J. Pozo, J. Casas, M. Menéndez, Salvador Mollá, I. Arostegui, A. Basaguren, Carmen M. Casado, E. Descals, J. García-Avilés, J. M. González, A. Larrañaga, E. López, Mirian Lusi, Ó. Moya, J. Pérez, T. Riera, Neftalí Roblas, M. Salinas
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Streams that were similar in size, flowed mainly over siliceous substrate in catchments with scarce human settlements and activities, and fell within a range of low nutrient concentrations were chosen in each region. Breakdown rates were regionally variable and were low (0.109–0.198% ash-free dry mass [AFDM]/degree day [dd]) in the Cornisa Cantábrica, the most mesic and Atlantic region, and high (0.302–0.639% AFDM/dd) in Sierra de Guadarrama, one of the coldest and most inland areas. Temperature was not the determining factor affecting differences in breakdown rates among regions, and breakdown rates were not related to concentrations of dissolved nutrients. However, microbial reproductive activity (sporulation rates) was significantly correlated with dissolved P concentration. Breakdown rates were explained better by presence and feeding activities of detritivores than by decomposer activity. 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Breakdown rates were regionally variable and were low (0.109–0.198% ash-free dry mass [AFDM]/degree day [dd]) in the Cornisa Cantábrica, the most mesic and Atlantic region, and high (0.302–0.639% AFDM/dd) in Sierra de Guadarrama, one of the coldest and most inland areas. Temperature was not the determining factor affecting differences in breakdown rates among regions, and breakdown rates were not related to concentrations of dissolved nutrients. However, microbial reproductive activity (sporulation rates) was significantly correlated with dissolved P concentration. Breakdown rates were explained better by presence and feeding activities of detritivores than by decomposer activity. Incorporation of breakdown rates in assessment schemes of stream ecological status will be difficult because leaf processing does not respond unequivocally to environmental factors when climatic regions are considered. 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引用次数: 58
摘要
摘要本研究的主要目的是阐明西班牙少营养源流凋落叶分解速率地理差异的影响因素。在伊比利亚半岛4个不同气候区(Cornisa Cantábrica、Cordillera Litoral Catalana、Sierra de Guadarrama和Sierra Nevada)的22条水源中进行了桤木(Alnus glutinosa)凋落叶分解实验。在每个区域选择的河流大小相似,主要在人类住区和活动稀少的集水区流过硅质基质,并且在低营养浓度范围内。分解率存在区域差异,在corisa Cantábrica(最湿润和大西洋地区)低(0.109-0.198%无灰干质量[AFDM]/度日[dd]),在Sierra de Guadarrama(最寒冷和最内陆地区之一)高(0.302-0.639% AFDM/度日)。温度不是影响区域间分解率差异的决定性因素,分解率与溶解营养物浓度无关。微生物繁殖活性(产孢率)与溶磷浓度显著相关。分解率用腐食动物的存在和摄食活动比用分解者的活动更能解释。在河流生态状况评估方案中纳入分解率将是困难的,因为当考虑气候区域时,树叶加工并不明确地响应环境因素。因此,需要在参考条件下对基准标准进行区域调整。
Leaf-litter decomposition in headwater streams: a comparison of the process among four climatic regions
Abstract The main purpose of our work was to elucidate factors responsible for the geographical differences in leaf-litter decomposition rates in Spanish oligotrophic headwater streams. Decomposition experiments with alder (Alnus glutinosa) leaf litter were carried out in 22 headwater streams in 4 different climatic regions across the Iberian Peninsula (Cornisa Cantábrica, Cordillera Litoral Catalana, Sierra de Guadarrama, and Sierra Nevada). Streams that were similar in size, flowed mainly over siliceous substrate in catchments with scarce human settlements and activities, and fell within a range of low nutrient concentrations were chosen in each region. Breakdown rates were regionally variable and were low (0.109–0.198% ash-free dry mass [AFDM]/degree day [dd]) in the Cornisa Cantábrica, the most mesic and Atlantic region, and high (0.302–0.639% AFDM/dd) in Sierra de Guadarrama, one of the coldest and most inland areas. Temperature was not the determining factor affecting differences in breakdown rates among regions, and breakdown rates were not related to concentrations of dissolved nutrients. However, microbial reproductive activity (sporulation rates) was significantly correlated with dissolved P concentration. Breakdown rates were explained better by presence and feeding activities of detritivores than by decomposer activity. Incorporation of breakdown rates in assessment schemes of stream ecological status will be difficult because leaf processing does not respond unequivocally to environmental factors when climatic regions are considered. Thus, regional adjustments of baseline standards in reference conditions will be required.