By Alexander Clement
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Ca. 1350 K and down to 700 K+). They point out that studies of volcanic gases suggest equilibrium may be maintained down to 700 K (Gerlach 1993; Symonds et al. ) catalysts may be important at still lower temperatures. In the case of smaller impacts where the impact cloud expands and cools relatively quickly, there would probably be plenty of catalytic material (silicate and metal dust) still entrained in the cloud to maintain equilibrium. In the case of both small and large impacts, the likely accompaniment by smaller meteoroids would add both local energy and catalytic material.
G. Yamagata et al. 1991), by acting as a dehydrating agent. In addition, some of the most critical compounds for life (and presumably necessary before life could emerge) are mono and polyphosphates of nucleotides such as AMP, ADP and ATP, respectively the mono-, di- and triphosphates of adenosine. Synthesis of these compounds presumably requires the presence (especially under pre-biotic conditions) of rather high concentrations of phosphate. Phosphorus is an important trace element in igneous rocks, probably the most abundant rock type present in Hadean crust.
In fact, the presence of isolated pools may not be as important for concentrating organics as for providing “test reactors” and “reservoirs” for more highly processed prebiotic materials. If the previous arguments for pervasive reducing conditions during degassing are correct, the production of reduced CHNO compounds from a high degree of degassing of accreted late veneer, and early generation of an ocean approximately the same volume as at present (by the end of accretion and degassing), leads to interesting conclusions about the organic content of that early ocean.