| I also do not believe that our RNA and complex amino acids are likely to be universal. On the other hand, the simple amino acids are known to be universal, both from chemical analyses of celestial bodies and from abiotic syntheses in laboratories. In theory, sugars can be produced abiotically by the polymerization of formaldehyde. However, sugars are not very stable chemically and suitable catalysts for formaldehyde polymerization seem to be rare, because sugars are much less ubiquitous than amino acids in lifeless environments. The role of phosphorus in biology is determined entirely by the property of the phosphate anions that they can eliminate water and condense into polyphosphates, then the polyphosphates can extract water from other molecules, forcing condensation reactions, which can be used for various purposes, e.g. for building polymers. The nucleoside parts of ATP and related substances play only the role of a "handle", which can be used to control the location of the polyphosphate parts, so that they will perform their function where intended. Thus for controlling the polyphosphates other molecules may also be suitable. Disulfide bonds, which already exist in the pyrite mineral, must have had a crucial role in the origin of life. But their role is very different from that of polyphosphates, because they extract hydrogen, instead of extracting water, so they perform redox reactions, not condensation/hydrolysis reactions. Thioesters are the sulfur compounds that can play the same role as ATP, by taking part in condensation/hydrolysis reactions. There is no doubt that all the 5 elements H, C, N, O and S, which happen to be the most abundant electronegative elements in the entire Universe, must be used by any living being, since the origin of life. Whether phosphorus has also been used since the beginning, or it is a later addition, is uncertain, because thioesters could have been used originally for performing all the functions now done with phosphates like ATP. Both nitrogen and phosphorus are affected by similar availability problems. While nitrogen is too volatile and most of it would always have been stored in dinitrogen gas, which is inert, instead of being stored in easy to use ammonia or hydrogen cyanide molecules (while hydrogen cyanide and carbon monoxide are now toxic for most living beings, it is likely that they both are very important for the appearance of life), for phosphorus the problem is that most of it is stored in insoluble phosphate minerals. This must have been alleviated around the origin of life by the fact that the early oceans were much more acidic than today, so much more phosphate ions would have remained dissolved in sea water, than today. Unlike for phosphorus, there is no substitute for nitrogen in biology. The role of nitrogen in organic molecules is the same as the role of dopants in semiconductor devices. When nitrogen substitutes carbon in an organic molecule, that position in the molecule becomes positively charged, instead of being electrically neutral. These electric charges play very important roles in many chemical reactions. The poor availability of nitrogen must have been the main constraint in the growth of the early forms of life, until the development of the nitrogenase catalysts that allow the use of dinitrogen from the atmosphere. Similarly, it is likely that the earliest forms of life used carbon from carbon monoxide, whose lower availability limited growth until the development of a catalyst that reduces carbon dioxide to formic acid, which allowed the use of the more abundant carbon dioxide. Both catalysts, which are used to capture carbon dioxide and dinitrogen, appear to have used in their earliest variants molybdenum, or possibly the related tungsten. While molybdenum seems to be a later addition to the set of chemical elements used for life, iron, cobalt and nickel are all necessary for the appearance of life as catalysts, while potassium is also necessary since the beginning for maintaining the electrical neutrality of a water solution without producing solid precipitates that would cause death. The abilities to use directly carbon dioxide and dinitrogen, which are the main constituents of most planetary atmospheres, and which were also the main constituents of the early atmosphere of the Earth, must have greatly expanded the environments suitable for life, which previously must have been restricted to small neighborhoods of hydrothermal vents or sources of volcanic gases. |
These suggest that the life chemistry evolved in the proto solar cloud (and exploring the conditions in there would yield how that happened) and the life on Earth evolved from the already complex stuff that fell on it after the hadean phase.