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1. Ocean acidification effects on in situ coral reef metabolism

   https://doi.org/10.1038/s41598-019-48407-7  

   Doo, Steve S.; Edmunds, Peter J.; Carpenter, Robert C. (August 2019, Scientific Reports)

   Abstract The Anthropocene climate has largely been defined by a rapid increase in atmospheric CO_2,causing global climate change (warming) and ocean acidification (OA, a reduction in oceanic pH). OA is of particular concern for coral reefs, as the associated reduction in carbonate ion availability impairs biogenic calcification and promotes dissolution of carbonate substrata. While these trends ultimately affect ecosystem calcification, scaling experimental analyses of the response of organisms to OA to consider the response of ecosystems to OA has proved difficult. The benchmark of ecosystem-level experiments to study the effects of OA is provided through Free Ocean CO₂Enrichment (FOCE), which we use in the present analyses for a 21-d experiment on the back reef of Mo’orea, French Polynesia. Two natural coral reef communities were incubatedin situ, with one exposed to ambient pCO₂(393 µatm), and one to high pCO₂(949 µatm). Our results show a decrease in 24-h net community calcification (NCC) under high pCO₂, and a reduction in nighttime NCC that attenuated and eventually reversed over 21-d. This effect was not observed in daytime NCC, and it occurred without any effect of high pCO₂on net community production (NCP). These results contribute to previous studies on ecosystem-level responses of coral reefs to the OA conditions projected for the end of the century, and they highlight potential attenuation of high pCO₂effects on nighttime net community calcification. 

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2. Contrasting responses of photosynthesis and photochemical efficiency to ocean acidification under different light environments in a calcifying alga

   https://doi.org/10.1038/s41598-019-40620-8  

   Briggs, Amy A.; Carpenter, Robert C. (March 2019, Scientific Reports)

   Abstract Ocean acidification (OA) is predicted to enhance photosynthesis in many marine taxa. However, photophysiology has multiple components that OA may affect differently, especially under different light environments, with potentially contrasting consequences for photosynthetic performance. Furthermore, because photosynthesis affects energetic budgets and internal acid-base dynamics, changes in it due to OA or light could mediate the sensitivity of other biological processes to OA (e.g. respiration and calcification). To better understand these effects, we conducted experiments onPorolithon onkodes, a common crustose coralline alga in Pacific coral reefs, crossing pCO₂and light treatments. Results indicate OA inhibited some aspects of photophysiology (maximum photochemical efficiency), facilitated others (α, the responsiveness of photosynthesis to sub-saturating light), and had no effect on others (maximum gross photosynthesis), with the first two effects depending on treatment light level. Light also exacerbated the increase in dark-adapted respiration under OA, but did not alter the decline in calcification. Light-adapted respiration did not respond to OA, potentially due to indirect effects of photosynthesis. Combined, results indicate OA will interact with light to alter energetic budgets and potentially resource allocation among photosynthetic processes inP. onkodes, likely shifting its light tolerance, and constraining it to a narrower range of light environments. 

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3. Physiological acclimatization in Hawaiian corals following a 22-month shift in baseline seawater temperature and pH

   https://doi.org/10.1038/s41598-022-06896-z  

   McLachlan, Rowan H.; Price, James T.; Muñoz-Garcia, Agustí; Weisleder, Noah L.; Levas, Stephen J.; Jury, Christopher P.; Toonen, Robert J.; Grottoli, Andréa G. (March 2022, Scientific Reports)

   Abstract Climate change poses a major threat to coral reefs. We conducted an outdoor 22-month experiment to investigate if coral could not just survive, but also physiologically cope, with chronic ocean warming and acidification conditions expected later this century under the Paris Climate Agreement. We recorded survivorship and measured eleven phenotypic traits to evaluate the holobiont responses of Hawaiian coral: color, Symbiodiniaceae density, calcification, photosynthesis, respiration, total organic carbon flux, carbon budget, biomass, lipids, protein, and maximumArtemiacapture rate. Survivorship was lowest inMontipora capitataand only some survivors were able to meet metabolic demand and physiologically cope with future ocean conditions. MostM. capitatasurvivors bleached through loss of chlorophyll pigments and simultaneously experienced increased respiration rates and negative carbon budgets due to a 236% increase in total organic carbon losses under combined future ocean conditions.Porites compressaandPorites lobatahad the highest survivorship and coped well under future ocean conditions with positive calcification and increased biomass, maintenance of lipids, and the capacity to exceed their metabolic demand through photosynthesis and heterotrophy. Thus, our findings show that significant biological diversity within resilient corals likePorites, and some genotypes of sensitive species, will persist this century provided atmospheric carbon dioxide levels are controlled. SincePoritescorals are ubiquitous throughout the world’s oceans and often major reef builders, the persistence of this resilient genus provides hope for future reef ecosystem function globally. 

