What was life's first sunblock?Since the early Earth lacked a protective layer of atmospheric ozone, researchers have wondered what shielded the primordial building blocks of life from destruction by ultraviolet (UV) light. Two chemists now argue that tarlike organic polymers in the oceans could have provided an ancient sunscreen sunscreen /sun·screen/ (-skren) a substance applied to the skin to protect it from the effects of the sun's rays. sun·screen n. for the amino acids and nucleic acid nucleic acid, any of a group of organic substances found in the chromosomes of living cells and viruses that play a central role in the storage and replication of hereditary information and in the expression of this information through protein synthesis. bases forming there. Biochemists Stanley L. Miller and H. James Cleaves at the University of California, San Diego UCSD is consistently ranked among the top ten public universities for undergraduate education in the United States by U.S. News & World Report.[3] It is a Public Ivy. [1] For graduate studies, most of UCSD's Ph.D. used an experimental approach that Miller had pioneered 45 years ago. In that 1953 study, Miller showed how the organic building blocks of life could have developed in the primordial ocean. In the new study, published in the June 23 issue of Proceedings of the National Academy of Science, Miller and Cleaves focused on a class of UV-screening polymers called tholins, which resemble kerogen kerogen or kerogen shales or kerogenites Complex mixture of compounds with large molecules containing mainly hydrogen and carbon but also oxygen, nitrogen, and sulfur. Kerogen is a precursor of petroleum and the organic component of oil shales. , a gunky material in oil shale oil shale Any fine-grained sedimentary rock that contains solid organic matter (kerogen) and yields significant quantities of oil when heated. This shale oil is a potentially valuable fossil fuel, but the present methods of mining and refining it are expensive, damage the that yields petroleum. As in the 1953 experiment, they simulated organic reactions in the early oceans by heating a mixture of nitrogen, methane, and water. Tholins and other organic compounds resulted. Tholins, which absorb UV light well, may have given those seas a yellowish hue, Miller says. Tholins in the top 2 millimeters of ocean water would have blocked all but 1 percent of a damaging wavelength of UV light, Miller says. He suggests that this screening would have been adequate for protecting newly formed organic building blocks. Furthermore, the biochemists argue, a variety of ocean-based compounds, including dissolved salts, sulfur or iron, an ice cap, or a worldwide slick of naturally produced oil, could have supplemented this UV protection. "This shows that there could have been a whole variety of shielding candidates in the early oceans, and that's good to know," said Christopher E Chyba, a planetary scientist at the University of Arizona (body, education) University of Arizona - The University was founded in 1885 as a Land Grant institution with a three-fold mission of teaching, research and public service. in Tucson. |
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