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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Main Authors: Ern, Rasmus, Johansen, Jacob L., Rummer, Jodie L., Esbaugh, Andrew J.
Format: Dataset
Language:unknown
Published: 2017
Subjects:
Online Access:https://zenodo.org/record/4944724
https://doi.org/10.5061/dryad.77pq8
id ftzenodo:oai:zenodo.org:4944724
record_format openpolar
spelling 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
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic 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