Loutit, Tom S (1981): (Table 2) Stable carbon and oxygen isotope ratios of foraminifera in Late Miocene and Early Pliocene sediments of DSDP Hole 22-218, South Tasman Rise [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.688469, In supplement to: Loutit, TS (1981): Late Miocene paleoclimatology: Subantarctic water mass, Southwest Pacific. Marine Micropaleontology, 6(1), 1-27, https://doi.org/10.1016/0377-8398(81)90010-4
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 8.007000 * Longitude: 86.282800
Date/Time Start: 1972-03-01T00:00:00 * Date/Time End: 1972-03-01T00:00:00
Minimum DEPTH, sediment/rock: 12.90 m * Maximum DEPTH, sediment/rock: 93.00 m
Event(s):
22-218 * Latitude: 8.007000 * Longitude: 86.282800 * Date/Time: 1972-03-01T00:00:00 * Elevation: -3749.0 m * Penetration: 773 m * Recovery: 59 m * Location: Indian Ocean//FAN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 251 m cored; 0 m drilled; 23.5 % recovery
Comment:
Isotopic results are represented with respect to the powder B-1.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Sample code/label | Sample label | Loutit, Tom S | DSDP/ODP/IODP sample designation | ||
| 3 | Uvigerina sp., δ18O | Uvigerina sp. δ18O | ‰ PDB | Loutit, Tom S | >250 µm | |
| 4 | Uvigerina sp., δ13C | Uvigerina sp. δ13C | ‰ PDB | Loutit, Tom S | >250 µm | |
| 5 | Globocassidulina subglobosa, δ18O | G. subglobosa δ18O | ‰ PDB | Loutit, Tom S | >250 µm | |
| 6 | Globocassidulina subglobosa, δ13C | G. subglobosa δ13C | ‰ PDB | Loutit, Tom S | >250 µm | |
| 7 | Orbulina universa, δ18O | O. universa δ18O | ‰ PDB | Loutit, Tom S | 250-350 µm | |
| 8 | Orbulina universa, δ13C | O. universa δ13C | ‰ PDB | Loutit, Tom S | 250-350 µm |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
253 data points
Data
| 1 Depth sed [m] | 2 Sample label | 3 Uvigerina sp. δ18O [‰ PDB] | 4 Uvigerina sp. δ13C [‰ PDB] | 5 G. subglobosa δ18O [‰ PDB] | 6 G. subglobosa δ13C [‰ PDB] | 7 O. universa δ18O [‰ PDB] | 8 O. universa δ13C [‰ PDB] |
|---|---|---|---|---|---|---|---|
| 12.90 | 22-218-2-4,90-92 | 3.82 | -0.94 | ||||
| 12.90 | 22-218-2-4,90-92 | 3.68 | -1.14 | ||||
| 14.40 | 22-218-2-5,90-92 | 3.97 | -1.13 | ||||
| 14.40 | 22-218-2-5,90-92 | 3.99 | -1.13 | ||||
| 16.40 | 22-218-2-1,90-92 | 3.48 | -0.99 | ||||
| 17.10 | 22-218-3-1,10-12 | 3.71 | -1.32 | ||||
| 17.90 | 22-218-3-1,90-92 | 3.20 | -1.02 | ||||
| 18.60 | 22-218-3-2,10-12 | 3.42 | -0.90 | ||||
| 20.10 | 22-218-3-3,10-12 | 3.30 | -1.25 | ||||
| 20.90 | 22-218-3-3,90-92 | 2.99 | -1.03 | ||||
| 26.50 | 22-218-3-CC, | 2.76 | -1.18 | ||||
| 36.10 | 22-218-5-1,10-12 | 2.71 | -0.94 | 0.97 | 0.76 | ||
| 36.10 | 22-218-5-1,10-12 | 2.83 | -0.84 | ||||
| 36.10 | 22-218-5-1,10-12 | 2.81 | -1.49 | ||||
| 36.90 | 22-218-5-1,90-92 | 2.53 | -0.84 | 2.57 | -1.17 | 0.21 | 0.91 |
