Hello, friends! Today’s post is about the planet Venus, but the real lesson today is this: never say never.
Could Venus have supported life at some point in the past? Yes. In theory, yes. Despite being closer to the Sun than Earth, Venus still orbits within the so-called habitable zone of our Solar System (this depends a little on whom you ask; some sources say Venus is inside the habitable zone while others will tell you she’s skirting the habitable zone’s edge). So it is plausible that, at some point in the distant past, Venus could have had more Earth-like temperatures and more Earth-like surface conditions.
But then something went catastrophically wrong. Carbon dioxide gas somehow started accumulating in Venus’s atmosphere. Carbon dioxide is naturally good at trapping heat, so rising CO2 levels caused the temperature to also rise. Rising temperatures caused more CO2 to outgas from the planet’s crust. The outgassing of more CO2 caused the temperature to rise further, which caused more outgassing of CO2, which caused temperatures to rise further, which caused more outgassing of CO2, which caused… you get the idea. This process is known as a runaway greenhouse effect.
I don’t think anyone knows for certain what started the runaway greenhouse effect on Venus (or at least, I’ve read many different ideas about what the initial cause might have been). All we know for certain is what Venus is like today: hell. Insane heat. Insane atmospheric pressure. Insane levels of CO2 plus insane weather, most notoriously sulfuric acid rain. I think it’s safe to say that no planet in the Solar System is more hostile to life as we know it than modern day Venus.
But the runaway greenhouse effect was not the only catastrophe to befall Venus. Venus also experienced something called a global resurfacing event. Resurfacing may sound like something you’d do to a parking lot, but when we’re talking about planets, resurfacing means spreading fresh lava over a planet’s surface, essentially paving over whatever surface features might have been there before.
So could Venus have supported life at some point in the past? Sure. It’s possible. But this always seemed like an untestable hypothesis to me. The runaway greenhouse effect would have killed everything (well, almost everything… see my post script), and the global resurfacing event would have paved over any fossils or other evidence of past Venusian life. So if there ever was life on Venus, we’d never know about it. Never.
We now come to the “never say never” part of today’s post. On Venus, there are patches of rough terrain called tesserae (singular, tessera). As longtime readers of this blog know, Venus is my favorite planet, so naturally I have heard about the tesserae on Venus before; however, I was previously led to believe tesserae were formed by thrust faults, volcanic eruptions, or some other relatively modern geological activity. But recently, I read a research paper that mentioned, rather casually, that tesserae might also be the remnants of ancient continental crust jutting up above the otherwise smooth, resurfaced landscape.
So the tesserae we see today could be ancient Venus’s version of the Rocky Mountains, the Alps, or the Himalayas. They are (or were) the highest of high elevation regions on ancient Venus—regions high enough to survive the global resurfacing event. If true, then the tesserae of Venus may preserve some hard evidence of what Venus used to be like before the runaway greenhouse effect and the global resurfacing event wrecked the place.
So was there ever life on Venus? It’s possible, but we don’t know for sure. I once resigned myself to the belief that we could never know, but you should never say never. Signs of ancient water and ancient life may be preserved on Venus after all, just waiting for us to discover.
P.S.: Some scientists believe there may be life on Venus today. There is some very circumstantial evidence of microorganisms floating around in Venus’s upper atmosphere. I do have some thoughts about that, but I’ll save that for another blog post.
Want to Learn More?
Here is the research paper I mentioned that casually mentions tesserae might be the remnants of ancient continental crust.
And here is a paper I found describing possible signs of water erosion on Venus’s tesserae. Water erosion could not possibly happen on Venus today, so this would be further evidence that tesserae have preserved something of Venus’s ancient history.
And lastly, just because this “tesserae equals continental crust” idea is new to me, that doesn’t mean it’s new to science. Here’s a paper from 1990 discussing the possibility. Even if some of the information in this paper is out of date, I think it’s still worth a look, if only to see how much history this idea has.







