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Changes in microplanktonic protists assemblages promoted by the thermocline induced stratification around an oceanic archipelago

机译:由温跃层引起的海洋群岛分层引起的微浮游生物原生生物组合的变化

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In the area around the archipelago of S?o Pedro e S?o Paulo (ASPSP), a set of small rocky islands in the Equatorial Atlantic, the thermocline begins at a more superficial depth than in the surrounding waters. This raises the question if there is any change in heterotrophic microplanktonic protists assemblages occurring in the surface mixed layer and in the subsurface layer. To answer this question, we sampled seawater in seven depths (between 1-100 m) with a 10L Niskin bottle and obtained temperature and salinity profiles with a CTD at eight sites around the ASPSP. The depth of the surface mixed layer varied between 18-63 meters. Dinoflagellates dominated in terms of abundance representing over 80% and 65% of the individuals found in the surface and subsurface layers, respectively. A PERMANOVA test revealed significant differences ( p 0.001) among the dinoflagellate and tintinnid assemblages occurring in both layers, but no evidence for difference in the radiolarian assemblage was detected. Good ecological indicators were found mainly within the dinoflagellate assemblage. The thermocline induced stratification allowed the development of different microplanktonic protists assemblages above and under the depth of the surface mixed layer in the upper 100 m of the water column.
机译:在赤道大西洋的圣佩德罗和圣保罗群岛(ASPSP)周围,这是一个由赤道大西洋组成的小岩石岛,比起周围的水域,热跃层的起点更浅。这就提出了一个问题,即在表面混合层和地下层中发生的异养微浮游生物原生生物组合是否发生变化。为了回答这个问题,我们用10升Niskin瓶在7个深度(1-100 m之间)对海水进行了采样,并在ASPSP周围的8个位置用CTD获得了温度和盐度分布图。表面混合层的深度在18-63米之间变化。鞭毛藻的丰度占优势,分别代表了表层和地下层中超过80%和65%的个体。 PERMANOVA测试显示,在两层中的鞭毛和丁锡醛组合之间存在显着差异(p <0.001),但未检测到放射虫组合存在差异的证据。良好的生态指标主要在鞭毛藻类组合中发现。温跃层诱导的分层允许在水柱上部100 m的表面混合层深度之上和之下形成不同的微浮游生物质子群。

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