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Impacts of coinciding ocean acidification and warming on the fatty acid profile of the pteropod Limacina helicina within the Northeast Pacific coastal region

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Under global climate change, the co-occurrence of ocean acidification (OA) and warming presents significant threats to marine ecosystems, particularly in the Strait of Georgia, where aragonite undersaturation is prevalent year-round. This study investigates the impacts of these conditions on the fatty acid profile and survival of the pteropod Limacina helicina, a crucial component of local zooplankton communities. Findings reveal that short-term OA can alter fatty acid composition, potentially affecting nutritional quality and energy transfer within the ecosystem.

The recent study on the impacts of ocean acidification (OA) and warming on the fatty acid profile of the pteropod Limacina helicina in the Strait of Georgia offers critical insights into how climate change is reshaping marine ecosystems. This research is particularly timely, as it highlights the dual threat posed by these stressors and their potential cascading effects on marine food webs. As the study indicates, the conditions of aragonite undersaturation, coupled with rising seawater temperatures and increasing instances of marine heatwaves, underscore the urgency of understanding the implications for species that play foundational roles in oceanic ecosystems. The findings resonate with other studies, such as the Long-term changes of summer larval fish community in relation to environmental trends in the NW Mediterranean and the Short-term and long-term prediction of South China Sea SST based on multiple meteorological factors and machine learning, which emphasize the interconnectedness of environmental changes and marine life.

Pteropods, such as Limacina helicina, are integral to the marine food web, serving as a key food source for various fish species. The study’s results reveal that OA significantly alters the fatty acid composition of these organisms within just 48 hours, raising concerns about their nutritional quality and, consequently, the health of the species that rely on them for sustenance. The interactive effects of OA and warming further complicate this picture, suggesting that as ocean conditions continue to evolve, the nutritional landscape of marine ecosystems may undergo significant transformation. This is especially relevant in the context of a warming planet, where understanding the specific biochemical changes in marine organisms can provide insights into broader ecological shifts.

Moreover, the investigation into historical plankton samples over the years provides a crucial perspective on how marine species adapt—or fail to adapt—to changing environmental conditions. The lack of significant differences in fatty acid fractions among years, except for a notable trend in myristic acid proportions, indicates that while some aspects of marine life may remain stable, others may be more susceptible to shifts in ocean chemistry and temperature. This underscores the importance of longitudinal studies to track these changes over time, ensuring that we are not only reacting to current conditions but also anticipating future shifts in marine biodiversity. The findings align with the broader themes explored in the Response of offshore wind turbine monopile-liquefiable seabed-seawater coupled system to vertical and horizontal seismic excitations, which call for an integrated approach to understanding the multi-faceted challenges facing our oceans amid climate change.

As we move forward, it is imperative that researchers, policymakers, and ocean stewards take these findings into account when developing strategies for marine conservation and management. The importance of empirical, validated research cannot be overstated, as it lays the groundwork for informed decision-making that prioritizes the health of marine ecosystems. The interaction between OA, warming, and the nutritional profiles of key marine organisms like Limacina helicina serves as a clarion call for action. The question that remains is: how will we adapt our conservation strategies to address these emerging challenges, and what innovative solutions can we develop to ensure the resilience of our oceans in the face of ongoing climate change? The answers will not only shape the future of marine ecosystems but also impact global food security and biodiversity as a whole.

Impacts of coinciding ocean acidification and warming on the fatty acid profile of the pteropod Limacina helicina within the Northeast Pacific coastal region
Under global climate change, co-occurrence of ocean acidification (OA) and warming poses a substantial threat to marine ecosystems. The present study focused on the Strait of Georgia within the Northeast Pacific region, where conditions of aragonite undersaturation exist year-round across the majority of the water column, with further intensification expected under OA. These conditions coincide with persistent rises in mean seasonal seawater temperatures and increased prevalence of acute stressor events, such as marine heatwaves and low-pH upwelling events. Limacina helicina, a pteropod species well-represented within the region’s zooplankton communities, is susceptible to OA and warming, with documented impacts including altered shell development, growth, and survival. To date, however, there has been minimal investigation into the effects of OA and warming on the species’ fatty acid profile under regionally-relevant conditions, thereby contributing to a lack of understanding of how impacts at lower trophic levels may relay across ecosystems. To address this knowledge gap, we examined the survival and fatty acid profile of L. helicina under future conditions via a laboratory experiment during which pteropods were exposed to singular and coinciding warming (mean summer seawater temperature + 4 °C) and OA (Ωarag < 1) conditions, with fatty acid analyses carried out via gas chromatography at 48-h and 5-d timepoints. OA conditions significantly altered fatty acid proportions at 48 h, and there was an additional interactive effect of OA and warming. Temperature significantly affected survival at 5 d, although experimental starvation conditions likely confounded this result. Additionally, fatty acid analyses of L. helicina picked from historical plankton samples collected in the region over 2014–2023 were carried out to examine time-series changes in fatty acid profiles in relation to temperature records. Results indicated no significant differences in fatty acid fractions among years, though there was suggestion of a changing proportion of myristic acid over a number of year groups. Overall, findings suggest that short-term OA conditions may result in altered fatty acid composition in pteropods, potentially leading to shifts in nutritional quality and associated impacts on trophic energy transfer.

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#interactive ocean maps#marine science#marine biodiversity#climate change impact#marine life databases#ocean data#ocean circulation#climate monitoring#ocean acidification#warming#Limacina helicina#fatty acid profile#pteropod#Northeast Pacific#Strait of Georgia#aragonite undersaturation#marine ecosystems#temperature#trophic energy transfer#zooplankton communities