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Evidence for climate-driven synchrony of marine and terrestrial ecosystems in northwest Australia

机译:气候驱动的澳大利亚西北部海洋和陆地生态系统同步性的证据

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The effects of climate change are difficult to predict for many marine species because little is known of their response to climate variations in the past. However, long-term chronologies of growth, a variable that integrates multiple physical and biological factors, are now available for several marine taxa. These allow us to search for climate-driven synchrony in growth across multiple taxa and ecosystems, identifying the key processes driving biological responses at very large spatial scales. We hypothesized that in northwest (NW) Australia, a region that is predicted to be strongly influenced by climate change, the El Nino Southern Oscillation (ENSO) phenomenon would be an important factor influencing the growth patterns of organisms in both marine and terrestrial environments. To test this idea, we analyzed existing growth chronologies of the marine fish Lutjanus argentimaculatus, the coral Porites spp. and the tree Callitris columellaris and developed a new chronology for another marine fish, Lethrinus nebulosus. Principal components analysis and linear model selection showed evidence of ENSO-driven synchrony in growth among all four taxa at interannual time scales, the first such result for the Southern Hemisphere. Rainfall, sea surface temperatures, and sea surface salinities, which are linked to the ENSO system, influenced the annual growth of fishes, trees, and corals. All four taxa had negative relationships with the Nino-4 index (a measure of ENSO status), with positive growth patterns occurring during strong La Nina years. This finding implies that future changes in the strength and frequency of ENSO events are likely to have major consequences for both marine and terrestrial taxa. Strong similarities in the growth patterns of fish and trees offer the possibility of using tree-ring chronologies, which span longer time periods than those of fish, to aid understanding of both historical and future responses of fish populations to climate variation.
机译:对于许多海洋物种而言,气候变化的影响很难预测,因为过去人们对气候变化的反应知之甚少。但是,长期的生长时间序列是一个综合了多种物理和生物学因素的变量,现在可用于几种海洋生物分类群。这些使我们能够在多个分类群和生态系统中寻找气候驱动的增长同步性,并确定在很大的空间尺度上驱动生物反应的关键过程。我们假设在澳大利亚西北部(一个预计将受到气候变化强烈影响的地区)中,厄尔尼诺南方涛动(ENSO)现象将是影响海洋和陆地环境中生物生长模式的重要因素。为了检验这一想法,我们分析了海水鱼类Lutjanus argentimaculatus,珊瑚Porites spp的现有生长时间。以及Callitris columellaris树,并为另一种海水鱼类Lethrinus nebulosus开发了新的年表。主成分分析和线性模型选择显示了ENSO驱动的所有四个类群在年际尺度上同步增长的证据,这是南半球的第一个这样的结果。与ENSO系统相关的降雨,海面温度和海面盐度影响了鱼类,树木和珊瑚的年生长。所有四个分类单元都与Nino-4指数(衡量ENSO状况)呈负相关,在强劲的拉尼娜年期间出现正增长模式。这一发现表明,ENSO事件强度和频率的未来变化可能会对海洋和陆地生物分类产生重大影响。鱼和树木的生长模式的高度相似性提供了使用树环年代学的可能性,该树环年代学的时间范围比鱼的时间跨度更长,以帮助理解鱼群对气候变化的历史和未来响应。

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