Nick Lane – Life as we know it is chemically inevitable
Nick Lane has some pretty wild ideas about the evolution of life.
He thinks early life was continuous with the spontaneous chemistry of undersea hydrothermal vents.
Nick’s story may be wrong, but I find it remarkable that with just that starting point, you can explain so much about why life is the way that it is — the things you’re supposed to just take as givens in biology class:
* Why are there two sexes? Why sex at all?
* Why are bacteria so simple despite being around for 4 billion years? Why is there so much shared structure between all eukaryotic cells despite the enormous morphological variety between animals, plants, fungi, and protists?
* Why did the endosymbiosis event that led to eukaryotes happen only once, and in the particular way that it did?
* Why is all life powered by proton gradients? Why does all life on Earth share not only the Krebs Cycle, but even the intermediate molecules like Acetyl-CoA?
His theory implies that early life is almost chemically inevitable (potentially blooming on hundreds of millions of planets in the Milky Way alone), and that the real bottleneck is the complex eukaryotic cell.
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Timestamps
(00:00:00) – The singularity that unlocked complex life
(00:08:26) – Early life continuous with Earth's geochemistry
(00:23:36) – Eukaryotes are the great filter for intelligent life
(00:42:16) – Mitochondria are the reason we have sex
(01:08:12) – Are bioelectric fields linked to consciousness?
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Transcript
Today, I'm chatting with Nick Lane, who is an evolutionary biochemist at University College London.
And he has many books and papers which help us reconceptualize life's four billion years in terms of energy flow and helps explain everything from how life came to be in the first place to the origin of eukaryotes to many contingencies we see today in how life works.
So, Nick, maybe a good place to start would be: why are eukaryotes so significant in your worldview of why life is the way it is?
Well, first, thanks for having me here.
This is fun.
I love talking about this kind of thing.
So, eukaryotes, what's a eukaryote?
It's basically the cells that make us up, but also make up plants and make up things like amoeba or fungi, algae.
So, basically, everything that's large and complex that you can see is composed of this one cell type called the eukaryotic cell.
And we have a nucleus where all the DNA is, where all the genes are, and then all those kind of machinery cell membranes and things.
So, there's just basically a lot of kit in these cells.
And the weirdness is, if you look inside a plant cell or a fungal cell, it looks exactly the same under an electron microscope as one of our cells.
But they have a completely different lifestyle.
So why would they have all the same kit if they evolved to be a single-celled alga living in an ocean doing photosynthesis?
It's still got the same kit that our cells have.
So we know that because they share all of these things, they arose once.
in the whole history of life on Earth.
There could have been multiple origins, but there's no evidence for that.
If there was, it disappeared without trace.
So we've got this kind of singularity, which happened about two billion years ago, about two billion years into the history of life on Earth, then this thing happens once that gives rise to all complex life on Earth.
And the one thing which I guess you could conclude from that is bacteria and archaea,
in terms of their genetic repertoire, they're actually, they've got a lot more genes, a lot more versatility than eukaryotes do.
It's just that a single bacterial cell has much less in it, but there's so many different types of bacterial cell that overall they've kind of explored genetic sequence space.
They had four billion years to have a go at that, and they never came up with a trick, which says it's not in the genes, it's not about information.
There's something else which is
controlling it.
And that's something, I think, is the acquisition of these power packs in our cells called mitochondria.
Now, let's go to the origins of life.
And you have this really compelling story where you imagine that the first life forms were continuous with Earth's geochemistry.
If you can recapitulate the story a little bit, and then I want to ask this question.
I mean, I'll tell you how I got there first, because I started out working on mitochondria, and that took me into the evolution of eukaryotes.
And eukaryotes acquire these endosymbiotes that...
that become mitochondria and they change the potential of evolution.
It doesn't change everything immediately, but it changes where the endpoints can be.
And it allows the evolution of these large, complex cells and eventually multicellular organisms and us.
So what modern mitochondria are actually doing, well, what they're actually doing is respiration.
They're generating energy for cells.
They're doing plenty of other things as well.
But the main thing we can think about is they're the energy producers.
And they're derived from bacteria, and bacteria produce their energy in exactly the same way.
They're generating energy by generating an electrical charge on the membrane.
And that charge, it's small, but the membrane is really thin.
So the charge is about 150 to 200 millivolts.
But the membrane is five nanometers in thickness.
So that's five millionths of a millimeter.
So if you shrank yourself down to the size of a molecule or stood next to that membrane,
you would experience 30 million volts per meter, which is equivalent to a bolt of lightning.
So
that's the strength of the force
of the voltage across the membrane, which is colossal.
And it's generated by really sophisticated proteins that pump protons across the membrane.
And then it's ATP synthase, which is again pretty much universal.
And it's a rotating nanomotor that sits in the membrane.
This is colossally complex, interesting machinery, and it's universally conserved.
It's as conserved as, say, a ribosome, the protein-building factor.
It's pretty much everywhere across life.
So you wonder how on earth did life come to be that way?
And if it's conserved universally across life, it looks like it goes right back to the common ancestors of all the cells.
And so
there's the question: how did it arise in the first place?
And that was actually for me tremendously thrilling because it's a way in as a researcher to the origin of life.
It says, how did these energy generating systems arise in the first place?
And
my way in was really, the gates were opened by Bill Martin and Mike Russell, who around the early 2000s were publishing some amazing papers together where they were saying that in this deep sea hydrothermal vent, vent, rather than it being like a black smoker with a chimney with smoke belching out of the top, it's like a mineralized sponge with lots of pores that are cell-like in their structure.
And you've got an acidic early ocean and you've got alkaline fluids coming out of these.
And you've got mixing going on in this whole system.
And so you could at least imagine that you've got a pore in here, which is a bit like a cell in terms of its size and its shape.
And on the outside, you've got acid ocean waters percolating in.
And on the inside, you've got these hydrothermal fluids.
So you've got a barrier, you've got an inside and an outside, and you've got more protons outside coming in, potentially driving work.
So, it's very much like a cell is structured.
And the other thing is,
what are these minerals?
You've got these mineralized sponge that pours with minerals.
Well, the minerals we think on the early Earth would have been a lot of metals in there.
So, things like iron sulfide or nickel sulfides and things like that.
Now, the reason that's important is that
what plant cells do but also what autotrophic bacteria do is they take CO2 and they take hydrogen and they react them together to basically make all the building blocks of life.
Now plants do, plants get the hydrogen from water, H2O.
They take the H2 out of water and throw away the oxygen and that collects in the atmosphere.
But what bacteria very often do is they've got hydrogen bubbling out of a hydrothermal vent.
They just take the hydrogen as gas and they react it with CO2 and they make all the building blocks of life.
So
what are the enzymes that they use to do that?
Well, they're very often using these same metals that you would have found in the early oceans, nickel and iron, and so on.
And how are they powering the reaction between hydrogen and CO2?
Well, they're using this membrane potential, the electrical potential, the difference in protons between the outside and the inside, to drive that work.
So, effectively, to power the reaction between hydrogen and CO2 to make organics and drive growth.
So,
this was all kind of in place before I came along.
This was coming from Mike Russell and Bill Martin.
And the details are very uncertain, and whether or not you can really drive any biochemistry that way is very uncertain.
But it's a thrilling idea because
you've got a continuity between a geological environment and cells as we know them.
And
if it did emerge that way, then it would say, well, here's why bacteria have got this charge on their membrane because it was there in a hydrothermal vent from the beginning.
It always powered work from the very beginning.
And that's why, in the end, an endosymbiosis that gives rise to eukaryotes
would allow the, it's kind of free you from the constraints of generating a charge on a membrane.
Now you internalize that in eukaryotes and now you're free to become larger and more complex.
So you've gone from thinking about a puzzle about why eukaryotes are special to thinking about planetary systems and thinking about the origin of life and what are the forces that are going to give rise to life and how would that constrain life and would we see the same things on other planets or something different or what are what are the fundamental reasons that it works this way so it becomes astrobiology really and and and uh it's a it's a thrilling change of perspective uh to come from my my own background was to do with mitochondrial biology actually an organ transplantation once upon a time uh and and and spinning on a pinhead you end up working on the origin of life it's fantastic yeah i mean it's it's so fascinating so just to recapitulate for my own understanding of the audiences
let's just break down what we have here.
