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Table T16. Mean paleomagnetic direction for each core, Site U1335. (See table notes.)

Core Inclination
(°) 		Declination
(°) 		N α95
(°)
320-U1335A-
1H 10.7 109.8 317 3.1
2H 7.7 223.5 344 2.0
3H 1.1 164.2 331 3.1
4H –2.7 315.0 310 2.8
5H –8.9 87.6 173 5.2
6H –0.2 191.9 224 11.6
7H 12.9 103.6 254 4.0
8H–16H NA NA NA NA
17H –14.6 118.9 158 4.2
18H 4.2 76.7 171 3.4
19H –10.5 116.9 327 1.4
20H 3.5 266.8 173 2.2
21H 17.8 38.3 159 4.0
22H –57.8 179.5 153 4.1
23H–36H NA NA NA NA
320-U1335B-
1H 19.8 200.6 119 2.9
2H 4.5 207.9 321 2.0
3H 2.5 15.1 343 2.7
4H –75.9 251.0 313 3.0
5H –64.6 9.9 347 7.2
6H –16.3 206.1 344 5.6
7H 43.7 272.1 343 9.9
8H 4.1 81.8 346 2.1
9H–12H NA NA NA NA
13H 5.0 248.6 345 2.8
14H 4.7 284.8 346 4.4
15H –10.2 187.7 348 2.0
16H –9.2 292.6 332 2.7
17H 21.6 253.0 308 6.1
18H –1.6 276.0 289 2.0
19H 0.5 272.8 358 1.3
20H –13.3 71.3 350 1.6
21H 2.0 204.2 301 2.0
22H 45.6 272.1 231 5.9
23H–41H NA NA NA NA

Notes: Mean paleomagnetic directions and statistics calculated using Bingham statistics for each core. We used data from stable polarity intervals. Reversed polarity intervals were inverted prior to computing mean directions and statistics. Inclination = mean paleomagnetic inclination from stable polarity intervals in core, declination = mean paleomagnetic declination from stable polarity intervals in core. By subtracting this value from observed paleomagnetic declinations measured along core, core can be approximately reoriented back into geographic coordinates. After reorientation, normal polarity intervals will have ~0° declination and reversed polarity intervals will have ~180° declination. N = number of paleomagnetic observations used in calculating mean, α95 = 95% confidence angle for mean direction.

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