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  • 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  (1)
  • Metabolic rate  (1)
Document type
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  (1)
  • Metabolic rate  (1)
  • Hypoxia  (2)
  • Acidification  (1)
  • Aerobic scope  (1)
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Years
  • 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: 2022-05-27
    Description: Author Posting. © Company of Biologists, 2021. This article is posted here by permission of Company of Biologists for personal use, not for redistribution. The definitive version was published in Journal of Experimental Biology 224(8), (2021): jeb242210, https://doi.org/10.1242/jeb.242210.
    Description: The critical oxygen partial pressure (Pcrit), typically defined as the PO2 below which an animal's metabolic rate (MR) is unsustainable, is widely interpreted as a measure of hypoxia tolerance. Here, Pcrit is defined as the PO2 at which physiological oxygen supply (α0) reaches its maximum capacity (α; µmol O2 g−1 h−1 kPa−1). α is a species- and temperature-specific constant describing the oxygen dependency of the maximum metabolic rate (MMR=PO2×α) or, equivalently, the MR dependence of Pcrit (Pcrit=MR/α). We describe the α-method, in which the MR is monitored as oxygen declines and, for each measurement period, is divided by the corresponding PO2 to provide the concurrent oxygen supply (α0=MR/PO2). The highest α0 value (or, more conservatively, the mean of the three highest values) is designated as α. The same value of α is reached at Pcrit for any MR regardless of previous or subsequent metabolic activity. The MR need not be constant (regulated), standardized or exhibit a clear breakpoint at Pcrit for accurate determination of α. The α-method has several advantages over Pcrit determination and non-linear analyses, including: (1) less ambiguity and greater accuracy, (2) fewer constraints in respirometry methodology and analysis, and (3) greater predictive power and ecological and physiological insight. Across the species evaluated here, α values are correlated with MR, but not Pcrit. Rather than an index of hypoxia tolerance, Pcrit is a reflection of α, which evolves to support maximum energy demands and aerobic scope at the prevailing temperature and oxygen level.
    Description: This project was supported by National Oceanic and Atmospheric Administration grants NA18NOS4780167 and NA17OAR4310081 and National Science Foundation grant OCE-1459243 to B.A.S., the Jack and Katharine Ann Lake Fellowship to A.A., the Anne and Werner Von Rosenstiel Fellowship and Garrels Memorial Endowed Fellowship to A.W.T., the Hogarth Fellowship to C.J.W., the Southern Kingfish Association Fellowship to A.L.B., and a National Science Foundation postdoctoral fellowship (DBI-1907197) to M.A.B.
    Description: 2022-04-30
    Keywords: Aerobic scope ; Hypoxia ; Metabolic rate ; Ocean deoxygenation ; Oxygen and capacity limited thermal tolerance ; Oxygen supply ; Respirometry
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
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