Hey!
Kallie here.
Today’s episode was made in collaboration with the Smithsonian National Museum of Natural
History.
Blake and I were lucky enough to visit the museum's Deep Time Hall during its renovation
and that’s not all!
On Friday June 15th, I will be back in the Deep Time Hall, hosting a livestream
We’ll be getting a behind-the-scenes tour of the exhibit and an expert from the Smithsonian
will be answering your questions.
More information on where to watch the stream will be in the description.
Now let’s talk about evolution.
The story of life on Earth is a story of change.
Living things have changed the atmosphere and the climate.
They’ve endured the movements of the continents, and the rise and fall of the seas.
And they’ve responded to these changes, over the long course of Earth’s history,
through a process that still continues today: evolution.
This powerful force is, in the simplest terms, just change over time.
And it’s responsible for the shape of the tree of life, and for generating the diversity
that we see in the fossil record as well as in modern ecosystems.
It’s the very foundation of our understanding of biology, and it continues to help us make
sense of the world around us.
As a scientific concept, evolution was revolutionary when it was first introduced.
Charles Darwin and Alfred Russell Wallace were the first to put all of the pieces together
into a unified explanation that would radically alter our understanding of life on our planet.
But our understanding of evolutionary theory didn’t stop there.
We’ve learned a lot -- and we’re still learning.
In the last 160 years, we’ve learned what Darwin and Wallace didn’t know, and we’ve
figured out a lot about how evolution actually works - like how it can produce the incredible
array of animals you see here, and how we know they’re all related.
When the Smithsonian opened its first exhibit of fossil animals in the early 1900s, it was
called the Hall of Extinct Monsters.
Today, Kallie and I are in a space that’s completely renovated and re-imagined:
the David H. Koch Hall of Fossils: Deep Time, also known as the Deep Time Hall.
And it depicts, more vividly than ever, the staggering variety of animal forms that have
arisen and disappeared over time.
A monument to the fact that, as Darwin himself put it, “endless forms most beautiful and
most wonderful have been, and are being, evolved.”
Charles Darwin and Alfred Russell Wallace were both British naturalists whose thinking
about the natural world was deeply shaped by long voyages of exploration.
Darwin famously traveled to South America and the Galapagos Islands, and Wallace went
to South America and Southeast Asia.
And together they observed an incredible diversity of life.
They saw first-hand how very similar organisms seemed to be slightly modified in ways that
made them ideally suited to their environments.
For Darwin, he saw this in the different shapes in the beaks of finches on the different islands
of the Galapagos archipelago.
For Wallace, it was the differences between monkeys living on different riverbanks in
the Amazon.
And they both realized that the patterns they observed meant that these species all probably
arose from the same place - a common ancestor.
The bodies of these animals, they realized, had been shaped over time by the conditions
in their environments, resulting in the different forms they found on different islands and
riverbanks.
But, in addition to being well-traveled, Darwin and Wallace were also well-read.
And their ideas were deeply influenced by other, earlier thinkers, in natural history,
geology, and even economics.
Scholars like Georges Cuvier, Charles Lyell, Jean-Baptiste Lamarck, and Thomas Malthus
helped establish the ideas that were critical to evolutionary thinking -- namely, that the
Earth was very old, that species seemed to change and go extinct over time, and that
individuals competed over limited resources.
Darwin and Wallace used these insights -- along with their own observations -- to both arrive
at the same mechanism by which species evolve: natural selection.
In a paper read to a meeting of scientists in London in 1858, they presented their theory
of natural selection based on a series of principles:
The first key idea was that, in a population of living things, natural variations will
occur, and as a result of those changes, some members of the population will survive and
reproduce more than others.
Then, they posited that those that survive and reproduce will pass on their traits to
their offspring.
And this meant that traits that give individuals an advantage in a certain environment will
get passed on more often.
And as a result, more members of the population will have that trait.
Therefore, gradually and over time, this will result in certain traits showing up more or
less often in a population.
Today, when this series of events happens within a species, we call it microevolution.
It’s how a single species responds to changes in the environment.
On a broader scale, we call it macroevolution.
This is how these changes accumulate over long periods of time to produce entirely new
body plans, new species, and the grander patterns of diversity in the tree of life.
And one of the most incredible things about the development of the theory of evolution
by natural selection was that Darwin and Wallace didn’t have a good explanation for how traits
were passed from parent to offspring.
Genetics as a field was still a long way off, and neither of them were aware of the experiments
that were being done on pea plants at the time, by a Czech monk named Gregor Mendel.
In the 1850s, while Darwin and Wallace were putting all the puzzle pieces of natural selection
together, Mendel was breeding peas at his monastery to try to figure out how heredity
worked.
And he figured out that traits didn’t simply blend together when living things reproduced.
Instead, only some were inherited as discrete traits by different numbers of offspring.
Mendel’s results were rediscovered around the turn of the 20th century, when a new generation
of biologists was investigating genetics.
And it was this new wave of researchers that brought our understanding of evolution to
the next level.
One of these scientists was American biologist Thomas Hunt Morgan.
Instead of peas, he bred flies, and in 1910, he bred a fly with an odd trait.
It had eyes that were white, instead of red
What’s more, he was able to breed that white-eyed trait back into the parent population.
