When geologist Clarence Dutton first saw the
Grand Canyon in 1880, he was spellbound by its colorful walls. The Grand Canyonâs walls are made up of
rock layers, each representing a distinct period of Earthâs history. And some of the lower rock beds--deep down
in the canyon--look kind of tilted. Dutton knew these layers were made up of very
old sediments. Originally, theyâd been laid down as horizontal
beds, mostly in rivers or shallow seas. Then, the sediments hardened over time and
geologic forces pushed some layers upward at an angle. As time passed, the tops of these tilted layers
were sheared off by erosion. And later, new layers of sediment--which stayed
more or less horizontal--were deposited right on top of them. And he knew every step of this process took
time - because you generally donât get horizontal layers on top of tilted ones unless thereâs
an age difference between them. In his examinations of the Grand Canyon, Dutton
got a firsthand look at what geologists call an unconformity. Basically, thatâs a gap in the geological
record. It shows that sedimentation didnât happen
continuously, and that thereâs an age difference between sets of rock layers...and sometimes
that age gap can be millions of years...or more. In 1882, Dutton named this particular break
âThe Great Unconformity.â At first, nobody realized just how great it
was. Today, we know from radiometric dating that
the rocks directly on top of the Great Unconformity were laid down during the Cambrian Period
about 500 million years ago. But in some places, the rocks below this âGreat
Unconformityâ are about 1.2 billion years older! Thatâs⌠a big gap. I mean, the Earth itself is only about 4.5
billion years old. So at this spot in the Grand Canyon, 25% of
the planetâs entire history is gone - those layers just arenât there anymore. And the Grand Canyon isnât the only place
where this happens. You can see this gap from Siberia to Antarctica--and
plenty of spots in between. Scientists are still trying to figure out
what caused the Great Unconformity - but they have some ideas. This missing chapter in Earthâs history
might be linked to a fracturing supercontinent, out-of-control glaciers, and maybe--just maybe--the
diversification of life itself. Sedimentary rock layers are formed by a process
called deposition - when eroded geological materials- like sand -are laid down by wind,
water, or even ice. They accumulate to build up layers of sediment
that later turn into rock. And when youâve got a layer of rock thatâs
distinct from everything above and below it, thatâs called a stratum. Pile up a bunch of strata on top of each other--with
each level representing one span of time--and together, theyâll create a rock sequence. And an unconformity is a boundary dividing
two strata with an age difference between them. An unconformity might mean that no new material
was deposited at this place for a long time, interrupting the rock sequence. But this isnât always the case. Usually, unconformities are made when an entire
layer gets eroded away somehow. And it turns out that the Grand Canyonâs
picturesque walls are full of unconformities. For example, thereâs a 150 million-year
gap between two strata of limestone: a layer from the Early Carboniferous Period and another
one from the Cambrian Period. But thatâs nothing compared to the Great
Unconformity. It begins under the Tapeats Sandstone, a stratum
laid down by the ancient tides of a shallow sea about 508 to 501 million years ago during
the Cambrian. Below this, youâll find a stretch of 1.75
billion year-old metamorphic rock called the Vishnu Schist, along with tilted rock layers
ranging between 1.25 billion and 740 million years old known as the Grand Canyon Supergroup. And figuring out what happened in that gap
is the key to explaining the existence of the Great Unconformity. Right now, weâre living in the Phanerozoic
Eon, which began 541 million years ago at the dawn of the Cambrian Period. But before the Phanerozoic, there was the
Proterozoic, a much longer Eon that kicked off some 2.5 billion years ago. Yeah, thatâs billion with a âb.â The Proterozoic saw the rise and fall of three
supercontinents - and the last one is known as Rodinia. Scientists think it formed between 1.3 billion
and 900 million years ago. And when it was fully assembled, Rodinia contained
just about all the known continents that were around at the time. But supercontinents donât last forever. Rodinia started breaking apart around 750
million years ago--well before the Cambrian started. And its break-up might be linked to something
else that happened late in the Proterozoic. It wouldâve been another major event--and
a pretty cool one. Literally. Since the 1930s, scientists have been finding
evidence that glaciers were common at the equator late in the Proterozoic. Places like Western North America and southern
Australia were tropical or subtropical back in those days. And if you look at deposits from the late
Proterozoic, youâll find a haphazard mixture of sand, mud, gravels, and boulders. Those deposits are called tillites and theyâre
the material that gets left behind by glaciers. In places that were at low latitudes during
the late Proterozoic, geologists often find these tillites sandwiched between limestone
beds that probably developed in warm, tropical waters. This finding--along with paleomagnetic data
and other clues--gave rise to the âSnowball Earthâ hypothesis, which Iâve talked about
before. According to this idea, glaciers once covered
all or most of the worldâs surface, from the poles all the way down to the equator. And this may have happened more than once
in the late Proterozoic. So there couldâve been multiple âSnowball
Earthâ episodes--with the first starting around 716 million years ago--and the last
one ending just 635 million years ago. And these cold periods might be related to
