Hi Folks,

This idea is just an early thought and may not be practical....But, here it 
goes.

If you take a look at this paper 
http://www.mumm-research.de/download_pdf/treude_et_al_aom_hr.pdf Pg 2

"The AOM consortium predominant at HR consists
of sulfate-reducing bacteria of the branch Desulfosarcina/Desulfococcus and 
archaea of the ANME-2
group (Boetius et al. 2000b). The archaea are surrounded by the 
sulfate-reducing bacteria and both
grow together in dense aggregates that comprise up
to 90% of the microbial biomass in hydrate-bearing
sediments. The current hypothesis on the functioning
of AOM assumes that archaea oxidize methane in a
process that is reverse to methanogenesis (Valentine
& Reeburgh 2000, and references therein). The role
of the sulfate-reducing bacteria in AOM-consortia is
the oxidation of a *so far unknown intermediate *by
simultaneous reduction of sulfate, thus maintaining
thermodynamic conditions allowing methane oxidation to proceed 
exergonically."

Now take a look at this: 
http://www.physorg.com/news/2011-05-scientists-links-biology-cloud-formation.html

The "so far unknown intermediate" seems to have been found by the second 
group. Thus, I believe sulfite enhancement might be used to both feed the 
sulfate-reducing bacteria in the vent areas to enhance the biomass around 
vents and thus methane oxidation. There may also be a synergistic link 
between increasing this process and.... believe it on not.....cloud 
nucleation.

This brings up the possibility of transplanting biotic colonies to less well 
populated vents to kick start the natural process. Methane hydrates 
are associated with local sulfate production in some vents. This may be a 
clue as to how we might get new biotic masses growing....feed them sulfate 
through dispersing blocks of compressed sulfate around vents.

Just a thought....Any comments, suggestions?       

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