Alpine glacier-fed turbid lakes are discontinuous cold polymictic rather than dimictic

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Glacier-fed streams are the cold, ultra-oligotrophic, and unstable streams that are fed by glacial meltwater. Despite these extreme conditions, they harbour a diverse and abundant microbial diversity that develops into biofilms, covering the boulders and s ...

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Alpine glacier-fed turbid lakes are discontinuous cold polymictic rather than dimictic

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