Perhaps, but the main point I was trying to make is that the biochemical system we know, in its gross aspects (carbon-hydrogen-oxygen based), is by far the one we are most likely to encounter elsewhere, because its major constituents are supremely abundant and interact chemically within favorable and probably also common temperature/pressure regimes. We are made of this stuff precisely because it constitutes the common stuff of our planet. In particular, liquid water, owing to the peculiar nature of the water molecule, is the supreme solvent/catalyst, permitting complex and rapid chemical reactions in a way that no other common substance is known to do. That's not an accident or a coincidence. It only makes good sense to look for places in which the temperature/pressure regimes would be favorable to carbon-based life, because the carbon-hydrogen-oxygen triumvirate will almost always be there.
As another hint of something to look for: silica in pure form. Frank Herbert didn't have it far wrong in his invention of the desert planet Arrakis, covered by its sand ocean. Silica (SiO2), while not of itself organic in origin, is present in abundance on our planet's surface in the form of widespread beds of sand in deserts, beaches, dunes. It is winnowed from primordial rock through weathering processes that require liquid water, and are a signal both of the presence of water in the liquid state and of an active geological planetary surface. The "sands" of Mars, for instance, aren't silica; they are primarily iron oxides. Mars is not known to have an active planetary crust in the manner the earth does, where both mineral matter and water are recycled many many times, and get to interact chemically to sort and winnow and concentrate various materials. What silica Mars has (and it undoubedly has a lot of silicon and oxygen) is almost exclusively locked up in more complex silicate minerals typical of primordial igneous rocks.
If you can find a place with lots of silicon dioxide exposed at the surface, you almost certainly have a place which has, or had, a long period of atmospheric weathering involving lots of liquid water. In other words, the kind of place to look for carbon-based living things.
caw