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Zoology · Ch 6 — Evolution

Biological Evolution — Formation of Protobionts

6.3

Biological Evolution — Formation of Protobionts

Biological evolution begins with the transition from simple organic chemistry to structures that behave like living matter. Abiotically produced molecules can spontaneously self-assemble into droplets that enclose a watery interior chemically distinct from their surroundings — scientists call these spheres protobionts. Liposomes are one such example: lipids in solution that self-assemble into a lipid bilayer membrane; once some of the enclosed proteins acquired enzyme-like activity, the molecules inside could multiply faster. Coacervates containing nucleoprotein and nutrients, bounded by a limiting membrane, began to resemble a virus or a free-living gene; as more genes came together, they formed 'proto-viruses' broadly comparable to present-day viruses. Two early cell types are thought to have emerged from this process: one, containing loose clumps of nucleoprotein within the cell substance, resembled the Monera and is considered ancestral to modern bacteria and blue-green algae; the other, whose nucleoprotein clumps condensed into a membrane-bound central mass, is called Protista-like. As food sources in the primitive ocean dwindled, the descendants of these early Monera- and Protista-like cells had to diversify their nutrition — evolving parasitism, saprophytism, predation, and chemosynthesis or photosynthesis. As photosynthetic organisms increased, free oxygen accumulate …

Experimental Approach to the Origin of Life — Urey–Miller Experiment

Stanley Miller and Harold Urey (1953) put the Oparin–Haldane hypothesis to an experimental test, and their result is depicted in Fig. 6.1. They circulated a mixture of gases representing the primitive atmosphere — ammonia, methane and hydrogen — through a closed apparatus, continuously mixed with steam from a separately boiled flask of water. An electric spark discharge from a tungsten electrode, standing in for lightning, was passed through the gas mixture inside the main chamber. The circulating vapour was then cooled in a condenser and collected as liquid at the base of the apparatus. The experiment ran continuously for a week, after which the collected liquid was chemically analysed. Glycine, alanine, beta-alanine and aspartic acid — all genuine amino acids — were identified among the products, even though the only carbon source supplied was methane gas. This was powerful evidence that abiogenic synthesis of organic building blocks was chemically plausible under early-Earth-like conditions. Later, simil …

Figure 6.1Fig. 6.1 Diagrammatic representation of Urey–Miller's experiment

What this figure shows. The apparatus diagram shows a large glass reaction chamber holding a circulating gaseous mixture of methane (CH4), ammonia (NH3), hydrogen (H2) and water vapour (H2O). A separate flask of boiling water is connected to the chamber so that its steam mixes continuously with the gas mixture. Inside the large chamber, a pair of tungsten electrodes produce a spark discharge that simulates lightning striking the primitive atmosphere. The gases and steam then pass into a condenser, labelled with 'water out' and 'cold water in' to show the direction of cooling-water flow, which cools the circulating vapour back into liquid. The condensed liquid collects at the base of the apparatus as an 'aqueous medium containing organic compounds', and a tap is shown at this collection point for withdrawing a sample for chemical analysis. The whole assembly forms a continuous closed loop so the …