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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:树木年轮中的15 N作为改变热带森林中氮循环的生物指标:使用两种采样方法在三个地点进行评估

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摘要

Anthropogenic nitrogen deposition is currently causing a more than twofold increase of reactive nitrogen input over large areas in the tropics. Elevated 15N abundance (δ15N) in the growth rings of some tropical trees has been hypothesized to reflect an increased leaching of 15N-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 δ15N 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, δ15N values were compared across a fixed diameter (the “fixed-diameter” method). We sampled 400 trees that differed widely in size, but measured δ15N 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 δ15N values over time with an explicit control for potential size-effects on δ15N values. We found a significant increase of tree-ring δ15N across the stem radius of large trees from Bolivia and Cameroon, but no change in tree-ring δ15N values over time was found in any of the study sites when controlling for tree size. This suggests that radial trends of δ15N 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 δ15N 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 δ15N 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的 15 N-丰度(δ 15 N)升高反映了 15 N-的淋溶增加。在过去的几十年中,由于人为的氮沉积,土壤中的硝酸盐消耗尽。为了找到进一步的证据来证明热带森林中氮循环的改变,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本: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棵树木进行了采样,这些树木的大小差异很大,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个值。我们发现,来自玻利维亚和喀麦隆的大树的茎径上的树环δ 15 N显着增加,但在整个树丛中,树环δ 15 N值没有变化控制树木大小时,在任何研究地点都发现了时间。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,而不太可能由氮循环的变化。因此,我们强调要在树环的δ 15 N值能够正确解释之前考虑树的大小。

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