There is a war going on (not only in this thread but in our aquaria

) As in all wars – it’s about resources. The one that will win is the one that can get needed resources in the best way. Different organisms have developed different strategies for surviving and domination. We often concentrate our discussions around two of these resources – inorganic phosphorus and nitrogen because they are the most limited resources in pristine waters and our primary producer need them in large quantities. The reasons why you measure so low concentrations of inorganic P and N near and in a coral reef is because if there suddenly should be a free resource of inorganic P or N - it should be as short-lived as vodka at a Swedish crayfish party. The water concentrations of these nutrient are low but the flux through and in a coral reef of these compounds are enormous.
In this war – different organisms have different strategies and it’s not a surprise that the oldest has the most advanced techniques to sustain a guarantee for these nutrients for themselves. Cyanobacteria is one of the oldest (if not the oldest) now living organism in the world – dinos are rather old organism too. Cyanobacteria is probably the one that start the process that lead to an oxygen concentration of 20 % in the air. It means that Cyanobacteria exist before oxygen become a necessary part of what we call life!
Some cyanobacteria have developed a special cell in the body that are able to process N2 gas too form nitrogen species that their body can take up. ( Let me say directly – that this is not the case with the species that form mats – I think they solve these problems in another way.) To be able to convert N2 to useful species – an anaerobic environment must be created. These Cyanobacteria create that in this special cell – and the rest of the cells can use these N species (mostly NH3/NH4) This means that a Cyanobacteria can survive and thrive in an environment that lack dissolved inorganic N species like Nh3/NH4, NO2, NO3 and NOx.
The species that we have problems with – the mat building benthic species of cyanobacteria – how do they solve the problem. I think they do the same – they create an anaerobic environment and "farm" bacteria that fix nitrogen – in the space between the mat and the substrate. These cyanobacteria always exist in our aquaria, they are small narrow organisms like small sticks but sometimes they come together and form these awful mats. And below the mats – the magic happens. IMO if there is a limitation of inorganic N species dissolved in the water – the sticky benthic cyanobacteria can do its trick and concur for space that they during normal conditions can’t fight for. But I think it’s more that happens below the mats. Many metals (most known calcium, iron and aluminium) can bind phosphorus in metal/phosphate complexes and these complexes will fall at the substrate. These processes are the ones that GFO use as an example. Is known since long time ago that these bindings can be broken during anaerobic conditions and hence free bound phosphorous from the substrate. Lately – it has been shown that this process needs another condition also – the forming of hydrogen sulfide. If this happen below the mats – the dam cyanobacteria will have free phosphorus for themselves also and I rather sure that – if there is a lack of iron in the water column – they will have a free supply of iron and other trace metals also – all below the mats.
Ten years ago – a very important study was done in Sweden according cyanobacteria blooms in freshwater lakes. The study did not cover the benthic forms but the pelagic forms. It shows that in some lakes – the pelagic forms (with capability to produce useful inorganic nitrogen in their own body) was able to use phosphorous sources that was not dissolved in the water column. During night time they was migrating down to the bottom (if the bottom layer was anaerobic) and picked up phosphorous that they use in the sunlight during the day. But only in some lakes with anaerobic bottom layers – in some lakes – despite the fact that’s the bottom water was anaerobic – no cyanobacteria blooms were observed. The thing this lakes with no cyanobacteria blooms but anaerobic bottom conditions had in common was a NO3 concentration over 2 ppm. Below that – cyanobacteria bloom.
It’s a well-known fact that NO3 in the water column normally block the production of hydrogen sulfide. Hence – I have listed two important reasons why you should have some NO2 in your water – your normal algae growth need an inorganic nitrogen species in the water and you should not create a condition that can create hydrogen sulphide in the upper bottom layer of your substrate. And – all of you that have your GFO in a sock without a steady flow of oxygen rich water through it – be aware of the risk that your bound phosphorus can be realised again.
To address this balance question of the macro nutrients we discuss – IMO – you need some concentrations of these nutrients in the water and probably there is threshold concentrations according to different organisms – and IMO these threshold concentrations for cyanobacteria is zero – they can fix these nutrients I other ways. According Dinos – I do not know so much but they are mobile, and they disappear during nighttime. Where – my guess – down in the substrate – what are they doing there? Maybe to collecting phosphorus and nitrogen to use that during daytime?
What’s my general way of defeating Cyanobacteria if they occur – be sure that I have dissolved inorganic N and P species in my water column (NO3 > 2 ppm normally) and most important – disturb the mats as much as possible – the mats is the secret of the benthic cyanobacteria – IMO
I´m sorry for a long post and I have been thinking if I should put on my boots and walk into this discussion or not. All of this is IMO and it’s based on some studies I have seen and my own experiences and thoughts – true? I do not know but certainly a new perspective on the matter
Sincerely Lasse