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In this lesson students compare differences in amino acids in the beta hemoglobin from representative primates, complete a matrix of those differences, and from these data, construct and interpret cladograms as they reflect relationships and timing of divergence.
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Choosing & Using this resource...
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Pedagogical help
Misconceptions:
Read (2)
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This
lesson
plan
is
part
of
a
high
school
course
on
astronomy,
Newtonian
mechanics
and
spaceflight
and
provides
a
closer
look
at
the
pole
star
and
the
neighboring
constellations,
especially
the
Big
Dipper
and
Cassiopeia.
One
objective
is
for
the
student
to
know
the
constellations
of
the
Big
Dipper
and
Cassiopeia,
and
their
use
in
finding
the
Pole
Star.
The
student
will
also
realize
that
other
celestial
...
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Choosing & Using this resource...
Educational standards associated with this resource:
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This
lesson
plan
serves
as
an
introduction
to
the
ecliptic,
the
zodiac
and
the
apparent
motions
of
the
Sun,
Moon
and
planets
across
the
sky.
The
objectives
are
to
help
the
student
know
about
the
apparent
motion
of
the
Sun,
Moon
and
planets
across
the
sphere
of
fixed
stars
(celestial
sphere)
and
understand
that
the
reason
all
of
these
objects
travel
along
very
similar
paths
is
that
the
solar
system
...
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Choosing & Using this resource...
Educational standards associated with this resource:
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In
this
lesson
the
ellipse
is
studied
in
polar
coordinates
(r,f),
with
the
function
cos(f).
This
places
the
origin
point
at
a
focus
(more
appropriate
for
planetary
motion)
and
introduces
the
eccentricity
e.
It
is
also
noted
that
planets
actually
orbit
the
center
of
gravity
of
the
solar
system
and
that
distant
planets
may
be
detected
by
motions
of
their
central
star
around
the
centers
of
gravity
of
...
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Choosing & Using this resource...
Educational standards associated with this resource:
National Science Education Standards (NSES): Read
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This
lesson
presents
an
introduction
to
solar
observations
by
eye
or
telescope
and
during
eclipse.
It
also
explores
the
distance
to
the
Sun,
its
layers,
the
corona
and
the
solar
wind.
Safety
rules
for
observing
the
Sun
are
stressed
as
students
are
informed
about
the
visible
layers
of
the
Sun
-
photosphere,
chromosphere,
corona.
Students
learn
about
the
high
temperature
of
the
corona,
the
evidence
...
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Choosing & Using this resource...
Educational standards associated with this resource:
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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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Choosing & Using this resource...
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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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Choosing & Using this resource...
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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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Choosing & Using this resource...
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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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Choosing & Using this resource...
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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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Choosing & Using this resource...
Educational standards associated with this resource:
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