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未来温度的升高超过凋落物质量的下降可能会影响溪流中微生物对凋落物的分解。

Future increase in temperature more than decrease in litter quality can affect microbial litter decomposition in streams.

机构信息

IMAR-CMA, Department of Life Sciences, University of Coimbra, Coimbra, Portugal.

出版信息

Oecologia. 2011 Sep;167(1):279-91. doi: 10.1007/s00442-011-1976-2. Epub 2011 Apr 3.

Abstract

The predicted increase in atmospheric CO(2) concentration for this century is expected to lead to increases in temperature and changes in litter quality that can affect small woodland streams, where water temperature is usually low and allochthonous organic matter constitutes the basis of the food web. We have assessed the individual and interactive effect of water temperature (5 and 10°C) and alder litter quality produced under ambient CO(2) levels (ambient litter) or under CO(2) concentrations predicted for 2050 (elevated litter) on litter decomposition and on fungal activity and assemblage structure. Litter decomposition rates and fungal respiration rates were significantly faster at 10 than at 5°C, but they were not affected by litter quality. Litter quality affected mycelial biomass accrual at 5 but not at 10°C, while increases in temperature stimulated biomass accrual on ambient but not on elevated litter. A similar pattern was observed for conidial production. All variables were stimulated on elevated litter at 10°C (future scenario) compared with ambient litter at 5°C (present scenario), but interactions between temperature and litter quality were additive. Temperature was the factor that most strongly affected the structure of aquatic hyphomycete assemblages. Our results indicate that if future increases in atmospheric CO(2) lead to only slight modifications in litter quality, the litter decomposition and fungal activities and community structure will be strongly controlled by increased water temperature. This may have serious consequences for aquatic systems as faster litter decomposition may lead to food depletion for higher trophic levels.

摘要

本世纪大气中 CO(2)浓度的预测增长预计将导致温度升高和凋落物质量变化,从而影响小的林地溪流,这些溪流的水温通常较低,异养有机物质构成食物网的基础。我们评估了水温(5 和 10°C)和在大气 CO(2)水平(大气凋落物)或预测 2050 年 CO(2)浓度(升高凋落物)下产生的桤木凋落物质量的单独和交互作用对凋落物分解以及真菌活性和群落结构的影响。凋落物分解率和真菌呼吸速率在 10°C 时明显快于 5°C,但不受凋落物质量的影响。凋落物质量仅在 5°C 时影响菌丝体生物量的积累,而在 10°C 时则不受影响,而温度升高则刺激了大气凋落物上的生物量积累,但对升高凋落物没有影响。对于分生孢子的产生,也观察到了类似的模式。与 5°C 时的大气凋落物(当前情景)相比,所有变量在 10°C 时的升高凋落物(未来情景)上都得到了刺激,但温度和凋落物质量之间的相互作用是相加的。温度是最强烈影响水生真菌群落结构的因素。我们的结果表明,如果未来大气 CO(2)的增加仅导致凋落物质量的轻微改变,那么凋落物分解以及真菌活动和群落结构将主要受到水温升高的控制。这可能对水生系统产生严重后果,因为更快的凋落物分解可能导致更高营养级别的食物枯竭。

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