| Mars has a lot less sun and atmosphere then the Earth, so terraforming it would involve a large investment in greenhouses and nuclear energy. But Venus has an excess of sun and heat, and parts of its super dense atmosphere could potentially host floating algae, which absorb CO2 and rain down to the surface when they die. (Where they could burn and release all the CO2 again, but maybe a tiny bit stays out of the atmosphere.) I guess what I'm saying is, we might be able to "seed" Venus and then sit by and watch as a carbon sink is created. And with less CO2 the atmosphere would start to cool off. Now my very amateur understanding of Venus is that because the greenhouse effect creates super hot temperatures the magma underneath the crust of Venus does not form hot and hold spots like it does on Earth, it does not flow or erupt. There are no volcanoes, the crust is too "baked", too hard and thick. But over long periods of time the crust still tends to break up: At a massive scale, planet wide, the whole planet surface is then covered with lava, the lava eventually cools and the cycle starts again. This is why the surface of Venus looks suspiciously smooth except for a very few, very recent craters. Now imagine we are able to "infect" Venus with life and it does manage to suck CO2 of the atmosphere and cool down Venus to the point where the surface of Venus can support liquid water. It seems that could either trigger another planet wide cracking of the crust or maybe just huge volcanic eruptions.
But I think once life is widely distributed even that could not expunge it. And with a much cooler atmosphere softer elements would not be baked out of the crust and the Venus crust would start to resemble Earth's crust, complete with softer and harder and lighter and heavier components and volcanoes. And one day we could move in. |
By this point it's probably easier to tow Mars to a better orbit. Or just blow Venus up and make a (partial) Dyson sphere.