So, you have the analog of a cell in these pores.
You have something which concentrates the buildup of these organics so that they don't just all diffuse in some big primordial soup.
And so, this is why you think like some primordial lake is not where this happened.
It had to be concentrated in some entity.
Then, you've got a chemiosmotic gradient, a proton gradient, which drives work.
And specifically, it favors the fixation of carbon dioxide and to, you know, to drive the reaction with hydrogen gas to make organics.
And then you've got along this membrane, you've got catalysts, which are basically early enzymes.
So you've got enzymes, you've got the cell, you've got the proton gradient.
And then the story is basically that
you make very simple organics with CO2 and H2.
And then those simple organics are then recatalyzed to make more and more complex organics and like basically TLDR metabolism and fatty acids and cleotides, everything else.
Yeah, that's basically it.
So, what do you get if you react hydrogen and CO2?
What you get are what are called Krebs cycle intermediates, so carboxylic acids, small molecules made only of carbon, hydrogen, and oxygen with this organic acid group at the end, which can be two, three, four, five carbon units in the chain.
And this is your basic building blocks.
You add on ammonia to this, and you get an amino acid.
You add more hydrogen on and you're going to get a sugar.
You react amino acids with sugars and you're going to get nucleotides.
You know, there's lots of steps along here, but
this is the basic kind of starting point for all of biosynthesis in biochemistry.
Then if you make fatty acids, they will sort of spontaneously, because of the hydrophilic nature of their different sides, they will spontaneously form the membrane if they're created.
So as I say, Krebs cycle intermediates are short-chain carboxylic acids.
The fatty acids are long chain.
You know, you're 10, 12, 15 carbons in the chain instead of four or five.
And they will spontaneously, not just alone usually, but if you've got other long-chain hydrocarbons mixed up with them, then you will form a bilayer membrane spontaneously.
And we've done this in the lab.
And it's pretty robust to, you know,
you can make these things at 70 degrees, 90 degrees centigrade across a range of pH from around about pH 7 up to about pH 12.
And in the presence of ions like calcium and magnesium and other salts and so on.
So you can and you make a vesicle with a bilayer membrane around it, which is basically the same as a cell membrane.
They're amazingly dynamic things.
They're always fusing with each other and breaking apart, kind of fissioning, separating into two or three.
And they're very, very dynamic things under a microscope.
You could have had, imagine that life is this like, there's like Frankenstein-like moment where things zaps alive.
And then now you've got life.
I hate that as an idea.
But
Yeah, so that's the alternative where like the bolt of lightning makes these organics, et cetera.
And here you have the story
where
every life form you see is continuous with something, which is continuous with something, which is eventually just continuous with entirely spontaneous chemical reactions.
And so that's just a very interesting way to think about the evolution of life.
One thing, you know, a cell is effectively, it's reduced inside, which is to say, it's got electrons inside, and outside it's relatively oxidized, and outside it's relatively, you pump all these protons out, it's acidic outside, it's alkaline inside,
it's reduced inside.
That's like the Earth.
The Earth is, all the electrons are in the iron, in the core, and the mantle of the Earth, relatively alkaline inside.
That's why the alkaline fluids in these vents.
The outside is relatively oxidized.
You've got all the CO2 in the ocean.
So cells are a kind of little
battery with the same structure as the Earth.
And if you look in a hydrothermal system, the cell membranes around, you know, the Earth, the crust of the Earth is like the membrane, and where you have traffic going between the inside and the outside is the hydrothermal systems.
And the pores in these hydrothermal systems are little cell-like entities as well.
So you keep having on multiple scales the same kind of.
So the idea that the Earth is a giant battery that produces little living cell
mini batteries, it's a rather beautiful idea.
I mean, you can't allow yourself to get too hung up on on a metaphor, but it's a beautiful image.
Yeah, 100%.
So just basically, you've got Earth as this sort of like giant cell, and then this, like, from the hydrothermal vent, this little bubble pops off that's bubbling off mini copies of the Earth.
Yeah, it's such a fascinating theory.
So the thing I want to understand is what part of
life the way it works now is contingent and which would you expect to be shared even if you found life on another planet?
And so it sounds like you're saying, look, carbon, the chemical profile,
this is the obvious candidate to build life on top of.
Proton gradients, is there another way you could build sort of chemiosmotic gradients that drive work, right?
Like we have other chemistry surroundings.
In principle, yes, you could use sodium ions instead of protons,
but it's very different.
Because if you're starting with carbon dioxide, And the first thing to realize about that is carbon is extremely good at the chemistry that it does.
It's forming very strong bonds with all kinds of molecules.
So you can form complex, interesting molecules.
And you're effectively, I think of CO2 as a kind of a Lego brick that you pluck out of the air and you bind it onto something.
You can build things one brick at a time that way.
And then you can build really interesting, complex molecules like DNA and RNA from doing that.
You can't do that with silicon.
So you can, you know, with intelligent design, you can make really complex AI robots, whatever it may be, but the whole thing requires humans to do it.
But if you're thinking about how would life start on a planet where there aren't, you know, there isn't an intelligent designer who's putting it all together, you need molecules that can do that kind of chemistry.
And CO2 is the outstanding example.
And water is everywhere.
Hydrogen, oxygen, these are all elements that are very, very common in the universe.
So you're going to keep on getting this same kind of chemistry everywhere.
We know that there are from...
from discoveries of exoplanets in recent years, if you extrapolate how many we've not seen yet, the number of wet, rocky planets or moons in, say, the Milky Way is probably probably in the order of 20, 30, 40 billion of them.
What fraction of them would you expect to have a non-eukaryotic life?
I mean,
I'll take a punt here.
I would expect that if you've got these same kind of conditions on a wet, rocky planet, you're going to be producing these same kind of vents because it's the same chemistry that's going to happen.
You're going to be dealing with hydrogen.
The vents are not contingent in your network.
No, the vents are produced by a mineral called olivine, which again is really common in interstellar dust.
And the mantle of the Earth is made of this mineral called olivine.
And it will react with water.
And when it reacts with water,
it's slow.
If you were to put a lump of olivine in a bucket of water, you'll not see very much.
But if you're dealing with the pressures down at the bottom of the ocean and warmer temperatures and so on, you're producing bucket loads of hydrogen gas in alkaline fluids.
So that's what these hydrothermal vents are.
So any wet, rocky planet will produce these vents.
There's evidence for them on Mars from the early days of Mars when there were oceans on Mars.
There's evidence now on moons,
the icy moons, Enceladus and Europa.
This is going on in our own solar system right now.
Right.
So if there's 20, 30 billion Earth-like planets which have
presumably some big fraction of them have these vents, if they all have these rock formations, so like, is there a view that a notable fraction of them have life that also operates?
I mean, my view would be yes.
Any wet, rocky planet would have a decent yes.
And if you're starting with CO2 and hydrogen, what what I'm saying is the metabolism is thermodynamically favored chemistry.
This same chemistry will just go on happening because if you react hydrogen with CO2 and with another CO2 molecule, the parts of the molecule that are going to react are quite predictable.
Sorry, this is a naive question, but what is there is to think that there's no alternative chemistries which lead to alternative metabolisms.
Perhaps under very different conditions, you could end up with a, but if you've got essentially similar conditions, you're...
And the other thing is, we know that even with very different chemistries, you end up with basically a similar subset of molecules.
So, from
on the kind of organics you see on meteorites, utterly different chemistry going on.
You're dealing with helium radicals, but you're still seeing amino acids and you're still seeing nuclear bases and so on.
So, there's a tendency, there's a kind of these are molecules which are basically stable and tend to be formed under a wide range of conditions.
Aaron Powell, 20 billion Earth-like planets with water and these rocks in not necessarily Earth-like, but wet and rocky.
If If you just had to pull a number out of nowhere and just say
this fraction have nucleotides, what fraction would you say?
I would say a substantial fraction.
Like over 1%?
Yes.
I mean,
I would imagine 50% or something.
Really?
I mean,
you say pull a number out of a hat.
I'm doing
pulling a number out of a hat.
I think this kind of chemistry is going to give you the same nucleotides repeatedly.
Again, I know you're just, we're just, you know, chatting here, but like, according to this story, pretty sophisticated organics are extremely abundant through the universe, right?
That's not to say they're collecting in an ocean at a high concentration.
