Great extinctions are
times when the number of species that cease to exist per century gets a lot
higher than the average. There are always extinctions going on, and
the vast majority of species that ever existed are already extinct.
It seems to be a common destiny of a species to begin, to flourish,
to plateau, to diminish and then to become extinct. Lots of things
make species go extinct, such as the food supply being cut off, some
environmental change or catastrophe such as their only habitat being
flooded, long-term or short-term. New predators can evolve. More
efficient species can out-compete them for food supplies or nesting
spaces. And so on.
Species counts are
done by checking fossil records. It seems from fossils that there
were multiple times when a large fraction of the existing land and/or
sea animal species ceased to appear in later fossils, meaning they
became extinct. These extinctions typically happen over a
geologically short time, and geology being what it is, there is a
minimum time that can be determined by fossil research, so no
understanding of exactly how long the extinction lasted can be
obtained, if it was shorter than the minimum measurable geological
interval. Nonetheless, there are multiple periods in Earth’s
history when a large number of animals became extinct, up to 96% as
reckoned by fossil counts on the worst of these great extinctions.
The causes of such
extinctions are obviously of great interest to geologists and many
other scientific specialties. The earliest one is sometimes
attributed to the oxygenation of the atmosphere, meaning that all sea
creatures which could not tolerate the oxygenation of the atmosphere,
and correspondingly, the seas, died off. No other atmospheric change
seems to have caused other extinctions, but climate change has been
called on as one possibility for some of them, although not the
largest ones, unless you call a temporary clouding and the subsequent
cooling of the Earth a climate change. Instead, some of these
largest ones are attributed to either a large asteroid strike or a
basalt flooding. A controversy arose over the last one, the
End-Cretaceous extinction. Someone came up with a measurement that
76% of animal species became extinct during this one.
One of the earliest
theories as to the cause of this extinction was the Decca Basalt
Flooding, which was chronologically pinpointed to occur at the time
of the extinction. A basalt flooding, when thousands of square
kilometers become like a volcano, with exposed mantle material,
produces such massive amounts of dust in the atmosphere that sunlight is blocked and
photosynthesis stopped. The flooding lasts for many millennia,
unlike a volcano whose principal eruption lasts only a matter of days
or weeks. It certainly is reasonable that this could cause mass
extinction.
Later, a large
crater was discovered on the coast of the Yucatán
peninsula, and it was timed to also be at the time of the
End-Cretaceous extinction. The crater was named Chicxulub.
Asteroidal material, specifically a higher than normal
concentration of iridium, was discovered all over the world and dated
in sediments to have been deposited by the Yucatán
asteroid. The impact would have filled the atmosphere with dust as
well, although for a much shorter period. If the End-Cretaceous
extinction happened within a very short period, a few years which is
the dust residence time from a single near-instantaneous event, this
could also have been the cause of the extinction.
It is curious that
the Deccan Traps, the current geological formation from the basalt
flooding there, and the Chicxulub crater are almost on opposite
sides of the planet. When a rapidly flying object hits a large
obstacle, shock waves are generated which move from the impact
location in the direction of the incoming object. These shock waves
carry some of the momentum of the incoming object, and when they
strike the opposite surface, they tend to spall off the outermost
layer. Spallation of this type occurs when very fast projectiles
strike armor plate, for example. On something of the size of a
planet, it would mean that the crust at the arrival point of the
center of the shock wave would heave upward, rupturing it and leaving
it no longer intact. The Deccan volcanic activity may have been
going on before the impact, but the shock wave may have been the
cause of the large size and huge amount of atmospheric debris that
was deposited.
The crater and the
traps are not on exactly the opposite sides of the planet, now, but
tectonic plate motions are of the right magnitude to make it more so
60 million years ago. Both India and South America have been moving
north. Furthermore, if the impact was not perpendicular, there would
have been some deviance of the shock wave direction from directly through the center of the planet so it did not go from a
point on one side to the exact opposite.
The crater and the
traps can be used to backwards track the asteroid, and doing this
shows that if the impact was in the spring or fall, the asteroid
would have been traveling in the sidereal plane, where all planets
and almost all asteroids reside. Thus, the two events, asteroid
impact and basalt flooding, may have been closely connected.
What is considered
the most serious great extinction, the End-Permian one about 250
million years ago, is often attributed either to the Siberian basalt
flooding, near the north pole, or to the Wilkes Land crater, in Antarctica near the south pole. The details of these two events are
much, much less certain than those related to the End-Cretaceous one,
but the possibility of a basalt flooding event triggered by an
asteroid impact on the opposite side of the globe exists. For some
other great extinctions, there are even less certain connections to
basalt flooding and asteroid impact.
What happens after
an extinction? When the atmosphere returns to transparency, there is
much less life around. Most of the species have gone entirely
extinct, and the remaining ones were greatly reduced in numbers. It
has become a field day for evolution, because the constraints on new
life are largely removed. Resources are available in abundance, and
competition is less. Predation is almost absent. Thus, evolution
goes much faster in creating new species that it could in a crowded
environment where all ecological niches were already filled. Within some tens
of millions of years, hordes of new species exist everywhere.
We humans arose from
the chaos of new life that occurred after the End-Cretaceous
extinction. Life was not extinct, and what life existed still kept
many of the genetic tricks that had evolved up to that point. Thus,
evolution took off again, but from a much higher starting point genetically.
This is not to say that life could not have evolved intelligence
without the extinctions, but it would have taken much longer. Maybe
a factor of ten in speedup happened.
What exactly does
that mean for a planet somewhere in the galaxy with eukaryotic,
multicellular life already started. To get to this point might have
taken 3 billion years of evolution. It will take another billion
years of evolution, if the rate of evolution is the same as Earth’s,
to get to intelligent life. However, Earth’s evolution rate was
governed and greatly accelerated by all the mass extinctions our
planet has known. If there were no extinctions, or only very few,
it might take ten times longer to get to that point, or ten billion
years. Almost no planets are that old.
So, one interesting
thing to ponder is: Can an intelligent alien civilization come into
extinction in a solar system where there are no or very little
asteroid impact? Is the answer: Yes, but only billions of years from
now. Thus we might have another peculiarity of our solar system
which might be essential to the eventual capability for
contemporaneous space travel: huge numbers of large asteroids.