1993
DOI: 10.1006/ecss.1993.1067
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Late Summer Trophic Conditions in the North-east Gulf of Finland and the River Neva Estuary, Baltic Sea

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Cited by 44 publications
(35 citation statements)
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“…1) can be divided into 4 main subareas according to the geomorphological and hydrodynamical features ( Fig. 2; Pitkanen et al 1993). The 2 easternmost areas form the Neva Estuary, separated from the open Gulf by a belt of islands, reefs and shallows (referred as the transition zone or the gradient area).…”
Section: Study Areamentioning
confidence: 99%
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“…1) can be divided into 4 main subareas according to the geomorphological and hydrodynamical features ( Fig. 2; Pitkanen et al 1993). The 2 easternmost areas form the Neva Estuary, separated from the open Gulf by a belt of islands, reefs and shallows (referred as the transition zone or the gradient area).…”
Section: Study Areamentioning
confidence: 99%
“…that discharge into this enclosed brackish water sea area evidently greatly affect nutrient conditions. However, studies on nutrient and eutrophication dynamics in the most loaded estuarine areas (Gulf of Riga, eastern Gulf of Finland) were not done until in the 1990s (Pitkanen et al 1993, Yurkovskis et al 1993.…”
Section: Introductionmentioning
confidence: 99%
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“…Effects of winds are commonly reported, for example, in San Francisco Bay estuary (Cloern 1996), Chesapeake Bay estuary (Horrigan et al 1990), and in coastal oceans such as the one off the coast of Washington, USA (Dortch & Poste1 1989) and Dogger Bank in the North Sea (Riegman et al 1990). Blooms often occur in summer after wind events (Iverson et al 1974, Hitchcock et al 1987, Pitkanen et al 1993.…”
Section: Introductionmentioning
confidence: 99%
“…The trend is in fact gen-198 Lehtiniemi & Gorokhova: Alien cladoceran affects native copepods eral for zooplankton biomass distribution in the Gulf (Telesh 2004), suggesting that both species maintain residency in the proximal part of the estuary. Several mechanisms could be responsible for this, including low salinity water (3 to 4 PSU) and low rate of water exchange (Pitkänen et al 1993), elevated concentrations of food available due to higher nutrient loading (Telesh 2004), and reproduction mode of these zooplankters, which is favored in estuarine shallow water conditions (both species carry their eggs/embryos until the release, and produce resting eggs). In the water column, C. pengoi is most abundant above the thermocline, although it also occurs in deeper waters (this study), while in E. affinis, the major part of the population is confined to the thermocline during daytime and migrates upwards to the surface at night (Vuorinen 1987).…”
mentioning
confidence: 99%