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Practice English Speaking&Listening with: Lec 31 | MIT 7.014 Introductory Biology, Spring 2005

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So, for today's lecture as you can see up there is molecular -- 00:00:08

evolution, and ecology. 00:00:16

And what I mean by this, it's basically the study or

what we try to figure out in molecular evolution and ecology

is what genes or gene sequences can tell us about the evolution

and ultimately also the ecology of organisms in the environment.

And it's particularly relevant for thinking about

microorganisms, prokaryotes and the

environment.

And I hope I can actually convince you today of that.

This is interesting.

The topics that I want to cover today is, first of all,

I want to review a little bit what we know about life on

Earth, sort of give an overview of the evolution of life on

Earth.

Then, I want to go into specific topic that's of

particular relevance for the evolution of eukaryotes.

That's the endosymbiosis theory.

And then I'll explain how we can use gene sequences to

actually reconstruct events that have happened a very,

very long time ago.

OK, so we'll look at what we call molecular phylogenies,

with the use of gene sequences to reconstruct the evolutionary

history of organisms on Earth.

Derived from that, we'll look at what we call the

tree of life.

That's sort of the big picture overview of the evolutionary

relationships of all organisms on the planet.

And then finally, I'll introduce you to a topic

called molecular ecology.

Again, that's how we can use gene sequences to learn

something about the diversity of microorganisms in the

environment that lead us then, next time, when I come back on

Monday, into this big topic of environmental genomics,

how we can actually expand this analysis to learn much more

about organisms in the environment.

So, first of all, let's look at life on Earth.

Does anybody know how old we think Earth is?

Say again?

Yeah, 4.5 to 4.6,

I haven't my notes 4.6.

So, Earth's thought to have originated about 4.6 billion

years ago.

When did the first solid rocks appear on earth?

So, when was the surface kind of solidified?

Anybody know?

About 3.9 billion years ago,

OK?

And when do we think life started to develop on the

planet?

Any ideas?

Take a guess.

Two?

One? 3.5 billion years ago,

OK?

So, this is really remarkable.

We think it didn't, I mean, of course it took a

long time because were talking about millions of years and

hundreds of millions of years, but still, if you look at the

big picture, it didn't actually take life that long to evolve on

the planet.

So, why do we think that is the case?

What's the evidence for that?

Well, we look into sedimentary rocks, so old rocks that arose

from sediments, what you find around this time,

you find that chemicals start to appear, organic molecules

that really resemble organic molecules in modern life.

So, we have sort of chemical tracers, or chemical fossils. 00:04:47

So, tracers that indicate the presence of organisms.

But what we also find is so-called micro-fossils,

and I have a picture of that here where when you actually

take rocks and actually slice them into very,

very then slices, you can put them under specific

microscopes.

And what you then find is that many rocks that are very,

very old, have those kinds of inclusions in them.

And these things really resemble very much modern

prokaryotic cells, modern bacterial cells,

for example.

And so, those micro-fossils are generally taken as an

indication, also, that life is already present

during those times.

Now, when we take a quick sort of overlook of the evolution of

life on the planet, again this graph here

summarizes sort of the last 4.6 billion years or so when life

originated.

We see that there was a period of chemical evolution,

and then somewhere here that region, it's,

of course, not really well understood when that exactly

happens, the origin of life is placed.

But I want to alert you to a couple of really,

really critical steps here that are shown on this graph which

we'll actually talk more about.

It is thought that life very early on is split into three

major lineages: the bacteria,

the archaea, in what is called here nuclear

line.

And I'll come back to that in a minute or so.

Then, a further major event which you may remember is

oxygenic photosynthesis actually evolved --

-- which means that cyanobacteria evolved that

started to produce oxygen as a byproduct of photosynthesis.

And that really fundamentally changed the chemistry of the

Earth.

It actually became an oxidizing atmosphere.

And what you see here is, once the oxygen concentration

goes over a certain level, it allowed the development of

an ozone shield.

Now, what does that mean?

What was the critical significance of the presence of

an ozone shield?

Does anybody know?

What does it block out?

Anybody remember that?

What's the big significance of the ozone hole over Antarctica

for example?

It allows UV radiation to heat the Earth's surface,

and in fact if there were no ozone, the UV radiation would be

so strong that there would be no life possible on land.

So, once the ozone shield actually developed,

organisms could conquer, basically, the land's surface

and settle on the land surface.

In this, then, is thought to be at least

correlated with the development of endosymbiosis.

And I'll explain what I mean by that.

But it basically led to the origin of modern eukaryotes,

so your ancestors essentially.

But there was still a long time, obviously,

until humans appeared.

