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This
description
of
the
fossil
record
of
bacteria
focuses
on
one
particular
group
of
bacteria,
the
cyanobacteria
or
blue-green
algae,
which
have
left
a
fossil
record
that
extends
far
back
into
the
Precambrian.
The
oldest
cyanobacteria-like
fossils
known
are
nearly
3.5
billion
years
old
and
are
among
the
oldest
fossils
currently
known.
Cyanobacteria
are
larger
than
most
bacteria
and
may
secrete
a
thick
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Information
on
this
page
pertains
to
dinoflagellates,
the
fossil
record
of
which
may
extend
into
the
Precambrian.
Spherical
organic-walled
microfossils
known
as
acritarchs,
some
of
which
may
be
dinoflagellate
hystrichospheres,
first
appear
in
rocks
about
1.8
billion
years
old.
Exactly
what
the
acritarchs
were
is
not
known
with
certainty;
they
probably
included
a
number
of
clades
of
eukaryotic
algae,
...
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This
site
describes
some
unusual
fossils
of
the
late
Precambrian
age,
found
on
exposed
rock
surfaces
along
the
southern
coast
of
the
Avalon
Peninsula
in
Newfoundland.
The
most
famous
locality
where
these
fossils
can
be
seen
is
at
Mistaken
Point
at
the
southernmost
tip
of
the
Avalon
Peninsula.
The
Mistaken
Point
fossils
were
preserved
by
being
blanketed
with
layers
of
fine
volcanic
ash
and
are
dated
...
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This
site
describes
the
White
Mountains,
the
Inyo
Mountains,
and
associated
ranges
along
the
California-Nevada
border
north
of
Death
Valley.
This
location
presents
one
of
the
most
important
and
best-known
Late
Proterozoic
to
Cambrian
sections
in
the
United
States.
Starting
with
the
unfossiliferous
Precambrian
rocks
of
the
Wyman
Formation,
paleontologists
can
work
their
way
through
a
complete
section
...
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The
Tommotian
Age
began
about
530
million
years
ago
and
is
a
subdivision
of
the
early
Cambrian.
Named
for
rock
exposures
in
Siberia,
the
Tommotian
saw
the
first
major
radiation
of
the
animals,
or
metazoans,
including
the
first
appearance
of
a
great
many
mineralized
taxa
such
as
brachiopods,
trilobites,
archaeocyathids,
molluscs,
and
echinoderms.
A
few
million
years
before
the
Tommotian,
in
the
Vendian,
...
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This
site
describes
the
Cambrian
fossil
record,
which
indicates
a
distinct
development
from
simple
organisms
to
organisms
comparable
in
morphology
and
organization
to
present-day
animals.
The
development
is
documented
by
faunal
assemblages
represented
by
the
Ediacara
fauna,
the
first
complex
trace
fossils,
the
earliest
shelly
faunas,
and
the
onset
of
the
typical
Cambrian
macrofaunas.
This
rapid
evolution
...
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This
site
describes
the
fossils
in
the
Stephen
Formation
near
the
Burgess
Pass
in
present-day
Yoho
National
Park,
British
Columbia,
known
today
as
the
Burgess
Shale.
More
than
65,000
specimens
have
been
collected
from
the
dark
shale,
many
of
which
have
partially
or
entirely
preserved
soft-parts
that
provide
a
unique
window
to
Cambrian
and
Early
Paleozoic
biota.
The
fossiliferous
strata
of
the
Burgess
...
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This
site
describes
the
Chengjiang
fauna,
one
of
the
most
exciting,
oldest,
and
best
preserved
Paleozoic
biota.
With
a
wealth
of
different
taxa
that
was
never
expected
for
the
Early
Cambrian,
it
is
said
to
be
the
most
spectacular
paleontologic
discovery
since
the
Burgess
Shale
of
British
Columbia
and
one
of
the
most
important
fossil
archives
known
so
far.
After
information
on
stratigraphy
and
preservation,
...
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This
site
describes
the
Silurian
period,
a
time
during
which
the
Earth
underwent
considerable
changes
that
had
important
repercussions
for
the
environment
and
life
within
it.
The
stratigraphy
link
describes
the
subdivisions
of
the
period
into
four
epochs.
Each
epoch
is
distinguished
from
the
others
by
the
appearance
of
new
species
of
graptolites.
Two
other
links
lead
to
a
detailed
discussion
of
life
...
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This
lesson
will
clarify
the
development
of
the
geologic
time
scale.
It
will
also
introduce
students
to
the
major
time
periods
in
the
history
of
Earth,
as
well
as
to
the
role
fossils
play
in
helping
us
understand
this
history.
This
lesson
is
based
on
an
online
booklet
that
provides
an
introduction
to
the
study
of
the
history
of
Earth,
published
by
the
U.S.
Geological
Survey.
Using
careful
analogies
...
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