Evidence for evolution Flashcards
Evidence for evolution
Fossils, comparative studies (biochemistry)
Fossil
Preserved trace (E.g foot print) or evidence left by a previously living organism, E.g bones, exoskeletons (shells), teeth
Artefact
Any object made by a human, E.g tools, coins, boomerang, pyramids
What do fossils show
Show the sequence of development in plant and animal species and establishes evolutionary links between species/shows common ancestry
What do fossils provide
Evidence of which organisms lived on Earth in the past, Examples of organisms which may now be extinct, Examples of transitional organisms (exists between species) between species
Good conditions for fossil formation (3)
Rapid burial helps in the formation of fossils at time of death, E.g drifting sand (desert), mud (mud slides), volcanic ash, Specific sediment features are required for fossilisation such as no or lack of oxygen (means bacteria can’t break fossil down)/alkaline soils- Alkaline soils produce the best fossils as minerals from the soil are deposited in the pores of the bone, replacing the organic matter that makes up the bone, petrifying it but preserving the structure, Fossil is left undisturbed for a long period time
Poor conditions for fossil formation (5)
Scavengers (bacteria, worms, vultures, rats), Micro-organisms (bacteria) that decay the fossil, Destruction of the fossil by volcanic eruption (melts fossil) or earthquakes, folding/faulting of the earth moving the fossils deep into the earth’s surface, Weathering (breaking down through chemicals or water) or erosion (moves fossil by natural conditions), Human (mining, building) or anima (burrowing) activity
Reasons for incomplete fossil record
Fossils may not be recognised by humans, Humans may not be looking in the right place for the fossils, Layers of rock containing fossils may not be exposed at the surface (hard to find deeply buried fossils)
Absolute dating
Stating actual age in years (Potassium-Argon dating, Carbon 14 dating)
Relative dating
Giving comparisons between the age of fossils (Stratigraphy)
Carbon 14
Radioactive isotope produced by cosmic radiating changing nitrogen 14 into carbon 14 in the upper atmosphere, Half-life (time it takes to get to half itself) is around 5700
How does carbon dating work
Amount of C14 in the atmosphere is constant and is absorbed by plants through photosynthesis meaning it is passed through the food chain when organisms eat plants or other animals which have eaten the plans, Constant amount of C14 in a living organism but decreases when an organism dies, Amount of C14 in the remains indicates the number of half-lives that have passed
Limitations of carbon dating
Only used on organic fossils (once living, E.g charcoal) that are less than 70,000 years old, Normal radiocarbon dating (most common) requires at least 3 grams of organic material whilst Accelerator mass spectrometry (expensive) requires only 100 micrograms of organic matter
Comparative biochemistry
DNA, mitochondrial DNA, protein sequences, genomics
How does comparative DNA work
All living organisms use the same bases in DNA (nucleotide) which supports the idea that organisms are related to each other and have a common ancestor, Because speciation and extinction occur, there should be gradual differences in the DNA as organisms become more distantly related, Closely related organisms should have more similar DNA