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Diversity, Ecology and Biogeochemistry of Cyst-Forming Acantharia (Radiolaria) in the Oceans

机译:海洋中形成囊肿的棘皮(Radiolaria)的多样性,生态学和生物地球化学

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摘要

Marine planktonic organisms that undertake active vertical migrations over their life cycle are important contributors to downward particle flux in the oceans. Acantharia, globally distributed heterotrophic protists that are unique in building skeletons of celestite (strontium sulfate), can produce reproductive cysts covered by a heavy mineral shell that sink rapidly from surface to deep waters. We combined phylogenetic and biogeochemical analyses to explore the ecological and biogeochemical significance of this reproductive strategy. Phylogenetic analysis of the 18S and 28S rRNA genes of different cyst morphotypes collected in different oceans indicated that cyst-forming Acantharia belong to three early diverging and essentially non symbiotic clades from the orders Chaunacanthida and Holacanthida. Environmental high-throughput V9 tag sequences and clone libraries of the 18S rRNA showed that the three clades are widely distributed in the Indian, Atlantic and Pacific Oceans at different latitudes, but appear prominent in regions of higher primary productivity. Moreover, sequences of cyst-forming Acantharia were distributed evenly in both the photic and mesopelagic zone, a vertical distribution that we attribute to their life cycle where flagellated swarmers are released in deep waters from sinking cysts. Bathypelagic sediment traps in the subantarctic and oligotrophic subtropical Atlantic Ocean showed that downward flux of Acantharia was only large at high-latitudes and during a phytoplankton bloom. Their contribution to the total monthly particulate organic matter flux can represent up to 3%. High organic carbon export in cold waters would be a putative nutritional source for juveniles ascending in the water column. This study improves our understanding of the life cycle and biogeochemical contribution of Acantharia, and brings new insights into a remarkable reproductive strategy in marine protists.
机译:在整个生命周期中进行垂直活动的海洋浮游生物是海洋中向下的粒子通量的重要贡献者。棘叶藻是分布于全球的异养生物,在构建天青石(硫酸锶)骨架方面具有独特性,它可以产生繁殖孢囊,该孢囊被沉重的矿物壳覆盖,从表面迅速沉入深水。我们结合了系统发育和生物地球化学分析,以探讨这种繁殖策略的生态和生物地球化学意义。对在不同海洋中收集到的不同囊肿形态的18S和28S rRNA基因进行的系统进化分析表明,形成囊肿的棘棘属属于Chaunacanthida和Holacanthida顺序的三个早期分化且基本上非共生的进化枝。环境高通量的V9标签序列和18S rRNA的克隆文库显示,这三个进化枝广泛分布在印度,大西洋和太平洋的不同纬度,但在初级生产力较高的地区表现突出。此外,形成囊肿的棘棘序列在光生区和中生骨区均等分布,这种垂直分布归因于它们的生命周期,其中鞭毛成群的群在深水中从沉没的囊肿中释放出来。在南极和贫营养的亚热带大西洋中的浮游沉积沉积物表明,棘棘的向下通量仅在高纬度和浮游植物开花期间才大。它们对每月总颗粒有机物通量的贡献可高达3%。冷水中有机碳的大量出口将成为水柱中未成年幼鱼的假定营养来源。这项研究增进了我们对棘棘生命周期和生物地球化学贡献的理解,并将新的见识带入了海洋生物界杰出的繁殖策略。

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