Seawater carbonate chemistry and oxygen uptake rates of coral reef fishes

Ocean acidification, resulting from increasing atmospheric carbon dioxide (CO2) emissions, can affect the physiological performance of some fishes. Most studies investigating ocean acidification have used stable pCO2 treatments based on open ocean predictions. However, nearshore systems can experience substantial spatial and temporal variations in pCO2. Notably, coral reefs are known to experience diel fluctuations in pCO2, which are expected to increase on average and in magnitude in the future. Though we know these variations exist, relatively few studies have included fluctuating treatments... Mehr ...

Verfasser: Hannan, Kelly D
Munday, Philip L
Rummer, Jodie L
Dokumenttyp: dataset
Erscheinungsdatum: 2020
Verlag/Hrsg.: PANGAEA
Schlagwörter: Acanthochromis polyacanthus / Aerobic scope of oxygen / Alkalinity / total / standard error / Amblyglyphidodon curacao / Animalia / Aragonite saturation state / Bicarbonate ion / Calcite saturation state / Calculated using CO2SYS / Calculated using seacarb after Nisumaa et al. (2010) / Carbon / inorganic / dissolved / Carbonate ion / Carbonate system computation flag / Carbon dioxide / Chordata / Coast and continental shelf / Comment / Containers and aquaria (20-1000 L or < 1 m**2) / Factorial aerobic scope / Fugacity of carbon dioxide (water) at sea surface temperature (wet air) / Glucose / Growth/Morphology / Haematocrit / Haemoglobin / Height / Identification / Laboratory experiment / Lactate / Length / standard / Mass / Mean corpuscular haemoglobin concentration / Nekton / OA-ICC / Ocean Acidification International Coordination Centre / Other / Other studied parameter or process / Oxygen uptake rate / Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) / Pelagos / pH
Sprache: Englisch
Permalink: https://search.fid-benelux.de/Record/base-28974862
Datenquelle: BASE; Originalkatalog
Powered By: BASE
Link(s) : https://doi.pangaea.de/10.1594/PANGAEA.925711

Ocean acidification, resulting from increasing atmospheric carbon dioxide (CO2) emissions, can affect the physiological performance of some fishes. Most studies investigating ocean acidification have used stable pCO2 treatments based on open ocean predictions. However, nearshore systems can experience substantial spatial and temporal variations in pCO2. Notably, coral reefs are known to experience diel fluctuations in pCO2, which are expected to increase on average and in magnitude in the future. Though we know these variations exist, relatively few studies have included fluctuating treatments when examining the effects of ocean acidification conditions on coral reef species. To address this, we exposed two species of damselfishes, Amblyglyphidodon curacao and Acanthochromis polyacanthus, to ambient pCO2, a stable elevated pCO2 treatment, and two fluctuating pCO2 treatments (increasing and decreasing) over an 8 h period. Oxygen uptake rates were measured both while fish were swimming and resting at low-speed. These 8 h periods were followed by an exhaustive swimming test (Ucrit) and blood draw examining swimming metrics and haematological parameters contributing to oxygen transport. When A. polyacanthus were exposed to stable pCO2 conditions (ambient or elevated), they required more energy during the 8 h trial regardless of swimming type than fish exposed to either of the fluctuating pCO2 treatments (increasing or decreasing). These results were reflected in the oxygen uptake rates during the Ucrit tests, where fish exposed to fluctuating pCO2 treatments had a higher factorial aerobic scope than fish exposed to stable pCO2 treatments. By contrast, A. curacao showed no effect of pCO2 treatment on swimming or oxygen uptake metrics. Our results show that responses to stable versus fluctuating pCO2 differ between species – what is stressful for one species many not be stressful for another. Such asymmetries may have population- and community-level impacts under higher more variable pCO2 conditions in the future.