the Great Unconformity - but how depends on who you ask. Either the formation of the Great Unconformity
was part of what caused Snowball Earth or Snowball Earth was what formed the Great Unconformity. One study published in 2018 made the case
that the Great Unconformity helped set up the start of Snowball Earth. It looked at North Americaâs Ozark Plateau,
where 500 million-year old Cambrian sandstone sits on top of granite thatâs 1.4 billion
years old. Here, as in the Grand Canyon, the Great Unconformity
is plain to see. To date the Great Unconformity, they used
uranium isotopes and helium trapped in zircon crystals. From those crystals, they concluded that the
area was tectonically uplifted and eroded from about 850 to 680 million years ago. And this coincides with the breakup of Rodinia. Tectonic uplift on a big scale may be a side-effect
of fragmenting supercontinents. In this case, the studyâs authors think
several kilometers of rock were lifted up, only to get whittled down by erosion. Since the Ozarks were really far inland back
then, the scientists suspect there was a continent-wide--and maybe even worldwide--outbreak of large-scale
erosion. If this really was a global phenomenon, it
may be what created the Great Unconformity, eroding away rock layers that now appear as
gaps in the geological record. And thereâs more. The authors think the erosion of all that
Proterozoic bedrock affected the climate, by capturing large quantities of carbon in
the Earth and its oceans, keeping it out of the atmosphere. Thatâs because rainwater often pulls carbon
from the atmosphere during the weathering process. Since rainwater is weakly acidic, it dissolves
rock and releases ions. These ions can get washed into the ocean where
they form calcium carbonate, which is eventually buried, and traps the carbon in rock. And carbonâs a key component of greenhouse
gases. So if a lot of carbon didnât end up in the
atmosphere, that might've promoted global cooling--along with other factors like volcanic
events and a dimmer sun. And as the world grew colder, glaciers couldâve
gone unchecked. In other words, welcome to Snowball Earth. So according to this timeline of events, Rodiniaâs
breakup resulted in lots and lots of erosion. And not only did that erosion create the Great
Unconformity, but it also impacted the climate, helping to set the stage for Snowball Earth. But not everyone agrees. A different study, published in 2019, argues
the opposite: that Snowball Earthâs glaciers created the Great Unconformity by grinding
up the surface of our planet. The glaciers wouldâve eroded away a lot
of the outer continental crust, dumping it into the oceans. This massive increase of eroded material wouldâve
also increased the amount of crust being driven down into the Earthâs mantle, where some
of it was recycled into fresh magma and sent back toward the surface. And the evidence of this comes - again - from
isotopes trapped in zircon crystals. But this time, theyâre isotopes of the element
hafnium. Some hafnium isotopes are more likely to form
at the surface than down in the mantle - and that signature is preserved. This can show where the isotopes came from. And remember, zircons are also used in radiometric
dating. So by looking at the ratios of different hafnium
isotopes in these zircons and dating the zircons themselves, the researchers figured that the
crust erosion and recycling probably happened after Snowball Earth started. And this is because they found a lot of surface
hafnium trapped in the zircons - and the zircons formed after Snowball Earth got underway. So if thatâs true, the erosion--and all
the crust recycling that wouldâve gone with it--could not have set up Snowball Earth. Instead, it could have been glaciers that
stripped away over a billion yearsâ worth of rock layers, creating the Great Unconformity. Or at least, thatâs the hypothesis. Hopefully, future research will tell us which
came first: The Snowball or the Unconformity. But either way the loss of so much material
couldâve been important for life on earth. Complex life really diversified during the
Ediacaran Period--which closed out the Proterozoic--and then life exploded during the Cambrian. Scientists have wondered if this might be
related to the Snowball Earth and the Great Unconformity. Some researchers have suggested that when
all that crust was destroyed, it fundamentally changed the oceanâs chemistry. The weathering process might have transported
a lot of geologic material from land to sea. As a result, scientists think our oceans were
filled with calcium, potassium, iron, phosphorus and other vital elements. This couldâve revolutionized life on our
planet by giving it the chemical building blocks it needed to really get going. One hypothesis even suggests that these new
ingredients helped to encourage biomineralization, the process by which living things create
minerals for their shells and skeletons. So maybe when Clarence Dutton first saw the
Great Unconformity way down in the Grand Canyon, he was actually looking at the calling card
of a phenomenon that made his own existence possible. I must give big shoutouts to all these researchers
who consulted on this episode! Your input was greatly appreciated. Also grand high fives to this monthâs Eontologists:
Patrick Seifert, Jake Hart, Jon Davison Ng, Sean Dennis, and Steve! Become an Eonite by pledging your support
at patreon.com/eons. And thank you for joining me in the Konstantin
Haase Studio. If you like what we do here, subscribe at
youtube.com/eons.
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Cool Video. Little too much redundancy at the beginning but interesting nonetheless
That snowball earth hypothesis is so bizarre. I wonder if it could ever occur again over geologic time.
Ozarks!
Sounds like a female Mark Rober