间趋势主要是由树木个体发育引起的,而氮的变化不太可能引起循环。因此,我们强调在树环δ〜(15)N值可以正确解释之前,要考虑树的大小。

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