We often get a white milky layer in our local lake once a strong thermocline has been established. I've always figured it's calcium sulphate. Calcium sulphate has the somewhat unusual property of being more soluble in cold water than it is in warm ,so will precipitate out when it meets warm water.
I also wonder if there is a bacterial element to this. Hydrogen sulfide formed from rotting vegetation in a low oxygen environment is acidic and will dissolve limestone to form calcium sulfide. When this calcium sulfide meets shallow,better oxygenated water the sulfide will be oxidized to sulfate. (possibly aided by bacteria?? )
Whatever the exact mechanism, it's pretty neat to see a thin white wisp right at the themocline.


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