| Autor: |
Todd ZR; Department of Earth and Space Sciences, University of Washington, Seattle, Washington, USA.; Department of Chemistry, Department of Astronomy, University of Wisconsin-Madison, Madison, Wisconsin, USA., Lozano GG; Center for Astrophysics, Harvard and Smithsonian, Cambridge, Massachusetts, USA., Kufner CL; Center for Astrophysics, Harvard and Smithsonian, Cambridge, Massachusetts, USA., Ranjan S; Lunar & Planetary Laboratory/Department of Planetary Sciences, University of Arizona, Tucson, Arizona, USA., Catling DC; Department of Earth and Space Sciences, University of Washington, Seattle, Washington, USA., Sasselov DD; Center for Astrophysics, Harvard and Smithsonian, Cambridge, Massachusetts, USA. |
| Abstrakt: |
Ultraviolet (UV) light is likely to have played important roles in surficial origins of life scenarios, potentially as a productive source of energy and molecular activation, as a selective means to remove unwanted side products, or as a destructive mechanism resulting in loss of molecules/biomolecules over time. The transmission of UV light through prebiotic waters depends upon the chemical constituents of such waters, but constraints on this transmission are limited. Here, we experimentally measure the molar decadic extinction coefficients for a number of small molecules used in various prebiotic synthetic schemes. We find that many small feedstock molecules absorb most at short (∼200 nm) wavelengths, with decreasing UV absorption at longer wavelengths. For comparison, we also measured the nucleobase adenine and found that adenine absorbs significantly more than the simpler molecules often invoked in prebiotic synthesis. Our results enable the calculation of UV photon penetration under varying chemical scenarios and allow further constraints on plausibility and self-consistency of such scenarios. While the precise path that prebiotic chemistry took remains elusive, improved understanding of the UV environment in prebiotically plausible waters can help constrain both the chemistry and the environmental conditions that may allow such chemistry to occur. |
