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pfdietz 2 days ago

Oh, I didn't say the results wouldn't be utterly catastrophic. It's more a comment on just how surprisingly large an impact would be needed for sterilization.

https://iopscience.iop.org/article/10.3847/psj/ac66e8

(extrapolated > 700 km impactor needed for sterilization)

jajko 2 days ago | parent | next [-]

I don't think anymore absolutely 100% sterilization of all life on Earth is possible, we always end up talking about 99.999999% or similar. With exception of maybe super/hypernova of our Sun which ain't possible, or black hole passing directly through/very close to Earth, tearing apart every single atom making up this planet including all of us on quark level.

s1artibartfast 2 days ago | parent [-]

Colision with a planet or moon would do it, anything that turns the surface to lava really.

sebzim4500 2 days ago | parent | next [-]

Even then there's a chance a few tardigrades hibernate on some material that shoots up and then comes back a few years later once the earth has cooled a bit.

pfdietz 2 days ago | parent [-]

I think they could be cooked by thermal radiation as the ejecta expands.

sebzim4500 2 days ago | parent | next [-]

Probably most would be, but there are a lot of microorganisms and only a few need to get lucky.

blooalien 2 days ago | parent | prev [-]

Tardigrades were placed in the "extremophile" class with good reason. If anything could survive a truly catastrophic impact event, I'd say the smart money goes on the lowly "water bear" to win. :)

Keysh a day ago | parent [-]

Tardigrades are not "extremophiles", which refers to organisms that live (grow, reproduce) in "extreme" environments ("phile" = "like, love"). Tardigrades can temporarily survive some rather extreme conditions, but they generally require fairly ordinary environments to actually live. (As suggested by common names like "water bear" and "moss piglet".)

dekhn 2 days ago | parent | prev [-]

Deep-earth chemoautotrophs might survive that. But ultimately, if the deep subsurface exceeds 150C, it would be hard to survive.

fecal_henge a day ago | parent [-]

Intollerable stuffyness.

southernplaces7 a day ago | parent | prev [-]

I think you should read the text a bit more closely. A 700km impactor would be required to completely boil the oceans into vapor, but the article mentions that a much more insanely huge impactor of between 2000 and 2,700km would be needed to genuinely sterilize the earth because it entirely melts the crust.

However, (and here I speak from reading many other sources on this subject), even something the size of that latter object (basically something the size of a planet like Pluto) might not be enough.

Other studies have indicated that it might be exceptionally hard for heat to transfer enough through the vast mass of the earth's upper mantle and crust to actually melt it uniformly even if hit by something like the object that may have formed the moon.

This impactor was also supposed to be roughly 2,500km across and some of the theoretical concepts around it argue that even in that absolutely cataclysmic scenario, at least a part of the crust remains intact and relatively cool below a depth of several hundred meters.

If such a thing were to be true in the context of modern earth, which teems with life in every single possible remotely habitable nook and cranny and crevasse, then even a colossal impact by a 2,700km planet-type object wouldn't sterilize the Earth of life.

If only part of the crust remained intact as described above, then after hundreds of thousands or a few million years, as the earth's partially molten surface cools, and an atmosphere reforms, water that also reforms from vapor would rain down to the surface again in a vast global storm like something out of the bible. As this happens and the oceans refill, the tiny organisms concealed during all that time inside the deep cracks hundreds of meters below the surface of that surviving part of our world's crust would then recolonize the surface eventually and cause life to flourish again.

The key things in this scenario are that for one, at least one small part of the crust remains intact and cool, at least below a certain depth, and secondly, that water vapor eventually re-condenses into rain.

One might think that water would be vaporized right into separation of its hydrogen and oxygen atoms by the heat of such impacts, but mostly no. For that to happen the water on Earth would need to be subjected to at least something like 3,000 degrees Celsius of sustained heat, and even a planet-sized impact wouldn't generate such temperatures over most of the world.

pfdietz a day ago | parent [-]

I wrote "> 700 km". I did that deliberately, and was not asserting that 700 km was enough.

southernplaces7 17 hours ago | parent [-]

Fair enough but why not just say the much larger other size they specifically mentioned. It's not about it being bigger than 700km but about it being enormously bigger (bearing in mind how volume expands cubed) to a specific size they also name.

Anyhow, sparked me into really thinking about all this again and the link you added was wonderful for that.