
Lifeless Planet Ending
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Was a very interesting game, quite enjoyed myself. The Ending though; can anyone explain this to me? The girl becomes one of the Alien root things and the guy (astronaut) is in the future because 1 week equals 1 month of his time on the lifeless planet.
So does that mean his wife that he left on Earth is still alive as he didn't take her off life support and they get together again? Perhaps im wrong, would have been nice if he found some kind of antidote for her illness or something would have made the story more amazing.
.We claim a Hadean geochemical scenario with a reduced methane-rich atmosphere and initial silica-rich alkaline oceans.Over time, the Hadean oceans slowly became less alkaline and obtained higher CO 2/CO-CH 4 ratios.Mineral self-organized structures (MISOS), such as silica-carbonate biomorphs and silica-metal membranes, formed unavoidably during the Hadean.Silica and MISOS played a key role as catalysts for prebiotic chemistry reactions.We propose that during the first 500 million years of Earth history there was a large-scale factory of simple and complex organic compounds. It has been experimentally demonstrated that, under alkaline conditions, silica is able to induce the formation of mineral self-assembled inorganic-inorganic composite materials similar in morphology, texture and nanostructure to the hybrid biomineral structures that, millions of years later, life was able to self-organize. Panda pop online.
These mineral self-organized structures (MISOS) have been also shown to work as effective catalysts for prebiotic chemical reactions and to easily create compartmentalization within the solutions where they form. We reason that, during the very earliest history of this planet, there was a geochemical scenario that inevitably led to the existence of a large-scale factory of simple and complex organic compounds, many of which were relevant to prebiotic chemistry. The factory was built on a silica-rich high-pH ocean and powered by two main factors: a) a quasi-infinite source of simple carbon molecules synthesized abiotically from reactions associated with serpentinization, or transported from meteorites and produced from their impact on that alkaline ocean, and b) the formation of self-organized silica-metal mineral composites that catalyze the condensation of simple molecules in a methane-rich reduced atmosphere.

We discuss the plausibility of this geochemical scenario, review the details of the formation of MISOS and its catalytic properties and the transition towards a slightly alkaline to neutral ocean.