We have here the origin of animals and metazoans,

and then the age of the dinosaurs is already a very

small blip here on this graph.

And humans don't even get featured on that because we are

so recent.

So, but what I want to show you here is that three major

lineages evolved early on.

These are the bacteria, archaea, and what we call a

nuclear lineage.

And the significance of those nuclear lineages is that it

basically combined with bacteria to form the modern eukaryotic

cell.

So, the eukarya, or eukaryotes they're also

called.

And it was this combination that we called the endosymbiosis

event.

I want to explain this a little bit more, and then I'll show you

finally why we actually know that those things are very

likely to have occurred a long time ago.

Yes?

It means the bacteria and the nuclear lineages combine to form

a eukaryote, OK?

And I'm actually going to explain this on the slide here.

So, if you have any more questions after that,

please let me know.

So, again, this shows you this early evolution,

this early split in two archaea, bacteria,

and this sort of nuclear line.

It is thought that this nuclear line, this was single celled

organisms that increased in cell size, and then developed or

partitioned the DNA into a nucleus, basically.

So exactly how you find it in modern eukaryotic cells.

But then what happened is the cell took up a bacterial cell,

and over time this bacterial cell became symbiont.

In fact it became the mitochondria.

And so what this mitochondria now does in the moderate

eukaryotic cell as you all know is it really took over the

energy metabolism.

So, the proto-eukaryotic cell took up a heterotrophic bacteria

that form the mitochondria.

And this ultimately then gave rise to protozoa and to

modern-day animals.

But there was a secondary symbiotic event.

This cell, once it had taken up a heterotrophic bacterium,

it took up an autotrophic bacterium, a cyanobacterium,

an oxygenic photosynthesizer.

And this actually that led to the development of modern algae

and modern plants.

So what we can say is that mitochondria our ancient

heterotrophic bacteria -- 00:12:13

And the chloroplasts are ancient cyanobacteria,

so, oxygenic, photosynthetic bacteria.

And these obviously have coevolved to then form animals

and finally your plants.

So now, obviously we are talking here about events that

happened a very, very long time ago.

And so, the big question is really how do we really know

this?

But this takes me to the third topic, which is that of

molecular evolution.

So, we can state the problem again,

And that is very simply put, evolution is incredibly slow,

OK?

And therefore, its processes are not directly

observable. 00:13:47

And we need to actually use inference techniques to

reconstruct evolutionary processes.

Now, what do we use when we want to reconstruct the

evolutionary history of animals and plants usually?

Anybody?

Fossils.

Exactly.

So you take a shovel, essentially,

and dig down into the different layers.

And there's different techniques that you can actually

determine the age of different sedentary rocks.

For example, and then you can construct,

if you're lucky, you'll find enough fossils of a

particular lineage.

You can reconstruct the evolution of the lineage.

I'm sure you all have seen the example of the horse,

for example, where we have actually quite

good evidence when ancient horses look like.

And we can reconstruct the sequence of events that led to

the evolution of modern-day horses.

Now, you can imagine, though, that when we talk about

such ancient events like these there really is no fossil

record.

OK, so what people have figured out, then, is that that was

really a stroke of genius that came about in the late 60s,

that DNA molecules can act as evolutionary chronometers. 00:15:00

OK, now what do I mean by that?

I mean that you can take DNA sequences or gene sequences from

different kinds of organisms.

Based on those gene sequences you can reconstruct the

relationships to each other.

You can determine whether two organisms are closely related or

whether they are only very distantly related.

And the underlying mechanism of that, is that mutations happen

with a certain probability all the time.

So, the idea is that as time passed on, DNA molecules will

change.

So they will accumulate, actually, mutations,

and so this will lead to, and that the idea is that the

amount of change in a particular DNA sequence is proportional to

the time of separate evolution of two different lineages or two

different organisms.

So, the amount is more or less proportional -- 00:17:26

-- to time since the last common ancestry. 00:17:42

So, let me explain how this is actually done.

What you really need in order to do this, is you need genes

that are related to each other, OK?

So, genes, they need to be universally distributed.

That meets all organisms that you want to compare need to have

this type of gene.

And, those genes need to have conserved function. 00:18:41

In these genes, we can then compare to each

other, and I will explain how this is actually done.

Any questions so far?

OK, so the example that I actually want to bring is the

16S ribosomal RNA genes. 00:19:09

We oftentimes abbreviate this rRNA.

Now, does anybody remember what the ribosomal RNAs are and do?

What's the ribosome?

Yes?

Right, and what does it do?

Exactly, it's the location where messenger RNA is

translated into protein.

