According to Redfield (via a summary in wikipedia)
Understanding that the problem is akin to the classical
the chicken or the egg causality dilemma, Redfield proposed two mutually non-exclusive mechanisms:
I) The N

in plankton tends to the N

composition of seawater. Specifically, phytoplankton species with different N and P requirements compete and, as the result, balance each other so that “the ratio of the elements in the plankton as a whole might come to reflect the ratio of the nutrient substances in sea water rather closely” (Redfield 1934).
II) The N

in seawater “must tend to approach that characteristic of protoplasm in general” (Redfield 1934). Furthermore, Redfield proposed thermostat like scenario in which the activities of nitrogen fixers and denitrifies keep the nitrate to phosphate ratio in the seawater near the requirements in the protoplasm. Considering that at the time little was known about the composition of “protoplasm,” Redfield did not attempt to explain why its N

ratio should be approximately 16:1.
In 1958, almost a quarter century after first discovering the ratios, Redfield leaned toward the latter mechanism proposing in his seminal manuscript the idea of "the biological control of chemical factors" in the ocean (Redfield, 1958). Redfield proposed that the ratio of Nitrogen to Phosphorus in plankton resulted in the global ocean having a remarkably similar ratio of dissolved nitrate to phosphate (16:1). He considered how the cycles of not just N and P but also C and O could interact to result in this match.
Lets start over: I'll 'tear it apart' (and agree with some of it) piece by piece at your request (in your original post

). Because the studies you quoted DID focus on the levels of nitrate and phosphate in the environment - and the recommendations in your original post DO reference levels of nitrate/PO4 (i.e. adding them or reducing them) so perhaps it lead me off track a bit.
This implied what you were posting about was personal experience/anecdotal. You may have looked at all the science - I just was reading what you posted and perhaps misinterpreted (sorry)
There is no reference for this. How is 'non-harmful bacteria' defined? What are the 'non-harmful' bacteria that are increased with carbon? Most bacteria increase with carbon dosing. Im not sure that you can assume that because 'non-harmful' bacteria have an N

ratio of 50:1 implies that one needs a phosphate reducer. Thats not to say that people that dose carbon don't need a phosphate reducer - just that it has no relation to the N

ratio or the bacteria. For example I would call nitrosomonas a 'non-harmful' bacteria - it will certainly rise with nitrate contentration.... Bacteria are not phytoplankton - so you cannot really compare Redfields conclusions to bacteria in any case. I.e. the ratio of 50:1 in bacteria may have a completely different reason than in a photosynthetic organism (cyano and Dino)
As in the article I just posted - different cyanobacteria - there are LOTS of them - grow at different nitrate levels (high and low) - so how does adding nitrate help? How does the ratio imply that adding PO4 will help? (in this instance the ratio you quote is a factor of 500% different). I do not think you can use the ratio of the C:N

in the organisms to suggest that this gives cyanobacteria an ability to thrive in a low nitrate environment.
This is not true - not all dinos have a high need for nitrates (depending on what 'high' means - you dont explain it). The Purpose of the Redfield ratio was to show the consistency of phytoplankton with regards to their C:N

ratios in all areas of the ocean. There is no rationale given in your post as to why the 'ratio of C:N

'being all over the place' has anything to do with dosing phosphates or silicates as your post suggests.
Zooxanthellae are dinoflagellates. Many people say that a way to rid an aquarium of dinoflagellates is to allow nutrient levels to rise (including nitrates) ... (I dont necessarily believe this - but - its all over this forum). Adding PO4 may help - but I dont see the relation to the ratio
I assume you mean algae in a refugium - rather than encouraging algae in the tank. There are many articles stating that iron benefits both cyanobacteria and dinoflagellates. But what you say may make sense.
So - my conclusion based on your post - 1. The N

ratio is not measurable in the aquarium (nor is it possible to measure the N

of the bacteria in the aquarium. 2. A refugium with algae and iron supplementation will outcompete cyanobacteria and dinoflagellates. I support the idea that fiddling with the chemistry of the water will likely improve/aggravate the presence of certain bacteria.
IMHO - and its only my opinion - the rest of the recommendations are taking an extremely complex topic and trying to generalize it to your personal experience. There is no reason to assume that the ratios you are quoting are helpful (i.e. the ratio in bacteria may have quite a different meaning is different than the ratio in cyanobacteria and dinoflagellates. I have read a bunch of the science and depending on which part of the ocean, which species of cyano or Dino you are studying, the temperature of the water, other local influences of the study area (Fe concentration), you can find justification for almost any position on the N

ratio of the phytoplankton present.