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首页> 外文期刊>Global change biology >In situ litter decomposition and litter quality in a Mojave Desert ecosystem: effects of elevated atmospheric CO2 and interannual climate variability
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In situ litter decomposition and litter quality in a Mojave Desert ecosystem: effects of elevated atmospheric CO2 and interannual climate variability

机译:莫哈韦沙漠生态系统中的原地凋落物分解和凋落物质量:大气CO2升高和年际气候变化的影响

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Rising atmospheric CO2 has been predicted to reduce litter decomposition as a result of CO2 -induced reductions in litter quality. However, available data have not supported this hypothesis in mesic ecosystems, and no data are available for desert or semi-arid ecosystems, which account for more than 35% of the Earth's land area. The objective of our study was to explore controls on litter decomposition in the Mojave Desert using elevated CO2 and interannual climate variability as driving environmental factors. In particular, we sought to evaluate the extent to which decomposition is modulated by litter chemistry (C:N) and litter species and tissue composition. Naturally senesced litter was collected from each of nine 25 m diameter experimental plots, with six plots exposed to ambient [CO2 ] or 367 muL CO2 L-1 and three plots continuously fumigated with elevated [CO2 ] (550 muL CO2 L-1 ) using FACE technology beginning in April 1997. All litter collected in 1998 (a wet, or El Nino year; 306 mm precipitation) was pooled as was litter collected in 1999 (a dry year; 94 mm). Samples were allowed to decompose for 4 and 12 months starting in May 2001 in mesh litterbags in the locations from which litter was collected. Decomposition of litter produced under elevated CO2 and ambient CO2 did not differ. Litter produced in the wetter year showed more rapid initial decomposition (over the first 4 months) than that produced in the drier year (27+/-2% yr(-1) or 7.8+/-0.7 g m(-2) yr(-1) for 1998 litter; 18+/-3% yr(-1) or 2.2+/-0.4 g m(-2) yr(-1) for 1999 litter). C:N ratios of litter produced under elevated CO2 (wet year: 37+/-0.5; dry year: 42+/-2.5) were higher than those of litter produced under ambient CO2 (wet year: 34+/-1.1; dry year: 35+/-1.4). Litter production in the wet year (amb. CO2 : 25.1+/-1.1 g m(-2) yr(-1) ; elev. CO2 : 35.0+/-1.1 g m(-2) yr(-1) ) was more than twice as high as that in the dry year (amb. CO2 : 11.6+/-1.7 g m(-2) , elev. CO2 : 13.3+/-3.4 g m(-2) ), and contained a greater proportion of Lycium pallidum and a lower proportion of Larrea tridentata than litter produced in the dry year. Decomposition, viewed across all treatments, decreased with increasing C:N ratios, decreased with increasing proportions of Larrea tridentata and increased with increasing proportions of Lycium pallidum and Lycium andersonii . Because litter C:N did not vary by litter production year, and CO2 did not alter decomposition or litter species/tissue composition, it is likely that the impact of year-to-year variation in precipitation on the proportion of key plant species in the litter may be the most important way in which litter decomposition will be modulated in the Mojave Desert under future rising atmospheric CO2 . [References: 38]
机译:据预测,由于CO2引起的垫料质量下降,大气CO2升高会减少垫料分解。但是,现有的数据并不能支持内陆生态系统中的这一假设,也没有沙漠或半干旱生态系统的数据,沙漠或半干旱生态系统占地球陆地面积的35%以上。我们研究的目的是探索利用更高的CO2和年际气候变化作为驱动环境因素来控制莫哈韦沙漠垃圾分解的控制措施。特别是,我们试图评估分解的程度受垫料化学(C:N)和垫料种类及组织组成的调节。从9个25 m直径的实验地块中的每一个中收集自然衰落的凋落物,其中6个地块暴露于环境[CO2]或367μLCO2 L-1,三个地块使用升高的[CO2](550 muL CO2 L-1)连续熏蒸。 FACE技术始于1997年4月。汇集了1998年(潮湿或厄尔尼诺年; 306毫米降水)收集的所有垃圾,以及1999年(干燥年; 94毫米)收集的垃圾。从2001年5月开始,在收集垃圾的地点的网状垃圾袋中将样品分解4个月和12个月。在升高的CO2和环境CO2下产生的垃圾的分解没有差异。在较湿的一年中产生的垃圾(在最初的4个月内)显示出比较干燥的年份(27 +/- 2%yr(-1)或7.8 +/- 0.7 gm(-2)yr( -1)1998年垃圾; 18 +/- 3%yr(-1)或2.2 +/- 0.4 gm(-2)yr(-1)(1999年垃圾)。 CO2升高(湿年:37 +/- 0.5;干燥年:42 +/- 2.5)下产生的垃圾的C:N比高于环境CO2(湿年:34 +/- 1.1;干燥)下产生的垃圾的C:N比年:35 +/- 1.4)。潮湿年份的垃圾产量(amb。CO2:25.1 +/- 1.1 gm(-2)yr(-1); elev。CO2:35.0 +/- 1.1 gm(-2)yr(-1)大于是干燥年份的两倍(含二氧化碳量:11.6 +/- 1.7 gm(-2),较高的二氧化碳量:13.3 +/- 3.4 gm(-2)),并且含有更大比例的苍白枸杞和与干旱年份生产的凋落物相比,Larrea tridentata的比例更低。在所有处理中观察到,分解随着C:N比的增加而降低,随着三角毛拉尔(Larrea tridentata)比例的增加而降低,而随着苍白枸杞和安德森的枸杞的比例增加而增加。由于凋落物C:N随凋落物生产年的变化而变化,并且CO2不会改变分解或凋落物种类/组织的组成,因此,降水量的逐年变化可能会影响凋落物中关键植物种类的比例。在未来大气CO2升高的莫哈韦沙漠中,凋落物可能是调节凋落物分解的最重要方式。 [参考:38]

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