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Influence of the Amazon River discharge on the biogeography of phytoplankton communities in the western tropical north Atlantic

机译:亚马逊河流量对热带北大西洋西部浮游植物群落生物地理学的影响

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摘要

An Advanced Laser Fluorometer (ALF) capable of discriminating several phytoplankton pigment types was utilized in conjunction with microscopic data to map the distribution of phytoplankton communities in the Amazon River plume in May-June-2010, when discharge from the river was at its peak. Cluster analysis and Non-metric Multi-Dimensional Scaling (NMDS) helped distinguish three distinct biological communities that separated largely on the basis of salinity gradients across the plume. These three communities included an "estuarine type" comprised of a high biomass mixed population of diatoms, cryp-tophytes and green-water Synechococcus spp. located upstream of the plume, a "mesohaline type" made up largely of communities of Diatom-Diazotroph Associations (DDAs) and located in the northwestern region of the plume and an "oceanic type" in the oligotrophic waters outside of the plume made up of Trichodesmium and Synechococcus spp. Although salinity appeared to have a substantial influence on the distribution of different phytoplankton groups, ALF and microscopic measurements examined in the context of the hydro-chemical environment of the river plume, helped establish that the phytoplankton community structure and distribution were strongly controlled by inorganic nitrate plus nitrite (NO_3 + NO_2) availability whose concentrations were low throughout the plume. Towards the southern, low-salinity region of the plume, NO_3 + NO_2 supplied by the onshore flow of subsurface (~80 m depth) water, ensured the continuous sustenance of the mixed phytoplankton bloom. The large drawdown of SiO_3 and PO_4 associated with this "estuarine type" mixed bloom at a magnitude comparable to that observed for DDAs in the mesohaline waters, leads us to contend that, diatoms, cryptophytes and Synechococcus spp., fueled by the offshore influx of nutrients also play an important role in the cycling of nutrients in the Amazon River plume.
机译:利用能够区分几种浮游植物色素类型的高级激光荧光计(ALF)结合微观数据,绘制了2010年5月至2010年6月亚马逊河羽流中浮游植物群落分布的图,当时该河流的排放量达到了峰值。聚类分析和非度量多维标度(NMDS)帮助区分三个不同的生物群落,这些生物群落在很大程度上基于整个羽流的盐度梯度而分开。这三个社区包括一个“河口类型”,它由高生物量的硅藻,催生植物和绿水集球藻属组成。位于羽状流上游的“中卤型”,主要由硅藻-重氮营养协会(DDAs)组成,位于羽状体的西北区域,而在羽状富营养化水域中的“海洋型”由羽状体组成毛线虫和Synechococcus spp。尽管盐度似乎对不同浮游植物群的分布有很大影响,但是在河羽水化学环境的背景下进行的ALF和显微测量有助于确定浮游植物的群落结构和分布受无机硝酸盐的强烈控制。加上亚硝酸盐(NO_3 + NO_2)的可用性,在整个羽流中其浓度都较低。朝向羽流的南部,低盐度地区,由陆上(〜80 m深度)地下水流提供的NO_3 + NO_2确保了浮游植物混合花序的持续维持。 SiO_3和PO_4与这种“河口型”混合水华的大量下降,其幅度与在中卤水域中DDA的观测值相当,这使我们认为,硅藻,隐生植物和Synechococcus spp。是由近海藻类涌入推动的。养分在亚马逊河羽流中养分的循环中也起着重要作用。

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  • 来源
    《Progress in Oceanography》 |2014年第1期|29-40|共12页
  • 作者单位

    Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA;

    Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA;

    Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA;

    Romberg Tiburon Center, San Francisco State University, Tiburon, CA 94920, USA;

    School of Biology, Georgia Institute of Technology, Atlanta, GA 30332, USA;

    Horn Point Laboratory, University of Maryland Center for Environmental Science, Cambridge, MD 21613, USA;

    Department of Marine Sciences, University of Georgia, Athens, CA 30602, USA;

    Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089, USA;

    Department of Biological Sciences and Wrigley Institute for Environmental Studies, University of Southern California, Los Angeles, CA 90089, USA;

    Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Bremen, Germany;

    Virginia Institute of Marine Science, Gloucester Point, VA 23062, USA;

    Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA;

    Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA;

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