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Prebiotic Chemstry

Prebiotic Chemstry. Jeff G. Wardeska, PhD Jan. 24, 2008. Two Questions. 1. How were the molecules necessary for the first living organisms synthesized? 2. Could life as we know it exist elsewhere in the universe?.

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Prebiotic Chemstry

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  1. Prebiotic Chemstry Jeff G. Wardeska, PhD Jan. 24, 2008

  2. Two Questions • 1. How were the molecules necessary for the first living organisms synthesized? • 2. Could life as we know it exist elsewhere in the universe?

  3. 1. How were the necessary molecules for the first living organisms synthesized? • What molecules are needed to make the simplest cell, e.g., virus?

  4. 1. How were the necessary for the first living organisms synthesized? • What molecules are needed to make the simplest cell, e.g., virus? • 1. Protein; 20 amino acids.

  5. 1. How were the necessary molecules for the first living organisms synthesized? • What molecules are needed to make the simplest cell, e.g., virus? • 1. Protein; 20 amino acids. • 2. DNA; 4 bases (A, G, C, T), PO4-3, ribose.

  6. 1. How were the necessary molecules for the first living organisms synthesized? • What molecules are needed to make the simplest cell, e.g., virus? • 1. Protein; 20 amino acids. • 2. DNA; 4 bases (A, G, C, T), PO4-3, ribose.

  7. 1. How were the necessary molecules for the first living organisms synthesized? • What molecules are needed to make the simplest cell, e.g., virus? • 1. Protein; 20 amino acids. • 2. DNA; 4 bases (A, G, C, T), PO4-3, ribose. • 3. Proper conditions

  8. Today’s Atmosphere • Oxidizing: N2, O2, CO2, H2O • Organic Molecules are oxidized. • CH4 + 2 O2 -> CO2 + 2 H2O • Unique to Earth. • Fe3+; Fe(OH)3, Ksp ~ 10-39.

  9. A. I. Oparin, 1938 • The Origin of Life. (Dover, 2nd edition) • Original atmosphere- reducing. • H2, CO, CH4, NH3, H2O, (H2S). • Oxygen is the result of Life on Earth. • Fe2+ primary form of iron.

  10. Miller-Urey Experiment • 1950. • Reacted Mixture of CH4, NH3, H2, H2O.

  11. Miller-Urey Experiment • 1950. • Reacted Mixture of CH4, NH3, H2, H2O. • Produced about 20 amino acids (<2% yield, each),+ HCN. • Reacted about 15% of C.

  12. Miller-Urey, cont’d • Can form amino acids under a variety of conditions; • UV light energy. • Sound. • Heat. • + H2S -> cysteine. • HCN -> A, G • +HCCCN -> C, U (Cyanoacetylene)

  13. What’s the evidence that this chemistry might have actually happened? • Murchison Meteorite, Australia, 1969. • Geologic Record.

  14. Murchison Meteorite • Sept. 1969, Australia

  15. Murchison Meteorite • 1. Large number of amino acids, > 50 not found on earth. • 2. Slight enantiomeric excess of l-enantiomers in some. • 3. Diff. 15N/14N ratio from terrestial samples. Same ratio in both d & l enantiomers.

  16. Precambrian Era, Mya

  17. Precambrian, cont’d. • 3800. Oldest rocks, oceans form. • 3500-2800. 1st prokaryotes, photosynthesis produces O2. • 2800-1600. Banded Iron Formations.

  18. Stromatolites

  19. Banded Iron Formations

  20. Issues • Origin of l-forms of amino acids. • Mechanism of synthesis of nucleosides and nucleotides. • Chicken vs. egg; which came first, DNA or proteins? • RNA world?

  21. Are we alone?

  22. Further reading • Stanley L. Miller and Leslie E. Orgel, “The Origins of Life on the Earth”, Prentice-Hall, 1974. • Antonio Lazcano* and Stanley L. Miller, “The Origin and Early Evolution. Review of Life: Prebiotic Chemistry”, the Pre-RNA World, and Time.Cell, Vol. 85, 793–798, June 14, 1996. • Leslie E. Orgel, “Prebiotic Chemistry and the Origin of the RNA World”, Critical Reviews in Biochemistry and Molecular Biology, 39:99–123, 2004

  23. Thank You!

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