Toxic Algal Blooms: Expert Adaptors to Climate Change

Most people think of algae as the bothersome green stuff that grows on the tops of ponds and needs to be removed from the inside of fish tanks, but algae also provides clues about the environment. The response of Harmful Algal Blooms (HABs) to climate change, for example, provides evidence that some algae are extremely efficient environmental adaptors.

HABs are formed when colonies of algae living in fresh or saltwater grow out of control and begin producing toxic effects that can threaten the health and lives of animals and humans. According to NOAA, they have occurred in every coastal state in the United States and are increasing in frequency due to rising temperatures associated with climate change. As a result, HAB responses to climate change, including changes in pH and CO2, have been increasingly studied.

These responses include the expansion of the blooms into larger areas and an increased release of toxic poisons with warming temperatures. In a recently published paper, Mardones et al examine a special type of algal bloom found to be an expert adaptor to climate change. This strain of algal blooms called Alexandrium catenella occurs in highly variable fjord systems in southern Chile. 

These Chilean fjords have had to respond to fluctuations in CO2 and pH. They experience huge freshwater inputs from Patagonian ice fields and heavy precipitation events. When dissolved in water, CO2 forms carbonic acid, which has a low pH. Therefore, levels of CO2 and pH are inversely correlated. As CO2 increases due to climate change, algal blooms in the fjords produce more Paralytic Shellfish Toxin (PST). This toxin could have long-term effects on the fish population and therefore the entire food web and ecosystem in the fjord.

In an article by Pedro Costa, he describes how these neurotoxins can have a lasting impact: poisoned fish can be consumed by seals and humans, causing health issues or even death. As we expect CO2 to continue to rise, it is very likely harmful algal blooms like the ones in Chile will produce more PST, leading to more fish kills, disturbed ecosystems in the fjords, and possible human health issues.

A view of a Chilean fjord (Source: Wikimedia Commons)

During their research, Mardones et al explored six levels of CO2/pH and two light conditions to examine how the algal blooms react. The scientists identified key differences in the waters in the fjord closest to the melting ice fields and the waters in the fjord further offshore. The near-shore water in the fjord experiences the largest impact of the freshwater inputs from the ice fields. The freshwater means that the upper layers of the water are much less salty compared to lower layers. This creates an intense halocline (stronger layers of differences in salinity) in the water column.  Strong winds in the region mix the layers, which produce highly fluctuating differences in carbonate chemistry. As Patagonian glaciers continue to melt, even more freshwater will be introduced into the fjords, which will continue to change the conditions of the water.  

On the other hand, the more stable offshore waters have CO2 equilibrium with the atmosphere. The main environmental driver offshore is human-caused ocean acidification. As CO2 emissions increase in the atmosphere, it dissolves in oceans and lowers the pH of the water. For most species, this causes huge problems, but certain types of algal blooms are able to adapt to these conditions.

Previous studies done by Tatter et al. show that a type of the same algal bloom from Southern California have previously changed their physiological responses due to changing pCO2/pH. Under higher CO2 conditions, production of Paralytic Shellfish Toxin increased. In 2015, there was an unprecedentedly large algal bloom that stretched from Central California to the Alaskan peninsula.

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An aerial shot of a toxic algal bloom (Source: Wikimedia Commons)

Mardones et al. found similar results in the Chilean algal blooms by examining the strains of the bloom under lab conditions. The blooms had been previously harvested years before and kept in culture. They analyzed these HAB responses to changes in pH and CO2. While they had optimal physiological performance at near-equilibrium levels of pH/CO2, the algal blooms showed an ability to adapt to changing conditions. They found that the blooms are in fact able to adapt their cell size based on the pH/ CO2 levels. In conditions with high pH/low CO2, the blooms adapted to a smaller cell size. In conditions with low pH/high CO2, their cell size increased, which means they are able to change their shape to not only survive changing conditions, but to thrive in them. In low CO2, high pH could increase chain formation (they could increase their swim speed to maintain their location without being moved in the current).

These factors, in addition to others, contribute to the resiliency of the harmful algal blooms in changing conditions, demonstrating they are expert adaptors to climate change.

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Glaciers + Algal Blooms = Good?