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4. Long-term coral microbial community acclimatization is associated with coral survival in a changing climate

   https://doi.org/10.1371/journal.pone.0291503  

   Price, James T; McLachlan, Rowan H; Jury, Christopher P; Toonen, Robert J; Wilkins, Michael J; Grottoli, Andréa G (September 2023, PLOS ONE)

   Keshavmurthy, Shashank (Ed.)

   The plasticity of some coral-associated microbial communities under stressors like warming and ocean acidification suggests the microbiome has a role in the acclimatization of corals to future ocean conditions. Here, we evaluated the acclimatization potential of coral-associated microbial communities of four Hawaiian coral species (Porites compressa,Porites lobata,Montipora capitata, andPocillopora acuta) over 22-month mesocosm experiment. The corals were exposed to one of four treatments: control, ocean acidification, ocean warming, or combined future ocean conditions. Over the 22-month study, 33–67% of corals died or experienced a loss of most live tissue coverage in the ocean warming and future ocean treatments while only 0–10% died in the ocean acidification and control. Among the survivors, coral-associated microbial communities responded to the chronic future ocean treatment in one of two ways: (1) microbial communities differed between the control and future ocean treatment, suggesting the potential capacity for acclimatization, or (2) microbial communities did not significantly differ between the control and future ocean treatment. The first strategy was observed in bothPoritesspecies and was associated with higher survivorship compared toM.capitataandP.acutawhich exhibited the second strategy. Interestingly, the microbial community responses to chronic stressors were independent of coral physiology. These findings indicate acclimatization of microbial communities may confer resilience in some species of corals to chronic warming associated with climate change. However,M.capitatagenets that survived the future ocean treatment hosted significantly different microbial communities from those that died, suggesting the microbial communities of the survivors conferred some resilience. Thus, even among coral species with inflexible microbial communities, some individuals may already be tolerant to future ocean conditions. These findings suggest that coral-associated microbial communities could play an important role in the persistence of some corals and underlie climate change-driven shifts in coral community composition. 

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5. Examining the impacts of elevated, variable pCO2 on larval Pacific razor clams (Siliqua patula) in Alaska

   https://doi.org/10.3389/fmars.2024.1253702  

   Alcantar, Marina W; Hetrick, Jeff; Ramsay, Jacqueline; Kelley, Amanda L (January 2024, Frontiers in Marine Science)

   An increase in anthropogenic carbon dioxide is driving oceanic chemical shifts resulting in a long-term global decrease in ocean pH, colloquially termed ocean acidification (OA). Previous studies have demonstrated that OA can have negative physiological consequences for calcifying organisms, especially during early life-history stages. However, much of the previous research has focused on static exposure to future OA conditions, rather than variable exposure to elevatedpCO₂, which is more ecologically relevant for nearshore species. This study examines the effects of OA on embryonic and larval Pacific razor clams (Siliqua patula), a bivalve that produces a concretion during early shell development. Larvae were spawned and cultured over 28 days under threepCO₂treatments: a static highpCO₂of 867 μatm, a variable, dielpCO₂of 357 to 867 μatm, and an ambientpCO₂of 357 μatm. Our results indicate that the calcium carbonate polymorphism of the concretion phase ofS. patulawas amorphous calcium carbonate which transitioned to vaterite during the advanced D-veliger stage, with a final polymorphic shift to aragonite in adults, suggesting an increased vulnerability to dissolution under OA. However, exposure to elevatedpCO₂appeared to accelerate the transition of larvalS. patulafrom the concretion stage of shell development to complete calcification. There was no significant impact of OA exposure to elevated or variablepCO₂conditions onS. patulagrowth or HSP70 and calmodulin gene expression. This is the first experimental study examining the response of a concretion producing bivalve to future predicted OA conditions and has important implications for experimentation on larval mollusks and bivalve management. 

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