Abundance and biomass of zooplankton collected in 1995 and 1998 in the frontal zone between the Gulf Stream and the Labrador current ...

Vertical distribution of meso- and macroplankton was studied in the region of the most sharply pronounced climatic frontal zone between the Gulf Stream and the Labrador current. Hauls with a plankton net BR 113/140 and visual counts of macroplankton from the Mir submersible were used. In the frontal...

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Bibliographic Details
Main Authors: Vinogradov, Mikhail E, Vereshchaka, Alexander L, Shushkina, Elvira A, Arnautov, Genrikh N
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.760868
https://doi.pangaea.de/10.1594/PANGAEA.760868
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Summary:Vertical distribution of meso- and macroplankton was studied in the region of the most sharply pronounced climatic frontal zone between the Gulf Stream and the Labrador current. Hauls with a plankton net BR 113/140 and visual counts of macroplankton from the Mir submersible were used. In the frontal zone a contact occurs between arctic-boreal communities and communities of the North Atlantic subtropical gyre. The community of the North Atlantic subtropical gyre is more mature in terms of succession; many macroplanktonic carnivores-scavengers (mainly shrimps Acanthephyra) develop there and form a ''living network'' feeding on those transported from the north rich arctic-boreal mesoplankton. As a result biomass of shrimps appears to be significantly higher than biomass of their preys. Peculiarities of vertical distribution and population structure of shrimps were analyzed. Data on quantitative vertical distribution of total biomass of meso- and macroplankton and its principal groups, including gelatinous ... : Supplement to: Vinogradov, Mikhail E; Vereshchaka, Alexander L; Shushkina, Elvira A; Arnautov, Genrikh N (1999): Structure of zooplankton communities of the frontal zone between the Gulf Stream and the Labrador current. Translated from Okeanologiya, 1999, 39(4), 555-566, Oceanology, 39(4), 504-514 ...