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Are Hotspots Always Hotspots? The Relationship between Diversity Resource and Ecosystem Functions in the Arctic

机译:热点总是热点吗?北极多样性资源与生态系统功能之间的关系

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摘要

The diversity-ecosystem function relationship is an important topic in ecology but has not received much attention in Arctic environments, and has rarely been tested for its stability in time. We studied the temporal variability of benthic ecosystem functioning at hotspots (sites with high benthic boundary fluxes) and coldspots (sites with lower fluxes) across two years in the Canadian Arctic. Benthic remineralisation function was measured as fluxes of oxygen, silicic acid, phosphate, nitrate and nitrite at the sediment-water interface. In addition we determined sediment pigment concentration and taxonomic and functional macrobenthic diversity. To separate temporal from spatial variability, we sampled the same nine sites from the Mackenzie Shelf to Baffin Bay during the same season (summer or fall) in 2008 and 2009. We observed that temporal variability of benthic remineralisation function at hotspots is higher than at coldspots and that taxonomic and functional macrobenthic diversity did not change significantly between years. Temporal variability of food availability (i.e., sediment surface pigment concentration) seemed higher at coldspot than at hotspot areas. Sediment chlorophyll a (Chl a) concentration, taxonomic richness, total abundance, water depth and abundance of the largest gallery-burrowing polychaete Lumbrineristetraura together explained 42% of the total variation in fluxes. Food supply proxies (i.e., sediment Chl a and depth) split hot- from coldspot stations and explained variation on the axis of temporal variability, and macrofaunal community parameters explained variation mostly along the axis separating eastern from western sites with hot- or coldspot regimes. We conclude that variability in benthic remineralisation function, food supply and diversity will react to climate change on different time scales, and that their interactive effects may hide the detection of progressive change, particularly at hotspots. Time-series of benthic functions and its related parameters should be conducted at both hot- and coldspots to produce reliable predictive models.
机译:多样性与生态系统功能的关系在生态学中是一个重要的话题,但是在北极环境中并没有引起足够的重视,并且很少对其时间稳定性进行测试。我们研究了加拿大北极地区在两年内热点(底栖边界通量较高的站点)和寒冷地区(通量较低的站点)的底栖生态系统功能的时间变化。底质再矿化功能以沉积物-水界面处的氧气,硅酸,磷酸盐,硝酸盐和亚硝酸盐的通量测量。此外,我们确定了沉积物色素的浓度以及分类学和功能性大型底栖动物的多样性。为了将时间变异与空间变异分开,我们在2008年和2009年同一季节(夏季或秋季)对Mackenzie架子至Baffin湾的相同9个地点进行了采样。我们观察到,热点下底栖矿化作用的时间变异性高于寒点。而且分类和功能大型底栖动物多样性在几年之间没有显着变化。热点地区的食物供应量随时间变化(即沉积物表面色素浓度)似乎比热点地区高。沉积物最大叶廊polyChambete Lumbrineristetraura的沉积物叶绿素a(Chl a)浓度,分类学丰富度,总丰度,水深和丰度共同解释了通量总变化的42%。粮食供应的代表(即沉积物Chl a和深度)从热点区分开了热源,并解释了时间变异性轴上的变化,而大型动物群落参数则解释了沿沿热点或热点区分开东西向的轴线的变化。我们得出的结论是,底栖矿化作用,食物供应和多样性的可变性将在不同的时间尺度上对气候变化做出反应,并且它们的相互作用可能掩盖了渐进性变化的发现,尤其是在热点地区。底栖功能及其相关参数的时间序列应在热点和冷点进行,以产生可靠的预测模型。

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