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Processus advectifs et répartition du zooplancton dans un fjord

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Abstract

In order to study the influence of advective processes on the zooplankton distribution in a shallow sill-fjord, we examined the temporal variations (tidal and seasonal) of currents, density, abundance and composition of zooplankton in the Saguenay fjord, Québec, Canada, in August 1978 and October 1979. Our results demonstrate the existence of a regular exchange of water (every tidal cycle) between the St. Lawrence estuary and the two outer basins of the Saguenay fjord which is characterized by an important transport of mesoplankton from the estuary into the deep waters of the Saguenay during the rising tide and from the surface waters of the Saguenay to those of the estuary during falling tide. Variations of abundance and composition of zooplankton in the outer basin are therefore mainly controlled by advective processes. The plankton community of the downstream region of the fjord is strongly influenced by variations of abundance and composition taking place in the estuary, and the establishment and development of local populations of zooplankton are made difficult. In the upstream region of the fjord, the advective processes are less intense and endogeneous mesoplankton populations thrive under local temperature conditions.

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Communicated by R. W. Doyle, Halifax

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De Ladurantaye, R., Therriault, JC., Lacroix, G. et al. Processus advectifs et répartition du zooplancton dans un fjord. Mar. Biol. 82, 21–29 (1984). https://doi.org/10.1007/BF00392760

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  • DOI: https://doi.org/10.1007/BF00392760

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