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  • Copernicus Publications on behalf of the European Geosciences Union  (1)
  • PANGAEA  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Birk, Matthew A; McLean, Erin L; Seibel, Brad A (2018): Ocean acidification does not limit squid metabolism via blood oxygen supply. Journal of Experimental Biology, 221(19), jeb187443, https://doi.org/10.1242/jeb.187443
    Publication Date: 2024-06-06
    Description: Ocean acidification is hypothesized to limit the performance of squid owing to their exceptional oxygen demand and pH sensitivity of blood–oxygen binding, which may reduce oxygen supply in acidified waters. The critical oxygen partial pressure (Pcrit), the PO2 below which oxygen supply cannot match basal demand, is a commonly reported index of hypoxia tolerance. Any CO2-induced reduction in oxygen supply should be apparent as an increase in Pcrit. In this study, we assessed the effects of CO2 (46–143 Pa; 455–1410 μatm) on the metabolic rate and Pcrit of two squid species - Dosidicus gigas and Doryteuthis pealeii – through manipulative experiments. We also developed a model, with inputs for hemocyanin pH sensitivity, blood PCO2 and buffering capacity, that simulates blood oxygen supply under varying seawater CO2 partial pressures. We compare model outputs with measured Pcrit in squid. Using blood–O2 parameters from the literature for model inputs, we estimated that, in the absence of blood acid–base regulation, an increase in seawater PCO2 to 100 Pa (1000 μatm) would result in a maximum drop in arterial hemocyanin–O2 saturation by 1.6% at normoxia and a Pcrit increase of 0.5 kPa. Our live-animal experiments support this supposition, as CO2 had no effect on measured metabolic rate or Pcrit in either squid species.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Behaviour; Benthos; Bicarbonate ion; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Containers and aquaria (20-1000 L or 〈 1 m**2); Doryteuthis pealeii; Dosidicus gigas; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gender; Growth/Morphology; Identification; Laboratory experiment; Mantle, length; Mass; Metabolic rate of oxygen; Mollusca; Nekton; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Oxygen, partial pressure; Oxygen, partial pressure, critical; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Registration number of species; Respiration; Salinity; Single species; Species; Temperate; Temperature, water; Type; Uniform resource locator/link to reference; Ventilation rate
    Type: Dataset
    Format: text/tab-separated-values, 2908 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 9 (2012): 747-757, doi:10.5194/bg-9-747-2012.
    Description: Shelled pteropods (Thecosomata) are a group of holoplanktonic mollusks that are believed to be especially sensitive to ocean acidification because their aragonitic shells are highly soluble. Despite this concern, there is very little known about the physiological response of these animals to conditions of elevated carbon dioxide. This study examines the oxygen consumption and ammonia excretion of five pteropod species, collected from tropical regions of the Pacific Ocean, to elevated levels of carbon dioxide (0.10%, 1000 ppm). Our results show that pteropods that naturally migrate into oxygen minimum zones, such as Hyalocylis striata, Clio pyramidata, Cavolinia longirostris and Creseis virgula, were not affected by carbon dioxide at the levels and duration tested. Diacria quadridentata, which does not migrate, responds to high carbon dioxide conditions with reduced oxygen consumption and ammonia excretion. This indicates that the natural chemical environment of individual species may influence their resilience to ocean acidification.
    Description: Funding of the National Science Foundation (grant OCE-0526502 to Wishner and Seibel, OCE – 0526545 to Daly, and OCE – 0851043 to Seibel), the University of Rhode Island, and the Rhode Island Experimental Program to Stimulate Competitive Research Fellowship Program.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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