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Hydrography and phytoplankton in an isolated and non-pristine ria area: the A Coruna Harbour (NW Spain)

机译:孤立的非原始ria地区的水文和浮游植物:拉科鲁尼亚港口(西班牙西北部)

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The hydrography and phytoplankton cycle were examined from April 1994 to April 1995 in the harbour of the Ria of A Coruna, an area subjected to anthropogenic influence. The seasonal changes in the hydrography found elsewhere in Galicia (spring bloom, upwelling, summer stratification, autumn bloom and winter mixing) also occurred in the harbour. However, the phytoplankton cycle presented some local peculiarities. Phytoplankton biomass was very high in all periods (mean chlorophyll ranged from 4.7 mug l(-1) in summer to 16.7 mug l(-1) in spring, and phytoplankton carbon ranged from 337 mug l(-1) during upwelling to 547 mug l(-1) in spring), except winter. No significant differences were found among these periods. Sewage from the city of A Coruna and benthic remineralisation in summer (essentially for silicates) are the main source of nutrients in the harbour. Unlike the Rias Bajas, upwelling is a very poor source of nutrients due to the isolated situation of the harbour. The NIP ratio is lower than the Redfield ratio, with nitrogen being the limiting nutrient. As a result of these special hydrological and biogeochemical conditions, the phytoplankton community exhibits a high biomass and is dominated by large diatoms, with a negligible contribution from flagellates except during winter mixing. The anthropogenic origin of the nutrients, together with high phytoplankton biomass and water oxygen super-saturation from high primary production are all indicative of an eutrophication. Nevertheless, anoxic episodes were not observed. In the Galician Rias, eutrophication is a natural consequence of upwelling. However, the A Coruna Harbour is now described as the most important eutrophic area on the Galician coast owing to anthropogenic activities. (C) 2003 Editions scientifiques et medicales Elsevier SAS. All rights reserved. [References: 42]
机译:1994年4月至1995年4月,在受到人为影响的拉科鲁尼亚河Ria港口检查了水文和浮游植物的循环。在加利西亚其他地方发现的水文学季节变化(春季开花,上升流,夏季分层,秋季开花和冬季混合)也发生在港口。但是,浮游植物的循环表现出一些局部性。在所有时期,浮游植物的生物量都很高(平均叶绿素的范围从夏季的4.7马克升(-1)到春季的16.7马克升(-1),浮游植物的碳含量在上升期间从337马克升(-1)到547马克。 l(-1)在春季,冬季除外。在这些时期之间没有发现显着差异。来自拉科鲁尼亚(A Coruna)市的污水和夏季的底栖矿化(主要是硅酸盐)是海港营养的主要来源。与Rias Bajas不同,由于海港地理位置偏僻,上升流是营养的极差来源。 NIP比率低于Redfield比率,其中氮是限制营养素。由于这些特殊的水文和生物地球化学条件,浮游植物群落显示出很高的生物量,并以大型硅藻为主,鞭毛虫的贡献可忽略不计,除了冬季混合期间。营养素的人为来源,以及高浮游植物生物量和高初级生产产生的水氧超饱和都表明富营养化。然而,没有观察到缺氧发作。在加利西亚里亚斯,富营养化是自然上升的结果。然而,由于人为活动,拉科鲁尼亚港现在被描述为加利西亚海岸上最重要的富营养化地区。 (C)2003版《科学与医学》 Elsevier SAS。版权所有。 [参考:42]

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