What you have in a hydrothermal vent is a continuous through flow and within pockets within this vent, within the pores within this vent, bound to the walls, pretty much, within cells.
So within a vent system, you could have very high concentrations of things, ultimately.
But not necessarily in the oceans or in the atmosphere or anywhere else.
Yeah, I guess you could have have prokaryotes
then who did just take over.
I mean, we did have this, right?
We
kind of proliferated through the oceans and changed the composition of the atmosphere.
So I mean, not just the atmosphere, but also the whole, you know, the whole of geology.
Hundreds of minerals are basically the product of life.
So your view is that the fundamental bottleneck to that, if eukaryotes are the fundamental bottleneck, you can go from...
geochemistry to early life is easy.
Early life to just changing the entire composition composition of the Earth through early prokaryotes is easy.
And if those two things are easy, and then you've got 10 billion planets in the Milky Way, that we've gone to the middle step.
Does that imply that there's like on the order of 10 billion planets?
I mean, I think
to get to nucleotides, from nucleotides, you've then got to get to RNA and DNA
and ribosomes and
molecular machines.
So there's a long gap there as well.
So just having nucleotides, that's a kind of, it's a requirement to get any further.
I see.
And then what fraction would you, again, you had to pull the number out of the air?
Well, a lower fraction, obviously.
Right.
But over a billion?
I mean,
I would like to be, let's say, optimistic.
I would like to think that these processes are going to drive life into existence on a substantial proportion of these planets
or moons.
And I would expect that there would be similarities in the genetic code.
I would expect that a lot of metabolism would look similar.
I would expect that they would have a membrane potential driving the kind of work because it's fun.
You know, know, if you're dealing with CO2 and hydrogen, you've got this same fundamental problem.
How do you make them react?
But so basically there's hundreds of millions of planets in the Milky Way, which like presumably have something like ribosomes and
DNA and to get to RNA.
Yes,
that's my own thinking.
I think
we're talking about
serious planetary driving forces driving fairly deterministic chemistry that's going to give you the same kind of intermediates, which are going to have the same kind of chemistry, the same kind of feedbacks.
They're going to push things into similar directions.
Now, the further from CO2 fixation towards genetics you get,
the less similarity there's going to be.
So, this happens to be the 101st episode of the Thorcache podcast.
And obviously, that doesn't include, you know, clips and shorts and the other content that we put out on the channel.
So, at this point, it's gotten a bit tough to keep track of all of this data.
But since Google Sheets has Gemini built in, I was able to just throw our channel data into a sheet and ask Gemini whatever questions that I wanted answered.
For example, it's hard to evaluate patterns for our full episodes given that some of the clips were in the same channel.
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Another example, I was curious to see how many episodes we had done about different topics.
And I didn't have any historical tags that I'd made for this, but I was just able to ask Gemini to use each episode's description to assign topics and then sum everything together to get a breakdown by category.
Gemini lets you turn these big chunks of unstructured text into the type of data that you can actually sum and count and then use as the basis of different formulas.
Gemini in Sheets is now available for Google Workspace users.
I found it helpful for my podcast and you might find it helpful as well.
All right, back to Nick.
This is not my inclination, but if I was a sort of God-fearing person,
I would hear this and I'd be like, wow, this is a sort of vindication of intelligent design, where the laws of the universe just favor this chemistry, which leads to life, at least according to this story, so strongly that it's
hard to resist this formation.
Curious how you mean that interpretation.
I mean, I agree with you.
I find it a little almost disturbing.
And I have to say,
I'm not a religious person either, but neither am I a I don't object to religion.
I'm not a militant atheist at all.
I rather
like the fact that religions have searched for meaning and searched for origins.
And I have some kind of fellow feeling with that search.
And I suppose truth in some sense with a small T in my own case.
But insofar as this
is consistent with the idea of a God, the God would be a deist God that effectively set the laws of the universe in motion and they're left to play out.
Now,
you know, this is kind of Einstein's God, really.
In terms of what most people understand by God, I think most people look for comfort in God and are looking for something which is meaningful to them and who's been involved in humanity.
And
so
this is a very cold kind of
God as thermodynamics sets the laws of the universe in motion,
reproducibly gives rise to the same kinds of things.
Yes, you could interpret it in a kind of theistic, natural theistic way, but I don't think many people would get that much comfort or meaning from that way of seeing the world.
Okay, so very basic question.
But if life is not only abundant, but almost inevitable in all these rocky planets, then the bottleneck to not seeing aliens everywhere, presumably, is eukaryotes, which lead to complexity.
Yeah.
Well, there's probably more than one bottleneck, but Eukaryotes is, in my own mind, would be the big one, yes.
So it would have to be the case that out of billions of potential planets
that could give rise to eukaryotes,
only on Earth does this chance occurrence happen.
I wouldn't argue that.
Okay.
I mean, only on Earth.
No, I don't think so.
But is there, I suppose what I would dig my heels in a little bit is there's a
kind of Carl Sagan cosmological view that
once you've got, you know, we're talking about the inevitability almost of life arising according to to these laws of chemistry and thermodynamics and so on, and you get life.
And then is it going to roll on and inevitably give rise to complex life and to humans and to intelligence?
It's a beautiful thought.
It would be lovely if that was how the universe worked.
But what we know on Earth is that you have two billion years of stasis where you, and then, and then this apparent singular event where Eukaryotes arose, and then another long gap before you get to animals.
And then if you roll back the clock two million years, there aren't any humans around either.
So
we're just
icy.
Why is it supposedly this hard to
have this
successful endosymbiotic event?
Well,
there's multiple reasons.
I mean, one of them is that prokaryotes, we should say archaea and bacteria, well, they're pretty small things.
So just having another cell inside you is already a difficult thing to do.
It's not, and there are no,
there are occasional phagocytes in bacteria that can engulf other cells, but it's pretty uncommon.
And once you've got these cells inside you, you know, it may have, that may have happened scores of occasions.
There's some tentative evidence that suggests that the archaea, I mean, there's one nice example where the halo archaea seem to have acquired more than a thousand bacterial genes from the same source, implying perhaps they had got an endosymbiont that they then lost later on.
So the question is, how often would it go wrong and you lose your endosymbiont?
And I guess that would be the more likely outcome: is that you pick up a bunch of genes and you lose your endosymbiont.
It simply doesn't work out.
So, it's hard to know exactly what are all the bottlenecks here, but there have been some modeling work done to see: okay, you get an endosymbiont.
Are you going to grow faster if you don't have the endosymbiont or you do have the endosymbiont?
And if you're the endosymbiont, are you going to grow faster if you're outside or if you're inside?
And under most conditions that these people have looked at, there are Santa Fe,
the answer is, well, you do better if you're not part of the symbiosis.
Only under certain conditions will you do better.
So predictably, the end point is it doesn't work.
I guess
given how many bacteria in RKI there are, you know, through Earth history, there's like trillion, trillion, trillion of these running around.
And there's many situations in which there was an endosymbiosis.
And in only one case, it succeeded.
So
the odds would have to just be like remarkable, it would try to be like extremely extremely tough.
It is a vivid way of seeing it.
We know what bacteria and archaea look like.
And people have been studying these things and finding new examples.
And there's a group discovered 10 years ago called the Asgard Archaea.
And they're relatively eukaryotic-like, which is to say, they've got proteins in there and genes that are pretty similar to eukaryotic ones.
And they're...
They're interesting cells.
They've got long processes and they can, possibly they can move vesicles around inside them.
So they're doing a few eukaryotic things but if you look at their internal structure it's not very complex it's nothing like a eukaryotic cell and if you look at their genome size it's basically a standard prokaryotic genome size you're talking four or five thousand genes so they're they these are these are these are not eukaryotic by any stretch of the imagination And then you look at a eukaryotic cell, and I said this at the beginning, you look at a plant cell or an animal cell or a fungal cell or an alga or amoeba under a microscope, and they've all got the same stuff.
And it's kind of weird.
Why would a single-celled alga living in the ocean have all the same kit that one of my kidney cells has?
Well, the easiest way to understand that is to say, well, it wasn't adaptation to an external environment, to a way of life.
It was adaptation to an internal selection pressure.
