676
Paul eta!'
0
45
200
42:'
E' 400
375
:I:
e- 600
[l.
L..
3.
0
3.25
00
3
'000
2,75
0
25
1000
2,~5
2
~ 2000
175
..s
15
,:!: 3000
1.2:>
[l.
u..o
4000
075
0.5
5000
0.25
D
60'S
.lO·S
o·
30·\
60·N
90·1\
a
LATITL DE
0
700
E 400
I
e- 600
a.
w
0
800
1000
0
1000
~ 2000
..s
:I: 3000
lt\.
""' 0
~OOO
5000
b
LATiTUOE
Fig.n. Equilibriwn fractionation 6, computed from the paleotemperature equation ofErez and Luz (1983). (a) Temperature taken from Experiment B. (b) Temperature taken from climatology. Contour interval is 0.25 %0.
Paul eta!'
0
45
200
42:'
E' 400
375
:I:
e- 600
[l.
L..
3.
0
3.25
00
3
'000
2,75
0
25
1000
2,~5
2
~ 2000
175
..s
15
,:!: 3000
1.2:>
[l.
u..o
4000
075
0.5
5000
0.25
D
60'S
.lO·S
o·
30·\
60·N
90·1\
a
LATITL DE
0
700
E 400
I
e- 600
a.
w
0
800
1000
0
1000
~ 2000
..s
:I: 3000
lt\.
""' 0
~OOO
5000
b
LATiTUOE
Fig.n. Equilibriwn fractionation 6, computed from the paleotemperature equation ofErez and Luz (1983). (a) Temperature taken from Experiment B. (b) Temperature taken from climatology. Contour interval is 0.25 %0.