Loutit, Tom S (1981): (Table 1) Stable carbon and oxygen isotope ratios of Uvigerina sp. in Late Miocene and Early Pliocene sediments of the Blind River section, New Zealand [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.688467, 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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Coverage:
Latitude: -43.683300 * Longitude: 174.500000
Minimum SECTION, height: 181 m * Maximum SECTION, height: 1165 m
Event(s):
Comment:
Section hight is Tickness (m). Isotopic results are represented with respect to the powder B-1.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | SECTION, height | Section | m | Geocode | ||
| 2 | Sample code/label | Sample label | Loutit, Tom S | |||
| 3 | Uvigerina sp., δ18O | Uvigerina sp. δ18O | ‰ PDB | Loutit, Tom S | ||
| 4 | Uvigerina sp., δ13C | Uvigerina sp. δ13C | ‰ PDB | Loutit, Tom S |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
111 data points
Data
| 1 Section [m] | 2 Sample label | 3 Uvigerina sp. δ18O [‰ PDB] | 4 Uvigerina sp. δ13C [‰ PDB] |
|---|---|---|---|
| 181 | 73 | 0.74 | 0.31 |
| 203 | 72 | 1.38 | -0.16 |
| 203 | 72 | 1.40 | -0.17 |
| 217 | 71 | 1.10 | 0.04 |
| 251 | 68 | 0.51 | 0.53 |
| 369 | 64 | 1.46 | -0.40 |
| 369 | 64 | 1.36 | -0.54 |
| 404 | 62 | 1.56 | -0.20 |
| 404 | 62 | 1.72 | -0.42 |
| 447 | 60 | 1.19 | -0.38 |
| 491 | 58 | 1.28 | -0.36 |
| 565 | 55 | 1.29 | -0.63 |
| 613 | 53 | 1.39 | -0.98 |
| 613 | 53 | 1.12 | -1.04 |
| 706 | 52 | 1.56 | -1.05 |
| 706 | 52 | 1.39 | -1.33 |
| 716 | 51 | 1.74 | -0.90 |
| 726 | 2 | 1.06 | -0.95 |
| 740 | 5 | 1.39 | -0.74 |
| 740 | 5 | 1.25 | -0.95 |
| 795 | 8 | 1.14 | -0.68 |
| 795 | 8 | 1.30 | -0.75 |
| 807 | 10 | 1.46 | -1.02 |
| 807 | 10 | 1.38 | -0.83 |
| 853 | 14 | 1.67 | -0.89 |
| 879 | 17 | 1.61 | -0.74 |
| 879 | 17 | 1.41 | -0.77 |
| 889 | 18 | 1.13 | -0.85 |
| 889 | 18 | 1.27 | -1.02 |
| 911 | 20 | 1.02 | -0.85 |
| 911 | 20 | 1.65 | -0.58 |
| 971 | 27 | 1.59 | -0.94 |
| 1029 | 34 | 1.44 | -0.74 |
| 1056 | 38 | 1.26 | -0.46 |
| 1056 | 38 | 1.11 | -0.54 |
| 1081 | 40 | 1.42 | -0.88 |
| 1165 | 48 | 1.35 | -0.64 |