by Max Breitbarth
Ocean acidification—the absorption of atmospheric CO2 by the ocean—has increased due to anthropogenic emissions of CO2, resulting in growing concentrations of CO2 in our oceans. Flynn et al. (2015) created models based on projections of increasing ocean acidity to explore the effects of algae blooms at decreasing pH levels and the effects of these blooms on phytoplankton populations that keep the ocean’s acidity within a manageable spectrum. Continue reading
by Weronika Konwent
Ocean acidification is predicted to increase as global warming accelerates, affecting marine habitats and especially coastal areas experiencing episodic upwelling, such as the California Current Large Marine Ecosystem (CCLME). Hofmann et al. (2014) are studying this particular habitat due to its wide variety of conditions and its particular susceptibility to rapid environmental change, To do this, they are using data collected by the Ocean Margin Ecosystems Group for Acidification Studies (OMEGAS) to pair oceanographic and biological data to create a more thorough understanding of genetic variability within key species populations, and how this can affect adaptation to the conditions caused by climate change. Using the biological data to measure responses of sea creatures to oceanographic factors that are affected by climate change, Hofman et al (2014) hope to plot the future survival of CCLME species. Continue reading
by Jennifer Fields
Ocean acidification is known to have an impact on the calcified structure of many marine invertebrates. However, there is recent evidence to suggest that ocean acidification also impacts other key biological processes, such as survival, growth, and behavior. Manríquez et al. (2013) observed the impacts of ocean acidification on shell growth, survival, metabolism, and self-righting ability of a marine gastropod. The authors found there was no significant impact of ocean acidification on net shell growth, survival, or metabolism; however, increased CO2 resulted in faster self-righting times in the marine gastropod. Faster self-righting behavior can reduce the duration of vulnerability to predators and chance of being dislodged by waves of intertidal gastropods. The behavior could be a positive consequence of ocean acidification on marine invertebrates that use a turnover response as a common trait for avoid predation and wave removal. This adaptive trait could induce a co-evolution between predator and prey that would alter predator-prey dynamics within the whole intertidal ecosystem. Continue reading
by Jennifer Fields
Ocean acidification is known to have significant impacts on marine invertebrates in terms of calcification and reproduction; however, the effects of increased CO2 on marine invertebrate behavior are largely unknown. Watson et al. (2014) predicted marine conch snail predator-escape behavior to its predator cone shell would be impaired with near-future CO2 levels. The authors found that the decision-making of the conch snail was in fact impaired by ocean acidification, leaving the snails more vulnerable to predation. The change in behavior was fully restored by treatment with gabazine, suggesting that changes in acid-base regulation caused by increased CO2 in the ocean interfere with the invertebrate’s neurotransmitter receptor function. These alterations in behavior in marine invertebrates could have wide-ranging implications for the whole entire marine ecosystem. Continue reading
by Dawn Barlow
Both ocean temperatures and pH are projected to increase due to climate change in the near future—it is predicted that temperatures will be raised by 2°C and that acidity will increase by ~0.2 pH units by the end of the century. While much investigation has been done on the effects of temperature and acidity on the ability of adult corals to form the structure necessary to maintain the integrity of the reef, Chua et al. (2013) investigated the direct effects of increased temperature and acidity on the early life history stages of corals. They looked at fertilization, development, survivorship, and metamorphosis of coral larvae under control conditions as well as under elevated temperature and acidity, both separately and in combination. When the two factors were combined, the results were inconsistent. Overall, the conclusion drawn from this study was that acidification alone is unlikely to be a direct threat to early life history stages of corals, at least in the near future. Increasing temperature, on the other hand, was found to increase the rate of larval development and thereby affect coral population dynamics by changing patterns of connectivity. Continue reading
by Dawn Barlow
This study by Venn et al. (2013) addresses how ocean acidification reduces the calcification rate of corals by reducing internal pH at the calcifying tissue-skeleton interface. They aim to predict how corals will respond and potentially acclimate to ocean acidification by looking at how acidification impacts the physiological mechanisms that drive calcification itself. Coral skeletons are formed from calcium carbonate crystals (aragonite), produced in the fluid-filled subcalcioblastic medium (SCM), which underlies the calcifying tissue. The calcifying tissue elevates pH the SCM relative to the pH of the exterior seawater, favoring the conversion of bicarbonate to carbonate, and enhancing precipitation at the site of calcification. This ability of corals to regulate internal pH is anticipated to be critical in their resilience to ocean acidification, and overall, findings from this study suggest that reef corals may be able to mitigate the effects of seawater acidification by regulating pH in the SCM. Continue reading
by Dawn Barlow
This study addresses the effects of enhanced CO2 levels in the ocean by looking at how increased acidity might indirectly cause phase shifts in community structure of coral reef and kelp forest ecosystems in temperate and tropical waters. Under elevated acidity and temperature conditions, productivity of certain photosynthetic organisms such as mat-forming algae (low-profile ground-covering macroalgal and turf communities) can increase, making CO2 not only a direct stressor but also an indirect stressor by being a resource for certain competitive organisms, creating enormous potential for shifts in species dominance. Additionally, ocean acidification acts together with other environmental stressors and primary consumers, and these factors also influence community response to acidic conditions. Connell et al. (2013) investigate the prevalence of mat-forming algae in three different scenarios where CO2 levels were either ambient or elevated: in the laboratory, in mesocosms in the field, and at naturally occurring CO2 vents that locally alter the seawater chemistry. They find that in all the scenarios, the algae mats respond positively to the elevated conditions, increasing growth rate and cover to so that the algae became a majority space holder regardless of any herbivory. This is likely because the new environmental conditions favor species with fast growth and colonization rates and short generation times, and these are the species that are capable of completely… Continue reading
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A Blog about the Meera Trilogy
An online journal of International Energy Trends, Green Building, Sustainability and Climate, A&E, Data, Security, CryptoCurrency and Social Media
Dynamic conservation ecology for global change
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Oceans are active, just not always for the right reasons
Sniffing out good climate research.
Sniffing out good climate research.
Sniffing out good climate research.
Sniffing out good climate research.
Sniffing out good climate research.
Sniffing out good climate research.