If you think about it in terms of a kind of a battle between the host cell and the endosymbiont for finding a way of living together, you can argue for the nucleus arising that there's all kinds of genetic parasites coming out of the mitochondria, forcing you to do something to protect your own genome.
So you can construct a lot of this history of
eukaryogenesis, it's called.
So you start with simple cells with a cell inside, and you end up with the same cell structure everywhere, all these endomembrane systems and everything else.
Okay, so I guess the broader thing we're trying to figure out here is if this story is true, there's life everywhere, but eukaryotes giving rise to intelligent life, which is about to go through, you know, explore the cosmos, is, as far as we can tell, happening only in one place in our light cone.
So why is that?
And now
you could say, well, look, the bottleneck is the eukaryote, and
it's just very hard to get a successful endosymbiosis, which then continues over time.
But what is the fundamental problem this is solving?
What's solving the problem that in order to...
Exactly.
So
to have a multicellular organism where effectively you're deriving from a single cell,
and that restricts the chances of effectively all the cells having a fight.
There's plenty of examples of multicellular slime moles, for example, where the cells come together and they can form structures like a stalk, for example, which loosens spores into the environment.
But they basically fight because they're genetically different to each other.
So you start with a single cell and you develop so there's less genetic fighting going on between the cells than there would be if they come together.
But that means then if you want to have complex functions, if you want to have a liver doing one thing and kidneys doing something else and the brain doing something else, all of the cells have to have the same genes, but you express this lot in the liver and that lot in the brain.
So you must have a large genome.
The only way you can have a large genome is by having mitochondria and having a eukaryotic cell.
There are no examples of this level of sophistication of a multicellular bacterium.
Aaron Ross Powell,
that's quite interesting.
The reason you need a large genome is actually just to put all your eggs in one basket so that every cell in the body feels incentivized to make the
amount of fighting.
Yeah, yeah.
They're all incentivized to make the jury life continue.
But the thing I was getting at is like, okay, the eukaryot is having a large genome and it's allowing the cell to get much bigger.
Why are we so confident that this is the only way this problem could have been solved?
It just seems like if there's billions of planets which have like gotten to the precursor stage here, none of them can find an alternative solution to mitochondria for just letting themselves get bigger.
Biggest belief.
Yeah, I know where you're coming from.
It kind of makes me wonder whether we're like, because we've only observed one way to solve the solution, we're sort of assuming that there must be only one way to solve the solution problem.
Whereas the problem itself doesn't seem like, okay, you just want a smaller copy of your genome sitting next to the site of respiration, right?
That's like the basic problem.
Like there's no other way to solve that.
Well, maybe there is, but I think we have to look at the probability of certain things happening.
So if you want to have a giant bacterium,
there are a bunch of giant bacteria around on Earth.
There's at least six or seven different quite unrelated species that have evolved giant size.
And the thing that they all have in common is they have what's called extreme polyploidy, which is to say they have literally tens of thousands of copies of their complete genome.
So it may be a small genome, but we're talking a three-megabase genome, so kind of 3,000 genes in it.
And you've got tens of thousands of copies.
Sometimes, you know, the very largest one have 700 or 800,000 copies of their complete genome.
The energy requirements for copying and expressing all of those genomes are colossal.
What we have with an endosymbiosis, we still have extreme polyploidy, but we've whittled away all the genes that you don't need.
So, a symbiosis is based on effectively complementarity.
You've got a symbiont that's doing something for the host cell, and the host cell that's taking something or giving something back to the endosymbiotic.
So, it's a kind of a relationship which is based on mutual needs.
One of them becomes much smaller, and that allows the other one to become much larger.
So, a symbiosis will do it.
Now, there could be be multiple ways of having a symbiosis, but
there's no examples on it.
There's all of these examples of very large bacteria and they all have extreme polyploidy.
None of them have come up with a complex trafficking network where you effectively take things in and you ship it over there.
There's just not enough genetic space to be able to do that.
But just to make sure I understood the feature request correctly, it's basically like you want
a smaller copy of the genome that is only relevant to respiration
sitting across the entire membrane and many copies of it sitting across the entire membrane i guess i'm just yeah it seems hard for me to you're incredulous that this this same thing
on like the billions of planets because if there was another way to solve it
then what you would expect is that as soon as you get to the stage of
prokaryotes
that have other niches that they could colonize if only they could drive towards complexity, this would somehow be solved.
And then you'd have ekaryots, dot, dot, dot, intelligence.
I mean, a couple of things I'd say.
Number one, there's a thing called Orgel's second rule, which is that evolution is cleverer than you are.
So, yeah, of course, I cannot say that there's no other way that it could possibly happen.
But it's also hand-waving to say, oh, you know, evolution's so clever, the universe is so big, there's got to be another way that it can happen.
Okay, you know, engage your brain and tell me is how it's going to work.
Because
I cannot say it's the only way it could possibly happen.
But what I've said is that there's, you know, wet rocky planets are common.
They're everywhere.
You're going to have these same serpentinizing things.
You're going to have CO2.
You're going to have a similar biochemistry.
You're going to give rise to bacterial cells that have got a charge on their membrane.
That constrains them.
And every example that we know on Earth where they seem to have got bigger,
there's a constraint that probably probabilistically happens every time.
They always end up with extreme polyploidy and they don't end up with sophisticated transport networks.
So that's not to say it's got to happen that way every time.
Maybe there's a way around it, but it's not an easy way around it because they haven't done it regularly on Earth.
They haven't done it at all on Earth.
The only occasion where it worked on Earth was where they came up with Eukaryus.
That's not to say it's the only possible way of doing it, but if you try and dissect what are the alternatives, I can't think of any alternatives.
Okay, I'm limited.
I can't think of any.
But, but, but you know, if you think there are some, then you tell me what they might be and you test them.
So it's, you know, there's, there's a, there's a level, and I get this a lot, and it's fair enough because if I just, if I assert to you that life's going to be this way somewhere else in the universe, and you know, I grew up watching
you know, Star Wars and Star Trek
and reading Hitchhiker's Guide to the Galaxy.
I love the idea that the universe is full of all kinds of stuff as much as anybody.
So I don't like my position of saying actually it's quite limited and you're going to see the same kind of things elsewhere.
It's not a position that I
dreamt of having or anything.
It's just a position that I've been forced into by everything that I've learned about life on Earth.
Now, maybe I'm just wrong,
but
I suppose if you simply say, ah, you're limited by your imagination, you're wrong because you just can't think of it.
Well, that's not science anymore.
Now we're talking about
just imagination and hand waving, but it's not science.
So I'm giving reasons why probabilistically it's going to be this way.
What I would say is if you've got a thousand planets with life on, Maybe life is going to be the same way 999 out of 1,000 times because it's going to be carbon-based, it's going to be water, it's going to be cells, it's going to be charges, it's going to be hydrogen and CO2, and you're going to face the same constraints.
But maybe one other occasion, it's something completely different that I never thought of under very different conditions.
But there's a kind of a probabilistic thing that carbon is so common, water is so common.
You are going to keep seeing the same constraints again and again.
If it's the case that a significant fraction of rocky planets should have at least organics and cells and so forth, it feels like we should be be able to learn pretty soon whether this story is kind of correct, right?
Because obviously, if that part ends up being true, and also we don't see eukaryotes elsewhere, then the whole picture is lent a lot more credence.
But, like, we, I don't know, are we about to go to a couple moons and see if we can find some organics there and so forth?
It may take us a while, but yeah, we already know that there are organics in so on Enceladus, for example, one of the moons of Saturn,
when Cassini flew by some years ago, there are kind of plumes coming through cracks in the ice of water, but with organics dissolved in the water, and hydrogen and organic molecules.
pH is around about eight or nine or something.
So it implies that underneath that frozen surface, which people say is about five kilometers thick, underneath that there's a liquid ocean.
Underneath that, there are hydrothermal systems producing alkaline fluids, which have made the oceans alkaline.
And it's the same kind of chemistry going on.
So we know there's organics in these plumes.
We don't know what's under the ice.
I do think that the incentives to go to these places and drill into the ice and have a look will get the better of us.
There will always be people saying, oh, we shouldn't introduce bacteria from our own system into there.
I would have said, you know, bacteria from the Earth would probably survive extremely well in a place like Enceladus.
So it'd be lovely to know.
Yes.
And I'm all in favor, really, of exploration.
