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geologic time scale
calendar of events
geologic time scale
earths history of life
chronological order
earths geo time scale is arranged in wht
eon
largest unit of time
era
unit of time shorter than an eon but longer than a period
periods
A unit of time shorter than an era but longer than epoch.
epochs
A unit of time shorter than a period but longer than an age
precambrian
542
M ago
precambrian
single-celled bacteria
came into existence
precambrian
no life on land
precambrian
atmosphere
begins to accumulate the
O
for
higher-
order animals to survive. (
higher
/
lower
)
precambrian
end of this
era,
is the rise of complex animals in the OCEAN
precambrian
that
complex animal nga nagrise
in the
ocean
.
PC ERA
paleozoic
began with cambrian explosion
paleozoic
rapid period of
speciation
kicked off a long period of
life
flourishing on
earth
paleozoic
living orgs
from
ocean
moved towards
land
paleozoic
end of this
era, largest
mass extinction
paleozoic
wiped out
75
% of marine life and
70
% life on land
paleozoic
first to magriate towards
land
; plants, then
invertibrates
and so on...
age of
dinosaurs
mesozoic
era
mesozoic
humid and tropical climate
mesozoic
green plants
and
lush sprouted
all over the
earth
herbivores, small mammals
in mesozoic era, they thrived and came into existence
mesozoic
what era "
birds
developed turned into
dinosaurs
"
cenozoic
65 million
yrs ago to the present
cenozoic
final
era of the
geo
timescale
cenozoic
era where
smaller mammals
survived and become
dominant
cenozoic
climate is
cool ad drier
compared to that one era
, cenozoic
anwer
what era, its name __ cuz its covered with glaciers bla bla
cenozoic
all species of life (+ humans) evolved troughout this era
fossils
evidence that organisms lived
fossils
remains like burrows, nests, and dino footprints
U P R C R A
six ways of fossilization
Unaltered preservation
organism
is
trapped
in amber, hardened plant is being observed
per mineralization
aka
petrification
, organic content of bone and wood, are replaced by
SILICA
,
CALCITE
OR
PYRITE.
FORMING A
ROCK-LIKE
FOSSIL
carbonization
aka
coalification
, TWO OTHER ELEMENTS, are
ionized
and
CArbon
remained
recrystallization
hard parts, converted to more stable minerals or small to large crystals
authigenic preservation
molds and casts are formed after most of the organisms have been dissolved.
type of fossils
casts
,
petrified
,
original remains
,
carbon film
,
trace/ichnofossils
molds
substrate negative image of an organism
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