Abstract:Abstract. Iron and manganese are poorly soluble elements in oxic and alkaline solutions, whereas they are much more soluble under anoxic conditions. As a result, the formation of authigenic mineral phases rich in Fe and/or Mn has traditionally been viewed as diagnostic of global or local anoxic conditions. Here we reveal that some specific picocyanobacteria can biomineralize abundant, authigenic Fe(III)- and Mn(IV)-rich amorphous silicates under oxic conditions in an alkaline lake in Mexico. The resulting biom… Show more
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