Abstract
THE Oparin–Haldane hypothesis about the origin of life has provided a rational theoretical model for laboratory research. Almost thirty years of experiments have supported this hypothesis. Verification of the hypothesis in terrestrial environments, however, has not been documented. Some environments such as thermal springs in the Kuril Islands have been reported to have possible chemical precursors but lack of sterility and other factors have not made it possible to establish evidence for natural, terrestrial abiotic synthesis1. We identify here the Atlantis II Deep brine as a promising site for searching for chemical precursors, report finding thiocyanate in the brine and suggest a relationship between chemical evolution and the evolution of the Earth's crust.
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DOWLER, M., INGMANSON, D. Thiocyanate in Red Sea brine and its implications. Nature 279, 51–52 (1979). https://doi.org/10.1038/279051a0
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DOI: https://doi.org/10.1038/279051a0
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