2003
DOI: 10.1242/jeb.00141
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Biological impacts of deep-sea carbon dioxide injection inferred from indices of physiological performance

Abstract: SUMMARYA recent proposal to store anthropogenic carbon dioxide in the deep ocean is assessed here with regard to the impacts on deep-living fauna. The stability of the deep-sea has allowed the evolution of species ill-equipped to withstand rapid environmental changes. Low metabolic rates of most deep-sea species are correlated with low capacities for pH buffering and low concentrations of ion-transport proteins. Changes in seawater carbon dioxide partial pressure (PCO2) may thus lead to large cellular PCO2 and… Show more

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Cited by 172 publications
(109 citation statements)
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“…Full compensation for these changes often takes up to 48-72 h (Seibel and Walsh, 2003). The response measured in our experiments, being after only 6-18 h of exposure, may not be one of a final stable steady state and cannot be interpreted as indicative of a response to chronic acidification, only to the type pteropods would experience during short migrations into regions of hypercapnia.…”
Section: Speciesmentioning
confidence: 57%
“…Full compensation for these changes often takes up to 48-72 h (Seibel and Walsh, 2003). The response measured in our experiments, being after only 6-18 h of exposure, may not be one of a final stable steady state and cannot be interpreted as indicative of a response to chronic acidification, only to the type pteropods would experience during short migrations into regions of hypercapnia.…”
Section: Speciesmentioning
confidence: 57%
“…However, the ability to cope with chronic exposure to elevated pCO 2 conditions appears to be characterized by the acquisition of moderately lower metabolic rates (on average 223% in this study) in both the acclimatized and the adapted species. While metabolic depression in the short term helps an organism to maintain a balance between energy supply and demand [15,16,25,26,111], in the longer term it can rstb.royalsocietypublishing.org Phil Trans R Soc B 368: 20120444 involve the reorganization of its energy budget, often leading to a decrease in its scope for growth and reproduction [2].…”
Section: (A) Discriminating Between Acclimatization and Adaptationmentioning
confidence: 99%
“…Oxygen consumption rates have now been measured for deep-and shallow-living representatives of many major phyla, both benthic and pelagic, and in several regions. Biochemical proxies of metabolism have provided estimates of metabolic capacity in many additional species (Torres & Somero 1988;Childress & Somero 1990;Seibel et al 1998Drazen 2002a;Seibel & Walsh 2003;Treberg et al 2003;Dalhoff 2004;Thuesen et al 2005b), while submersibles, landers and new tagging techniques have provided detailed studies of locomotion and behaviour in the deep sea (Priede et al 1990;Marshall & Diebel 1995;Villanueva et al 1997;Hunt & Seibel 2000;Bailey et al 2003Bailey et al , 2005Drazen & Robison 2004;Robison 2004;Seibel et al 2005). More than 10 years have passed since the last specific reviews of deep-sea metabolic rates (Childress 1995;Mahaut et al 1995).…”
Section: Introductionmentioning
confidence: 99%