| 37.04 | 22-218-5-1,104-106 | 2.77 | -1.16 | 3.03 | -0.69 | ||
| 37.04 | 22-218-5-1,104-106 | 2.72 | -0.90 | 2.56 | -0.91 | ||
| 37.60 | 22-218-5-2,10-12 | 2.72 | -0.74 | 2.64 | -0.75 | 1.08 | 0.60 |
| 38.40 | 22-218-5-2,90-92 | 2.92 | -0.84 | 3.37 | -0.62 | 0.88 | 1.11 |
| 38.40 | 22-218-5-2,90-92 | 2.78 | -0.84 | ||||
| 45.50 | 22-218-5-CC, | 2.82 | -0.97 | 2.78 | -0.63 | 1.94 | 0.92 |
| 45.50 | 22-218-5-CC, | 2.78 | -1.03 | ||||
| 45.75 | 22-218-6-1,25-28 | 1.98 | 1.72 | ||||
| 45.98 | 22-218-6-1,48-51 | 2.63 | -0.15 | 1.21 | 1.68 | ||
| 46.25 | 22-218-6-1,75-78 | 3.08 | 0.00 | 1.55 | 1.49 | ||
| 46.50 | 22-218-6-1,100-103 | 3.16 | -0.01 | 0.92 | 1.65 | ||
| 46.75 | 22-218-6-1,125-128 | 0.93 | 2.00 | ||||
| 46.97 | 22-218-6-1,147-150 | 2.86 | -0.09 | 1.32 | 1.52 | ||
| 47.25 | 22-218-6-2,25-28 | 2.90 | 0.06 | ||||
| 47.40 | 22-218-6-2,40-43 | 3.00 | 0.16 | ||||
| 47.40 | 22-218-6-2,40-43 | 2.69 | -0.27 | ||||
| 47.50 | 22-218-6-2,50-52 | 3.02 | -0.36 | ||||
| 47.60 | 22-218-6-2,60-63 | 3.01 | 0.08 | ||||
| 47.60 | 22-218-6-2,60-63 | 2.88 | 0.11 | ||||
| 47.80 | 22-218-6-2,80-83 | 2.80 | 0.09 | ||||
| 47.80 | 22-218-6-2,80-83 | 2.80 | 0.09 | ||||
| 47.90 | 22-218-6-2,90-92 | 2.43 | -0.22 | 0.82 | 1.63 | ||
| 48.60 | 22-218-6-3,10-12 | 2.86 | -0.44 | 0.73 | 1.93 | ||
| 48.90 | 22-218-6-3,40-43 | 2.89 | -0.01 | 0.29 | 1.52 | ||
| 49.40 | 22-218-6-3,90-92 | 1.47 | -0.15 | 0.73 | 1.96 | ||
| 49.40 | 22-218-6-3,90-92 | 1.76 | 0.01 | ||||
| 50.45 | 22-218-6-4,45-48 | 1.23 | 1.88 | ||||
| 50.90 | 22-218-6-4,90-92 | 1.35 | 1.64 | ||||
| 51.60 | 22-218-6-5,10-12 | 2.85 | 0.09 | 1.11 | 1.61 | ||
| 52.65 | 22-218-6-5,105-108 | 1.10 | 1.49 | ||||
| 53.10 | 22-218-6-6,10-12 | 2.68 | 0.01 | 1.31 | 1.69 | ||
| 53.10 | 22-218-6-6,10-12 | 3.02 | 0.14 | ||||
| 53.90 | 22-218-6-6,90-92 | 0.63 | 1.54 | ||||
| 55.00 | 22-218-6-CC, | 2.92 | 0.16 | ||||
| 55.00 | 22-218-6-CC, | 2.88 | 0.17 | ||||
| 55.00 | 22-218-6-CC, | 2.81 | 0.09 | ||||
| 57.80 | 22-218-7-2,128-130 | 2.40 | -0.41 | ||||
| 58.90 | 22-218-7-3,90-92 | 3.08 | 0.00 | ||||
| 59.60 | 22-218-7-4,10-12 | 2.56 | -0.04 | ||||
| 60.55 | 22-218-7-4,105-107 | 2.40 | -0.16 | ||||
| 60.55 | 22-218-7-4,105-107 | 2.94 | -0.06 | ||||
| 64.50 | 22-218-7-CC, | 2.60 | -0.20 | ||||
| 74.90 | 22-218-9-1,90-92 | 2.32 | -0.22 | ||||
| 75.60 | 22-218-9-1,10-12 | 2.34 | -0.03 | ||||
| 75.60 | 22-218-9-1,10-12 | 2.47 | 0.02 | ||||
| 79.40 | 22-218-9-4,90-92 | 2.63 | -0.37 | ||||
| 81.60 | 22-218-9-6,10-12 | 2.76 | 0.00 | ||||
| 86.53 | 22-218-10-3,53-55 | 2.63 | -0.81 | ||||
| 87.62 | 22-218-10-4,12-14 | 2.27 | 0.37 | ||||
| 88.43 | 22-218-10-4,93-95 | 2.24 | 0.27 | ||||
| 89.10 | 22-218-10-5,10-12 | 2.13 | 0.23 | 2.69 | 0.24 | ||
| 89.10 | 22-218-10-5,10-12 | 2.27 | 0.31 | ||||
| 91.40 | 22-218-10-6,90-92 | 2.35 | 0.64 | ||||
| 93.00 | 22-218-10-CC, | 2.17 | 0.44 | 2.21 | 0.52 |