Table T6. Paleolatitude of Leg 171B sites.
Age | Hole 1049A | Hole 1050A, C | Hole 1051A | Hole 1052A, E | Hole 1053A | |||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Paleolatitude | (N*,
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Paleolatitude | (N*,
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Paleolatitude | (N*,
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Paleolatitude | (N*,
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Paleolatitude | (N*,
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|||||
Eocene |
22.8
|
(31.5, 2.7) |
|
23.6
|
(54.5, 2.9) |
|
22.3
|
(61.5, 2.7) |
|
28.5
|
(28.5, 4.7) |
|
27.1
|
(14.5, 9.6)
|
Paleocene |
22.7
|
(8.5, 9.4) |
|
17.1
|
(57.5, 2.1) |
|
20.8
|
(12, 7.7) |
|
23.2
|
(14.5, 5.5) |
|
|
|
Maastrichtian |
22.2
|
(4.5, 12.3) |
|
23.3
|
(21.5, 5.8) |
|
|
|
|
22.4
|
(6, 9.3) |
|
|
|
Coniacian-Turonian |
|
|
21.9
|
(2.5, 19) |
|
|
|
|
|
|
|
|
||
Cenomanian |
|
|
26.2
|
(8.5, 4.9) |
|
|
|
|
24.7
|
(4.5, 10.5) |
|
|
|
|
Albian |
|
|
|
|
|
|
|
20.9
|
(40, 2) |
|
|
|
||
Aptian-Albian |
35.6
|
(11.5, 10.9) |
|
18.4
|
(10, 6) |
|
|
|
|
23.0
|
(720, 2.6)
|
|
|
|
Notes:
Paleolatitudes are in °N. Parameters N* and 95
are the weighted number of samples of N, NP, RP, and R polarity rating
("P"-rated are given half weight) and the 95% confidence on the
paleolatitude computed by the method of Kono (1980). The second Albian listing
for Site 1052 is from the mean inclination of 720 shipboard pass-through
cryogenic magnetometer measurements at 5-cm intervals within the recovered
sediments of Hole 1052E (Shipboard Scientific Party, 1998e).