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temperatures (e.g., ). It has been highlighted that the disappearance of glaciers among the many water provide sources results in a big reduction in the alpine invertebrate range (α-, β-, and γ-diversity; ) of proglacial river techniques . This is partly due to the reality that the turbid streams present extraordinarily low-diversity and extremely specialized invertebrate communities that additionally include a few endemic taxa. This state of affairs does not appear to use to benthic algae and cyanobacteria because the relatively few species that colonize turbid streams are also found in high-altitude running waters of various origin. However, the genetic traits of those species and the potential presence of cryptic diversity haven’t been verified. Turbid streams fed by giant, energetic glaciers are among the few aquatic habitats that seem to be only scarcely colonized by diatom microalgae, most likely because of mechanical harm (i.e., scouring effect) and the intense reduction in transparency caused by fantastic mineral detritus in suspension. They look like colonized only by very low-diversity and simplified diatom
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