Astrum Space - The Time It Rained for 2 Million Years - The Carnian Pluvial Event
Episode Date: April 24, 2025How the Carnian Pluvial Event forever change the course of life on Earth, the latest episode in our Earth History series. Discover our full back catalogue of hundreds of videos on YouTube: https://www....youtube.com/@astrumspaceFor early access videos, bonus content, and to support the channel, join us on Patreon: https://astrumspace.info/4ayJJuZ
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In the centre of the arid and ancient supercontinent, Pangea, thousands of miles away from the sea,
our time-travelling aliens have returned to witness a key moment in Earth's history.
As they arrived, the rain began to fall.
Just off Pangaea's west coast, in what is now Canada, epoch-ending volcanic activity
sent off a chain of events that all but made this downpour.
inevitable. It would never look the same, because this was the start of a rain that wouldn't
abate for over one million years, a rain that changed the course of life on Earth, a rain that
allowed the dinosaurs to take over the world in an evolutionary coup.
What's all the more surprising to me, and to our aliens who witness life on Earth develop,
is that the kind of event that caused this rain is, ordinarily, the most of the most of the most of the
most reliable and powerful extinction event the world has ever known.
But this one was different.
One that takes the butterfly effect to its limits.
Imagine if a butterfly flapping its wings can cause a tornado 1,000 miles away, what does
an eruption 100 times larger than a super volcano cause?
I'm Alex McColgan and you're watching Astrum.
Join me today as we discover how an extinction
level event 230 million years ago increased the richness of life on Earth and accelerated the
evolution of the dinosaurs, learning as we move through Earth's major cycles how burning fossil fuels
contributed to climate change way ahead of the Industrial Revolution. What came before the rain?
Pangea was the largest continent that has ever existed on Earth by a long way, a record not
likely to ever be beaten, given it was the size of every current continent combined.
Its huge size meant that the centre was far removed from coastal climates, and therefore received
very little rain, favouring the evolution of species that required less water to survive.
During this dry period around 300 million years ago, in the Carboniferous period,
several species emerged that are still important today, including dragonflies, millipedes,
and spiders. Throughout this period, the diabsids also exploded, a group containing lizards and snakes
as well as, archosaurs. Now, you may not know that name, but you certainly know what this group
contains. Crocodiles, birds, and yes, eventually dinosaurs. But we'll come back to those later.
If you've seen our previous episodes on ancient earth, you'll know that it was a tumultuous and
unforgiving place, with impending threats left, right and center, and above and below for that
matter. While asteroids smashing into the crust better grab the attention of Hollywood,
it's under the crust where the real danger has always been, and it's here that we will find
answers to what caused a million-year storm. We live on a vanishingly thin crust that is so shallow
that if the earth was represented by the entire Lord of the Rings book trilogy, the layer harboring
all the known life in the entire universe would be confined to just one single page. Beneath hot plumes
rise up from the core, mushrooming as they rise and pushing molten magma up against the thin crust.
These huge plumes punched through the crust wherever they meet it, completely ignoring continental fault lines,
where Earth's modern volcanic activity is concentrated, like the Pacific Ring of Fire.
These plumes can release magma at the surface for over 1 million years,
in what are known as flood basalt eruptions.
It is these eruptions that are linked to the most incredible extinction events during Earth's history
and are probably the cause of the most destructive extinction event in history,
the Great Dying, where ocean temperatures rose to 40 degrees Celsius.
Despite life's ability to evolve, it is estimated that over 99% of every species that ever
lived on Earth have gone extinct.
Of course, you can't exactly evolve out of the way of a Mount Everest-sized asteroid travelling
at 20 kilometres per second, but these volcanic processes, though slower and far less
dramatic, can cause far greater devastation over a longer period.
evidence of flood volcanism is scattered across the world today.
The eruptions of these flood basalts result in the creation of huge, unmistakable swaths
of land, like the Siberian traps in northern Russia, the Deccan traps in western India, and
the Rangalian large igneous province across Canada and Alaska.
They are all cooled flows of basalt rock, kilometers deep, making them over 100 times larger
than supervolcanoes.
When we date these flood basalts, we see that many of these eruptions align with mass extinction events.
There is one though that doesn't.
That is our rainmaker event that triggered the so-called Karnian pluvial episode or the time
that it rained for over one million years.
It's believed that volcanic activity in the Ranglian province is responsible for this remarkable
transformation of an arid desert into an oasis.
jump-started the dinosaur's explosion.
So what separated Rangelia's eruption from the rest?
What made it different?
Well, I've got news for you, size does matter.
Although this was an extinction event with around 30% of the ocean species wiped out during
the CPE, Rangelia's eruption was just the right size to give life an overall boost on
Earth.
So the reason that the overall biodiversity was unchanged is because the level of extinction was
matched by the emergence of new, exciting species more suited to this wetter world.
What our aliens witnessed was less an extinction event, and more a reinvention period.
So how can slow eruption affect such an incredible change to Earth climate?
To understand how this transformational event shuffled the deck of life on Earth is to understand
something that we are living through right now, climate change.
Specifically, the release and production of carbon dioxide and the release of stored methane.
Eruptions like these directly release carbon dioxide already contained within the mantle,
but they can trigger its release from other stores too.
from a source of carbon I thought only humans had used.
Huge reservoirs of fossil fuels.
Now, whether you remember the fire triangle from school or not,
fuel, heat, and oxygen,
I think we can all appreciate that introducing 1,600 degrees Celsius magma
to the base of untapped virgin coal beds is going to get spicy.
Burning these crude coal beds would have released incredible amounts of particulates
and greenhouse gases, both important for driving cloud formation and rainfall.
