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(1)

Geologic Time Scale

Era

Period

Began Ended

(million years ago)

Major Events

(million years ago)

Cenozoic

Quaternary

Tertiary

1.6 Present

65 1.6

Major Glaciers in North America and Europe (1.5)

Rocky Mts. (65) Individual Continents Take Shape

Mesozoic

Cretaceous

Jurassic

Triassic

146 65

208 146

245 20

Dinosaurs Extinct (65) Western Interior Seaway and Marine Reptiles (144-65) Pangaea (One Land Mass) Begins to Break Up (200) First Mammals and Dinosaurs Paleozoic Permian Pennsylvanian Mississippian Devonian Silurian Ordovician Cambrian 290 245

322 290

362 322

408 362

439 408

510 439

545 510

Greatest Extinction on Earth (245) First Reptiles Coal-Forming Forests First Land Animals and First Forests (408) Life Invades Land First fish Great Diversity of Marine Invertebrates Precambrian Proterozoic Archean 2,500 545

4,600 2,500

Marine Fossil Invertebrates (600)

Earliest Fossils Recorded (3,500) Earliest Rocks (4,000)

(2)
(3)

Mi

d

-L

ate

Pr

ec

am

b

ri

an

Str

o

m

ato

lite

s

5"

Mi

d

-L

ate

Pr

ec

am

b

ri

an

C

o

n

t

Str

o

m

ato

lite

s

6"

Increasing Oxygen

A

R

es

u

lt

o

f

Ph

o

to

sy

n

th

es

is

Mi

d

-L

ate

Pr

ec

am

b

ri

an

C

o

n

t

7"

V

ery

La

te

Pre

ca

mb

ria

n

(4)

V

er

y

L

ate

Pr

ec

am

b

ri

an

C

o

n

t

Mu

lti

ce

llu

la

r

O

rg

an

is

m

s

9"

V

er

y

L

ate

Pr

ec

am

b

ri

an

C

o

n

t

A

n

in

te

rp

re

ta

ti

o

n

o

f

V

en

d

ia

n

li

fe

10"

Ea

rly

Pa

le

ozo

ic

11"

C

am

b

ri

an

L

ife

(Ea

rl

y

Pa

le

o

zo

ic

)

Ea

rl

y

C

am

b

ri

an

Cloudina

Olenellus

(5)

C

am

b

ri

an

L

ife

B

u

rg

es

s

Sh

al

e

F

au

n

a

13"

C

am

b

ri

an

L

ife

L

ife

o

n

th

e

Se

a

F

lo

o

r

14"

15"

O

rd

o

vi

ci

an

L

ife

Tr

ilo

b

ite

Brachiopods

(6)

O

rd

o

vi

ci

an

L

ife

L

ife

o

n

th

e

Se

a

F

lo

o

r

17"

Jawless Fish

O

rd

o

vi

ci

an

L

ife

Ea

rl

y

F

is

h

18"

Si

lu

ri

an

L

ife

Tr

ilo

b

ite

Ea

rl

y

L

an

d

Pl

an

ts

19"

Mi

d

d

le

D

ev

o

n

ia

n

L

ife

L

ife

o

n

th

e

Se

a

F

lo

o

r

(7)

Mi

d

d

le

D

ev

o

n

ia

n

L

ife

Devonian Fish

21"

Mi

d

d

le

D

ev

o

n

ia

n

L

ife

D

u

n

kl

eo

ste

u

s

22"

D

ev

o

n

ia

n

L

ife

Te

tr

ap

o

d

s

V

as

cu

la

r

Pl

an

ts

23"

Mi

d

d

le

D

ev

o

n

ia

n

L

ife

L

ife

o

n

L

an

d

(8)

25"

L

ate

Pa

le

o

zo

ic

L

ife

Pl

an

t

L

ife

(Sw

am

p

s)

R

ep

ti

le

s

26"

27"

Ea

rl

y

an

d

Mi

d

d

le

Me

so

zo

ic

L

ife

F

ly

in

g

R

ep

ti

le

s

(Pte

ro

sa

u

rs

)

Ma

ri

n

e

R

ep

ti

le

s

(I

ch

th

yo

sa

u

rs

)

(9)

Ea

rl

y

an

d

Mi

d

d

le

Me

so

zo

ic

L

ife

Ea

rl

y

Ma

m

m

al

s

29"

W

. W

. N

ort

on

Ea

rl

y

an

d

Mi

d

d

le

Me

so

zo

ic

L

ife

Ea

rl

y

B

ir

d

s

(

A

rc

h

ae

o

p

te

ry

x

)

Dinosaurs

(Sa

u

ro

p

o

d

s)

30"

31"

