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大气 CO2 浓度升高增加了沙漠灌木三齿滨藜对有机氮和无机氮的吸收。

Elevated CO2 increases plant uptake of organic and inorganic N in the desert shrub Larrea tridentata.

机构信息

Grassland, Soil and Water Research Laboratory, US Department of Agriculture, Agricultural Research Service, 808 E Blackland Road, Temple, TX 76502, USA.

出版信息

Oecologia. 2010 May;163(1):257-66. doi: 10.1007/s00442-010-1562-z. Epub 2010 Jan 22.

Abstract

Resource limitations, such as the availability of soil nitrogen (N), are expected to constrain continued increases in plant productivity under elevated atmospheric carbon dioxide (CO(2)). One potential but under-studied N source for supporting increased plant growth under elevated CO(2) is soil organic N. In arid ecosystems, there have been no studies examining plant organic N uptake to date. To assess the potential effects of elevated atmospheric CO(2) on plant N uptake dynamics, we quantified plant uptake of organic and inorganic N forms in the dominant desert shrub Larrea tridentata under controlled environmental conditions. Seedlings of L. tridentata were grown in the Mojave Desert (NV, USA) soils that had been continuously exposed to ambient or elevated atmospheric CO(2) for 8 years at the Nevada Desert FACE Facility. After 6 months of growth in environmentally controlled chambers under ambient (380 micromol mol(-1)) or elevated (600 micromol mol(-1)) CO(2), pots were injected with stable isotopically labeled sole-N sources ((13)C-[2]-(15)N glycine, (15)NH(4) (+), or (15)NO(3) (-)) and moved back to their respective chambers for the remainder of the study. Plants were destructively harvested at 0, 2, 10, 24, and 49 days. Plant uptake of soil N derived from glycine, NH(4) (+), and NO(3) (-) increased under elevated CO(2) at days 2 and 10. Further, root uptake of organic N as glycine occurred as intact amino acid within the first hour after N treatment, indicated by approximately 1:1 M enrichment ratios of (13)C:(15)N. Plant N uptake responses to elevated CO(2) are often species-specific and could potentially shift competitive interactions between co-occurring species. Thus, physiological changes in root N uptake dynamics coupled with previously observed changes in the availability of soil N resources could impact plant community structure as well as ecosystem nutrient cycling under increasing atmospheric CO(2) levels in the Mojave Desert.

摘要

资源限制,如土壤氮(N)的可利用性,预计将限制在大气二氧化碳(CO2)升高的情况下植物生产力的持续提高。在大气 CO2 升高的情况下,支持植物生长的一个潜在但研究不足的 N 源是土壤有机 N。在干旱生态系统中,目前还没有研究考察植物有机 N 吸收。为了评估大气 CO2 升高对植物 N 吸收动态的潜在影响,我们在受控环境条件下量化了优势沙漠灌木 Larrea tridentata 对有机和无机 N 形式的植物吸收。在莫哈韦沙漠(内华达州,美国)的土壤中种植 L. tridentata 的幼苗,这些土壤已经在内华达州荒漠 FACE 设施中连续暴露于环境或升高的大气 CO2 8 年。在环境控制室中生长 6 个月后,在环境(380 μmol mol(-1)) 或升高(600 μmol mol(-1)) CO2 下,将花盆注入稳定同位素标记的单一 N 源((13)C-[2]-(15)N 甘氨酸、(15)NH(4) (+)或(15)NO(3) (-)),并在研究的其余部分将其移回各自的室中。植物在 0、2、10、24 和 49 天时被破坏性收获。在升高的 CO2 下,植物对源自甘氨酸、NH(4) (+)和 NO(3) (-)的土壤 N 的吸收在第 2 和 10 天增加。此外,在 N 处理后第一个小时内,植物根系对有机 N(如甘氨酸)的吸收以完整氨基酸的形式发生,(13)C:(15)N 的富集比约为 1:1。植物对 CO2 升高的 N 吸收反应通常是物种特异性的,并且可能会改变共存物种之间的竞争相互作用。因此,根 N 吸收动态的生理变化加上先前观察到的土壤 N 资源可用性的变化,可能会影响莫哈韦沙漠大气 CO2 水平升高下的植物群落结构以及生态系统养分循环。

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