Loading…
Osmo-respiratory compromise in the mosshead sculpin (Clinocottus globiceps): effects of temperature, hypoxia, and re-oxygenation on rates of diffusive water flux and oxygen uptake
In nature, mosshead sculpins ( Clinocottus globiceps ) are challenged by fluctuations in temperature and oxygen levels in their environment. However, it is unclear how mosshead sculpins modulate the permeability of their branchial epithelia to water and O 2 in response to temperature or hypoxia stre...
Saved in:
Published in: | Fish physiology and biochemistry 2023-10, Vol.49 (5), p.853-866 |
---|---|
Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Summary: | In nature, mosshead sculpins (
Clinocottus globiceps
) are challenged by fluctuations in temperature and oxygen levels in their environment. However, it is unclear how mosshead sculpins modulate the permeability of their branchial epithelia to water and O
2
in response to temperature or hypoxia stress. Acute decrease in temperature from 13 to 6
o
C reduced diffusive water flux rate by 22% and ṀO
2
by 51%, whereas acute increase in temperature from 13 to 25
o
C increased diffusive water flux rate by 217% and ṀO
2
by 140%, yielding overall Q
10
values of 2.08 and 2.47 respectively. Acute reductions in oxygen tension from >95% to 20% or 10% air saturation did not impact diffusive water flux rates, however, ṀO
2
was reduced significantly by 36% and 65% respectively. During 1-h or 3-h recovery periods diffusive water flux rates were depressed while ṀO
2
exhibited overshoots beyond the normoxic control level. Many responses differed from those seen in our parallel earlier study on the tidepool sculpin, a cottid with similar hypoxia tolerance but much smaller gill area that occupies a similar environment. Overall, our data suggest that during temperature stress, diffusive water flux rates and ṀO
2
follow the traditional osmo-respiratory compromise pattern, but during hypoxia and re-oxygenation stress, diffusive water flux rates are decoupled from ṀO
2
. |
---|---|
ISSN: | 0920-1742 1573-5168 |
DOI: | 10.1007/s10695-023-01226-0 |