Re:Living microbes, possibly 100M years old, pulled from ben...
by wombatmobile on Tuesday January 19, 2021 @08:25AM
(#25833182)
> The presence of dissolved O2, nitrate (NO3−), phosphate (PO4−), and dissolved inorganic carbon (DIC) throughout the sedimentary sequence from the seafloor to the volcanic basement indicates that cell abundance and activity are not limited by availability of electron acceptors or dissolved major inorganic nutrients. From the Redfield stoichiometry of net dissolved O2 reduction to net nitrate production in the sediment, the microbial cells have been inferred to consume oxygen coupled to oxidation of marine organic matter at extremely slow rates.
-- D’Hondt, S. et al. Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sediments. Nature Geosci. 8, 299–304 (2015).
Re:Living microbes, possibly 100M years old, pulled from ben...
by londons_explore on Tuesday January 19, 2021 @05:49AM
(#25832082)
As they were buried deeper and deeper in the sediment, presumably oxygen levels fell lower and lower.
That will have caused selective pressure to manage to survive with so few resources. Those that can't simply become energy for others who can.
It did say that there were microscopic amounts of oxygen in the sediment. Presumably, that was enough to maintain a minimally-small MR.