2014
DOI: 10.1021/es501581j
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Multigenerational Exposure to Ocean Acidification during Food Limitation Reveals Consequences for Copepod Scope for Growth and Vital Rates

Abstract: 29The copepod Calanus finmarchicus is a key component of northern Atlantic food webs, linking 30 energy-transfer from phytoplankton to higher trophic levels. We examined the effect of different 53The carbonate concentration in seawater is declining due to increased pCO2 4 , and meta-analyses 54 indicate that calcifying organisms may be negatively affected by this phenomenon 5 . Marine 55 metazoans rely on a positive CO2 gradient from their body fluids to excrete metabolic CO2 by 56 diffusion. Elevated seawate… Show more

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Cited by 75 publications
(61 citation statements)
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“…finmarchicus do not respond to OA in the range tested here. While metabolic rates were found to increase linearly in a very wide range of OA from pH T 8.02 to pH T 7.16 in culture reared CVs of this species [57], this change would not be sufficient to create any significant difference by the OA scenario tested in the present study (pH T 8.10–7.70). Accordingly, wild caught C .…”
Section: Discussionmentioning
confidence: 75%
“…finmarchicus do not respond to OA in the range tested here. While metabolic rates were found to increase linearly in a very wide range of OA from pH T 8.02 to pH T 7.16 in culture reared CVs of this species [57], this change would not be sufficient to create any significant difference by the OA scenario tested in the present study (pH T 8.10–7.70). Accordingly, wild caught C .…”
Section: Discussionmentioning
confidence: 75%
“…Previously, copepods were considered to be relatively tolerant to OA [26, 27], but several processes in copepods may in fact be affected by low pH, including metabolism [28], pH balance [29], reproduction [30], development [31], growth [32] and survival [33]. Furthermore, diverse sensitivities to OA exist between different species and even between life stages within species [34].…”
Section: Introductionmentioning
confidence: 99%
“…OA is happening at a faster rate than at any time during the past 50 million years (Hön isch et al 2012) and has the potential to affect marine ecosystems throughout the world (Hofmann et al 2010, Kroeker et al 2013. Increased CO 2 affects both calcification and acid−base physiology in marine organisms; in some species, the increased metabolic costs of compensating for decreased pH can divert energy away from growth and reproduction (Melzner et al 2011, Thomsen et al 2013, Pedersen et al 2014. In general, increased CO 2 decreases survival, calcification, growth, and development in marine invertebrates, but with highly variable responses among different groups (Kroeker et al 2013).…”
Section: Introductionmentioning
confidence: 99%