ch 23: Natural Selection Flashcards
The current theory about how life arose consists of four main stages
- Small organic molecules were synthesized.
- These small molecules joined into macromolecules, such as proteins
- All these molecules were packaged into protocells, membranes containing droplets, whose internal chemistry differed from that of the external environment.
- Self-replicating molecules emerged that made inheritance possible.
Earth formed since …
4.6 Billion years ago, Because of the heat from the bombardment of rock left over from the formation of the universe any water available was vaporized and seas were prevented from forming.
What happened after rocks bombarded
When this slowed The atmosphere was theorized to be composed of water vapor, nitrogen, oxides, CO2, CH4, Ammonia, Hydrogen, and Hydrogen sulfides. (volcanos)
What happened as the earth cooled
As the earth cooled the water condescended and oceans formed much of the hydrogen escaped into space
When did life arise
Life emerged 3.8 to 3.9 Billion years ago (first ¾ Earth’s history all life was microscopic and primarily unicellular.) Prokaryotes fossils 3.5 Billion years ago
Oparin and Haldane
independently hypothesized that the atmosphere was a reducing environment.
What 2 steps were taken by Oparin and Haldane
- Powered by lightning and intense UV radiation
2. This reducing environment could cause organic synthesis
Miller and Urey
Test this hypothesis and produced a variety of amino acids.
However, the evidence is not yet convincing that the early atmosphere was in fact reducing
Miller-Urey–type experiments demonstrate that organic molecules could have formed with various possible atmospheres
instead in Miller and Urey experiment
Instead of forming in the atmosphere, the first organic compounds may have been synthesized near volcanoes or deep-sea vents
what was the first genetic mat
It is hypothesized that self-replicating (auto-catalytic) RNA (not DNA) was the first genetic material.
RNA
- Plays a central role in protein synthesis
2. Can also act as an enzyme
Relative dating
using the order of rock strata to determine the relative age of fossils.
Radiometric dating
using the decay of radioactive isotopes to determine the age of the rocks or fossils. Based on the Half-life (rate of decay) of isotopes.
The earliest living organisms were
prokaryotes
About 2.7 Billion years ago
Oxygen began to accumulate because of photosynthesis