Now, the ribosomal RNAs are an integral part of the ribosome.

They play both a catalytic role as well as a structural role in

the ribosome.

And so, fundamentally, because this is such a

fundamental organelle, all living organisms possess

it.

So, all organisms have it.

So this allows us to use these genes to really compare all

living organisms to each other.

OK, so this is a very important point.

I wanted to show you a, OK, if it wakes up.

There we go.

An example of these ribosomal RNA genes, now this is actually,

what you see here is a secondary structure of the

actual RNA, the ribosomal RNA.

Now, these molecules have a secondary structure because they

play a catalytic and structural role.

And so, the really amazing thing is when you look at the

structure, the structure determines really the function

of those molecules in different organisms.

And then look at this.

We have here a bacterium, and here are an archaea.

Now, if you think back to the first couple of slides,

what I showed you is that those organisms have not shared a

common evolutionary history for about four, or so,

billion years, or 3 billion years,

excuse me.

But, if you just glance very quickly at the structures,

you see that they look very similar to each other.

So, there's an indication that the function is really very

highly conserved of those molecules.

However, when you actually look at the sequences in detail,

what you'll find is that there's different regions.

And I'd given some examples here denoted by A,

B, C in those molecules.

And these different regions of the molecules are really the key

to its usefulness in figuring out the evolution and ecology of

many organisms.

The region number A here, or denoted by A,

a sequence stretches that are the same in all living

organisms.

So they are universally conserved, which means that if

you get a mutation in a gene in that particular region,

you are dead.

OK, that's why it's conserved essentially.

Then we have those regions B where the length is conserved,

but the sequence is not.

So, there are sequence change allowed, but the length needs to

be conserved.

And then there's the region C were neither length nor sequence

is actually conserved, and where we get a lot of

variation.

So, let me write this down.

We have three types of sequence stretches. 00:22:49

We have A, what I called the universally conserved sequences.

We have B where length, but not sequence is conserved.

And, we have C where neither length nor sequence is actually

conserved. 00:23:33

And the first two stretches, the first two types of sequence

stretches, are very important in figuring out the phylogeny or

the evolutionary relationships amongst organisms.

Whereas the sequence stretches number C because they vary so

dramatically, are very important in

identifying organisms.

And we'll talk more about this actually next time.

So what can we actually know do with those sequences?

Well, the first step is we need to generate an alignment. 00:24:29

OK, and this is actually shown here, where each row denotes a

gene from a particular organism.

OK, so these are all abbreviated here.

These actually aren't ribosomal RNA genes, but other genes.

And that what you will see here is we can recognize those three

different regions that I've pointed out before.

You have the regions A which tell you which nucleotides line

up with each other, so you use this sort of as an

anchor because the sequences never vary amongst organisms.

And that the sequence region B where you light up sequences

that vary or stretches that vary in sequence but not in length.

Now, why is this important?

It's important because you have in each column that nucleotides

that have originated from a common ancestral nucleotide,

and whose variation over time you can actually monitor.

Is everybody with that?

Any questions?

OK, great.

The second step, then, is the calculation of a

similarity. 00:26:04

And this is shown here.

Again, we have a very simplified alignment now of four

different organisms.

Here, we have the sequences that we want to compare.

And what you'll see is that they're overall very similar,

but there are different sort of nucleotides.

And so, what we simply do is for each pair of sequence

combinations, we calculate the sequence

similarity value.

So, what you see is that you have 12 nucleotides,

and the first pair differs in three nucleotides.

OK, so that tells us, or it's called actually a

distance here, I'm sorry.

Let me write this down here. 00:27:01

It's simply one minus the similarity, of course,

but so basically a quarter of the nucleotides differ where

it's between A and C, a third of the nucleotides

difference on.

OK, so you do this for each pair of sequences,

excuse me.

The third step, then, is to calculate the

correction for multiple mutations affecting the same

nucleotides. 00:27:54

Now, you can imagine that over time there's a probability that

a particular nucleotide mutates, say, twice.

So, in the first instance it may change from A to a G,

, but then it changes to a C.

But when you look at the modern-day sequences,

you don't know that this actually happened.

And so there's ways to statistically estimate what the

likelihood is that a sequence actually contains such multiple

events.

OK, and this, we called, a corrective

evolutionary distance then.

And what you will note is that the corrected evolutionary

distance is invariably larger than the actual observed one.

Now, what can we can do with those distances?

We can constrain them into a best fit tree of relationships.

So, we can draw what we call is a best fit tree.

That's shown here.

We have our four organisms, but when you look at those

branches of the tree what you'll see is that they add up roughly

to the correct evolutionary distance here.

