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20.7: Life Origins, A Summing Up

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    89046
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    Speculation about life’s origins begins by trying to identify a source of free energy with which to make organic molecules. The first cells might have been heterotrophs formed in a reducing Earth environment, from which autotrophs later evolved. On the other hand, the earliest cells may have been autotrophs formed under non-reducing conditions in the absence of a primordial soup. Then, only after these autotrophs had produced enough nutrient free energy to sustain themselves, did heterotrophs belatedly emerge. Evidence suggesting that the Earth’s atmosphere was a non-reducing one more than 4 billion years ago (soon after the formation of the planet) and suggesting life on Earth 3.95 billion years ago favor metabolic origins of autotrophic life in a thermal vent, likely an alkaline one. Questions nevertheless remain about life-origins under non-reducing conditions. Even the composition of the prebiotic atmosphere is still in contention. For now, let us put these concerns aside and turn to events that get us from the LUCA and its early descendants to the still more elaborated chemistries common to all cells today. The descriptions that follow are educated guesses about early pathways on the road to the familiar cellularity we see now on Earth. They mainly speculate on the selection of catalytic mechanisms, replicative metabolism, the web of intersecting biochemical pathways, and the even more intricate chemical communications that organize cell function and complexity.

    352 Phylogenetic Support for Autotrophs-First Origins of Life


    This page titled 20.7: Life Origins, A Summing Up is shared under a not declared license and was authored, remixed, and/or curated by Gerald Bergtrom.