LabelBox has this massive network of subject matter experts who they call aligners to help them generate data for training and evaluating frontier models.
In order to help prep for this episode, I asked LabelBox to connect me with one of their chemistry experts for a quick tutoring session.
I got to chat with Neil, who's a researcher that's currently working on chemistry ML models.
So, how did the first television happen?
I suppose, and this is just me speculating here, but in these hydrothermal events, you've got water flowing down, you've got hydrogen bumping up.
And this water is not just going to be flowing in a completely linear fashion.
There's going to be some shear.
There's going to be some side-to-side movement.
So I suppose perhaps you could begin to consider sharing somebody's cells, splitting them.
And I remember him saying that like the first version of division might have been like membranes naturally will split the same way like a bubble will split if it gets too big.
Yes.
Neil quizzed me on my understanding of redox chemistry.
The same way that he interrogates models to make sure that they are developing a non-superficial understanding of all the scientific topics.
Labelbox has experts like Neil in a bunch of different domains from chemistry, obviously, to math, coding, even creative fields.
Learn more at labelbox.com/slash thor cache.
Help me understand
how replicators arise in this world.
Because if you've got these independent pores and they're each individually accumulating their own organics through the spontaneous processes, but initially, at least, there's no shared inheritance.
It's not like if there's a very successful pore, it then causes there to be more pores exactly like it.
Think what I would call protocells inside these pores.
So you think that the organics that you're making are self-organizing.
A fatty acid bilayer membrane will form.
And what you really need for positive feedbacks is to be making the organics inside this protocell and for that protocell to grow and to make a copy of itself.
Now, it will make a copy of itself because the chemistry, if the chemistry is deterministic, it says this is the chemistry you're going to get.
If you drive that chemistry through by the pressure of hydrogen in the system, you're just going to make twice as many molecules and they're going to divide into, and now you've got two protocells.
So there's a form of heredity to that, which is they get the same molecules because that's effectively all you're allowed to do.
Aaron Powell, Jr.: And sorry, but what's happening is that the thing buds off and then like settles into another pore?
Yes.
I see.
Okay, got it.
And this happens relatively early in this process.
Yes.
And so the rise of replicators happens relatively early.
I would hesitate to use the word replicator here.
These are growing, I would say growing protocells that are effectively
making more of themselves.
You could call it a replicator, but I would prefer to use the word replicator for something more like RNA, which would be the conventional term for a replicator, where you are literally replicating the exact sequence of this RNA.
And so at what point do we get to the genes I point of view where the gene is the coherent unit of replication?
The sooner the better, which is to say,
If you've got this deterministic chemistry which is going to drive growth and make more cells, it's also a dead end.
You can't do anything else.
You're entirely dependent on the environment.
You can't kind of evolve into something more complex.
To some extent, you can, but basically you're always going to get the same in the same environment, we'll always give you the same thing.
Soon as you start introducing random bits of RNA into this, then you've got what you call evolvability, which is to say you can begin to resist the environment.
You can begin to do things which are not just dictated by the environment.
You can evolve and change and leave events in the end and do other things.
So as soon as you've got genes, you've got the potential to do almost anything.
If you've got naked bits of RNA, what tends to happen is they're selected for their replication speed.
They just go on making copies of themselves.
They don't become more complex.
They don't start encoding metabolism.
They just go on copying themselves and it's a dead end.
If you're trapping them inside growing protocells, then effectively they're sharing the same fate.
And if some of them are capable of making that protocell grow faster,
then they will get more copies of themselves because they're inside this protocell.
The protocell is growing faster.
It makes a copy of itself and it's still associated.
So you've got actually selection as we know it in cells today, where the replicator of the genes, but the system which is being reproduced is the cell.
So your sort of mitochondria first viewpoint helps explain why there's two sexes.
Maybe you can recapitulate that argument, but I'm curious if
there was a world where prokaryotes had evolved sex, do you think they would have likely evolved just one sex?
I'm going to unpack that a little bit because
so what have mitochondria got to do with sexes?
So what they have to do with sexes is effectively the female sex, and this goes even for single-celled things that don't have any obvious differences between gametes, which is to say they don't have oocytes and sperm or anything.
They produce little motile gametes that look more like sperm than anything else, both sexes would do that.
But by definition, the female sex passes on the mitochondria and the male does not.
And that's a kind of that's an approximation.
It's not always true.
There's exceptions to that rule, but it's a kind of a rule of thumb in biology that the females pass on the mitochondrial DNA.
So why would that happen?
With sex, what you're doing is you're increasing the variance in the nuclear genome and you're subjecting that to selection and the winners are coming through that and everything which is worse than it would have been gets eliminated by selection.
So you're effectively increasing variants on nuclear genes, the genomes,
and then selecting for what works.
With the mitochondria, they're not doing,
they're passing on asexually down the generations.
It's a very small genome, but there's multiple copies of it.
And so the question is: well, how do you keep that clean?
How do you prevent that from degrading and degenerating over time?
Because if you've got, let's say, if you've got 100 copies of mitochondrial DNA and two of them acquire mutations, but you've still got 98 which are doing their job fine.
What's the penalty for those two mutations?
It's not very much.
You'll hardly notice them.
So now you acquire another couple of mutations, and you can degenerate over time.
It's a process called Muller's Ratchet, but it's basically
these mutations are kind of somewhat screened from selection by being compensated for by clean copies that you have of other copies.
So how do you get rid of those mutations that are building up over time?
Well, the answer is what you need to do is increase variance of mitochondrial genes.
What you need to do is effectively segregate into these cells all the mutants and into those ones all the wild-type ones.
So, you can do that by multiple rounds of cell division, but it helps if you've got two sexes that effectively only one sex passes on the mitochondria.
So, you're already sampling.
So, you're already increasing the variance
and you're increasing visibility to selection.
So, you're basically
about the quality of mitochondrial genes.
Can you help me understand why it's the case that uniparental inheritance of mitochondria helps increase variance?
Because
so we're talking about variance between cells.
So if you imagine that you have 100 cells
and
they all come from the same parent, let's say, and you randomly give each cell,
if you give
all the mitochondria that you have kind of straight into a single cell
without changing any of the ratios there, then it's it's exactly the same as you are.
It's fully clonal.
But
if you take a small subsection of those and you say you take a random 10%, you give 10% to this one, a random 10% to that one, a random 10% to this one, randomly, this cell is going to happen to have got all the good copies.
And this cell is going to happen to have got all the bad copies.
And now you subject these hundred cells to selection and say, how are you doing?
And the one that got all the good copies, that does well, that gets on.
So what you're doing is increasing the variance between this kind of next generation of cells.
So the ones that got all their mutants, they get hit.
And the ones that got all the clean copies, they do all right.
The parent had got both the mutations and the clean copies, but
how do you distinguish between them?
Well, so it's about sampling, basically.
And uniparental inheritance, which is to say, is a form of sampling.
You're taking the mitochondria only from one of the two parents.
So you're not mixing up mutations that
both parents had.
You're kind of taking a subset.
So you're always increasing variance between the daughter cells, and uniparental inheritance is basically giving you a subset.
So then the question of why there's two sexes, well, we've explained why there's this evolutionary niche for only one parent to pass on the mitochondria.
So there's at least two niches, one is passed on to mitochondria, one is don't pass on on the mitochondria.
So once you've established those two, then you can ask the question, why aren't there more than two sexes?
And then you can just say, well, there would just be a repetitive one of these two.
These are the two fundamentals.
I mean, it's more complex.
But I mean, the thing about two sexes sexes is you could say it's the worst of all possible worlds.
So again, if you kind of
let's take it away from humans so we can be dispassionate about it.
You've got these
single-celled critters swimming around,
and they're all producing gametes, and the gametes look the same as each other,
and they'll fuse in the same way as sex, and they'll line up the chromosomes.
They basically do exactly the same thing that we do, but on a single-cell scale.
But having two sexes means that you can only mate with 50% of the population.
The other 50% is the same sex as you, and it's not going to accept
your gametes.
If you had three sexes or four sexes, then you would be able to mate with a larger proportion of the population.
And some fungi, they don't really have, they still have two sexes, but they have mating types as well.
And you can have 27,000 mating types in some fungi, which is all about outbreeding.
So you can mate with just about anything.
But you still need to.
We've been to some college campuses today, you know,
replicating some portion of that.
