• Possible solutions proposed:
◦
Volcanic settings or lightning strikes could transiently mobilize phosphates.
◦
Schreibersite (Fe₃P), found in meteorites, could have delivered reactive
phosphorus to early Earth. It forms phosphite, which is more soluble and
reactive.
◦
Some dry–wet cycling environments (like tide pools) may help concentrate
phosphates and drive condensation reactions.
But yes, phosphate scarcity remains a major bottleneck, and no single solution has been fully
demonstrated in a realistic prebiotic setting.
🔁 2. Partial synthesis of amino acids and nucleotides
• Miller-Urey: Only got 11 of the 20 proteinogenic amino acids. Later versions with
different atmospheric assumptions (e.g. volcanic gases, HCN chemistry) increased yields.
• Nucleobases: Adenine can be made from 5 HCN molecules in water. Guanine, cytosine,
and uracil are harder, but some prebiotic pathways have been demonstrated, especially
under UV or impact shock.
• Ribose: The formose reaction can make sugars from formaldehyde, but it’s messy and
yields are low. Ribose is chemically unstable, and this remains a problem.
• Nucleotides: The prebiotic synthesis of nucleotides from ribose + base + phosphate is
nontrivial. Yet in 2009, Sutherland et al. proposed a "unified pathway" where some
precursors can build ribonucleotides under plausible prebiotic conditions—bypassing the
need to bolt sugar, base, and phosphate together separately.
But again, polymerization into RNA remains hard without enzymes or activated phosphates—
requiring either chemical activation or speculative settings.
🧪 3. Polymerization Without Enzymes
You rightly point out that even if you get nucleotides, getting them to polymerize into
meaningful RNA or DNA is another big step.
• In lab settings, scientists use activated nucleotides (e.g., imidazole derivatives), which
wouldn’t be present naturally.
• Hypothetical workarounds include: