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首页> 外文期刊>Biogeochemistry >The stable carbon and nitrogen isotopic composition of vegetation in tropical forests of the Amazon Basin, Brazil.
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The stable carbon and nitrogen isotopic composition of vegetation in tropical forests of the Amazon Basin, Brazil.

机译:巴西亚马逊河流域热带森林中植被的稳定碳氮同位素组成。

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摘要

Here we present the within-site, seasonal, and interannual variations of the carbon ( delta 13C) and nitrogen ( delta 15N) isotope ratios of leaves, wood, bark and litter from four sites in the Amazon region, Brazil. Samples were collected in Manaus (3 degrees 06'07"S; 60 degrees 01'30"W), Ji-Parana (10 degrees 53'07"S; 61 degrees 57'06"W), and Santarem (2 degrees 26'35"S; 54 degrees 42'30"W) with mean annual precipitation of 2207, 2040 and 1909 mm respectively. The overall average for all leaf samples was -32.3+or-2.5 per mil for delta 13C and +5.8+or-1.6 per mil for delta 15N (n=756). The leaf delta values at these sites were often but not always statistically distinct from each other. The delta 13C values varied from -37.8 per mil to -25.9 per mil. Pronounced differences in delta 13C values occurred with height associated with differences in forest structure. The delta 13C of leaf dry matter showed seasonal variations associated with the length of the dry season, despite the fact that total annual precipitation was similar among the studied sites. Leaf delta 15N values ranged from +0.9 per mil to a maximum value of +10.9 per mil, and the Santarem sites showed more enriched values than Manaus and Ji-Parana sites. No seasonal variation was detected in the delta 15N of leaves, but significant differences were observed among sites and with changes in canopy height. The isotope ratio data are consistent with our current understanding of the roles of light, water availability, and recycling of soil-respired CO2 influences on delta 13C and consistent with our understanding that an open nitrogen cycle can lead to high delta 15N values despite a significant number of legumes in the vegetation..
机译:在这里,我们介绍了巴西亚马逊地区四个地点的叶子,木材,树皮和凋落物的碳(δ13C)和氮(δ15N)同位素比的场内,季节和年际变化。在马瑙斯(3度06'07“ S; 60度01'30” W),Ji-Parana(10度53'07“ S; 61度57'06” W)和圣塔伦(2度26 '35“ S; 54度42'30” W),年平均降水量分别为2207、2040和1909 mm。对于13C,所有叶片样品的总体平均值为-32.3 +或-2.5 / mil,对于15N而言,所有叶片样品的总体平均平均值为+5.8+或-1.6(mil)(n = 756)。这些站点的叶子变化量值通常(但不总是)在统计上彼此不同。 Δ13C值从每密耳-37.8到每密耳-25.9不等。 δ13​​C值出现明显差异,而高度与森林结构差异有关。尽管研究地点之间的年总降水量相似,但叶片干物质的δ13C值显示出与旱季长度相关的季节变化。叶δ15N值的范围从每密耳+0.9到最大值,每密耳+10.9,并且Santarem站点显示的富集值比Manaus和Ji-Parana站点更多。在叶子的三角洲15N中未检测到季节变化,但是在站点之间以及冠层高度的变化中观察到了显着差异。同位素比数据与我们目前对光,水的可用性以及土壤呼吸的CO2的再循环对三角洲13C的影响的理解相一致,并且与我们的理解(尽管氮浓度显着升高,开放的氮循环可能导致高三角洲15N值)相符。植被中豆科植物的数量

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