Oh, yeah.
It's becoming fungal.
Yes.
So two sexes, then, in that sense, is the worst of all possible worlds.
You can only mate with.
If you had only one sex, if everyone was a hermaphrodite, you could mate with everybody.
And if you had three sexes, you could mate with two-thirds of the population and so on.
So why two?
Well, this fundamental difference that one is passing on the mitochondria and the other is not.
Beyond that, if you've got multiple mating types, you still have one passes on the mitochondria and the other one doesn't.
So in these fungi that have all of these mating types, there's a kind of a pecking order that the dominant one will pass on the mitochondria and the less dominant one doesn't pass on the mitochondria.
So you end up with really complex systems.
You can imagine that it's pretty hard to enforce this.
It's pretty,
stuff can go wrong.
The more complex the system is, the more it will go wrong.
So I guess in that sense, why do you end up with two sexes?
It's partly minimization of error.
You have this really interesting discussion about how this not only explains why there's two sexes, but the particular differences in why eggs and sperm develop the way they do, why there's different amounts of
before they are mature, et cetera.
I wonder if you can recapitulate that.
Yeah, so as soon as you've got this fundamental difference, even in single-celled critters, that one of the sexes passes on the mitochondria and the other one doesn't.
So males do not pass on their mitochondria.
And then this is beginning to explain differences in multicellular organisms between the sexes, between the nature of the germline.
So in some sense, male men do not really have a germline in the sense that women have a germline.
So
in in the female germline, you make these oocytes and you put them on ice effectively.
You look after them.
You switch them off as much as you can.
You try and protect them from mutations.
You mollycoddle them effectively, whereas men just mass produce sperm, full of mutations.
I mean, there's a lovely phrase from James Crowe, who's a geneticist, who said there's no greater genetic health hazard in the population than fertile old men.
So why would you go on mass producing sperm all the time?
Well, part of it is you don't have to pass on the mitochondria.
So you're freeing yourself up to mass produce sperm.
And then you've got the same things out.
Some of them are full of mutations, but a lot of them aren't.
You mass produce them and
the chances are it's going to work out okay.
Because the ones that can swim best, for example, are the ones that are more likely to.
That's not strictly true, but you can imagine it along those lines.
But in the case of the oocytes, in the case of the egg cells,
you're passing on those mitochondria.
You don't want to be accumulating mutations in that mitochondrial DNA.
You want to switch them off as much as possible, keep them on ice as much as possible.
So very much the differences between
how the sexes end up kind of becoming different to each other boils down to what are the constraints
on your reproductive system.
Yeah.
Okay, so let's talk about the Y chromosome, which is also not recombined.
Now, just the same way that female egg cells try to minimize the amount of duplications in order to preserve the quality of the mitochondrial DNA and prevent errors, why isn't the same thing happened with the Y chromosome?
Shouldn't all the sperm duplication be the resulting and all kinds of errors in the Y chromosome that.
Well, it does.
Okay.
And the Y chromosome is degenerate.
I mean, I know you got the title.
Yeah, but I mean, there are some things that have lost their Y chromosome altogether.
And they still have sexes because it's not strictly dependent on the Y chromosome.
I mean, again, if you look at what determines sexes across the whole canvas of evolution, it's kind of weird because
amphibians, for example, have temperature-dependent sex determination.
So males would develop at a higher temperature than females, or sometimes it's the other way around.
And, you know, birds have different sex chromosomes to mammals, for example.
So sex chromosomes have evolved on multiple different occasions.
And what's the Y chromosome doing?
Well, the Y chromosome is basically encoding a growth factor, and that growth factor switches on other growth factors.
And the earliest difference that you could tell between the two sexes in embryonic development is not the activation of the Y chromosome, the SRY gene, it's actually the growth rate.
And
there was a woman at UCL where I am called Ursula Mitfock, who spent her career, she had about 15 nature papers in the 1960s.
She worked on these kinds of questions.
And she saw the growth rate as the common denominator.
The Y chromosome is basically saying grow fast.
Why would he grow fast?
Well, in part, you can grow fast.
You don't have any constraints on trashing your own mitochondria because you're not passing them on.
So you can grow fast.
And there'll be an advantage to growing fast.
If you're a male, you're going to get the resources.
You grow faster.
If you're a female, you don't want to grow so fast because you need to effectively cordon off your germline to preserve the oocytes for the next generation.
Until you've done that, you don't want to trash your mitochondria.
So you've got a delay phase before you can start growing fast.
Interesting.
Is this a woman live longer?
Ursula Mitvock argued that that was exactly the case.
We don't know for a fact that that's true, but it's quite common that females live longer than males, not just in humans, but in Drosophila as well.
They do, usually.
Suppose that evolution on humans just continued naturally for the next billion years, and we didn't have AGI and
human gene editing, et cetera.
Is the equilibrium that you'd anticipate that the Y chromosome would then just fade away altogether and there'd be some other way of determining sex and sex-dependent characteristics?
Well, there are, and it has disappeared altogether in some species.
And usually, what you retain is one gene,
which causes a different rate of growth.
I see.
So, really, the Y chromosome, yes, it's degenerate.
It's lost most of its genes.
The thing thing about Muller's ratchet, which is the degradation of things
when you don't have sex or you don't have any recombination, there's two factors that influence it.
One of them is the population size.
So, in bacteria, if you've got a small population and they're not sexual, then you accumulate mutations in that population.
But if you've got a much larger population, the closer you kind of get towards an infinitely large population, they're not all going to accumulate the same mutations.
And so, the population as a whole is going to be fine.
And this kind of goes back decades in population genetics.
But the other thing which is less explored in population genetics is the size of the genome.
So if you, with bacteria, if you increase their genome size up to eukaryotic size genomes, you can't maintain a larger genome.
You'll accumulate mutations in that genome and it'll shrink again.
And with the Y chromosome, yes, it's shrunk.
It's a tiny chromosome in comparison with all of the rest.
So it's really how many genes can you maintain in a good good state?
And with the Y chromosome, basically, you only need a couple of genes in there.
Basically, it's the SRY gene is saying grow faster.
I see.
And you only need that to remain functional.
And then selection at the level of fertile or infertile men will kind of weed out the ones that have got a non-functional SRY gene.
So it's not as if you've got a patchwork of mutate.
You can afford to degenerate your Y chromosome down to almost nothing and you'll still be functional.
I mean, it's quite interesting because
you were saying that the same thing happened to the mitochondrial DNA.
Which is a tiny genome.
And has shrunk over time, starting from the original bacteria that was engulfed.
It's gone down from, say, 3,000 or 4,000 genes to, in our own case, 37 genes.
So
you cannot sustain a large genome if you're inside.
I said, but population size matters.
If you were a free-living bacterium living out there in the wild with a population of a million, and now you shelter inside another cell and it's a small cell, now you've got a population of five.
So you will accumulate mutations and you can't resist them.
So you'll lose genes.
So your genome shrinks.
And that's what happened to the mitochondria.
You just can't maintain a bacterial-sized genome.
So maybe worth explaining why it's the case that sex is preferable to lateral gene transfer in the sense of being the systematic pooling and parallel search across gene space.
So if
there is this advantage of sex and then bacteria have some antecedent to it, why didn't they just get the whole thing?
Is it just that it's not compatible with their size?
I think they had no need for it.
So, what they do, it's lateral gene transfer is basically you pick up random bits of DNA from the environment.
It can be a bit more sinister than that.
You can kill the cell next to you and take its DNA and load that in.
That does happen, but for the most part, you pick up bits of DNA from the environment, usually small pieces, usually kind of one gene's worth or something.
And you'll only do that if you're a bit stressed.
If things aren't going well for you,
you will then pick up bits of DNA, bind it into your genome, and hope for the best.
And I guess for most critters, most of the time, it's not going to work.
But for one of them, it does, and then they will take over.
And so it kind of speeds up adaptation
to a changing environment.
So why are they only using one gene?
There's two ways of seeing this.
You've got a bacterial-sized genome.
It's pretty small.
You're going to replicate faster if you keep that genome small.
It's kind of a disadvantage to have a big, unwieldy genome.
Eukaryotes have that.
And it's kind of an interesting question.
Why would you have such a big, unwieldy genome?
It takes longer to copy and longer, you know, bacteria are really streamlined.
