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Photosynthetic enhancement and diurnal stem and soil carbon fluxes in a mature Norway spruce stand under elevated CO2

机译:高CO2浓度下成熟挪威云杉林分的光合增强和日变化茎干和土壤碳通量。

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Understanding the effects of elevated atmospheric CO2 on carbon (C) relations of mature forest trees is central to understanding ecosystem C fluxes and pools in a future high-CO2 world. Here, we investigated the CO2-induced photosynthetic enhancement and the diurnal variation in shoot carbon assimilation, stem CO2 efflux and soil respiration associated with ca. 110-year-old and 37 m tall Norway spruce trees (Picea abies (L) H. Karst.) growing under free air CO2 enrichment (FACE) in a mixed, near-natural forest in Northern Switzerland. Diurnal measurements of these major C fluxes were conducted simultaneously on three occasions: one week before and after the start of CO2 enrichment, and one year later. Under controlled leaf chamber conditions, an increase in the atmospheric CO2 concentration of ca. 150 ppm above ambient stimulated light-saturated rates of photosynthesis in previous- and current-year upper-canopy shoots equally by 73 +/- 2%. In the course of the day such large differences in C assimilation between trees growing under elevated CO2 (eCO(2)) and ambient conditions (aCO(2)) only occurred around midday under non-limiting light conditions. The CO2 efflux rates from spruce stems (CEstem) and surrounding soil (R-soil) shared a similar range during night- and daytime (3-5 mu mol m(-2) s(-1)) but were not stimulated by eCO(2). Both CEstem stem and R-soil were still rising when photosynthesis approached evening light compensation potentially reflecting the time lag in assimilate allocation to stem tissue and fine roots. Our findings suggest a strong photosynthetic enhancement during the initial CO2 enrichment phase but provide no evidence for an overall or daytime-dependent stimulation of respiratory CO2 fluxes indicating that the extra C was not quickly returned to the atmosphere through respiratory processes in spruce stems or surrounding soil. (C) 2015 Elsevier B.V. All rights reserved.
机译:了解大气CO2升高对成熟林木碳(C)关系的影响,对于了解未来高CO2世界中的生态系统碳通量和库至关重要。在这里,我们调查了CO2诱导的光合作用增强以及与Ca相关的芽碳同化,茎干CO2外排和土壤呼吸的昼夜变化。有着110年历史和37 m高的挪威云杉树木(Picea abies(L)H. Karst。)在自由空气CO2浓缩(FACE)下生长在瑞士北部一个近自然的混合森林中。这些主要碳通量的昼夜测量在三种情况下同时进行:开始富集二氧化碳之前和之后一周,一年后。在受控的叶室条件下,大气中CO2浓度大约增加。在前一年和当年的高冠梢中,光合作用的光合作用速率比周围环境高出150 ppm,提高了73 +/- 2%。在一天中的过程中,仅在非限制性光照条件下的中午左右才出现在二氧化碳浓度升高(eCO(2))和环境条件(aCO(2))下生长的树木之间C同化的巨大差异。云杉茎(CEstem)和周围土壤(R-土)的CO2外排速率在白天和黑夜都具有相似的范围(3-5μmol m(-2)s(-1)),但不受eCO的刺激(2)。当光合作用接近傍晚的光补偿时,CEstem茎和R土都仍在上升,这可能反映了同化分配给茎组织和细根的时滞。我们的研究结果表明,在最初的CO2富集阶段,光合作用会增强,但没有证据表明呼吸道CO2通量的整体或白天依赖性刺激,表明云杉的茎或周围土壤中多余的C不会通过呼吸作用迅速返回大气。 。 (C)2015 Elsevier B.V.保留所有权利。

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