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Astrobiology IV: Photosynthesis and energy

8 Post author: CellBioGuy 17 October 2016 12:30AM

Originally I sat down to write about the large-scale history of Earth, and line up the big developments that our biosphere has undergone in the last 4 billion years.  But after writing about the reason that Earth is unique in our solar system (that is, photosynthesis being an option here), I guess I needed to explore photosynthesis and other forms of metabolism on Earth in a little more detail and before I knew it I’d written more than 3000 words about it.  So, here we are, taking a deep dive into photosynthesis and energy metabolism, and trying to determine if the origin of photosynthesis is a rare event or likely anywhere you get a biosphere with light falling on it.  Warning:  gets a little technical.

https://thegreatatuin.wordpress.com/2016/10/17/energy-metabolism-and-photosynthesis/

In short, I think it’s clear from the fact that there are multiple origins of it that phototrophy, using light for energy, is likely to show up anywhere there is light and life.  I suspect, but cannot rigorously prove, that even though photosynthesis of biomass only emerged once it was an early development in life on Earth emerging very near the root of the Bacterial tree and just produced a very strong first-mover advantage crowding out secondary origins of it, and would probably also show up where there is life and light.  As for oxygen-producing photosynthesis, its origin from more mundane other forms of photosynthesis is still being studied.  It required a strange chaining together of multiple modes of photosynthesis to make it work, and only ever happened once as well.  Its time of emergence, early or late, is pretty unconstrained and I don’t think there’s sufficient evidence to say one way or another if it is likely to happen anywhere there is photosynthesis.  It could be subject to the same ‘first mover advantage’ situation that other photosynthesis may have encountered as well.  But once it got going, it would naturally take over biomass production and crowd out other forms of photosynthesis due to the inherent chemical advantages it has on any wet planet (that have nothing to do with making oxygen) and its effects on other forms of photosynthesis.

Oxygen in the atmosphere had some important side effects, one which most people care about being allowing big complicated energy-gobbling organisms like animals – all that energy that organisms can get burning biomass in oxygen lets organisms that do so do a lot of interesting stuff.  Looking for oxygen in the atmospheres of other terrestrial planets would be an extremely informative experiment, as the presence of this substance would suggest that a process very similar to the process that created our huge diverse and active biosphere were underway.

Comments (6)

Comment author: CellBioGuy 17 October 2016 05:57:49AM 2 points [-]

Timing of next post uncertain, three weeks of insane teaching and grant-writing and yeast-poking ahead.

Comment author: turchin 18 October 2016 12:25:33PM 1 point [-]

What about dissolved oxygen in water, which also supports large animals? Could it happen in underground oceans of icy moons?

Comment author: CellBioGuy 18 October 2016 01:56:25PM *  0 points [-]

Icy moons would need oxygen to come down from their surfaces, where ultraviolet light and particle radiation spatters hydrogen out of the ice and off into space leaving oxidized molecules (not just oxygen) behind in the ice. This is possible, as on Europa the surface is young and it is believed to recycle surface ice down towards the internal ocean on megayear timescales (and Europa has an exceedingly thin oxygen 'atmosphere', one trillionth of a bar, from radiation-split water).

Figures I've seen (see "Energy, Chemical Disequilibrium, and Geological Constraints on Europa" by Hand et al) suggest that on Europa, a maximum of 5*10^9 moles of 'oxidants' may be delivered to the interior of Europa from the ice crust per year. Let's assume that's all oxygen - in that case, it's about a millionth of the photosynthetic oxygen flux of the Earth, and if we assume it is oxidizing hydrogen sulfide provides an energy flux of only about 45 megawatts to the interior.

That's less than a hundred thousandth the geothermal energy flux of the moon (and thus probably much smaller than the geochemical energy flux), but like the geothermal/geochemical energy flux it would not be even, there would be areas of downwelling ice with oxidizing agents slowly oozing out as it melted where this energy would be concentrated.

Comment author: CellBioGuy 18 October 2016 12:41:03AM 1 point [-]

Dang. Some information I've been pointed to since publishing this suggests that there are multiple groups out there that consider it likely that photosynthesis was present very close to the root of the bacterial tree, and that large numbers of bacterial groups may have lost it rather than it going all around the tree by horizonal transfer. This would put photosynthesis as one of the rather earlier metabolic pathways on Earth.

I've also been pointed towards more modern evidence that oxygenic photosynthesis originated in the original bacterium that created both energy-producing and sulfer-creating photosynthesis rather than the two coming together via horizontal transfer later.

Comment author: chron 17 October 2016 04:24:11AM 1 point [-]

Stupid technical question. You write:

Oxygen producing photosynthesis, on the other hand, uses water itself as the chemical source of electrons, two H2O for every CO2.

Doesn't the standard equation have one H2O for every CO2?

Comment author: CellBioGuy 17 October 2016 05:53:02AM *  1 point [-]

Yes, but two of the hydrogens/electrons ripped from water in the process of photosynthesis effectively reduce one of the oxygens from the CO2, regenerating one water: 2 H2O + CO2 -> O2 + CH2O + H2O (multiply atom numbers by various numbers to get the actual biomolecules that comes out the other side of the various carbon fixation pathways). Still needed since the oxygen production all happens from the photosystems splitting water rather than from splitting CO2, the photosystems never touch the carbon directly. That water is produced no matter what you're using as your electron donor.