Chapter 10 Flashcards
Fossil Record
Information derived from fossils that help map out the history of life on Earth - Geologic time frame.
Fossil
Preserved body, impressions or traces of a dead organism.
Process of fossilisation
- Remanents of organisms covered by sediment, therefore not exposed to oxygen, microorganisms + other disturbances.
- Over sediment layers build + compact until pressure cements together to form sediments.
- Fossilised remains can take many forms including permineralised, mould or cast fossil.
Conditions that increase the chance of fossilisation
- Physical protection from scavengers + decomposers.
- Areas of rapid sediment accumulation.
- Constant cool temperatures.
- Low oxygen.
- Low light exposure.
Using the fossil record - relative dating
Uses the law of fossil succession to assign a relative age in relation to other fossils and rock strata.
- Use transitional fossils.
Transitional fossils
Assist in relative dating.
- Shows traits common to both ancestral and descendant groups. - Shows the evolutionary changes.
Is useful when the descendant group is physically distant from the ancestral species.
Using the fossil record - absolute dating
Known half-lives or different radioisotopes can be used to measure the absolute (estimated) age of a fossil.
Radioactive isotopes
Radioactive atom of a specific element that breaks down into a predictable + stable product.
Absolute dating is based on:
- Radioisotopes.
- Breakdown of these atoms is constant + can be modelled.
- Half-life; amount of time before half of the mass of the radioisotope is broken down into predictable + stable products. 14C –> 14N.
Radiocarbon dating
Form of absolute dating that determines the age of a fossil by measuring properties or radiocarbon (a radioactive isotope of carbon).
General principles of radiocarbon dating.
- Living things exist as a ratio between 12C (isotope; stable) and 14C (radioactive isotope).
- Death of an organism –> 14C decays and breaks down into 14N(stable). 12C remains the same.
- 14C is used to measure how long ago a fossil died. Comparing the ratio to the ratio in the atmosphere.
Homologous structures
Features found in different species that may look and function very differently from one another but derived from the same ancestor.
Analogous structures
Features present in 2 or more species with the same function, but don’t originate from a common ancestor.
Vestigial structures
Features that have lost all or most of their usefulness as a result of revolution.
eg. Human coccyx (tail bone) was used to balance in trees –> modern humans now use inner ears to help balance on the ground.
Aminoacid sequence similarity
Compare amino acid sequences to determine how related different organisms are.
- Haemoglobin
- Cytochrome c.