Morgan had discovered another key driver of evolution by natural selection: mutation.
He realized that the fly had undergone a random change in its genes that made it different
from the rest.
So Morgan theorized that mutations were a source of variation in living things - and
that it was the source of the variation that natural selection acted on.
Beneficial mutations would be passed on, he thought, and detrimental ones would eventually
disappear.
So by the early 1900s, we’d already recognized two of the four major forces of evolution:
Darwin and Wallace gave us natural selection, and Morgan brought mutation into the mix.
It wasn’t until the 1920s that things would really start to come together through the
work of three of the founders of the field of population genetics: Ronald Aylmer Fisher,
John Burdon Sanderson Haldane, and Sewall Wright.
Fisher and Haldane both looked at natural selection mathematically, especially in large
populations, using Mendel’s ideas about inheritance to figure out how often and how
fast natural selection worked on variations.
It was Haldane who did the math that explained the transition of England’s famous peppered
moths, in which a gene for dark color spread quickly, as pollution darkened the bark of
the trees they lived on.
Studies like this led Fisher and Haldane to conclude that natural selection acted slowly,
but also uniformly, in large populations.
Meanwhile, in the US, a geneticist named Sewall Wright was thinking about how evolution worked
in smaller, more isolated populations.
He did some research breeding animals like cattle and guinea pigs.
But it was his mathematical studies of genetics that led him to uncover another key idea:
genetic drift.
This is the idea that the frequency at which certain genes appear will sometimes change,
totally by chance, and randomly, and Sewell found that this has a greater effect in smaller
populations than in larger ones.
Another, somewhat related, idea that came up around this time, in the late 1930s, is
gene flow - the movement of genes between populations, by way of migration.
So, when members of one population of a species -- say, panthers from Texas -- breed with
members of another population -- like panthers in Florida -- that will change the makeup
of the gene pool in the Florida population.
And this, too, is a driving force of evolutionary change.
Together, the work of Fisher, Haldane, and Wright showed that natural selection acting
on genes was the most likely explanation for how evolution works
And in 1937, another biologist brought together all of the evidence from genetics and natural
history to show how evolution by natural selection could produce new species.
And this enabled us to make the enormous conceptual jump from microevolution to macroevolution.
His name was Theodosius Dobzhansky, and he had worked in Hunt’s fly lab.
He’d found that fly populations from different countries seemed to be genetically different,
even though they were considered to be the same species.
But, these flies weren’t so good at reproducing with each other.
So he wondered if they were actually different species.
And this took the scientific conversation all the way back to the 1800s, and the once-novel
idea that evolution could eventually, gradually produce new species.
From his experiments, Dobzhansky produced a theory about how new species originate.
Mutations happen naturally in populations, creating variations that can stick around
if they’re beneficial or just neutral.
And if populations are isolated, these variations can remain within a single group, with new
mutations popping up.
But none of these would spread to the rest of the species.
Over time, this would make one group genetically distinct from others, potentially causing
problems if it tried to interbreed with others.
And given enough time, it would lose the ability to interbreed with other populations entirely.
It would become a new species.
This was the beginning of “the Modern Synthesis,” a collaboration by many evolutionary biologists
of the time to explain large-scale patterns of evolution.
And while the Modern Synthesis has changed over time, it’s still the framework for
our current understanding of how evolution works.
In 1953, we added a better understanding of how genetics works, through the discovery
of the structure of DNA and how it functions.
So, now we know that mutations randomly happen when DNA is copied incorrectly during replication
- something Morgan didn’t know.
Now we also know that natural selection is only one of the mechanisms of evolution,
along with mutation, genetic drift, and gene flow.
And it’s this knowledge that allows us to witness -- first hand! -- microevolution taking
place today -- say, in studies of bacteria that develop resistance to antibiotics.
And it also helps us understand the story that the specimens around us right now are
trying to tell us, the story of macroevolution.
With this understanding, we can see how the aquatic mammal behind me, Pezosiren, is related
to the more recent Metaxytherium.
Separated by some 30 million years, these mammals lost their hind limbs and acquired
flippers instead of feet.
And today, their closest living relatives are the manatees and dugongs.
Places like the Deep Time Hall show us evolution at work, with specimens that take us from
the most ancient fossil ancestors, to transitional forms, all the way to the organisms we know
today.
In less than 200 years, scientific study has completely revolutionized our understanding
of the constantly changing nature of life.
We’ve been able to see how organisms are shaped by their environments to better survive
and reproduce there.
And we’ve learned that time is a key component of evolution.
This is why a deep look into the deep past is critical for our understanding how life
has changed over millions of years.
And, it’s why we’re so excited about the opening of the new Deep Time Hall
in the Smithsonian National Museum of Natural History in Washington, D.C.
If you can make it in person, pay them a visit!
And, if you can’t, follow them on social media to see some of the amazing specimens
now on display
And be sure to watch a new special about the evolutionary history of some of our planet’s
most fascinating animals.
When Whales Walked: Journeys in Deep Time premieres on PBS and Smithsonian Channel June
19th at 9 PM Eastern.
Check out the links in the description.
Thanks for joining me today in the Konstantin Haase studio.
And an extra big thanks to our current Eontologists: Jake Hart, Jon Ivy, John Davison Ng, and Steve