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Distribution Patterns of Isomorphic Cold-Water Dinoflagellates (Scrippsiella/Woloszynskia Complex) Causing ‘red tides’ in the Baltic Sea

机译:在波罗的海引起“赤潮”的同构冷水龙鞭藻(S草/沃洛斯基斯基复合体)的分布模式

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During the latest years medium-sized (15–30 μm), single-celled dinoflagellates have been reported to form blooms in the northern Baltic Proper and the Gulf of Finland in winter and spring. Recent studies (Kremp et al., 2003. Proceedings of the 7th International conference of Modern and Fossil Dinoflagellates, September 21–25, Nagasaki, Japan, 66 pp.) indicate that those blooms are caused by two isomorphic species – Scrippsiella hangoei (Schiller) Larsen, and a new species, tentatively belonging to the genus Woloszynskia. Until now there has been no report on how widely distributed these phytoplankton species are in the Baltic Sea. In this study, the occurrence of Scrippsiella/Woloszynskia complex in the entire Baltic Sea was investigated, by using monitoring data from 1997 to 2003. The species occurred in a salinity range from 2 to 8 PSU. Highest concentrations were observed at salinity 4.5–6.5 PSU. Maximum cell densities of Scrippsiella/Woloszynskia complex in the water column were mainly obtained in April or in the beginning of May by the water temperature <3 °C prior to stratification was formed. In the central Gulf of Finland, the second maximum was found in 1999 and 2002 by the temperature >6 °C. Bloom formations in the Baltic Proper and in the Gulf of Finland may not only be explained by optimum temperature and salinity, but also with other factors e.g. high nutrient concentrations and good seeding conditions from the sediments.
机译:在最近的几年中,据报道中等大小(15–30μm)的单鞭毛鞭毛虫在冬季和春季在波罗的海北部和芬兰湾形成水华。最近的研究(Kremp等人,2003年。第7届国际现代和化石恐龙鞭毛会议会议记录,9月21日至25日,日本长崎,第66页)表明,这些花是由两个同构物种-悬钩子(Scrippsella hangoei)(席勒)引起的。 )拉森(Larsen)和一个新物种,暂时属于Woloszynskia属。到目前为止,还没有关于这些浮游植物在波罗的海分布的报道。在这项研究中,通过使用1997年至2003年的监测数据,对整个波罗的海的链球菌/沃洛斯基斯基复合体的发生进行了调查。该物种的盐度范围为2至8 PSU。在盐度为4.5–6.5 PSU时观察到最高浓度。在形成分层之前,水温<3°C时,主要是在4月或5月初获得水柱中链霉菌/沃洛斯基斯基复合物的最大细胞密度。在芬兰中部,1999年和2002年,温度> 6°C,发现了第二个最高峰。波罗的海适当地区和芬兰湾的水华形成不仅可以用最佳温度和盐度来解释,还可以用其他因素来解释。营养物质浓度高,沉积物的播种条件好。

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