Abstract

Low dissolved oxygen levels in the water (hypoxia) can be provoked by oxygen consumption by fish and other organisms, organic matter decomposition, phytoplankton blooms, and temperature increase. The objective of the present study was to investigate Na+, Cl-, K+, and ammonia fluxes in silver catfish (Rhamdia quelen) exposed to different dissolved oxygen levels. Juveniles (9 ± 1g) maintained at 6.0 mg.L-1 dissolved oxygen were transferred to four 40 L aquaria with different dissolved oxygen levels (in mg.L-1): 6.0, 4.5, 3.5, and 2.5. In another series of experiments, juveniles were acclimated at 6.0 or 2.5 mg.L-1 dissolved oxygen levels, and then placed in two 40 L aquaria with 6.0 mg.L-1 dissolved oxygen. For both series of experiments, 1, 24, 48 or 120 h after transference juveniles were placed in individual chambers of 200 mL (with the same dissolved oxygen levels of their respective aquaria) for 3 h. Water samples were collected for analysis of Na+, Cl-, K+, and ammonia levels. The obtained results allow concluding that exposure to 2.5 mg.L-1 dissolved oxygen levels promotes loss of ions and lower ammonia excretion in silver catfish juveniles, but these losses are rapidly stabilized for Na+ and Cl-. Exposure to less hypoxic levels also changes ion fluxes and ammonia excretion, but there is no clear relationship between both parameters in this species. Therefore, silver catfish osmoregulation seems to be affected when this species is transferred from normoxic to hypoxic waters and vice-versa.

Highlights

  • Low dissolved oxygen levels in the water can be provoked by oxygen consumption by fish and other organisms, organic matter decomposition, phytoplankton blooms, and temperature increase (Rantin & Marins, 1984)

  • Silver catfish juveniles transferred to 2.5 mg.L-1 dissolved oxygen levels in the first hour showed significantly higher Na+ and Cl- effluxes than those maintained at 6.0 mg.L-1 dissolved oxygen levels

  • The adaptation of Na+ and Cl- fluxes in silver catfish juveniles exposed to this low oxygen level seems to be fast, as 24 h later these fluxes were similar to fluxes of those maintained at 6.0 mg.L-1 dissolved oxygen levels

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Summary

Introduction

Low dissolved oxygen levels in the water (hypoxia) can be provoked by oxygen consumption by fish and other organisms, organic matter decomposition, phytoplankton blooms, and temperature increase (Rantin & Marins, 1984). Fish compensate oxygen shortage by increasing ventilatory tidal volume and/or ventilation rate, which led to hyperventilation and an increase in gill ventilation (Sakuragui et al, 2003; Evans et al, 2005; Xu et al, 2006). This increase in gill ventilation is accompanied by haemodynamic alterations to increase blood flow in the gills to enhance gas exchange (Sundin, 1999). The increase in gill blood flow and perfusion pressure caused by hypoxia could lead to higher ion loss because it would stimulate diffusive efflux.

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