Life
Fossils- the remains of once-living organisms (plants/animals/bacteria/fungi)
Fossilization- remains of the dead organism were covered by sediment and preserved
Fossilization is extremely rare.
A person who studies fossils is a Palaeontologist.
A person who studies rocks, soils, and minerals are a Geologist.
Earth is 4,600,000,000
Geologic Time Scale= divides earth’s history into intervals of time defined by major events or changes
Categories are divided into the following:
- Eon- hundreds of millions/billions of years
- Era- tens of millions of years
- Period- millions of years
- Epoch- tens of thousands of years
- Age- hundreds to thousands of years
We are in the…
- Phanerozoic Eon
- Cenozoic Era
- Quarternary Period
- Holocene Epoch
- Meghalayan Age
7 TYPES OF FOSSILS
~permineralized fossil- the bones or tree have become rock
~carbonized fossil- only the carbon remains and leaves a film behind
~frozen remains- the whole organism is frozen including the organs
~cast and mold fossils- the impression made is called the mold and when minerals/sediment fill it in, it is called a cast
~amber fossil- the plant or animal is stuck in tree sap- over time the sap hardens into amber and is preserved
~tar pit fossil- organism gets stuck in a sticky tar- the tar preserves the bones
~trace fossil- a record of the activity of the animal- tracks, nests, burrows, scratch marks, etc.
1-6 are body fossils
Uniformitarianism- geologic events and phenomena that occur today, also happened in the past and will happen in the future
Ex: earthquake, volcano, tsunami, mud/landslides, erosion, weathering, plate tectonics
Law of Superposition- states that in a sequence of undisturbed rocks, the oldest layers are at the BOTTOM and the youngest are at the TOP
Relative Age- relates to whether one layer is older than another
Absolute Age- actual age
Radioactive decay- unstable particles in living things change into stable particles
Half-life- the amount of time needed for half of a sample of a radioactive substance to decay
Radiometric dating- the method of finding the absolute age of rock based on comparing the amounts of stable and unstable particles
Extinction- when all the members of a species die out
Fossil Record- a collection of all known fossils and their placement in order from most recent
Mass Extinction- large numbers of species die out in different parts of Earth during a relatively short period of time
REASONS FOR MASS EXTINCTION
Natural disasters
Meteor strike
Climate change
Low oxygen levels in oceans
Diseases
Solar events
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