Chapter Four: Evolution Flashcards
Evolution
The gradual development of organisms over time.
Common Descent (3)
- All organisms are composed of cells
- All take in chemicals and energy from the environment
- All reproduce, respond to stimuli, and evolve
Fossil
The preservation of the general shape of an organism. Formed when minerals in the earth harden over it’s body upon its death
Transition Fossil
A fossil representing an evolutionary link in the fossil record, indicating a common ancestor
Strata
Layers of the earth representing geological periods of time.
Relative Dating
- Fossil dating method using layers of strata to determine which era it came from. The lower the strata, the older the fossil
- Only accurate if the strata has not been twisted or upturned from natural processes
Radiometric/Absolute Dating
Dating method which uses the half-lives of isotopes present in the fossil to determine its age. In organic fossils, carbon is typically used.
Mass Extinction
Event that extinguishes a large number of organisms in a short period of time. This causes only the most well-adapted organisms to survive.
What is an example of a mass extinction?
The Cretaceous period; a large number of meteorites hit the earth and the debris blocked the sunlight. Many plants and animals died.
Biogeographical Evidence for Evolution
- Study of the distribution of plants and animals
- continental drift shown through distribution of similar fossils on different continents: evolving species unable to migrate
Homologous Structure ( + example)
Has same function and basic structure, indicates a common ancestor
ex) A human arm and a whale forelimb
Analogous Structure ( + example)
Same basic function but different origin
ex) bird’s wing and bee wing
Vestigial Structure ( + example)
Anatomical structure fully functional in one group and reduced or nonfunctional in another
ex) Human coccyx (tailbone)
Biochemical Evidence for Evolution
- All organisms have the same three basic biochemical molecules: DNA, ATP, and general enzymes
- The degree of similarity between DNA base sequences and amino acid sequences indicate the degree of relatedness
Evolution of micromolecules
Earth’s early atmosphere according to Miller was full of methane, hydrogen, and ammonia
-when applied with enough each (ex lightning) these molecules could form organic compounds and amino acids
Miller Experiment
Simulated conditions of early earth (methane, hydrogen, and ammonia) and applied an electric spark. Yielded amino acids without the use of oxygen.
Macromolecules: RNA first hypothesis
RNA functioned both as an enzyme and a substrate. Some viruses use RNA as their genetic material
Macromolecules: Protein first hypothesis
Sidney Fox’s experiments
- amino acids can form polypeptides when exposed to dry heat
- amino acids collected in puddles and formed proteinoids within microspheres
Microsphere
A chemical reaction separated from its environment
Macromolecules: Cairnes-Smith hypothesis
- Proteins and RNA at the same time: Clay attracted small organic molecules, which served as inorganic catalysts for polypeptide formation
- Fueled by energy from radioactive decay
The Protocell
- Proposed structure of a protein-lipid membrane which carried on an energy metabolism
- Microspheres were exposed to lipids, created a coacervate with a protein-lipid membrane
- the phospholipid automatically formed a liposome
Coacervate
Microscopic spontaneously formed spherical collection of lipid molecules, held together by electrostatic forces
Liposome
A spherical structure with at least one lipid bilayer
The Heterotroph Hypothesis
- Since nutrition was plentiful in the ocean, the first organism was probably a heterotroph
- used ATP first; was a fermentative process
- Had a catalytic ability like microspheres and took in available enzymes (beginning of glycolysis)
The True Cell (RNA first hypothesis)
-First true cell had RNA genes; reverse transcriptase produced DNA from RNA