CH 25 History of Life on Earth 1 1 start 11min 3s 10ms

Hi, everybody. Welcome back.

Today we're covering the content

that is in Chapter 25
of your textbook,

and this chapter largely covers
some broad patterns

with regard to the history of life
on the planet.

When we were together
last time,

we were looking at mechanisms

that could promote speciation,
right?

We talked
about allopatric speciation

and sympatric speciation.

You know,
today we're going to look at, again,

some broad-scale events
that occurred

over the history of life
on the planet

that include things
like mass extinction

and the phenomenon
that we call adaptive radiation

where we see many,
many species show up in--

in the fossil record.

And yeah, a lot of what we know,

with regard to what
we're going to talk about today,

comes from an exploration of

and interpretation
of that fossil record,

Starting
with this slide right here:

this is a amazing photo
of a skeleton of a whale

that was discovered
in the Sahara Desert.

So, you might be wondering,
well, how did that happen?

Researchers were--
were knowing where to look

when they were--
when they were trying to figure out

what are the origins
of marine mammals, for example.

And so, due to conversations
with geologists about,

you know,
where we might find fossils

of-- of particular creatures
from a particular time

in the history of life on Earth,

and other patterns of--
of events that--

that led researchers to predict

that they
might actually find whale bones

in the--
in the desert of the Sahara.

And, in fact, they did.

So, that's just one example
of some of the work

that paleontologists do.

Paleontology is the study
of the fossil record.

So, yeah, let's go ahead
and get started

building on the work that--
that we have learned

from paleontologists today.

So, again, when we
use the word macroevolution

now we're really talking
about broad patterns of evolution

that--
that are above the species level.

So, we're looking at groups
of organisms.

And when we look in the fossil record,
we do see some trends.

You know, we see the emergence,
for example,

of terrestrial vertebrates.

We see the emergence
of other groups of species as well,

that I'm going to share
with you today.

We also see
that mass extinctions occurred.

And then there's been, you know,

there's been-- that has affected

the evolutionary trajectory
of other species.

So, we'll talk about that today.

And then we'll focus
on some key adaptations

such as flight, for example.

So, when these new adaptations
arise,

it allows for what we
call "adaptive radiation".

I'll talk about that today
as well.

The possibility
for many new species

to emerge
over a relatively short period of time,

and I'm talking geologic time.

So, you know, short is relative here
in this conversation today.

But, yeah, when you
have a novel character that arises,

with the ability to fly,

that promotes the possibility
for the--

for a species
that has that particular character

to diverge into many other species

that include things
like mass extinctions,

and the phenomenon
of what we call adaptive radiation.

that the first thing that probably happened was number 1 here,

Abiotic meaning non-living, right?

Abiotic synthesis of very small organic molecules,

probably monomers of molecules.

Proto- meaning first, these-- these precursors to modern cells.

All right, let's take a look at each one of these in detail today.

according to that sequence of events

that I shared with you previously

is the abiotic synthesis of organic molecules.

And researchers in the 1950s were curious

well, what did planet Earth's atmosphere

look like at the time? Let me back up a minute.

We think that the planet formed about 4.6 billion years ago,

There was-- it was constantly being bombarded

by rocks and debris, and it was a very hot environment.

But about 4 point-- billion years ago,

4 billion years ago,

So, regardless of that,

this experiment right here shows you an apparatus

that was set up by a grad student

from the University of Chicago in 1953.

His name was Stanley Miller.

He and his-- his advisor worked on this project

where they-- they attempted to simulate

what they thought was the atmospheric and oceanic conditions

up on the planet 4 billion years ago, to see if they could

get the abiotic synthesis of organic molecules.

as they occupy new habitats that are available to them

because of that character that emerged.

So, yeah, we'll talk about each of these in detail today.

So, what you see in this apparatus

is a container that might simulate the ocean.

All right, if we're gonna have a conversation

about the history of life on Earth,

we might as well start at the very beginning.

So-- So, one of our big questions is

what is the origin of life?

How did life ever get started on planet Earth, right?

And so, I'm going to share with you some evidence

that supports the idea that the origin of life

occurred via these sequential steps that you see in my slide here.

So, it makes the most sense to us,

and the data support this idea,

abiotic synthesis.

And then, finally, polymers.

The joining of those together

to make those polymers probably occurred.

And then, at some point, those--

those molecules were probably captured inside

what we colloquially call, "protocells," right?

And then lastly,

of self-replicating molecules,

similar to what we see today, right,

self-replicating DNA and RNA.

if that-- if they could get that to occur.

And, you know, the conversations at the time were,

but for that first half a billion years,

so from 4.6 billion years ago to 4 billion years ago

the planet was probably not conducive

to life ever forming on the planet.

the planet cooled off, the seas formed,

and the environment was--

you know, the atmosphere, we don't know exactly

what it looked like,

but we have some indication

that there was methane in the atmosphere,

and there was ammonia in the atmosphere,

and there was hydrogen gas in the atmosphere.

And, whether or not it was a a reducing environment

or an oxidizing environment.

Not sure.

That refers to whether--

you know, today we're living in an oxidizing atmosphere, right?

There's oxygen gas in our atmosphere that will readily oxidize

other compounds, right--

steal electrons away from-- from other compounds.

There was some indication recently

that the environment was, in contrast to that,

a reducing environment full-- full of hydrogen gas,

like you see here, h2,

that would donate electrons to compounds.

And, you know, we know from volcanic activity in the ocean

in a matter of months.

that there are areas where it's-- it's very hot.

Three or four months later,

So, they-- they simulated that,

they found in their sample, when they sampled it for chemical analysis,

you know, providing thermal energy.

And then, you know, some of that water

would, of course, evaporate.

And this part of the chamber, here,

they found amino acids, amazingly enough.

is kind of representing what we think were atmospheric conditions.

So, this did represent,

Here's methane, here's ammonia, and here's hydrogen gas.

you know, the phenomenon that abiotic synthesis

He simulated lightning

with these electrodes here.

Again, providing energy.

of organic molecules can indeed occur.

And then, as that water vapor cooled--

here's a condenser here.

Input cold-- cold water to cool it off

This was an exciting moment

to simulate a cooler atmosphere.

because it set the stage for--

And then as that water condensed,

he sampled it from time to time.

And, honestly, his graduate advisor

you know, set the stage chemically

actually thought that there was no way

for the conditions for life.

that they were going to get any kind of

Another burning question, so to speak,

organic monomers anytime soon.

You know, we thought that, you know,

if this happened on the planet 4 million years ago,

how many million years did it take

that we have is, well, where did life originate on the planet?

to get synthesis of these organic molecules?

But, lo and behold, they actually got results

A lot of interested-- a lot of interest is being paid

to these alkaline vents that are in the deep sea.

Here's a picture of one of these vents in the slide here.

These vents release water with a very high pH;

nine, ten, eleven.

So, they're considered alkaline vents.

And also very warm water, 40 to 90 degrees C.

And the conditions in these vents

were probably very likely suitable

for the formation of some of these organic compounds.

And, indeed, researchers have looked at the surface

of the structures that formed these vents

and found organic molecules attached to those vents.

So, maybe this is where life arose.

Other people are very interested in looking at meteorites.

Meteorites may have been another source of organic molecules.

For example, the fragments of a meteorite

called the Murchison meteorite,

has been discovered to contain more than 80 amino acids

and other key organic molecules,

including lipids, some sugars, also some nitrogenous bases.

So, maybe these are the-- maybe we can--

maybe we can consider that that is

where we got these first organic molecules

is from the meteorites that are bombarding the planet.