Table T4. 40Ar-39Ar incremental heating ages from ash layers in the Neogene, Hole 1138A.
Core, section, interval (cm)
Designation
Material
Total gas age
(Ma)
±2 sd
39Ar (%)
Plateau
age
(Ma)
±2 sd
Steps
used
MSWD
Isochron age
(Ma)
±2 sd
MSWD
40Ar/36Ar (initial)
±2 sd
Depth (mbsf)
Top
Bottom
Average
183-1138A-
















12R-3, 5-7 A1 105.35 105.37 105.36 Glass 7.98 0.39 60.80 7.07 0.37 3 of 5 1.10 5.99 0.71 1.34 311 6
13R-1, 22-24 A2 112.22 112.24 112.23 Biotite 6.53 0.14 98.70 6.43 0.14 6 of 7 1.15 6.39 0.14 1.15 305 11
15R-1, 73-75 A3 131.93 131.95 131.94 Glass 16.47 1.68 83.30 12.22 1.47 3 of 6 1.02 6.93 2.96 0.02 306 4
19R-1, 110-112 A4 170.80 170.82 170.81 Biotite 11.32 0.25 99.70 11.31 0.25 8 of 8 1.24 11.28 0.26 1.24 297 17
19R-1, 110-112 A5 170.80 170.82 170.81 Glass 11.44 0.39 99.50 11.57 0.36 6 of 7 1.53 11.83 0.39 1.53 286 9

Notes: MSWD = mean square weighted deviation. All ages calculated relative to neutron fluence monitor FCT-2 biotite (28.04 ± 0.12 Ma), decay and abundance constants le = 0.581 x 10-10/yr; lb = 4.961 x 10-10/yr; 40K/K = 1.17 x 10-4, and corrected for 37Ar decay (half-life = 35.1 days) and interfering isotopes 36Ar/37Ar[Ca] = 2.64 x 10-4, 39Ar/37Ar[Ca] = 6.73 x 10-4, 40Ar/39Ar[K] = 1.0 x 10-3. Bold entries are considered the best estimates of crystallization ages (see text).