I have to say I have not noted any difference if I stir the precipitates up or if I add them when emptying the container.
At least for iron the usual view in my opinion is not quite complete or correct at all. Iron exists in alkalinic and oxygenic seawater as iron(III) and also dissolved iron is mostly iron(III).
How can that be? In such environments iron is dissolved as organic complexes. Organic ligands form complexes preferably with iron(III). The iron(III) ion is smaller and higher charged (one electron less and one positive charge more) and in this way it forms much stronger complexes with organic ligands. For takeup by organisms, mainly bacteria that also excreted the organic ligands, iron(III) is actively reduced to iron(II), the complex in this way is weakened, the iron(II) is released from the complex as ion and can be taken up.
All other things you may frequently read about iron(II) and solubility in saltwater is at least grossly incomplete. In the oceans iron(II) as permanent form of iron just doesn't exist in oxgenic water.