They get rid of genes they don't need and then they can grow faster.
But now the conditions change.
And now you need this gene.
So what do you do?
You pick it up.
You just pick up random genes and hope for the best.
Pick up the right one and off you go again.
So bacterial genome sizes are small.
They've got what you'd say is a small genome, but then a large pangenome, which is kind of all of the genes they have access to.
So an E.
coli cell might have three or four thousand genes in a single cell, but access to thirty or forty thousand genes.
What is keeping the metagenome around?
Why doesn't everybody just converge to this streamlined thing that is needed for the current gene?
I mean, I think what keeps the metagenome around is the fact that different strains of E.
coli, whatever bacteria they may be, are living in different environments.
So, you could have a commensal bacteria living in your gut, you could have bacteria's E.
coli living on your skin, very different environment.
You can then have non-commensal pathogenic E.
coli, which are behaving differently again.
They can differ in 50% of their genome.
So you've got all of these things going on side by side and they can all borrow genes from each other.
And this is basically within the same species, whatever species exactly means with bacteria, it doesn't quite have a meaning.
So this is the kind of dynamic of bacterial evolution is they retain small genomes with access to large pangenomes and they're forever borrowing, matching, and so on.
And they effectively remain competitive by keeping their own genome pretty small.
And then you carry it kind of through threw all of that out and got larger genomes.
And then the question is: well, if you try and do that with a large genome, a eukaryotic-sized genome, and then you go on picking up little bits of DNA from the environment, the chances of you replacing the right gene get lower.
I see.
So it just becomes less and less efficient the bigger your genome is.
So by the time you get to eukaryotes, they have a large genome.
Why do they have a large genome?
I would say it's because you acquired this endosymbiont and they become the mitochondria.
And now you have a lot more energy available.
There's all kinds of reasons why eukaryotes will tolerate a larger genome.
But the bottom line is you've got the energy to do something with it, which bacteria never really had.
And so now lateral gene transfer is just not good enough to maintain this larger genome.
You're going to have to do something more systematic.
So you pull on an entire genome, you line everything up, you crossover between them.
Now it's systematic, it's reciprocal, and you can maintain the quality of genes in a much larger genome.
So bacteria never had the need to do that.
Right.
As I was reading your book, just to ease my own ignorance, I was like trying to come up with an analogy.
And so, please let me know in which ways it's naive.
And also, thanks for tolerating all my other naive questions today.
But here in Silicon Valley, maybe an analogy that will work for us is to think about, let's say, a GitHub repository.
And then.
I'm already out of my depth now.
Basically, you just have this code base, and then you have ways in which you do version control.
So the usual way this is done, and this may be analogous to sexual recombination, is that somebody makes what is called, they make a new branch.
In that branch, they might make changes which are organized next to the function that they're trying to change.
And then so when the maintainer is looking at the code, they can see, here was what the original code was at this point.
Here's the modification to that point of code.
And you see the diff, and then you can merge it back if it seems sensible.
And so the analogy here might be sexual recombination that's organized along the relevant gene and you see this allele you see that allele and then i guess evolution here is a maintainer which is then driving one of them to fixation um
the analogy for asexual reproduction just uh cloning with mutation would be okay you fork the repository then you make a random change you just change some random variable you change a word you change a bit
And almost every single time, this will be deleterious.
And even when it's not deleterious,
there's no merge functionality.
So these different, you've got millions of repositories that are then spawning millions of other repositories.
And even if some improvement has been made on one of them, there's no systematic way in which the improvements can be merged together.
I mean, it sounds quite similar, yes.
Yeah.
And then finally, lateral gene transfer.
So here the analogy might be: okay, so
you've got one repository for, let's say, editing web pages and another repository for controlling airline software.
And what you just do is you take a random 500-line sequence in this web page editing software, and you just put it in a random point in the airplane management software.
And there's no systematic organization of like, here's where the relevant functionality is, and here's like well, there is a bit, which is to say, with lateral gene transfer, you would normally match the ends to something you've got already.
So I don't know enough about coding
to give a comparable example, but effectively
you would be picking up a module which
had some resemblance in terms of, okay, it fits into this part of the code.
So you'd only put that in, and it may or may not be useful there, but it's not just completely random.
It's plugged into a place where you know you have something like that that used to be there or could be there.
So
it's not just random, but at the same time,
you don't know what you put in.
So then I guess honestly,
I don't really have good intuition for why lateral gene transfer does not produce similar benefits to recombination.
It's really just a scaling thing.
If you pick up a random piece of DNA,
you've got a genome which is 10 times larger.
Then, you know, how fast can you pick up DNA from the environment?
You know, you'd have to pick up 10 times as much to do that.
Do you have the capacity to pick up 10 times as much?
And there's also a penalty for doing it, which is to say, like a mutation, you've got no idea what you're plugging in.
It could be almost anything.
You know where you're plugging it, you're plugging it in the right place, but what's in that cassette, you don't really know.
So the more you do of it, the more you will degenerate yourself as well.
I see.
So there's kind of costs and benefits to doing it.
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Okay, so maybe to close us off,
what is the
experiment or method of interrogation which would give us the most amount of information about
this story?
Yeah, I mean, there's so many aspects to this story.
There's so many possible answers I could give there.
I mean, in terms of
eukaryotes, giant bacteria, the likelihood of life, I think there's a lot depends on observation.
We simply don't know enough about what's out there.
And so it's not necessarily experimentation, simply, you know, if I assert that giant bacteria are always going to have
extreme polyploidy with multiple copies of their genome, you find an example that's not like that.
And already my ideas are breaking up.
So useful to know.
For the origin of life,
I really wish I could come up with a convincing reason why I should go down in a submersible to a deep sea hydrothermal system like Lost City.
I would love to go to Lost City.
But the trouble is that the ocean chemistry is completely different now to what it was 4 billion years ago.
It's now full of oxygen, it's full of bacteria and things as well, but the ocean chemistry is is different because there's oxygen, there's no iron, there's no nickel in the oceans.
So you can go to a vent like Lost City and the walls are not made of catalytic minerals anymore, they're made of aragonite and and brucite, so kind of uh calcium carbonate and and magnesium hydroxides and things like that.
Um
and so the chemistry it can do is very different and there's lots of bacteria living there.
So I would gain beyond just the sheer amazement of seeing it, there's not a lot it would be able to tell me.
So what we're actually doing is experiments in a lab, in an anaerobic glove box, where you exclude the oxygen so you can do these experiments, reacting hydrogen and CO2, how many of the molecules in biochemistry can we produce that way?
And it's slow and laborious and you get small amounts and sometimes you get contaminations and sometimes you have to start all over again.
And
it's slow work.
But it's moving forward.
It's not just us either.
I mean, there's other groups around the world.
So Joseph Morin's group, for example, has done a lot of really nice biochemistry along these lines.
So that's kind of moving forward.
But I think we're talking decades before we're getting to the level where we can say, right, we can drive flux through all of metabolism.
And here's the set of conditions that will do it.
Certainly some years.
There are big crux points like making purine nucleotides, where there's 12 steps in this synthetic pathway, and all the intermediates are unstable and break down easily.
It's being done in
things like methanol, so not in water.
In water, stuff breaks down.
So we're trying to do it.
It's difficult.
So
I believe, I think we'll get there, which is why we're trying to do it.
But maybe we won't, in which case, again, the hypothesis is wrong.
You've got to wake up every morning and think, you know, the hypothesis could be wrong.
It's beautiful.
It might make sense.
But, you know, there's so many beautiful ideas killed by ugly facts.
So there's no good believing that you're right.
You've got to believe you're probably wrong and keep going anyway.
And then the other thing which I'm excited about at the moment is work on anesthetics and mitochondria.
It turns out, I heard this from a guy called Luca Turin a few years ago now,
who pointed out to me that anesthetics affect mitochondria.
I had no idea that anesthetics affect mitochondria.
Well, they do.
We've been doing experiments on it.
And it seems
not fully established this yet, but it does seem as if their main effect is mitochondria.
And anesthetics work on all kinds of things, including things like amoeba.
So it's already saying, it doesn't prove anything, but it's beginning to say, well, if you can make an amoeba unconscious, then
was it conscious before?
Well, not as we understand consciousness.
But the way we would understand consciousness is really about neural nets and a nervous system and all the complexity of human consciousness.
