Iron-reducing, iron-oxidizing and sulfate-reducing bacteria are involved in the formation and alteration of Fe-bearing minerals through their capacity to transfer electrons beyond the cellular surface
The archived dataset was collected during a laboratory experiment, conducted between April 2021 and April 2022 at McGill University, in which we tested the competitive carbonate dissolution hypothesis
The conceptual diagram describes OPA-MOF synthesis, and bacterial processing and mineralisation of the structurally incorporated oxalate when applied to soil; plant nutrient release is proposed as a r
Fe-Mn aggregates are presented in the paper where flat and round concretions (from several mm to 10-12 cm in diameter) and Fe-Mn crusts on bivalves and polychaete tubes with...
