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Climate shifts the interaction web of a marine plankton community.

机译:气候改变了海洋浮游生物社区的互动网络。

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Climatic effects in the ocean at the community level are poorly described, yet accurate predictions about ecosystem responses to changing environmental conditions rely on understanding biotic responses in a food-web context to support knowledge about direct biotic responses to the physical environment. Here we conduct time-series analyses with multivariate autoregressive (MAR) models of marine zooplankton abundance in the Northern California Current from 1996 to 2009 to determine the influence of climate variables on zooplankton community interactions. Autoregressive models showed different community interactions during warm vs. cool ocean climate conditions. Negative ecological interactions among zooplankton groups characterized the major warm phase during the time series, whereas during the major cool phase, ocean transport largely structured zooplankton communities. Local environmental conditions (sea temperature) and large-scale climate indices (El Niino/Southern Oscillation) were associated with changes in zooplankton abundance across the full time series. Secondary environmental correlates of zooplankton abundance varied with ocean climate phase, with most support during the warm phase for upwelling as a covariate, and most support during the cool phase for salinity. Through simultaneous quantitation of community interactions and environmental covariates, we show that marine zooplankton community structure varies with climate, suggesting that predictions about ecosystem responses to future climate scenarios in the Northern California Current should include potential changes to the base of the pelagic food.
机译:关于海洋在社区一级的气候影响的描述很少,但是关于生态系统对不断变化的环境条件的反应的准确预测依赖于对食物网环境中生物反应的理解,以支持有关对自然环境的直接生物反应的知识。在这里,我们使用1996年至2009年北加利福尼亚洋流中海洋浮游动物丰度的多元自回归(MAR)模型进行时间序列分析,以确定气候变量对浮游动物群落相互作用的影响。自回归模型显示了在温暖和凉爽的海洋气候条件下,不同的社区相互作用。在时间序列上,浮游动物群之间的负生态相互作用是主要的暖期,而在主要的凉爽时期,海洋运输在很大程度上构成了浮游动物群落。在整个时间序列中,当地环境条件(海水温度)和大规模气候指数(厄尔尼诺/南方涛动)与浮游动物的丰度变化有关。浮游动物丰度的次要环境相关性随海洋气候阶段而变化,在温暖阶段,最多的支持是协变量,在上升阶段则主要支持盐度。通过对社区相互作用和环境协变量的同时定量,我们表明海洋浮游动物的群落结构随气候而变化,这表明关于北加州海流未来生态系统对生态系统反应的预测应该包括对中上层食物基础的潜在变化。

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