Abstract:Deoxygenation in coastal and open‐ocean ecosystems rarely exists in isolation but occurs concomitantly with acidification. Here, we first combine meta‐data of experimental assessments from across the globe to investigate the potential interactive impacts of deoxygenation and acidification on a broad range of marine taxa. We then characterize the differing degrees of deoxygenation and acidification tested in our dataset using a ratio between the partial pressure of oxygen and carbon dioxide (pO2/pCO2) to assess… Show more
“…Our meta-analysis revealed a prevalence of additive interactions between OA and heavy metals, indicating that cumulative effects of OA and heavy metals on marine biota can be reasonably well assessed by summing the single stressor impacts. The prevalence of additive interactions discovered in the present study agrees well with previous meta-analysis studies, in which most stressor interactions were additive across experimental studies (Darling and Côté, 2008;Przeslawski et al, 2015;Jin et al, 2019;Steckbauer et al, 2020), while overall synergisms or antagonisms were uncommon (Burkepile and Hay, 2006;Stephens et al, 2013;Jackson et al, 2016;Yue et al, 2017). Because OA had positive effects on organisms and most frequently interacted additively with heavy metals, our analysis found that OA alleviated the harmful effects of heavy metals, leading to an overall neutral effect co-exposure.…”
Ocean acidification (OA) may interact with anthropogenic pollutants, such as heavy metals (HM), to represent a threat to marine organisms and ecosystems. Here, we perform a quantitative meta-analysis to examine the combined effects of OA and heavy metals on marine organisms. The results reveal predominantly additive interactions (67%), with a considerable proportion of synergistic interactions (25%) and a few antagonistic interactions (8%). The overall adverse effects of heavy metals on marine organisms were alleviated by OA, leading to a neutral impact of heavy metals in combination with OA. However, different taxonomic groups showed large variabilities in their responses, with microalgae being the most sensitive when exposed to heavy metals and OA, and having the highest proportion of antagonistic interactions. Furthermore, the variations in interaction type frequencies are related to climate regions and heavy metal properties, with antagonistic interactions accounting for the highest proportion in temperate regions (28%) and when exposed to Zn (52%). Our study provides a comprehensive insight into the interactive effects of OA and HM on marine organisms, and highlights the importance of further investigating the responses of different marine taxonomic groups from various geographic locations to the combined stress of OA and HM.
“…Our meta-analysis revealed a prevalence of additive interactions between OA and heavy metals, indicating that cumulative effects of OA and heavy metals on marine biota can be reasonably well assessed by summing the single stressor impacts. The prevalence of additive interactions discovered in the present study agrees well with previous meta-analysis studies, in which most stressor interactions were additive across experimental studies (Darling and Côté, 2008;Przeslawski et al, 2015;Jin et al, 2019;Steckbauer et al, 2020), while overall synergisms or antagonisms were uncommon (Burkepile and Hay, 2006;Stephens et al, 2013;Jackson et al, 2016;Yue et al, 2017). Because OA had positive effects on organisms and most frequently interacted additively with heavy metals, our analysis found that OA alleviated the harmful effects of heavy metals, leading to an overall neutral effect co-exposure.…”
Ocean acidification (OA) may interact with anthropogenic pollutants, such as heavy metals (HM), to represent a threat to marine organisms and ecosystems. Here, we perform a quantitative meta-analysis to examine the combined effects of OA and heavy metals on marine organisms. The results reveal predominantly additive interactions (67%), with a considerable proportion of synergistic interactions (25%) and a few antagonistic interactions (8%). The overall adverse effects of heavy metals on marine organisms were alleviated by OA, leading to a neutral impact of heavy metals in combination with OA. However, different taxonomic groups showed large variabilities in their responses, with microalgae being the most sensitive when exposed to heavy metals and OA, and having the highest proportion of antagonistic interactions. Furthermore, the variations in interaction type frequencies are related to climate regions and heavy metal properties, with antagonistic interactions accounting for the highest proportion in temperate regions (28%) and when exposed to Zn (52%). Our study provides a comprehensive insight into the interactive effects of OA and HM on marine organisms, and highlights the importance of further investigating the responses of different marine taxonomic groups from various geographic locations to the combined stress of OA and HM.
“…Another meta‐analysis showed that hydrogen sulphide (H 2 S) also reduces the survival time of marine organisms under hypoxia by an average of 30% (Vaquer‐Sunyer & Duarte, 2010). Acidification was shown to have additive or synergistic negative effects combined with hypoxia (Gobler & Baumann, 2016; Steckbauer et al, 2020). Since all these factors usually co‐occur during hypoxic events, in situ sponge thresholds to hypoxia could be lower than determined through single stressor laboratory experiments (Diaz & Rosenberg, 1995; Steckbauer et al, 2020).…”
Section: Discussionmentioning
confidence: 99%
“…Acidification was shown to have additive or synergistic negative effects combined with hypoxia (Gobler & Baumann, 2016; Steckbauer et al, 2020). Since all these factors usually co‐occur during hypoxic events, in situ sponge thresholds to hypoxia could be lower than determined through single stressor laboratory experiments (Diaz & Rosenberg, 1995; Steckbauer et al, 2020). Future experiments that evaluate the combined effect of these factors will be crucial to understand the full response of sponges to hypoxia in natural ecosystems.…”
Anthropogenic emissions of carbon dioxide and other greenhouse gasses have increased exponentially since the industrial revolution, causing significant changes in the Earth's climate (IPCC, 2021;Raupach & Canadell, 2010). Climate change has three main effects on the marine environment: warming, acidification and oxygen decline (Bijma et al., 2013). Whilst most ecological and physiological research has targeted the first two stressors, deoxygenation remains comparatively neglected (Limburg et al., 2017). Despite the scant attention, recent research shows that oxygen loss is a major anthropogenic stressor for marine biota that may exceed the severity of the combined effects of ocean warming and acidification (Sampaio et al., 2021).
“…Importantly, recently reported time-series data suggest the occurrence of upwelling-induced continuous hypoxia events (~1–2 weeks) in shallower layers 37 . In our study, however, natural phytoplankton assemblages and the diatom T. weissflogii benefited from reduced O 2 concentrations that were low enough to be detrimental for most marine animals 15 , 38 . Accordingly, even under elevated CO 2 conditions, low O 2 -enhanced photosynthesis can accelerate “re-oxygenation” in illuminated waters by ~193–250% (based on the net photosynthetic values of day 5 in Fig.…”
Many marine organisms are exposed to decreasing O2 levels due to warming-induced expansion of hypoxic zones and ocean deoxygenation (DeO2). Nevertheless, effects of DeO2 on phytoplankton have been neglected due to technical bottlenecks on examining O2 effects on O2-producing organisms. Here we show that lowered O2 levels increased primary productivity of a coastal phytoplankton assemblage, and enhanced photosynthesis and growth in the coastal diatom Thalassiosira weissflogii. Mechanistically, reduced O2 suppressed mitochondrial respiration and photorespiration of T. weissflogii, but increased the efficiency of their CO2 concentrating mechanisms (CCMs), effective quantum yield and improved light use efficiency, which was apparent under both ambient and elevated CO2 concentrations leading to ocean acidification (OA). While the elevated CO2 treatment partially counteracted the effect of low O2 in terms of CCMs activity, reduced levels of O2 still strongly enhanced phytoplankton primary productivity. This implies that decreased availability of O2 with progressive DeO2 could boost re-oxygenation by diatom-dominated phytoplankton communities, especially in hypoxic areas, with potentially profound consequences for marine ecosystem services in coastal and pelagic oceans.
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