Fossils and Stuff Flashcards
Explain how the amount of potassium-40 can provide information about the age of the sample.
Potassium-40 is a radioactive isotope, it will decay into calcium-40 and argon-40. By measuring the amount of potassium-40 and argon-40 in a rock sample it is possible to calculate the age of the rock. As the rock ages, the proportion of potassium-40 decreases and the proportion of argon-40 increases.
What types of samples are able to be dated using potassium–argon dating?
Rocks, of volcanic origin that are at least 100 000 – 200 000 years old.
What types of samples are able to be dated using carbon-14 dating?
Organic samples that are less than 70 000 years old.
Explain why the principle of superposition cannot be considered without taking other factors into account.
The principle of superposition assumes the layers of sedimentary rock are not disturbed through Earth crust distortions or through human activities of burial or mining.
Describe index fossils and explain their relevance to relative dating.
Index fossils are distinctive fossils that were widely distributed and present on Earth for a limited period of time. They are used in correlation of rock strata and improve the reliability of relative dating of strata. If an index fossil is found in two strata layers, it can be confirmed that these strata layers are of the same age, even if they were located thousands of kilometres away from each other.
Suggest what happens when potassium-40 decays to form calcium-40 and argon-40.
When Potassium-40 undergoes beta-decay, one neutron is converted to a proton, changing the atom to Ca-40. This occurs about 89% of the time. Around 11% of the time, K-40 undergoes electron capture which converts a proton to a neutron, changing the atom to Ar-40.
Explain why carbon-14 dating can only be used to determine the age of samples that were once living.
Carbon-14 is formed in the upper atmosphere and enters the food chain through the process of photosynthesis converting the C-14 in the carbon dioxide molecule into a glucose molecule. The glucose is then consumed, and the C-14 isotope is assimilated into the body tissues of the organism. Once the organism dies the C-14 decays into nitrogen and the ratio of C-14 to C-12 can be measured.
Potassium-40 half life
1250 billion years
Carbon-14 half life
5730 years
Polymerase chain reaction
- Enables small quantities of DNA to be replicated → produce testable amount.
- Steps are repeated 2-3 times in thermocycling.
- Takes ~2-3 hours to produce a billion DNA copies.
Uses a heat-stable DNA polymerase like Taq polymerase, which is derived from the heat-loving bacterium Thermus aquaticus.
PCR step temperatures
Denaturation - 94-96 degrees (temp breaks hydrogen bonds.)
Annealing - 50-60 degrees (primers bind, serve starting point of DNA replication.)
Extension - 70 degrees (DNA polymerase joins new, complementary nucleotides to sections with primer.)
Restriction enzyme
- Added to DNA sample
- Cuts strand into different lengths dependent on the sample’s base sequence.
- Lengths of pieces can be analysed and compared with other DNA samples.
- Used before gel electrophoresis
Gel Electrophoresis
Technique that is able to separate DNA strands based on their lengths.
- DNA ladder contains DNA fragments of a known length.
- Results from unknown sample can be compared to the ladder to determine the length of the DNA strands in the sample.
DNA Sequencing
Determination of the precise order of nucleotides in a DNA sample.
Ethics DNA
- Autonomy: respect for the right to be self-determining and to choose whether or not to be tested, and if tested, to know and share the information.
- Confidentiality: genetic information use is treated sensitively, and only accessed by those authorised.
- Equity: right to fair and equal treatment regardless of genetic information.
- Privacy: right to be ‘left alone’ to make decisions regarding genetic testing and resulting information, independent of others.