Titlebook: Copepoda: Developments in Ecology, Biology and Systematics; Proceedings of the S Rubens M. Lopes,Janet W. Reid,Carlos E. F. Rocha Conferenc

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钢笔尖

The deep-sea copepod fauna of the Southern Ocean: patterns and processesouthern Ocean, the boundary is marked by the Sub-Tropical Convergence, which appears to be the major biogeographic boundary between it and surrounding provinces. Evidence for seasonality in various families is reviewed in light of what we know and can infer about their biology and particularly in re

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Production and fate of faecal pellets during summer in an East Antarctic fjordies. Additionally, we propose that the summer ice melt changes the physical characteristics of the water column and the phytoplankton species abundance and distribution; both of which potentially impact on the distribution and abundance of copepods, thereby regulating faecal pellet flux.

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Effects of the ice-edge bloom and season on the metabolism of copepods in the Weddell Sea, Antarctic . showed a similar pattern. The omnivorous copepods . and . showed no changes in metabolism between zones. Data on routine rates of copepods from the winter were available for . and . In ., rates were higher in the summer. . showed a higher metabolic rate in the summer than in the winter, but the d

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The effect of the receding ice edge on the condition of copepods in the northwestern Weddell Sea: reivity level. Citrate synthase activity in . and ., all herbivores, increased between pre-and post-bloom stations. . and ., which feed during winter, had large increases in LDH activity between pre- and post-bloom stations. . and ., the two largest species studied, showed variations in MDH activity,

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Patterns in stage duration and development among marine and freshwater calanoid and cyclopoid copepo states that the duration of a given life history stage is a constant proportion of the embryonic development time; the second rule states that the time spent in each stage is the same for all stages. This review focuses on the second rule. From the 80+ published studies of copepod stage-specific de

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The influence of coastal upwelling on the distribution of , in the Mejillones Peninsula (northern Ch temperature-dependent rates. The potential loss of biomass from the upwelling center because of advection in the upwelling plume was estimated from current data in the Ekman layer and biomass density. The mean cross-shelf component of the current was estimated at 10.4km d. within the upwelling plum

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