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First published online May 29, 2009
Journal of Experimental Biology 212, 1949-1964 (2009)
Published by The Company of Biologists 2009
doi: 10.1242/jeb.028464
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Regulation of gill transcellular permeability and renal function during acute hypoxia in the Amazonian oscar (Astronotus ocellatus): new angles to the osmorespiratory compromise

Chris M. Wood1,2,*, Fathima I. Iftikar1, Graham R. Scott3, Gudrun De Boeck4, Katherine A. Sloman5, Victoria Matey6, Fabiola X. Valdez Domingos7, Rafael Mendonça Duarte7, Vera M. F. Almeida-Val7 and Adalberto L. Val7

1 Department of Biology, McMaster University, Hamilton, Ontario, Canada, L8S 4K1
2 Division of Marine Biology and Fisheries, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL 33149, USA
3 Department of Zoology, University of British Columbia, Vancouver, Canada, V6T 1Z4
4 Department of Biology, University of Antwerp, Groenenborgerlaan 171, B-2020 Antwerp, Belgium
5 School of Biological Sciences, University of Plymouth, Devon PL4 8AA, UK
6 Department of Biology, San Diego State University, 5500 Campanile Drive, San Diego, CA 92182, USA
7 Laboratory of Ecophysiology and Molecular Evolution, Instituto Nacional de Pesquisas da Amazônia (INPA), Manaus, Brazil

* Author for correspondence (e-mail: woodcm{at}mcmaster.ca)

Accepted 16 March 2009

Earlier studies demonstrated that oscars, endemic to ion-poor Amazonian waters, are extremely hypoxia tolerant, and exhibit a marked reduction in active unidirectional Na+ uptake rate (measured directly) but unchanged net Na+ balance during acute exposure to low PO2, indicating a comparable reduction in whole body Na+ efflux rate. However, branchial O2 transfer factor does not fall. The present study focused on the nature of the efflux reduction in the face of maintained gill O2 permeability. Direct measurements of 22Na appearance in the water from bladder-catheterized fish confirmed a rapid 55% fall in unidirectional Na+ efflux rate across the gills upon acute exposure to hypoxia (PO2=10–20 torr; 1 torr=133.3 Pa), which was quickly reversed upon return to normoxia. An exchange diffusion mechanism for Na+ is not present, so the reduction in efflux was not directly linked to the reduction in Na+ influx. A quickly developing bradycardia occurred during hypoxia. Transepithelial potential, which was sensitive to water [Ca2+], became markedly less negative during hypoxia and was restored upon return to normoxia. Ammonia excretion, net K+ loss rates, and 3H2O exchange rates (diffusive water efflux rates) across the gills fell by 55–75% during hypoxia, with recovery during normoxia. Osmotic permeability to water also declined, but the fall (30%) was less than that in diffusive water permeability (70%). In total, these observations indicate a reduction in gill transcellular permeability during hypoxia, a conclusion supported by unchanged branchial efflux rates of the paracellular marker [3H]PEG-4000 during hypoxia and normoxic recovery. At the kidney, glomerular filtration rate, urine flow rate, and tubular Na+ reabsorption rate fell in parallel by 70% during hypoxia, facilitating additional reductions in costs and in urinary Na+, K+ and ammonia excretion rates. Scanning electron microscopy of the gill epithelium revealed no remodelling at a macro-level, but pronounced changes in surface morphology. Under normoxia, mitochondria-rich cells were exposed only through small apical crypts, and these decreased in number by 47% and in individual area by 65% during 3 h hypoxia. We suggest that a rapid closure of transcellular channels, perhaps effected by pavement cell coverage of the crypts, allows conservation of ions and reduction of ionoregulatory costs without compromise of O2 exchange capacity during acute hypoxia, a response very different from the traditional osmorespiratory compromise.

Key words: sodium flux, potassium flux, PEG-4000, diffusive water flux, urine flow rate, glomerular filtration rate, gill morphology, mitochondria rich cell, transepithelial potential, fish


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