Several mechanisms seem likely to have been delivering exogenous organics to the surface of the Earth, or shock-synthesizing them in impacts. In an early carbon dioxide-rich terrestrial atmosphere, these mechanisms would have quantitatively rivaled or exceeded terrestrial organic synthesis in situ. In an early reducing (methane-rich) atmosphere, the exogenous sources would have been quantitatively unimportant compared to atmospheric production.
CITATION STYLE
Chyba, C. F., & Sagan, C. (1997). Comets as a Source of Prebiotic Organic Molecules for the Early Earth. In Comets and the Origin and Evolution of Life (pp. 147–173). Springer New York. https://doi.org/10.1007/978-1-4757-2688-6_7
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