bio study
fossils
dating techniques
geological time scale
natural selection and Evolution
natural selection
speciation and evolution
human Evolution
global systems: Recycling in nature
Natural influences on climate
human influence on climate
formation of fossils
1 an organism dies. Anaerobic conditions exclude bacteria and other predators that consume bodies before burial, so organisms that die in the deepest ocean or in a deep lake are more likely to become fossils
2 the remains need to be buried in soft sediment. Rapid burial increases the chances of fossilisation because a body is less likely to be consumed or destroyed by the environment such as wind, waves and scavengers.
3 a period of burial, which can range from a few thousand years up to millions of years. During this time, the rocks around the body will change the shape, and the chemical and mineral composition, of the buried body parts.
4the rocks around the fossil need to be eroded, allowing them to become exposed to the Earth's surface in time for a palaeontologist to come past and find it.
types of fossils
original
replacement
carbon film
indirect
when the dead organism decays and leaves a thin black deposit of carbon e.g. plant fossil
nothing has change in the fossil e.g. hard shell see creatures.
when a part of the organisms is chemically changed into another mineral
preserved remains of the imprint of the body ( footprints and track)
preserving environments
permaforst (frozen)
Amber: plant sap
tar: oil
peat: swamps
Dry Air
Bactra
click to edit
chalers Darwin