So let's look quickly at the "prebiotic" synthesis of phospholipids.
In a cell, this is done in the endoplasmic reticulum using an enzymatic process. But we'd like to know how it could be done without a cell, using just the simple chemicals found in a very hot primitive atmosphere.
You'll recall, that a phospholipid has a glycerol backbone with some long chain hydrocarbons. So first, we need long chain hydrocarbons.
This part is pretty easy. We need hydrogen, carbon monoxide, and methane, and it helps if we have a catalyst like iron - all of which were present in large quantities in the "magma oceans" phase of early earth.
In chemistry this is called the Fischer-Tropsch process.
marspedia.org
en.wikipedia.org
Next we need fatty acids, also know as glycerides. (In the body these usually occur in groups of three, called triglycerides).
There's a traditional way of doing this. For this we depend on the minerals present during the "chondrite" phase of the hydrothermal systems in early earth.
But there are also other methods, for example using a nickel catalyst.
www.chemistryviews.org
So at this stage we already have multiple parallel pathways to get the needed fatty acids. The idea is that "all" of these reactions will occur, in proportion to the availability of precursors and catalysts.
Finally we have "phospholipid synthesis", which is a tad more complicated but again multiple abiotic pathways are known. Turns out your buddy Oro was among the first to study this, in the 1995 time frame. Here is a very thorough if somewhat complex review of what is known about abiotic phospholipid synthesis from hydrocarbons and free fatty acids.
So these processes will give you all the essential components of stable cell membranes (lipid bilayers with phospholipids to stabilize them and protect them from cations).
The Fischer-Tropsch process is an excellent example of combinatorial explosion. It works just like Pascal's triangle. You start with two 1-chain hydrocarbons, which then combine to form a 2-chain. Then the 2-chain combines with another 1-chain to build a 3-chain. And so on. The longer you let it run, the longer the resulting chains.
At the end of the process, you have a mixture of varying length chains, with smaller chains being more common. The proportion of each type of chain can be calculated from the chemical kinetics. You end up with a "soup" of hydrocarbons, but since they're all oily and hydrophobic they're going to try to separate from the water and aggregate with themselves. Therefore this process "drives" micelle formation, you end up with round globules with the hydrocarbon tails pointing in and the glycerol end pointing out (because glycerol has CO and OH moieties which are perfectly happy in water).
So now you have one of the essential components of cellular life, which are stable cell membranes. These will just float around in the water, and any time they encounter a calcium ion they will "invaginate" to form a small vesicle inside the larger membrane, taking with them any chemicals that happen to be in the vicinity. This is how you get "compartments" with varying (bio)chemical abilities. Since amino acid synthesis is occurring at the same time in parallel with fatty acid synthesis, some of your compartments will contain amino acids. And since those compartments are now isolated from the larger ocean, there is plenty of time for the amino acids to react with each other and form polypeptides.
In a cell, this is done in the endoplasmic reticulum using an enzymatic process. But we'd like to know how it could be done without a cell, using just the simple chemicals found in a very hot primitive atmosphere.
You'll recall, that a phospholipid has a glycerol backbone with some long chain hydrocarbons. So first, we need long chain hydrocarbons.
This part is pretty easy. We need hydrogen, carbon monoxide, and methane, and it helps if we have a catalyst like iron - all of which were present in large quantities in the "magma oceans" phase of early earth.
In chemistry this is called the Fischer-Tropsch process.
Hydrocarbon synthesis
Fischer–Tropsch process - Wikipedia
Next we need fatty acids, also know as glycerides. (In the body these usually occur in groups of three, called triglycerides).
There's a traditional way of doing this. For this we depend on the minerals present during the "chondrite" phase of the hydrothermal systems in early earth.
But there are also other methods, for example using a nickel catalyst.
Fatty Acids from CO2 and Hydrocarbons - ChemistryViews
Nickel catalyst allows green synthesis of valuable compounds
www.chemistryviews.org
So at this stage we already have multiple parallel pathways to get the needed fatty acids. The idea is that "all" of these reactions will occur, in proportion to the availability of precursors and catalysts.
Finally we have "phospholipid synthesis", which is a tad more complicated but again multiple abiotic pathways are known. Turns out your buddy Oro was among the first to study this, in the 1995 time frame. Here is a very thorough if somewhat complex review of what is known about abiotic phospholipid synthesis from hydrocarbons and free fatty acids.
So these processes will give you all the essential components of stable cell membranes (lipid bilayers with phospholipids to stabilize them and protect them from cations).
The Fischer-Tropsch process is an excellent example of combinatorial explosion. It works just like Pascal's triangle. You start with two 1-chain hydrocarbons, which then combine to form a 2-chain. Then the 2-chain combines with another 1-chain to build a 3-chain. And so on. The longer you let it run, the longer the resulting chains.
At the end of the process, you have a mixture of varying length chains, with smaller chains being more common. The proportion of each type of chain can be calculated from the chemical kinetics. You end up with a "soup" of hydrocarbons, but since they're all oily and hydrophobic they're going to try to separate from the water and aggregate with themselves. Therefore this process "drives" micelle formation, you end up with round globules with the hydrocarbon tails pointing in and the glycerol end pointing out (because glycerol has CO and OH moieties which are perfectly happy in water).
So now you have one of the essential components of cellular life, which are stable cell membranes. These will just float around in the water, and any time they encounter a calcium ion they will "invaginate" to form a small vesicle inside the larger membrane, taking with them any chemicals that happen to be in the vicinity. This is how you get "compartments" with varying (bio)chemical abilities. Since amino acid synthesis is occurring at the same time in parallel with fatty acid synthesis, some of your compartments will contain amino acids. And since those compartments are now isolated from the larger ocean, there is plenty of time for the amino acids to react with each other and form polypeptides.