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fossils
preserved remains/impression/traces of an old/ancient/extinct organism. This could be footprints, burrows, faeces, impressions of plant or animals, bones, shells or teeth
fossilisation steps
Death and decay- soft body parts are decomposed/scavenged leaving only hard body remains
deposition - the hard remains are rapidly covered with silt, clay, mud, and sand, over time layers build up
Permineralisation- pressure from covering layers of dirt/rock cause the hard organic material to be replaced by minerals
Erosion/exposure- movement of earth plates may displace the fossil and return it to the surface for discovery.
factors affecting
Type of organism- plants- petrified rock is fossilised plant material dissolved salts replace plant tissue.
Soil pH- high phalkaline soil conditions, anoxic (low oxygen) conditions like peat or limestone to protect against oxygen damage and prevent decomposition by saprotrophs( obtain nutirents by eating decay)
Mineral content of soil- high pressure to promote mineralisations,
Weathering- temperature could enough a fossil may be formed when the organism freezes rather than decomposing, due to being dehydrated and preserved
Erosion - only limited amount can occur to not destroy the fossil/organisms. Only for exposure
Time taken to become buried, environment, chemical destruction, mechanical destruction, biological destruction
factors affecting pt2
Time taken to become buried
Environment - some rock does not form fossils, sedimentation is necessary for fossils
Chemical destruction : soil pH, preservation of oxygen
Mechanical destruction : weathering and erosion, trampling by animals
Biological destruction : presence if microorganisms such as bacteria or fungi. Carrion may take away parts of the organism
pH - low pH (acidic envrionment) conditions can dissolve the minerals that form fossils, destroying them in the process.
fossil evidence
Shows past life/extinct organisms, shows the similarities and differences between them
Show that life/environment has changed over time or that life on earth has a long history
Show how one type of organism/structure has transitioned to another
Show us if the organism has developed into homologous or analogous structures- comparative
Evolution and common ancestor
Dating of strata
Identification of new species
fossil evidence pt2
Fossils give us an insight into past life forms
Fossils show the patterns and speed of evolutionary change through gradualism and punctuated equilibrium
Gradualism - evolution occurs as a steady, slow divergence lineages at an even pace -
Theory suggests that sudden bursts of evolution are an illusion
punctuated equilibrium - states that species will remain stable for long periods of time but may then quickly change into new species due to a rapid change in the environment.
Shows us the record of species over time
Gives scientists an understanding of similarities and differenced between current and extinct species demonstrating change.
The distribution of fossils over different continents supports the idea of evolution.
limitation of fossil record
Fossil record provides evidence of extinct organisms. That change has occurred in species and in groups of species over a long peroid of time is evidence by fossils, as well as by the progression of simple to more complex organisms in the fossil record.
Fossil record is total number of fossils discovered and gained information from
Geologic time scale is a system of chronological measurement that describes the timing and relationships between events that have occurred throughout earths history
Fossil record
Looks (shape, size, ect)
Where or how they lived
What other organisms they lived with
Transitional forms
Fossil record is incomplete:
Only hard parts are likely to form fossils or soft parts are unlikely to form fossils
Only organisms that avoid decomposition/scavengers/predators for fossils or fossils only form in areas with no oxygen/bacteria
Only orgnaisms that are buried in sediment/mineral rich water form fossils or rapid burial
Not all fossils have been found yet
Some fossils have been destroyed (volcanic eruptions/human activates/earthquakes)
Not all fossils can be found (too far underground/underwater)
Not all organisms represented
Taxonomic bias- not all fossils have been discovered some organisms may not be represented or other over represented
Undiscovered fossils- older fossils are more difficult to fine. Plate tectonic processes have destroyed or displace fossils
Geographic bias-not all areas produce fossils,
rainforests teeming with life and in a hot and moist climate are also poor places for fossils to form as a carcass can decay quickly and not have time to be buried. Similarly a rocky mountaintop is a poor place for fossils to form with no fine sediments being laid down