The Fossil Record Flashcards
Fossil
Preserved body, impressions or traces of a dead organism
Fossil record
The information derived from fossils
Conditions for fossil formation (7)
- Rapid sediment accumulation
- Constant cool temperatures
- Low light availability
- Protection from scavengers and decomposes
- Hard body parts
- Low winds
- Constant humidity (moderate + stable)
Steps in fossilisation
- Organism is covered by sediment
- Overtime, layers of sediment and pressure builds, forming sedimentary rock
- Lack of oxygen, microorganisms and disturbances allow preservation to occur
4 Types of fossils
Pre-mineralised fossils, trace fossils, mould fossils, cast fossils
Pre mineralised fossil
Formed when minerals from groundwater replace most or part of the actual structure if the organism
Trace fossils
A fossil indicating the existence of an organism rather than the organism itself (e.g nests, footprints, faeces)
Mould fossils
Formed when an organism completely decays after being buried in sediment, leaving its impression only
Cast fossils
Organism decomposes or leaves quickly, leaving a mold that gets filled with material and covered by sediment, creating a cast. This shows shape of organism without organic material
Two main techniques for dating fossils
Relative and absolute dating
Relative dating
Based on the law of fossil succession - fossils of the same age will be in the same layer of sedimentary rock, fossils found in lower sedimentary layer will be older. Also use index fossils to determine the age, and transitional fossils
Index fossils
Used as a reference to easily determine the age of unknown fossils
Index fossils must be…
-physically distinctive
-have had a large population
-have existed jn many geographical areas
-only lived within a short period of time
Transitional fossils
A fossil that shows traits common to both its ancestral and descendant groups.
What can a transitional fossil help with?
-help demonstrate evolutionary changes
-help the timeline
Events of earth in order
Prokaryotes -> photosynthesis -> eukaryotes -> multicellular organism -> animals in land -> mammals -> flowering plants -> genus homo
Absolute dating
Determines the absolute age of a fossil by measuring relative amounts of radioisotopes to their products
Carbon dating
- Carbon 14 breaks down into more stable product, nitrogen 14
- After 5730 yrs of an organisms death, half of its carbon 14 atoms would have broken down into nitrogen 14
Half lives
1 half life - 5730
2 half lives - 11 460
3 half lives - 17 190
4 half lives - 22 920
Limitations of carbon dating
After 50 000 years, carbon dating will not work as most of the carbon 14 already would have broken down