In a recent published Science article by Hurowitz et al (2017), Redox stratification of an ancient lake in Gale crater, Mars, it is suggested that there was atmospheric oxygen around in enough quantities to cause the oxidation of transition metals like iron and manganese, about 3.5 billion years ago. I was left with many questions regarding the questions, so I left the following commentary in the eLetters section:
The authors write: “The recognition of a stable
redox-stratified water body adds important detail to our understanding of the
potential for microbial chemoautotrophy within the ~3.8- to
3.1-billion-year-old Gale crater lake system.”
I am just wondering on what assumptions photoautotrophy is
excluded as a possibility. It is well known that, at the very least, anoxygenic
photosynthesis was ongoing 3.8 billion years ago (Nisbet & Fowler, 2014). While the exact date
for the origin of oxygenic photosynthesis on earth is debated, there are many
reports for the presence of biogenic oxygen hundreds of millions of years
before the Great Oxidation Event (Lyons et al., 2014). So it is not
unreasonable to think that some forms of biological water oxidation to oxygen
already existed before 3.0 billion years ago.
The authors write: “The model depends on the depth of
penetration of ultraviolet (UV) light and low levels of photochemically
generated atmospheric O2 into the water column
to establish a depth-dependent boundary between oxidized and anoxic zones”.
How much oxygen can be produced photochemically
on Mars? I am not a geochemist, but from discussions regarding the oxygenation
of Earth, I understand that it was an almost negligible contribution. With the
levels of O2 being only a maximum of 10-8 of the current
level by photochemistry alone (Kasting &
Walker, 1981). That is on Earth, Mars is farther from the
Sun and the young was fainter back then.
Unfortunately, I do not know the literature on
Mars early atmosphere, but is photochemical produced O2 really a
valid alternative?
What concentrations of oxygen do you need to account
for the level of iron and manganese oxides that you see?
Based on this work, can you put a minimum
constrain on the amount of oxygen present in the atmosphere of Mars at this
time?
Kasting, J. F.,
& Walker, J. C. G. (1981). Limits on oxygen concentration in the
prebiological atmosphere and the rate of abiotic fixation of nitrogen. Journal of Geophysical Research-Oceans and
Atmospheres, 86(Nc2), 1147-1158. doi:DOI 10.1029/JC086iC02p01147
Lyons, T. W., Reinhard, C. T., & Planavsky, N. J. (2014). The
rise of oxygen in earth's early ocean and atmosphere. Nature, 506(7488), 307-315. doi:10.1038/nature13068
Nisbet, E. G., & Fowler, C. F. R. (2014). The early history of
life. In K. D. M. & W. H. Schlesinger (Eds.), Treatise on geochemistry (2nd ed., Vol. 10, pp. 1-42). Amsterdam:
Elsevier Science.
Gale Crater, Mars. Was there ever life thriving in here? |
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