The crab-eating frog, Rana cancrivora, up-regulates hepatic carbamoyl phosphate synthetase I activity and tissue osmolyte levels in response to increased salinity

The crab‐eating frog Rana cancrivora is one of only a handful of amphibians worldwide that tolerate saline waters. They typically inhabit brackish water of mangrove forests of Southeast Asia, but live happily in freshwater and can be acclimated to 75% seawater (25 ppt) or higher. We report here that...

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Veröffentlicht in:Journal of experimental zoology. Part A, Comparative experimental biology Comparative experimental biology, 2004-07, Vol.301A (7), p.559-568
Hauptverfasser: Wright, Patricia, Anderson, Paul, Weng, Lei, Frick, Natasha, Wong, Wei Peng, IP, Yuen Kwong
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container_issue 7
container_start_page 559
container_title Journal of experimental zoology. Part A, Comparative experimental biology
container_volume 301A
creator Wright, Patricia
Anderson, Paul
Weng, Lei
Frick, Natasha
Wong, Wei Peng
IP, Yuen Kwong
description The crab‐eating frog Rana cancrivora is one of only a handful of amphibians worldwide that tolerate saline waters. They typically inhabit brackish water of mangrove forests of Southeast Asia, but live happily in freshwater and can be acclimated to 75% seawater (25 ppt) or higher. We report here that after transfer of juvenile R. cancrivora from freshwater (1 ppt) to brackish water (10 →20 or 20 →25 ppt; 4–8 d) there was a significant increase in the specific activity of the key hepatic ornithine urea cycle enzyme (OUC), carbamoyl phosphate synthetase I (CPSase I). At 20 ppt, plasma, liver and muscle urea levels increased by 22‐, 21‐, and 11‐fold, respectively. As well, muscle total amino acid levels were significantly elevated by 6‐fold, with the largest changes occurring in glycine and β‐alanine levels. In liver, taurine levels were 5‐fold higher in frogs acclimated to 20 ppt. There were no significant changes in urea or ammonia excretion rates to the environment. As well, the rate of urea influx (Jinurea) and efflux (Jouturea) across the ventral pelvic skin did not differ between frogs acclimated to 1 versus 20 ppt. Taken together, these findings suggest that acclimation to saline water involves the up‐regulation of hepatic urea synthesis, which in turn contributes to the dramatic rise in tissue urea levels. The lack of change in urea excretion rates, despite the large increase in tissue‐to‐water gradients further indicates that mechanisms must be in place to prevent excessive loss of urea in saline waters, but these mechanisms do not include cutaneous urea uptake. Also, amino acid accumulation may contribute to an overall rise in the osmolarity of the muscle tissue, but relative to urea, the contribution is small. J. Exp. Zool. 301A:559–568, 2004. © 2004 Wiley‐Liss, Inc.
doi_str_mv 10.1002/jez.a.54
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They typically inhabit brackish water of mangrove forests of Southeast Asia, but live happily in freshwater and can be acclimated to 75% seawater (25 ppt) or higher. We report here that after transfer of juvenile R. cancrivora from freshwater (1 ppt) to brackish water (10 →20 or 20 →25 ppt; 4–8 d) there was a significant increase in the specific activity of the key hepatic ornithine urea cycle enzyme (OUC), carbamoyl phosphate synthetase I (CPSase I). At 20 ppt, plasma, liver and muscle urea levels increased by 22‐, 21‐, and 11‐fold, respectively. As well, muscle total amino acid levels were significantly elevated by 6‐fold, with the largest changes occurring in glycine and β‐alanine levels. In liver, taurine levels were 5‐fold higher in frogs acclimated to 20 ppt. There were no significant changes in urea or ammonia excretion rates to the environment. As well, the rate of urea influx (Jinurea) and efflux (Jouturea) across the ventral pelvic skin did not differ between frogs acclimated to 1 versus 20 ppt. Taken together, these findings suggest that acclimation to saline water involves the up‐regulation of hepatic urea synthesis, which in turn contributes to the dramatic rise in tissue urea levels. The lack of change in urea excretion rates, despite the large increase in tissue‐to‐water gradients further indicates that mechanisms must be in place to prevent excessive loss of urea in saline waters, but these mechanisms do not include cutaneous urea uptake. Also, amino acid accumulation may contribute to an overall rise in the osmolarity of the muscle tissue, but relative to urea, the contribution is small. J. Exp. 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identifier ISSN: 1548-8969
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subjects Amino Acids - metabolism
Analysis of Variance
Animals
Biological Transport
Brackish
Carbamoyl-Phosphate Synthase (Ammonia) - biosynthesis
Enzyme Induction
Fresh Water
Freshwater
Liver - enzymology
Liver - metabolism
Marine
Muscle, Skeletal - metabolism
Rana cancrivora
Ranidae - metabolism
Ranidae - physiology
Seawater
Sodium Chloride - metabolism
Taurine - metabolism
Urea - metabolism
Water-Electrolyte Balance - physiology
title The crab-eating frog, Rana cancrivora, up-regulates hepatic carbamoyl phosphate synthetase I activity and tissue osmolyte levels in response to increased salinity
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