Stability of dissolved and soluble Fe(II) in shelf sediment pore waters and release to an oxic water column
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Shelf sediments underlying temperate and oxic waters of the Celtic Sea (NW European Shelf) were found to have shallow oxygen penetrations depths from late spring to late summer (2.2-5.8 mm below seafloor) with the shallowest during/after the spring-bloom (mid-... ...