Just as we are seeing today, the increasing levels of those greenhouse gases trap more of the
sun's energy, and that energy has to go somewhere.
So where does it go?
Earth systems work to distribute their energy, and the one best place to absorb this extra energy
is the water cycle, which becomes supercharged.
The sun's energy is absorbed by the land and sea, evaporating water from the surface.
Once in the atmosphere, the water can be carried great distances before precipitating onto land
and returning to the sea along a meandering route.
The more energy that is trapped by greenhouse gases, the faster the water cycle turns over.
In these flood basalt eruptions, we see an extreme example of the complex interplay
of the three major cycles, the geological carbon and water cycle.
The formation of the Ranglian large igneous province would have released huge amounts of CO2.
Our alien ship detected atmospheric levels exceeding 1,000 parts per million,
two and a half times what they are today, increasing temperatures by 3 to 4 degrees Celsius.
This supercharged the water cycle, greatly increasing evaporation and cloud formation,
And these clouds were increasingly able to deliver rain further and further into the centre of
Pangea.
Throughout this period, the Earth became warmer and more humid, a dramatic change in the climate.
Species that had adapted to a particular dry climate environment or niche before the rain
were put under stress from multiple fronts.
During this turnover period in Earth's history, our aliens watched as old niches were seemingly
destroyed as quickly as the new ones were created.
The status quo was changing.
Not only that, but species had to cope with a pH shift too.
Carbon oxide wasn't the only gas released by the Ranglian eruption.
Hydrogen sulfide gas erupted into the atmosphere along with it.
This egg-smelling gas reacted with oxygen and water to form sulfuric acid, which in this
form is more well known as acid rain.
As the rain fell, the soils and oceans became inundated with acidified water, which only
further contributed to the environmental stress some species were facing.
Interestingly, a large amount of amber can be found in the geological record from the
Karnian.
Amber is a protective mechanism for trees that they release when in peril, suggesting that
plant life came under significant stress during this period too.
The incredible volume of rain across the supercontinent resulted in deluges of surface runoff.
Accelerating across and through the arid terrain, these slightly acidic flows eroded the land
as it went.
Some of this acidic water seeped into and eroded small fissures in limestone and dolomite rocks.
Our aliens watched as rocks were literally dissolved in front of their eyes.
Over time, elaborate new cave systems were formed, like Britain's Tarracic.
caves carved from carboniferous limestone, which provided yet more unique habitats for life
to exploit. Eventually, the flow reached the sea, carrying the eroded rocks and minerals into the ocean,
further nudging the coastal ecosystems into new territory. The ocean species were particularly hard
hit, and large areas became anoxic, meaning they lacked oxygen, and highly acidified,
which was not suitable for the existing ecosystems that inhabit those areas. Species like
conodonts, ammonoids, crynoids, and green algae suffered particularly high extinction
rates during the CPE, as did reef builders, while dynoflagellates, a constituent of today's
ocean planktons, thrived.
ship, the aliens moaned in disbelief every time the ship's AI forecasted the ongoing miserable weather.
But back on land, one of the oldest known dinosaurs, Herarasaurus, was braving the elements and roaming
the earth. Some six meters in length and weighing more than 300 kilograms, it was an outlier
prior to the Karnian pluvial episode, when smaller reptiles and mammals were far more numerous.
Its home was the Ishigualasso formation, a volcanic floodplain defined by its dense jungle
in what is South America today, a warm and humid environment, which the Herrerasaurus
was well adapted to.
So when the rains began to fall, it won the geological lottery as its habitat spread across
Pangea.
Advancing deeper into the continent, hererosaurus was greeted with literal oases.
Untouched habitat that with the extinction of herbivores and other competition meant it was to be a boom time for the herarasaurus and similar dinosaurs.
We can only imagine the variety and richness of habitat available for all these wandering species to find and exploit and co-evolve with over time.
Further away in the Dolomites, the aliens saw herds of large dinosaur creatures roaming the plains,
and their wandering footsteps have been recorded deep in the rock.
Across a 3 to 4 million year period spanning the Khanian pluvial episode,
dinosaurs went from not featuring at all in the fossilized footprints to ecological dominance,
making up over 90% of fossilized imprints.
A remarkable takeover that agrees with other records in other parts of Pangea during this time period,
notably the Central European Formation and the Ischikolasto Basin in Argentina.
The two million year periods spanning the Kaniin pluvial event left its mark in indelible ways,
forever changing the trajectory of life on Earth, as well as the passage of water across
and through its surface.
The mega-monsoonal climate featured four distinct downpours, each carving a trace through
the landscape, making the biblical storm that remade the earth in 40 days and nights look
more like a typical British summer in comparison.
But the fifth period of rain never came.
Once the Ranglian eruption finally slowed, the emission of greenhouse and acid-forming
gases slowed, and it is likely that levels of carbon dioxide fell as it was consumed by the
rich flora that covered Pangea, some of which would again become buried and form coal-fossil
fuel deposits for us to use today, continuing the carbon cycle.
Now the storm has passed, we can answer our question.
If a butterfly flapping its wings can cause a tornado 1,000 miles away, what does an
eruption 100 times larger than a supervolcano cause?
Well, a complete terraforming of land, sea and air.
The aliens left, having witnessed the origin of the dinosaur's dominance.
and a remade earth.
Some of the 118 million years after the extinction event that gave dinosaurs their big break, another
would strike, wiping them from the face of the earth, for the earth giveth and the earth
taketh away.
From that point it has been the mammals who have come to dominate, including us humans.
A remarkable reminder both times of how much can change on a geological whim, but that at each time
of asking, as the rules change, life adapts and goes again.
As life evolves, it gets better and better suited for the environment it finds itself in.
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