Would love to hear the thoughts of @_Maq_
Well, coordination chemistry is a higher-grade field and I do not dare to share my amateurish thoughts on this. Next to that, I do not care much for artificial chelating agents because I've learned to live without them.
I can contribute only some side-remarks.
Plants take up Mn(II) ions. In the water column, bivalent manganese gets oxidized to Mn(III) - still mostly soluble - and then to Mn(IV), generally in the form of insoluble MnO2. Just like iron, except that the oxidation runs at slower pace. Therefore, manganese remains accessible for much longer time. In most circumstances.
MnO2 may get reduced in the sediment just like Fe(OH)3 and other iron compounds, and this is the way plants obtain most of both metals in natural conditions.
Iron and manganese are in competing relationship when taken up by plants. That means, excess of one may hinder uptake of the other. I don't know if this is ever relevant in our tanks. In nature, concentrations of
dissolved iron are often by an order or even more
lower than concentration of dissolved manganese (and often other transition metals as well) despite the fact that iron per se is regularly present in vastly larger amounts. In light of that, I assume that manganese deficiency induced by dissolved iron is possible in our tanks, after all, esp. when overdosing chelated iron. Of course, I don't know for sure.
In nature, acquiring iron regularly requires much more sophisticated effort from the plants than acquiring other transition metals. Cohabitation with soil microbes (in the rhizosphere) is often essential. I believe something similar may occur in the roots of floating plants as well. We often see "iron-rich" waters, but that usually means that the iron is not truly dissolved but oxidized and present in nanoparticles. These particles may get trapped on the surface of the roots of floating plants, and reduced/dissolved by the plants themselves (by exuding simple aliphatic acids, par example) or by microbes by so called siderophores.
In general, nature is full of natural chelators. Many common organic compounds can form complexes with metals. Also, particulate organic matter (detritus) acts as an adsorbent of transition metals and their compounds. Such a connection is attractive for microbes which can dissolve and utilize them. In the end, plants benefit from it, too. (That is not to say that we want the share of organic matter in the substrate higher than units of per cent.)
The only ground for using chelated micronutrients as fertilizers is therefore our desire to keep plants in conditions where their natural abilities in acquiring these metals are not sufficient. Very often it's the case of high pH and/or highly alkaline (rich in bicarbonates) environment. Some plants (and farmers' crops!) can't handle it without our artificial help.
I suspect that CO2 injection makes the issue more pronounced, or at least more murky, because CO2 injection enables pH decrease without concomitant alkalinity drop. That seems to be the reason that
Tonina is generally considered demanding species, while it grows like a weed in all my tanks. I don't inject CO2, so I must keep alkalinity truly low to get into acidic range.