mostly hard parts of organisms are fossilised - bones, shells, teeth
Fossil Formation
organisms must be protected from decay by micro-organisms
must be protected from scavengers
need to be buriedrapidly
lack of 02 in low pH soil is required
need to be left undisturbed for a long time
Fossil Record
a chronological list of living things over the history of the earth
establishes evolutionary links between species, showing common ancestry
provides evidence of which organisms lived on earth in the past
provides examples of which organisms may be extinct
provides examples of transitional organisms between species
Fossil Record is Incomplete
only a very small % of organisms leave fossilised remains
many fossils are destroyed by natural processes - weathering, erosion
fossils may be destroyed by human activity
fossils may be buriedtoodeep and are unable to be located or accessed
archaeologists may be looking in the wrong place
Principle of Superposition
indicates that the oldest layer of rock is found at the bottom, with each layer above being relatively younger
relative dating - there's no exact time
Transitional Forms
a fossil which exhibits traits common to both ancestral and derived groups - especially important when groups are sharply differentiated
can show how a species may adapt to survive their new conditions
Fossil Dating Methods
relative dating: gives a relative (older/younger) age of fossil - relies on the principle of superposition, older strata are lower down in rock layers
absolute dating: gives a numerical (exact/absolute) age of fossil - relies on radioactive decay, decay of isotopes in the fossil or the rock surrounding it
both rely on finding fossils of organisms that are no longer alive today
both provide evidence for evolution and show how species have changed over time
Biogeography
The distribution of organisms and ecosystems across the world and through geologic time