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paleontologists
study early life forms by interpreting fossil evidence
fossils
traces of once living things that are preserved in rocks
formations of fossils by mold and cast
remains sink in water and are quickly buried by sediment. Soft parts decay
over millions of years, the sediment turns to rock, the hard parts dissolve forming a mold
other sediments or minerals fill the mold, creating a cast of the remains
carbonaceous film
the remains of an organism were compressed under heat and pressure, leaving a thin carbon film
original remains
preserved in ice, tar or amber
trace fossils
evidence of animal activity, such as worm holes, burrows and footprints
petrified fossils
minerals permeated the remains, causing them to harden
geological column
in a geological, older layers of sedimentary rock are at the bottom and younger layers are on top.
can use layers to help determine the ages of fossils and the environment they formed
index fossils
can be used to identify a particular time period
uncertainties in fossil records
fossils are rare (need certain conditions to form)
fossils dont tell us everything
often, fossils are found in fragments that have to be reconstructed
earths first years
the earth is 4.6 billion years old
earth started as a swirling cloud of gas and dust around the sun
gas and dust collected together, forming planets
over time, the outer layers of earth cooled. eruptions of magma from underneath cooled to form an outer layer ok rock
Precambrian era
4.6b to 600m years ago
earth forms
first life (bacteria)
first invertebrates
paleozoic era
600 to 225m years ago
first reptiles
first large land animals (amphibians)
first insects
first large land plants
first fish with jaws
mesozoic era
225 to 65m years ago
dinosaurs
first flowering plants
first birds and mammals
cenozoic era
65m years ago to present
most modern species appear
more mammals
first grasses
first human like species