南澳大利亚沿海泻湖从咸水到高盐水的浮游微藻群落分布。

Mathilde Schapira, Marie-Jeanne Buscot, Thomas Pollet, Sophie C Leterme, Laurent Seuront
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摘要

背景:微小浮游植物(即蓝藻和微小真核生物)是浮游生物自养群落中数量丰富、生态重要的组成部分。这些微生物在包括高盐度水域在内的各种极端环境中定居。然而,这些生物在强盐度梯度上的分布情况几乎没有得到研究。本研究利用流式细胞仪研究了蓝藻和微微真核生物在自然连续盐度梯度(1.8% 至 15.5%)上的丰度和群落结构:在盐度为 8.0% 至 11.0% 的条件下,浮游微藻的丰度最高(1.3 x 106 至 1.4 x 106 cells ml-1)。沿盐度梯度确定了两个微囊藻群体(可能是 Synechococcus 和 Prochlorococcus)和 5 个不同的微真核细胞群体。随着盐度的升高,皮藻浮游生物的细胞计量学丰富度下降,在泻湖的咸海部分(即盐度低于 3.5%)观察到细胞计量学最多样化的群落(4 至 7 个种群)。在整个盐度梯度中,一个微核生物种群在群落中占主导地位,并在 8.0% 至 11.0% 的盐度范围内大量繁殖。最后,只有这一耐盐碱种群和类原绿球藻(Prochlorococcus-like picocyanobacteria)在高盐度水域(即高于 14.0%)中被发现。盐度被认为是潟湖沿岸浮游微藻分布结构的主要因素。然而,营养条件、病毒溶解和微型浮游动物放牧也被认为是控制泻湖沿岸浮游微藻数量和多样性的潜在重要因素:本文描述的复杂模式代表了对盐度从 1.8% 上升到 15.5% 的连续梯度上浮游微藻动态的首次观测。这一结果为了解沿强盐度梯度分布的微自养生物提供了新的视角,有助于更好地了解盐水系统中浮游生物的整体功能,这对于管理这些珍贵的、气候压力大的生态系统至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Distribution of picophytoplankton communities from brackish to hypersaline waters in a South Australian coastal lagoon.

Background: Picophytoplankton (i.e. cyanobacteria and pico-eukaryotes) are abundant and ecologically critical components of the autotrophic communities in the pelagic realm. These micro-organisms colonized a variety of extreme environments including high salinity waters. However, the distribution of these organisms along strong salinity gradient has barely been investigated. The abundance and community structure of cyanobacteria and pico-eukaryotes were investigated along a natural continuous salinity gradient (1.8% to 15.5%) using flow cytometry.

Results: Highest picophytoplankton abundances were recorded under salinity conditions ranging between 8.0% and 11.0% (1.3 x 106 to 1.4 x 106 cells ml-1). Two populations of picocyanobacteria (likely Synechococcus and Prochlorococcus) and 5 distinct populations of pico-eukaryotes were identified along the salinity gradient. The picophytoplankton cytometric-richness decreased with salinity and the most cytometrically diversified community (4 to 7 populations) was observed in the brackish-marine part of the lagoon (i.e. salinity below 3.5%). One population of pico-eukaryote dominated the community throughout the salinity gradient and was responsible for the bloom observed between 8.0% and 11.0%. Finally only this halotolerant population and Prochlorococcus-like picocyanobacteria were identified in hypersaline waters (i.e. above 14.0%). Salinity was identified as the main factor structuring the distribution of picophytoplankton along the lagoon. However, nutritive conditions, viral lysis and microzooplankton grazing are also suggested as potentially important players in controlling the abundance and diversity of picophytoplankton along the lagoon.

Conclusions: The complex patterns described here represent the first observation of picophytoplankton dynamics along a continuous gradient where salinity increases from 1.8% to 15.5%. This result provides new insight into the distribution of pico-autotrophic organisms along strong salinity gradients and allows for a better understanding of the overall pelagic functioning in saline systems which is critical for the management of these precious and climatically-stress ecosystems.

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