C

re

ta

ce

o

u

s

L

ife

Dinosaurs

(10)

F

lo

w

er

in

g

Pl

an

ts

L

ate

Me

so

zo

ic

(C

re

ta

ce

o

u

s)

L

ife

33"

D

ive

rs

it

y Curve

of L

ife

T

hrough t

im

e

M ode rn

M

as

s

E

xt

inc

ti

ons

E vol ut iona ry F auna s P al eoz oi c Ca m bri an E nd O rdovi ci an ! E nd D evoni an ! P erm o-T ri as si c ! Jura ss ic ! E nd Cre ta ce ous ! 34"

E

n

d

C

re

tac

e

o

u

s

M

as

s

E

x

ti

n

ct

io

n

D ec can T rap s F lood Bas al t !

35% of al

(11)

37"

Ma

m

m

al

s

Ea

rl

y

C

en

o

zo

ic

L

ife

38"

Ma

m

m

al

s

L

ate

C

en

o

zo

ic

L

ife

39"

Hominids

L

ate

C

en

o

zo

ic

L

ife

(12)

Climate Change

(3.2 & 3.3 in textbook)

Evidence for Repeated Glaciations

1.

2.

3.

Vocabulary

Glacier

Glacial Erratic

Drumlin

Esker

Kettle Lake

Calving

How Have Glaciers Shaped Alberta?

(13)

POSSIBLE CAUSES OF GLACIATIONS:

Cause

Description

Illustration

1)

2)

3)

4)

5)

6)

(14)

When di

d

Alberta look like th

(15)

2

. F

o

ss

il

s

5

3

. G

la

ci

al

L

an

d

fo

rm

s

6

G

la

ci

al

E

rr

at

ic

: a

b

o

u

ld

er

c

ar

ri

ed

a

n

d

d

ro

p

p

ed

b

y a

ic

e

sh

ee

t d

u

ri

n

g

t

h

e l

as

t i

ce

a

g

e

7

D

ru

m

li

n

: A

t

ea

rd

ro

p

-sh

ap

ed

h

il

l s

h

o

w

in

g

t

h

e

d

ir

ec

ti

o

n

t

h

e i

ce

s

h

ee

t

ad

van

ced

.

(16)

Ic

e s

h

ee

ts

le

av

e c

h

ar

ac

te

ri

st

ic

la

n

d

fo

rm

s l

ik

e:

E

sk

er

s:

A

lo

n

g

s

n

ak

in

g

h

il

l.

K

et

tl

e L

ak

e:

A

sm

al

l l

ak

e.

9

T

h

e l

as

t g

la

ci

at

io

n

(

W

is

co

n

si

n

G

la

ci

at

io

n

)

10

11

(17)

13

14

15

Ic

e a

cc

u

m

u

la

te

s

at

t

h

e c

en

tr

e o

f

th

e i

ce

s

h

ee

t,

t

h

en

fl

o

w

s o

u

tw

ar

d

t

o

th

e s

ea

.

(18)

C

al

vi

n

g

: b

ig

c

h

u

n

ks

o

f i

ce

b

re

ak

o

ff

t

o

fo

rm

ic

eb

er

g

s.

17

18

M

o

u

n

ta

in

G

la

ci

er

s f

lo

w

s

lo

w

ly

d

o

w

n

h

il

l.

19

W

h

en

t

h

e m

as

s o

f s

n

o

w

a

n

d

ic

e g

et

s h

ea

vy

en

o

u

g

h

it

f

lo

w

s d

o

w

n

h

il

l.

A

s i

t f

lo

w

s,

it

e

ro

d

es

th

e l

an

d

sc

ap

e.

(19)

G

la

ci

er

s l

ea

ve

c

h

ar

ac

te

ri

st

ic

la

n

d

fo

rm

s.

-U

-s

h

ap

ed

v

al

le

ys

21

A

s t

h

e i

ce

f

lo

w

s i

t

sc

ra

p

es

u

p

r

o

ck

s a

n

d

ca

rr

ie

s t

h

em

a

lo

n

g

.

W

h

en

it

m

el

ts

, i

t l

ea

ve

s

p

il

ls

o

f t

h

es

e r

o

ck

s a

n

d

sed

imen

ts

22

23

(20)

25

26

27

(21)

29

30

31

W

h

at

c

au

se

s g

la

ci

at

io

n

s?

(22)

1

) C

h

an

g

es

in

t

h

e a

m

o

u

n

t o

f e

n

er

g

y g

iv

en

o

ff

b

y t

h

e s

u

n

.

(w h en t h er e a re m o re s u n sp o ts , t h er e i s m o re e n er g y f ro m t h e s u n

) 33

(23)

References

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