Certainly. From the perspective of the public and the ecosystem use of the water, it could be argued that blue-green algae is part of the ecosystem and therefore part of the natural processes that exist. But I think when we talk about blue-green algae and nuisance algae blooms, we're talking more about the impact they have on the humans who are using the water. From that perspective, even the spectre of a blue-green algae bloom can cause problems with housing values. If there is an actual bloom, whether or not it's toxic, in the interim between it being expressed and it being identified, nobody can touch the water or drink the water, and you can't let your dog go into it, for fear that if it is toxic it's actually going to kill the pet or cause you problems. You can't touch it, because it can be absorbed. You have hepatotoxins—liver toxins—that can actually get into your system and cause significant health problems.
From an economic perspective—in Sturgeon Bay as an example—where blooms recur, you have the spectre of not being able to sell your cottage if that is a progressively worsening condition in that particular geographic location.
From the perspective of inland lakes, we've actually seen increases over the last couple of decades in the incidence of blue-green algae blooms. Part of our actual research was looking at these biochemical triggers that exist and asking why, when blue-green algae are always more efficient at scouring phosphorus out of their environment, they do not always express themselves in massive blooms. The eukaryotic algae—the other algae—dominate until something triggers the blue-green algae, and it takes over.
We were looking at the effect of anoxia in these bottom waters that have detritus, as Dr. Ciborowski was talking about. The normal eukaryotic algae die and go down to the bottom and rot, and they suck all the oxygen out of that water. At that point you go back to prehistoric, pre-oxygen conditions that existed on the earth when the blue-green algaes actually dominated. They are much more efficient at using chemicals other than oxygen in their biochemical processes than the eukaryotic—or oxygen-loving—types of algae are.
As soon as you go anoxic, you can get ferrous iron that can come out of the sediment, and that liberates phosphorus. Phosphorus is used as a kind of fertilizer, if you will, for those organisms, and they can actually migrate up and down in the water column. They can go up to the oxygenated kind of eutrophic areas where they can get to sunlight, and then they can drop themselves down like a diving bell, grab the nutrients they want, and then rise up again through the water levels. So they're actually motile; they can move up and down.
It's those kinds of triggers we've now written a paper about with York University's Dr. Lewis Molot, which has been accepted for publication in Freshwater Biology. It's an interesting, kind of esoteric, science that we wanted to find out about.
Once they dominate, then certainly with the amount of phosphorus that's available to them in the Great Lakes system—phosphorus is kind of the limiting nutrient—they can then manifest themselves in these huge surface scums that we all associate with the bloom. But the bloom was already happening in the water column. There were already lots of these organisms in existence throughout that water column.