Lyle, Mitchell W; Drury, Anna Joy; Tian, Jun; Wilkens, Roy H; Westerhold, Thomas (2019): Table SM-5: Offsets of IODP Site 320-U1335 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.904392, In supplement to: Lyle, MW et al. (2019): Late Miocene to Holocene high-resolution eastern equatorial Pacific carbonate records: stratigraphy linked by dissolution and paleoproductivity. Climate of the Past, 15(5), 1715-1739, https://doi.org/10.5194/cp-15-1715-2019
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Project(s):
Coverage:
Latitude: 5.312270 * Longitude: -126.283480
Minimum Elevation: -4330.0 m * Maximum Elevation: -4330.0 m
Event(s):
320-U1335 * Latitude: 5.312270 * Longitude: -126.283480 * Elevation: -4330.0 m * Campaign: Exp320 (Pacific Equatorial Age Transect I) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Comment:
These are the offsets for Holes U1335A and U1335B between mbsf (metres below seafloor) and rmcd (revised metres composite depth) for each core.
The relevant core for each row is given in the lefthand "Core number" column
Add the core-specific offset to the mbsf scale to convert to the rmcd scale.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Core | Core | Lyle, Mitchell W | |||
2 | Offset | Offset | m | Lyle, Mitchell W | U1335_A_Offsets | |
3 | Offset | Offset | m | Lyle, Mitchell W | U1335_B_Offsets |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
137 data points
Data
1 Core | 2 Offset [m] (U1335_A_Offsets) | 3 Offset [m] (U1335_B_Offsets) |
---|---|---|
1 | 0.140000 | 0.00000 |
2 | 1.010000 | -0.18000 |
3 | 1.310000 | 1.17000 |
4 | 3.040000 | 2.57000 |
5 | 5.170000 | 4.23000 |
6 | 5.990000 | 5.60000 |
7 | 7.090000 | 6.77000 |
8 | 9.190000 | 8.61000 |
9 | 10.090000 | 9.65000 |
10 | 11.050000 | 11.90000 |
11 | 12.860000 | 13.11000 |
12 | 14.090000 | 14.50000 |
13 | 13.240000 | 15.40000 |
14 | 15.300000 | 16.74000 |
15 | 16.350000 | 17.36000 |
16 | 16.350000 | 19.28000 |
17 | 20.000000 | 19.28000 |
18 | 20.470000 | 20.30000 |
19 | 21.310000 | 22.31000 |
20 | 22.730000 | 24.03000 |
21 | 24.120000 | 25.05000 |
22 | 25.980000 | 25.97000 |
23 | 28.420000 | 28.92000 |
24 | 31.630000 | 31.09000 |
25 | 32.770000 | 32.54000 |
26 | 34.640000 | 34.22000 |
27 | 36.940000 | 36.01000 |
28 | 37.780000 | 37.38000 |
29 | 39.490000 | 39.36000 |
30 | 40.560000 | 41.95000 |
31 | 42.630000 | 43.33000 |
32 | 43.960000 | 45.06000 |
33 | 45.740000 | 46.44000 |
34 | 48.420000 | 47.82000 |
35 | 50.830000 | 49.88000 |
36 | 52.000000 | 51.85000 |
37 | 52.000000 | 54.25000 |
38 | 52.000000 | 54.25000 |
39 | 52.000000 | 54.25000 |
40 | 52.000000 | 54.25000 |
41 | 52.000000 | 54.25000 |
42 | 52.000000 | 54.25000 |
43 | 52.000000 | 54.25000 |
44 | 52.000000 | 54.25000 |
45 | 52.000000 | 54.25000 |
46 | 54.25000 |