So, between A and B we have 0.23 and 0.08,

which roughly gives you 0.3 here, OK, whereas between A and

C the tree is constrain such that we have 0.31,

and here 0.15, and so overall you roughly get

the distance here that we have calculated.

And so what this means is that you ordered the organisms by

their calculated evolutionary distance.

And so you have now obtained, actually, a very intuitive

picture of the relationship of organisms to each other where A

and B are obviously the most closely related ones,

and A and D are the most distantly related.

Is everybody with it?

Any questions?

OK, now, this best fit tree is what we call a phylogeny. 00:30:31

Now, excuse me, these techniques really

revolutionized the study of evolutionary relationships,

and one of the things that it allowed us to do is to construct

universal phylogenetic trees or what we can also call the tree

of life.

And I will show you this on the next slide, and that I want to

make a few general statements about this.

So first of all, when you analyze all known

organisms, and obviously that would be a big task,

but representative of all known organisms, what you'll find is

that, indeed, we have three major lineages:

the bacteria, the archaea,

and the eukarya.

OK, so we have what we call three domains of life:

the archaea, bacteria, and the eukarya.

So, this really is the evidence that life really split very,

very early on into those three lineages that I showed you

before.

Interestingly, two of those major domains here

are prokaryotic, OK?

So, two of the domains are prokaryotes.

Moreover, if you actually look at the types of organisms that

are on here, you'll notice that even on the eukaryotic side of

the tree, most of the organisms here are actually microbial.

So, the single celled organisms: and that means that

most of the life on the planet is microbial.

The vast diversity of organisms on the planet are

microorganisms.

So, we can say that most life is microbial.

And when you, then, look at analysis of

mitochondria, and chloroplasts which all have

their own genetic machinery, and therefore also their own

ribosomes you'll see that the mitochondrion,

OK, and the chloroplasts both tree within the bacteria.

So, we really have an amazing confirmation of this

endosymbiont theory which actually developed in the

absence of gene sequences by some Russian scientists in the

early 20th century.

So, we have that mitochondria and chloroplasts tree within

bacteria, and this really supports the endosymbiont

theory.

So really, you could say eukaryotes are really just

walking, and swimming, and flying incubators for

bacteria, right?

So, just hosts for microorganisms.

OK, so basically you can, what you should take home from

this is the three domains of life.

Two are prokaryotic, and even more so most of the

diversity that we find is actually microbial,

and then finally the endosymbiont theory is actually

confirmed by those phylogenies.

Now, what I want to cover in the remaining time,

is how we can actually use now those sequences to learn

something about organisms in the environment.

That's the topic of molecular ecology. 00:35:32

To introduce this, I just want to show you a

couple slides that really sort of capture what the big problem

is that we're facing here.

Now, when we look at the abundance of prokaryotic cells

in different types of environments,

what we see is that there is an enormous number of different

prokaryotes out there.

This summarizes, here, different types of

environments.

We have the marine environment, freshwater environment,

sediment and soils, subsurface sentiments and

animal guts.

And that this number here gives you the average number of

prokaryotic cells either per milliliter or per gram.

And it here we have the total number of cells obtained by

multiplying the average number with the total volume of the

particular environment.

So what you can see is that in the marine environment,

we have an average half a million cells per milliliter of

water, OK?

It freshwater, we have about a million cells.

What is that telling you?

There's a ton of prokaryotes out there.

What you go swimming, you take a little gulp of

water: you've probably eaten several million prokaryotes,

that it's nothing to worry about because what this also

tells us is that very, very few prokaryotes out there

are really pathogens because otherwise you'd be sick all the

time.

Now, in sediments and soils, in as little as a gram you have

five times 10^9 prokaryotic cells almost.

5 billion prokaryotic cells are out there, and even in very,

very deep sediments that reach down to 3,000 m,

you have a substantial number of prokaryotic cells.

Well, and here's your guts, 10^5 times 10^6 gives you 10^11

per gram.

So again, you're just a walking incubator for a very complex

microbial community.

Here's the global abundance.

You see that steeps of surface sediments and the marine

environment, probably in terms of numbers at least,

the most important microbial environments.

Now, faced with this enormous abundance of prokaryotes out

there, very important question is how many of them are out

there?

Or, how diverse our prokaryotes in the environment?

That's important if you want to figure out their function and

the environment, and want to understand also

their evolution.

And what I want to show you here is that we've gone through

an amazing development in our understanding of prokaryotic

diversity in the environment over the last 10 to 15 years or

so.

Who knows about E.O.

Wilson here?

One person?

