2022
DOI: 10.1002/eap.2674
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Pelagic calcifiers face increased mortality and habitat loss with warming and ocean acidification

Abstract: Global change is impacting the oceans in an unprecedented way, and multiple lines of evidence suggest that species distributions are changing in space and time. There is increasing evidence that multiple environmental stressors act together to constrain species habitat more than expected from warming alone. Here, we conducted a comprehensive study of how temperature and aragonite saturation state act together to limit Limacina helicina, globally distributed pteropods that are ecologically important pelagic cal… Show more

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Cited by 7 publications
(27 citation statements)
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“…The present global dependencies of biomass on temperature can differ from the results of local studies (e.g., a negative dependency of pteropod biomass on temperature as found in Bednaršek et al. (2022) and species‐specific responses of foraminifers to a range of environmental parameters as found by Weinkauf et al. (2016)), as our models capture large‐scale climatological effects contrary to local models which reflect physiological responses to environmental gradients on a much smaller scale.…”
Section: Discussioncontrasting
confidence: 77%
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“…The present global dependencies of biomass on temperature can differ from the results of local studies (e.g., a negative dependency of pteropod biomass on temperature as found in Bednaršek et al. (2022) and species‐specific responses of foraminifers to a range of environmental parameters as found by Weinkauf et al. (2016)), as our models capture large‐scale climatological effects contrary to local models which reflect physiological responses to environmental gradients on a much smaller scale.…”
Section: Discussioncontrasting
confidence: 77%
“…Previous work identified carbonate chemistry as an important predictor for net calcification on a local scale (Bednaršek & Ohman, 2015; Bednaršek et al., 2022; Lischka et al., 2011; Manno et al., 2017; Mekkes, Renema, et al., 2021). CO 2 ‐rich waters characterized by low pH, low calcite, and low aragonite saturation states may negatively affect certain calcifying organisms by increasing their dissolution and lowering their calcification rate (Bednaršek, Feely, et al., 2017; Bednaršek et al., 2022; Mekkes, Renema, et al., 2021; Mekkes, Sepúlveda‐Rodríguez, et al., 2021).…”
Section: Discussionmentioning
confidence: 99%
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