James Bay, the southern end of Hudson Bay in Canada, is shown here in an image taken by the Suomi NPP satellite's VIIRS instrument around 1825Z on September 17, 2013. Sediment flow from rivers and algal blooms can be seen well in this clear view. (NOAA/NASA)
James Bay, the southern end of Hudson Bay in Canada, is shown here in an image taken by the Suomi NPP satellite’s VIIRS instrument around 1825Z on September 17, 2013. Sediment flow from rivers and algal blooms can be seen well in this clear view. (NOAA/NASA)

The pros and cons of algal blooms, high concentrations of phytoplankton in the oceans, are a subject of much debate. But several studies in recent months have examined links between changing polar environments, exponential growth of algal blooms, and potential for carbon reduction.

One study, appearing in the journal Nature Communications in May 2014, suggests that ocean iron from glacial melt could have positive effects for polar regions in the face of global warming because of the nutrient quality for algae. “The theory goes that the more iron you add, the more productive these plankton are,” John Hawking, a doctoral student at the University of Bristol and lead author of the study, told Scientific American in May.

The University of Bristol study examined the amount of a specific type of iron (bioavailable ferrihydrite) released in glacial melt water from the Leverett Glacier in Greenland. The levels of this form of iron found in the glacier allowed Hawking to estimate that an iron flux of up to 400,000 to 2.5 million metric tons could be flowing from Greenland annually. These releases have the potential to be transported up to 900 km from the site of origin and to greatly affect the global iron cycle.

The ICESCAPE mission, or "Impacts of Climate on Ecosystems and Chemistry of the Arctic Pacific Environment," is NASA's two-year shipborne investigation to study how changing conditions in the Arctic affect the ocean's chemistry and ecosystems. The bulk of the research takes place in the Beaufort and Chukchi seas in summer 2010 and 2011. (Kathryn Hansen/NASA)
The ICESCAPE mission, or “Impacts of Climate on Ecosystems and Chemistry of the Arctic Pacific Environment,” is NASA’s two-year shipborne investigation to study how changing conditions in the Arctic affect the ocean’s chemistry and ecosystems. The bulk of the research takes place in the Beaufort and Chukchi seas in summer 2010 and 2011. (Kathryn Hansen/NASA)

New findings coming out of a NASA-sponsored expedition off the coasts of Alaska discovered a massive algal bloom in this polar region as well. Contrary to Hawking’s study, the ICESCAPE expedition conducted by NASA in the Beaufort and Chukchi seas determined the growth in algae was a product of younger and thinning ice. Because of the changes in ice density due to Alaska’s warming climate, more sunlight is able to reach the water underneath the ice packs, according to researchers on the expedition. Therefore, the environment is more favorable for the phytoplankton.

Historically, expanding algae populations in other parts of the globe have generated many negative side effects. For example, the decay of algae during a bloom can suck nutrients and oxygen out of the water creating a dead zone. These low-oxygen areas reduce the productivity of wildlife, decrease their productive capacity, and can even kill them. Further, humans experience the effects of algal blooms through the ingestion of toxic substances via shellfish.

Yet, in the wake of information about the connection of algae growth and a warming world, studies are taking more effort to explore the positive consequences of algal blooms. A study conducted by the USGS Woods Hole Oceanographic Institution proposes that increases of phytoplankton in polar regions will serve as a new food source for wildlife and will offer increased carbon capture in these areas. The greater numbers of phytoplankton, the greater volume of carbon the population will consume during photosynthesis. Some scientists believe an increasing number of algal blooms will deplete carbon stores in the ocean, resulting in greater absorption of atmospheric carbon by the sea. Additionally, when the phytoplankton die, they often retain much of the stored carbon and carry it down to the ocean floor.

Scientists are not certain how the interplay between phytoplankton and ocean carbon will develop because ocean uptake of carbon (especially, in the deep water) can occur on a long timescale, and because it is not yet clear how much carbon is retained versus released during algae death.

With all of this in mind, scientists are hopeful that the correlation of glacial melt, encouraging environments, and algal growth will have a net-positive effect. Further study of this natural bioengineering project will definitely aide scientists in understanding climate change trends.

 

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Glacier stories you may have missed – 8/25/14

https://www.youtube.com/watch?v=qzCsQsmipq0
(John “STI” Kristensen/Royal Danish Air Force)

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Glacial Melt Pours Iron into Ocean, Seeding Algal Blooms

Scientists report in a new study this week that glacial melt may be funneling significant amounts of reactive iron into the ocean, where it may counter some of the negative effects of climate change by boosting algal blooms that capture carbon.

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