So, he wrote a very famous book on biodiversity,

which was published in 1988, where he tried to summarize,

really, how diverse the known organisms are on the planet it

also try to extrapolate to the total diversity.

And what you see is that he came up with about 1.4 million

different species here, mostly dominated by insects.

That's the big section here on this pie chart.

The plants: very important.

And if you look, the prokaryotes feature with

about 3,500 different species.

So, in 1988 we thought there were very few prokaryotic

species out there.

If you look about 10 years into the future and take the

assessment here, and this just exemplifies how

the thinking has changed, you see that we think now that

there is about 11 million different species out there,

and that the vast majority of them are prokaryotic,

OK, 10 million.

So, this big part of the pie chart is really the prokaryotic

diversity.

Now, what really has changed is that we've actually started to

use molecular techniques to determine the diversity of

prokaryotes in the environment.

So molecular ecology is really the use of molecular gene

sequences obtained directly from the environment -- 00:40:29

-- to learn about the diversity prokaryotic -- 00:40:46

-- diversity out there.

Now, this slide just quickly summarizes this.

Basically, the idea is that you go out into the environment and

collect either water or soil samples that,

as I just showed you, invariably contain a lot of

different prokaryotic cells.

You then lyse the cells and purify their DNA.

And so that you end up with a mixture of DNA that represents

the organisms out there, and then you can use universal

PCR primers to actually amplify ribosomal RNA genes from all the

organisms that are present in your samples.

Now, why can you use universal PCR primers?

Well, they target the regions number A that I showed you

before.

Those regions in the genes are invariant amongst all organisms.

You guys all remember how the PCR works, right?

We cover this.

OK?

Yes?

No?

Who doesn't?

You don't?

All right, come to the board.

Just kidding.

OK, you should look it up.

I don't have time to cover this, unfortunately,

but basically it's a technique that allows you to amplify

specific types of genes millions to billion fold.

And once you have done this, what you can do is that you can

purify the genes on gels, and then separate them by

cloning them into individual plasmids.

And those plasmids have been inserted into E.

coli cells, and the E. coli cells are then

individually grown up so that each culture contains only a

single plasmid, and you can then sequence these

ribosomal DNAs or ribosomal RNA genes from those clones.

And so, you have obtained a library of the ribosomal RNA

genes from the environment.

So, we use environmental ribosomal RNA gene libraries

from which we then can actually compare how many different types

of genes are out there.

So let me show you an example of this.

What we have done recently, we've gone out in one of the

first really comprehensive samplings of coastal bacteria

plankton, which means the bacteria that are present free

living in ocean water.

And so, we've done this, we've collected all those

clones, and then basically we constructed those phylogenetic

trees that I showed you before that really allow us see how

many different types are out there, and how closely related

they are to one another.

And what we found is that in this environment that you think

might be very simple because it just the water column right?

No, not much structure in there.

We found over 1500 bacterial 16S ribosomal RNA sequences to

occur, so an enormous diversity of prokaryotes of bacteria in

that particular environment.

And the important point is that when you actually look at a

collection of such studies that I just showed you,

what you find is that the vast majority of microorganisms in

the environment have never been cultured.

So traditionally what we do of course to learn about

microorganisms when you grow E. coli, or so,

you throw them onto culture plates.

You make lots of different cells, and that allows you to

study some of their properties.

But when you look, for example,

at results from the ocean, this summarizes now coastal and

open ocean environments, again, the bacteria plankton is

those free-floating bacterial cells in the water.

And you compare this to what we've actually been able to

culture from those environments.

What you see is that you have some dominant groups here.

They have all funny names, most of them,

because they're just clones and clone libraries.

But these are the dominant groups that show up in clone

libraries.

Here's their relative representation in different

clone libraries from a variety of environments.

And so here you have one very important one,

the SAR11 group, or this one,

the SAR86, that always show up in clone libraries.

But we've never see them in culture, so the important point

to realize here is that what is actually happening is that

whenever we go out, we find a great diversity of

bacteria out there, but we have no idea what they

actually do.

And this is one of the big questions that we need to answer

to understand, really, how the planet actually

works.

What are those uncultured microorganisms out in the

environment really doing, and what is their importance?

And we'll talk about this next time.

We're going to talk about environmental genomics because

essentially what we can do now, is we have techniques available

that allow us to isolate and least large fragments of the

genomes, sequence those, and look at what kinds of genes

they have present.

And that allows us, then, to infer some of their

function in the biogeochemical cycles in the environment.

OK, so with this I'm going to close today unless you have any

more questions.

The Description of Lec 31 | MIT 7.014 Introductory Biology, Spring 2005