Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes
Rising ocean temperatures are predicted to cause a poleward shift in the distribution of marine fishes occupying the extent of latitudes tolerable within their thermal range boundaries. A prevailing theory suggests that the upper thermal limits of fishes are constrained by hypoxia and ocean acidific...
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ftzenodo:oai:zenodo.org:4944724 2023-06-06T11:58:06+02:00 Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes Ern, Rasmus Johansen, Jacob L. Rummer, Jodie L. Esbaugh, Andrew J. 2017-06-15 https://zenodo.org/record/4944724 https://doi.org/10.5061/dryad.77pq8 unknown doi:10.1098/rsbl.2017.0135 https://zenodo.org/communities/dryad https://zenodo.org/record/4944724 https://doi.org/10.5061/dryad.77pq8 oai:zenodo.org:4944724 info:eu-repo/semantics/openAccess https://creativecommons.org/publicdomain/zero/1.0/legalcode Hypercapnia (water CO2) Cheilodipterus quinquelineatus Critical thermal maximum (CTmax) Oxygen- and capacity-limited thermal tolerance (OCLTT) Oxygen limit for thermal tolerance (PCTmax) Acanthochromis polyacanthus Chromis atripectoralis Critical oxygen tension (Pcrit) Oxygen uptake (MO2) info:eu-repo/semantics/other dataset 2017 ftzenodo https://doi.org/10.5061/dryad.77pq810.1098/rsbl.2017.0135 2023-04-13T21:04:25Z Rising ocean temperatures are predicted to cause a poleward shift in the distribution of marine fishes occupying the extent of latitudes tolerable within their thermal range boundaries. A prevailing theory suggests that the upper thermal limits of fishes are constrained by hypoxia and ocean acidification. However, some eurythermal fish species do not conform to this theory, and maintain their upper thermal limits in hypoxia. Here we determine if the same is true for stenothermal species. In three coral reef fish species we tested the effect of hypoxia on upper thermal limits, measured as critical thermal maximum (CTmax). In one of these species we also quantified the effect of hypoxia on oxygen supply capacity, measured as aerobic scope (AS). In this species we also tested the effect of elevated CO2 (simulated ocean acidification) on the hypoxia sensitivity of CTmax. We found that CTmax was unaffected by progressive hypoxia down to approximately 35 mmHg, despite a substantial hypoxia-induced reduction in AS. Below approximately 35 mmHg, CTmax declined sharply with water oxygen tension (PwO2). Furthermore, the hypoxia sensitivity of CTmax was unaffected by elevated CO2. Our findings show that moderate hypoxia and ocean acidification do not constrain the upper thermal limits of these tropical, stenothermal fishes. Data for individual animalsCritical thermal maximum (CTmax), maximum metabolic rate (MMR), standard metabolic rate (SMR), aerobic scope (AS), critical oxygen tension (Pcrit), body mass (BM) and experimental conditions for individual animals.Raw data for SMR and PcritIndividual MO2 points as a function of time for estimates of SMR Individual MO2 points as a function of water oxygen tension for estimates of PcritFunding provided by: National Science FoundationCrossref Funder Registry ID: http://dx.doi.org/10.13039/100000001Award Number: EF-1315290 Dataset Ocean acidification Zenodo |
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Hypercapnia (water CO2) Cheilodipterus quinquelineatus Critical thermal maximum (CTmax) Oxygen- and capacity-limited thermal tolerance (OCLTT) Oxygen limit for thermal tolerance (PCTmax) Acanthochromis polyacanthus Chromis atripectoralis Critical oxygen tension (Pcrit) Oxygen uptake (MO2) |
spellingShingle |
Hypercapnia (water CO2) Cheilodipterus quinquelineatus Critical thermal maximum (CTmax) Oxygen- and capacity-limited thermal tolerance (OCLTT) Oxygen limit for thermal tolerance (PCTmax) Acanthochromis polyacanthus Chromis atripectoralis Critical oxygen tension (Pcrit) Oxygen uptake (MO2) Ern, Rasmus Johansen, Jacob L. Rummer, Jodie L. Esbaugh, Andrew J. Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
topic_facet |
Hypercapnia (water CO2) Cheilodipterus quinquelineatus Critical thermal maximum (CTmax) Oxygen- and capacity-limited thermal tolerance (OCLTT) Oxygen limit for thermal tolerance (PCTmax) Acanthochromis polyacanthus Chromis atripectoralis Critical oxygen tension (Pcrit) Oxygen uptake (MO2) |
description |
Rising ocean temperatures are predicted to cause a poleward shift in the distribution of marine fishes occupying the extent of latitudes tolerable within their thermal range boundaries. A prevailing theory suggests that the upper thermal limits of fishes are constrained by hypoxia and ocean acidification. However, some eurythermal fish species do not conform to this theory, and maintain their upper thermal limits in hypoxia. Here we determine if the same is true for stenothermal species. In three coral reef fish species we tested the effect of hypoxia on upper thermal limits, measured as critical thermal maximum (CTmax). In one of these species we also quantified the effect of hypoxia on oxygen supply capacity, measured as aerobic scope (AS). In this species we also tested the effect of elevated CO2 (simulated ocean acidification) on the hypoxia sensitivity of CTmax. We found that CTmax was unaffected by progressive hypoxia down to approximately 35 mmHg, despite a substantial hypoxia-induced reduction in AS. Below approximately 35 mmHg, CTmax declined sharply with water oxygen tension (PwO2). Furthermore, the hypoxia sensitivity of CTmax was unaffected by elevated CO2. Our findings show that moderate hypoxia and ocean acidification do not constrain the upper thermal limits of these tropical, stenothermal fishes. Data for individual animalsCritical thermal maximum (CTmax), maximum metabolic rate (MMR), standard metabolic rate (SMR), aerobic scope (AS), critical oxygen tension (Pcrit), body mass (BM) and experimental conditions for individual animals.Raw data for SMR and PcritIndividual MO2 points as a function of time for estimates of SMR Individual MO2 points as a function of water oxygen tension for estimates of PcritFunding provided by: National Science FoundationCrossref Funder Registry ID: http://dx.doi.org/10.13039/100000001Award Number: EF-1315290 |
format |
Dataset |
author |
Ern, Rasmus Johansen, Jacob L. Rummer, Jodie L. Esbaugh, Andrew J. |
author_facet |
Ern, Rasmus Johansen, Jacob L. Rummer, Jodie L. Esbaugh, Andrew J. |
author_sort |
Ern, Rasmus |
title |
Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
title_short |
Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
title_full |
Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
title_fullStr |
Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
title_full_unstemmed |
Data from: Effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
title_sort |
data from: effects of hypoxia and ocean acidification on the upper thermal niche boundaries of coral reef fishes |
publishDate |
2017 |
url |
https://zenodo.org/record/4944724 https://doi.org/10.5061/dryad.77pq8 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
doi:10.1098/rsbl.2017.0135 https://zenodo.org/communities/dryad https://zenodo.org/record/4944724 https://doi.org/10.5061/dryad.77pq8 oai:zenodo.org:4944724 |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/publicdomain/zero/1.0/legalcode |
op_doi |
https://doi.org/10.5061/dryad.77pq810.1098/rsbl.2017.0135 |
_version_ |
1767966560030294016 |