Hi all,
I knew someone would bring up the stated pH range for L204, but it is a total red herring (all right it isn't, it is a black & white stripy Panaque), it is back to the buffering and pH equation.
If you have water with very little carbonate buffering the pH is a total movable feast, it will go up and down as the balance of H+ and OH- ions (or equivalents) change.
In this case it could be a simple as photosynthesising aquatic plants (including floating ones and algae). During the night pH will drop as the CO2 content of the water rises (the water has very little buffering so even the addition of a weak acid (CO2 + H2O <> H2CO3) will cause a rapid drop in pH) and during the day the pH will climb as the water becomes saturated with oxygen (O2). In this case the pH may swing from pH5 early in the morning to pH9 in the afternoon.
This is why pH8 in Lake Malawi has no real correlation with pH8 in the Upper Amazon.
L204 is a fish that comes from a river with low carbonate hardness, pH will swing up and down, we know there isn't much buffering in the water, we have the conductivity value that Lornek mentions.
Lake Malawi is almost infinitely buffered and the pH will hardly change at all, you would have gassed all the fish long before you could add enough CO2 to lower the pH by 0.1 of a unit.
I hope that makes sense, it really is quite important to remember that pH is a largely meaningless measurement on its own.
cheers Darrel