That's what we primarily think about.
But there's a deep problem
which goes back.
I mean, it's the mind-body problem, but it was framed by David Chalmers as the hard problem of consciousness, which boils down as my understanding of this is more or less: we don't know what a feeling is in physical terms.
So you can understand the information processing of a neural network, but what actually, if you feel miserable, or you feel pain,
or you feel love, or whatever it may be, what actually is that in the chemistry of a system?
And I suppose the problem is that you have all of these neural nets firing, and some of them are conscious.
We're aware
of what we're thinking about.
And others, which seem to have all the same properties in terms of then neurons, they have synapses, they have neurotransmitters, they depolarize, they pass on an action potential, but we're not conscious of it.
It's non-conscious information processing.
So there's this question, okay, so if anesthetics affect things that don't have neural nets
and feelings are something that we can't define in terms of a neural net, could it be that feelings are somehow linked more broadly to
life?
So why would they be?
So again, the way I think about this is as an evolutionary biologist.
So the first question is, would we think that
feelings are real?
I would say yes.
Do we think that they evolved?
I would say yes.
I think any evolutionary biologist would say yes to those
questions.
If it's real and it evolved, then natural selection must be able to see it and act on it in some way.
In other words, there's something physical about it that can be selected for.
Again, I don't think there's anything controversial about that statement.
But then if it's physical and real and has been selected on, you know, the implication is we should be able to measure it.
There should be,
it has to offer an advantage for selection to act on.
And if it's a physical process, it should be measurable.
But we don't really know what we're trying to measure here.
So I then kind of revert back to thinking, okay, what would a bacterial cell need to do?
And this is just kind of back of the envelope thinking.
And I immediately think about metabolism.
What's the difference between the inside of a bacterial cell and the outside world?
It's basically, you know, the inside is metabolically alive.
It's doing stuff with its chemistry all the time.
And it's at a colossal rate.
A bacterial cell will have about a billion reactions every second in this metabolism.
So I'm immediately left wondering: how is it all controlled?
How do you get this cell to have a coherent behavior so it decides, I'm going to crawl over there?
How do you even know what state you're in?
How do you kind of synchronize all of this biochemistry?
And probably most people's answer to that would be metabolic regulation of one sort or another.
But that's not really the driver.
The driver in the end is
the thermodynamic drivers.
How many electrons do you have?
That's in the form of food or NADH or whatever it may be.
How much energy do you have in the food, in the form of ATP?
These are the things that are going to synchronize reactions in the same kind of phase.
And the problem there is when you're dealing with molecules, you're dealing with tens of thousands of them.
So you've got a kind of large statistical sampling, which is time-consuming to figure out.
But there is a better way of doing it, which is to say if you're taking electrons from food in NADH and you're passing them to oxygen, but you're generating a membrane potential and that's driving ATP synthesis, you can actually measure the rate of change and the membrane potential and
the fields that will be generated, electrostatic and electromagnetic fields.
That's going to give you a handle on your state, on your metabolic state in relation to the outside world.
Is there enough food there?
Is there enough oxygen there?
Is it too hot?
Is there a virus?
Do I have enough iron to be able to do all these reactions?
So you've got all these potentially conflicting feedback loops, and you've got to make a decision.
So you're just thinking loosely about how a bacterial cell is going to behave.
You find that you're already framing it in terms of, well, as an entity, as a cell,
it's got to make some kind of decision about what to do.
It's got to integrate all this information and make a coherent decision as a self, as an entity.
Is that free will?
Probably not in any way that we recognize it, but it makes a decision in relation to its environment
and the outcome is survival or not.
So what I think a feeling is then is effectively
it's the electromagnetic fields generated by membrane potential, which is telling you what your physical metabolic state is in relation to the environment you're in.
But that leaves me to a question.
So
if consciousness is somehow about about mitochondria, are the mitochondria in that sense just really simply an ATP generating engine and you interfere with the way they make ATP?
And so, anesthetics work by effectively giving you an energy deficit so the brain closes down.
That would be dull if it were true, but it would be useful to know if it were true.
But much more excitingly would be, do mitochondria generate the kind of fields that I was talking about in bacteria that are giving some kind of indication of your status in certain mitochondria, certain neurons?
And that anesthetics interfere with that.
That would be magical if that were true.
That would be a whole new direction of research, which would be fantastic.
And we, you know, it's very difficult measuring fields.
It's very easy to measure artifacts that you don't know what you're really doing.
We need more physicists working in this area to
do the hard calculations.
And we need more data on, you know,
what actually,
is it really just just in one of these respiratory complexes, complex one?
So there's lots of standard molecular biology that we can do.
And it's beginning to point to this idea that, yes, there's something going on about the way that complex one works, which may link to generating fields that may link to how anesthetics work.
And that's
just fun.
The thing that's great about science is it's really fun.
And it's one thing I'm always trying to get across to the people in my lab.
You can't forget the fun.
If it becomes drudgery, then you best go because you'll make much more money somewhere else.
You'll have a better life somewhere else.
But if what you really care about
is the science and the experiments, it's got to be fun.
You've got to really enjoy wanting to go and do that.
And I have to say, one of the great things for me is it's always been fun.
Yeah.
And it's been great to vicariously get a sense of that feeling from reading your books.
Thank you.
For the audience, this conversation has been most coupled with Nick's book, The Vital Question.
And so I would recommend getting that if you want to better
follow the argument here.
And there's a way more detail there that
would be helpful.
And
I think, one, this is the thing I was telling you earlier, that it fills a niche of books, which unfortunately there's just very few of.
So there's textbooks, which, yeah, you can spend 2,000 pages learning about molecular biology, but a lay person just is practically, who's curious, is just practically not going to get a chance to do that.
On the other end, there's what are basically just like anecdotes about scientists or anecdotes about the history of science.
And this, you know, this one discoverer was really mercurial, and here's how he ran his lab, and here's what his parents were like.
But it never really talks about the actual relevant science.
And a book like this actually does fill the explanatory middle.
Yeah, thank you.
Yes.
I mean,
I think the physicists are very good at writing books about the big questions of the universe.
And there's a good large readership for having your mind blown by a book that you're not going to understand everything because you know it's difficult.
And how do we know anything at all about the Big Bang or how black holes work or background radiation or whatever it may be?
And with life, you know, the origin of life or the trajectory of life on a planet and whether we get complex life inevitably or whether we're going to get stuck with bacteria in most places.
These are big questions, you know, universe-sized questions.
And there's not many people writing about them and trying to take you to the edge of what we know
in the way that the physicists very often do.
And just say, well, you know, here's how I see it.
Here's the questions through my eyes.
And you've got to try and be honest and say, okay, I'm not, you know, I see it this way.
Other people see it differently.
Yeah.
But anyway, the fact that LLMs exist has made the process of reading a book like this much more feasible and productive.
So I had a book club with a couple of my friends, and
you know, we're just
not biologists, we're sort of lay people to this audience.
And so, it was,
I do encourage people for a book like this to see if you can form a book club or something, because, and just like talk to LLMs a bunch, because there's just a bunch of extremely basic remedial chemistry in biology that we were able to recapitulate with the help of the LLMs.
And so, you know, this whole thing of why is the CO2O and H2 reaction incentivized when one side is alkaline and one side is acidic in this early environment?
You just go through the remedial chemistry with the LLM.
Yes, I mean, I did my best to explain it in the book, and it seems that I didn't do a great job of it.
But
it's very, there's so much detail, and
you can't avoid that because it's there in the questions.
And this is a problem with biology, it's incredibly complex.
And, you know, physicists look at biology and they think, well, it's just too hard to explain.
And biologists who've got all of this terminology and often get lost in the terminology.
And I find myself by nature trying to find simple common denominators and that lends itself then to writing about them.
But of course, I probably oversimplify all the time or maybe I fail and don't simplify it enough.
But you wrestle with it and you try and make it work.
And it's actually, it's genuinely interesting for me to talk to you and the other guys in the book club
to see where you were struggling with it and where you were.
I will build this into next time I'm writing a book, I'll try and figure out, okay, how do I do that better?
Well, Nick, this has been great.
And yeah, thank you for the guide through both the remedial biology and chemistry, but also through many of the most interesting questions that you could ask about life.
Been great fun.
Thanks a lot.
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