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首页> 外文期刊>Global change biology >Elevated CO_2 alters carbon fluxes in early successional mediterranean ecosystems
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Elevated CO_2 alters carbon fluxes in early successional mediterranean ecosystems

机译:高浓度的CO_2改变了早期演替地中海生态系统中的碳通量

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Annual carbon budgets of ecosystems are central to our understanding of the biotic control of atmospheric composition, but they are not available under elevated CO_2 for most vegetation types. Using gas exchange techniques, we assessed carbon fluxes of four early successional Mediterranean model communities, consisting of grasses, legumes and composites. The assemblages were grown on the same monoliths for three consecutive years in greenhouses tracking field conditions except for CO_2 maintained at ambient (370 #mu#mol mol~-1) or elevated (700 #mu#mol mol~-1) concentration. During the third year of study, CO_2 enrichment consistently shifted the annual carbon balance towards lower efflux, with displacements between 4.3 and 26.2 mol m~-2 y~-1 (one assemblage became a net CO_2 sink, another just reached equilibrium, and the remaining two remained as a CO_2 source). At least 50% of the shift under elevated CO_2 originated from a decrease in belowground respiration. This indicates that, during this year, CO_2 enrichment did not predominantly enhance C-cycling, but on the contrary inhibited root respiration or microbial C-utilization. Although elevated-CO_2-grown systems acted as a net CO_2 sink during a longer period of the year (4-7months) compared with ambient-CO_2-grown systems (3-3.5 months), gross canopy photosynthesis was modified only to a limited extent (between-5.9 and + 14.8%). Interaction between the carbon and the water cycle was apparently responsible for this weak stimulation. In particular, reduced evapotranspiration under elevated CO_2 coincided with inhibited canopy photosynthesis in early spring, most likely resulting from water saturation of the soil. In addition, only the earliest-planted assemblages had an increased gross canopy photosynthesis during late autumn and early winter. This suggests that a longer summer drought, by delaying the establishment of such an annual type of vegetation, would reduce the positive impact of elevated CO_2 on productivity. Water ~gime appears to strongly govern the influence of CO_2 on the carbon fluxes in Mediterranean ecosystems with annual herbaceous vegetation.
机译:生态系统的年度碳预算对于我们理解大气成分的生物控制至关重要,但是对于大多数植被类型,在较高的CO_2下都无法获得。使用气体交换技术,我们评估了四个早期演替地中海模式社区的碳通量,这些模式社区由草,豆类和复合材料组成。除了使CO 2保持在环境浓度(370#mu#mol mol-1)或升高的浓度(700#mu#mol mol-1)外,这些组合物在温室中连续三年在相同的整体上生长,追踪田间条件。在研究的第三年中,CO_2的富集一直使年度碳平衡向较低的流出方向移动,排量在4.3至26.2 mol m〜-2 y〜-1之间(一种组合成为净CO_2汇,另一种组合刚刚达到平衡,并且其余两个作为CO_2来源)。在升高的CO_2下至少有50%的变化源于地下呼吸的减少。这表明,在这一年中,CO_2的富集并未主要增强C循环,但相反却抑制了根呼吸或微生物对C的利用。尽管与环境CO_2生长的系统(3-3.5个月)相比,CO_2生长的系统在一年的较长时期(4-7个月)中充当了净CO_2汇,但总冠层光合作用仅在有限程度上进行了修改(介于-5.9和+ 14.8%之间)。碳和水循环之间的相互作用显然是造成这种弱刺激的原因。尤其是,CO_2浓度升高时蒸散量的减少与早春的冠层光合作用受到抑制有关,这很可能是由于土壤水分饱和所致。此外,在秋季末和初冬期间,只有最早种植的组合具有较高的总冠层光合作用。这表明较长的夏季干旱会延迟建立这种年生类型的植被,从而减少CO_2升高对生产力的积极影响。水凝胶似乎强烈控制着CO_2对具有一年生草本植物的地中海生态系统中碳通量的影响。

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