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首页> 外文期刊>Marine ecology progress series >Onshore-offshore variations in copepod community structure off the Oregon coast during the summer upwelling season
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Onshore-offshore variations in copepod community structure off the Oregon coast during the summer upwelling season

机译:夏季上升季节俄勒冈州沿海co足类群落结构的陆上-近海变化

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During the summer of 1994, 1996, and 1997, we conducted hydrographic and plankton surveys of the upper 70 m in the nearshore, the continental shelf, and off-shelf oceanic waters off Oregon, USA. Copepod densities and biomass were estimated along 4 transects from each cruise. The on-shelf copepod biomass was 2.8 times greater than off-shelf biomass. Nonmetric multidimensional scaling identified an on-shelf and an off-shelf copepod community. The change in community composition usually occurred at or slightly offshore of the continental shelf break, defined here as 180 m water depth. Indicator-species analysis identified the subarctic neritic species, Calanus mar-shallae, Pseudocalanus mimus, and Acartia longiremis, as good indicators of continental shelf waters. 'Warm water' species Mesocalanus tenuicornis, Calocalanus styliremis, Clausocalanus spp., and Ctenocalanus vanus were indicators of off-shelf waters. The copepod communities off the coast of Oregon during the summer upwelling season reflect the origins of the dominating currents within each habitat. The coastal copepod community is subarctic neritic in origin, consistent with southward coastal flows. The offshore copepod community is a mixture of species with origins in the Transition Zone as well as species that are typical of the coastal region of the California Current off central and southern California. We speculate that the central and southern California Current species are present in offshore waters of Oregon in summer because they are transported north with the Davidson Current in winter but, with the initiation of the upwelling season in spring, they are transported into offshore waters where they establish viable populations.
机译:在1994年夏季,1996年和1997年夏季,我们对美国俄勒冈州近岸,大陆架和现成的海洋水域的上70 m进行了水文和浮游生物调查。每次巡游沿4个样带估算足类的密度和生物量。货架上的pe足类生物量比货架上的生物量大2.8倍。非度量多维标度确定了一个上架的和一个现成的co足类群落。群落组成的变化通常发生在大陆架断裂处或稍微离岸的地方,此处定义为水深180 m。指标种类分析确定了北极圈下的中性物种,Calaus mar-shallae,Pseudocalanus mimus和Acartia longiremis是大陆架水域的良好指标。 “温水”物种中Mesocalanus tenuicornis,Calocalanus styliremis,Clausocalanus spp。和Ctenocalanus vanus是现成水的指标。夏季上升季节期间,俄勒冈海岸外的pe足类群落反映了每个栖息地内洋流的起源。沿海co足类群落起源于北极,是与南岸沿海水流一致的。离岸co足类群落是起源于过渡区的物种与典型的加利福尼亚中部和南部沿海加州海岸带物种的混合物。我们推测加利福尼亚中部和南部洋流物种在夏季存在于俄勒冈州的近海水域中,因为它们在冬季与戴维森洋流一起向北运输,但随着春季上升流季节的开始,它们被运入近海水域中建立可行的人口。

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