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首页> 外文期刊>Frontiers in Marine Science >Phytoplankton realised niches track changing oceanic conditions at a long-term coastal station off Sydney Australia
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Phytoplankton realised niches track changing oceanic conditions at a long-term coastal station off Sydney Australia

机译:浮游植物认识到利基可以追踪澳大利亚悉尼附近一个长期沿海站点的不断变化的海洋状况

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Phytoplankton dynamics are closely linked to the ocean-climate system with evidence that changing ocean conditions are substantially altering phytoplankton biogeography, abundance and phenology. Here, using phytoplankton community composition and environmental data spanning 1965 to 2013 from a long-term Pacific Ocean coastal station offshore from Sydney, Australia (Port Hacking 100m), we used the Maximum Entropy Modelling framework (MaxEnt) to test whether phytoplankton realised niches are fixed or shift in response to changing environmental conditions. The mean niches of phytoplankton closely tracked changes in mean temperature, while the mean salinity and mixed layer depth niches were consistently at the extreme range of available conditions. Prior studies had shown a fixed niche for nitrate in some phytoplankton species at a site where nitrate concentration was decreasing and potentially limiting; however, at Port Hacking nitrate and silicate niches increased more rapidly than environmental conditions, apparently in response to periodic occurrences of elevated nutrient concentrations. This study provides further evidence that climate change model projections cannot assume fixed realised niches of biotic communities, whilst highlighting the importance of sustained ocean measurements from the southern hemisphere to enhance our understanding of global ocean trends.
机译:浮游植物的动力学与海洋-气候系统密切相关,有证据表明不断变化的海洋状况正在极大地改变浮游植物的生物地理学,丰度和物候学。在这里,我们使用澳大利亚悉尼近海的一个长期太平洋沿岸站(Port Hacking 100m)的1965年至2013年的浮游植物群落组成和环境数据,使用最大熵建模框架(MaxEnt)测试浮游植物实现的生态位是否为根据环境条件的变化而固定或转移。浮游植物的平均生态位密切跟踪平均温度的变化,而平均盐度和混合层深度生态位始终在可用条件的极端范围内。先前的研究表明,在某些浮游植物物种中,硝酸盐浓度正在下降并且可能会受到限制的地方,硝酸盐的生态位固定。然而,在哈克港,硝酸盐和硅酸盐生态位的增长速度比环境条件快得多,这显然是由于周期性出现的营养物浓度升高而引起的。这项研究提供了进一步的证据,表明气候变化模型的预测不能假设生物群落具有固定的已实现生态位,同时强调了南半球持续进行海洋测量对增进我们对全球海洋趋势的认识的重要性。

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