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Phytolith‐occluded carbon sequestration potential in three major steppe types along a precipitation gradient in Northern China

机译:沿中国北方沉淀梯度的三大草原类型的植物致盲碳封存潜力

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摘要

Phytolith‐occluded carbon (PhytOC) is an important long‐term stable carbon fraction in grassland ecosystems and plays a promising role in global carbon sequestration. Determination of the PhytOC traits of different plants in major grassland types is crucial for precisely assessing their phytolith carbon sequestration potential. Precipitation is the predominant factor in controlling net primary productivity (NPP) and species composition of the semiarid steppe grasslands. We selected three representative steppe communities of the desert steppe, the dry typical steppe, and the wet typical steppe in Northern Grasslands of China along a precipitation gradient, to investigate their species composition, biomass production, and PhytOC content for quantifying its long‐term carbon sequestration potential. Our results showed that (a) the phytolith and PhytOC contents in plants differed significantly among species, with dominant grass and sedge species having relatively high contents, and the contents are significantly higher in the below‐ than the aboveground parts. (b) The phytolith contents of plant communities were 16.68, 17.94, and 15.85 g/kg in the above‐ and 86.44, 58.73, and 76.94 g/kg in the belowground biomass of the desert steppe, the dry typical steppe, and the wet typical steppe, respectively; and the PhytOC contents were 0.68, 0.48, and 0.59 g/kg in the above‐ and 1.11, 0.72, and 1.02 g/kg in the belowground biomass of the three steppe types. (c) Climatic factors affected phytolith and PhytOC production fluxes of steppe communities mainly through altering plant production, whereas their effects on phytolith and PhytOC contents were relatively small. Our study provides more evidence on the importance of incorporating belowground PhytOC production for estimating phytolith carbon sequestration potential and suggests it crucial to quantify belowground PhytOC production taking into account of plant perenniality and PhytOC deposition over multiple years.
机译:植物闭塞碳(Phytoc)是草原生态系统中重要的长期稳定碳分数,在全球碳封存中发挥着前景作用。主要草地类型中不同植物的测定对于精确评估其植物碳封存潜力至关重要。沉淀是控制净初级生产率(NPP)和半干旱草原草原的物种组成的主要因素。我们选择了沙漠草原的三个代表性草原,干燥典型的草原和中国北部草原的湿典型草原沿着沉淀梯度,研究了它们的物种组成,生物质生产和植物植物含量,用于量化其长期碳封存电位。我们的研究结果表明,(a)植物中的植物和植物植物含量在物种中显着差异,具有相对高的内容物的主要草和莎草种类,并且在下面的地上含量显着较高。 (b)植物群落的植物含量为16.68,17.94和15.85克/千克,在沙漠草原下面的地下生物量,干燥典型的草原和潮湿的情况下为56.44,58.73和76.94g / kg。典型的草原分别;在三种草原类型的下面的地下生物质中,植物植物含量为0.68,0.48和0.59g / kg,1.11,0.72和1.02g / kg。 (c)气候因素主要通过改变植物生产,影响植物群落的植物植物和植物植物生产势态,而它们对植物植物和植物植物含量的影响相对较小。我们的研究提供了有关纳入地下Phytoc生产的重要性,以估算植物碳封存潜力,并表明在多年来植物常年和植物常年性和植物沉积的情况下量化地下植物生成至关重要。

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