(Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 22-217 in the Indian Ocean
| Cobertura |
LATITUDE: 8.926200 * LONGITUDE: 90.538800 * DATE/TIME START: 1972-02-24T00:00:00 * DATE/TIME END: 1972-02-24T00:00:00 * MINIMUM ORDINAL NUMBER: 1 * MAXIMUM ORDINAL NUMBER: 5 |
|---|---|
| Data(s) |
04/09/1982
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| Formato |
text/tab-separated-values, 20 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.701711 doi:10.1594/PANGAEA.701711 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.701741 Saltzman, Eric S; Barron, EJ (1982): Deep circulation in the Late Cretaceous: oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores. Palaeogeography, Palaeoclimatology, Palaeoecology, 40(1-3), 167-181, doi:10.1016/0031-0182(82)90088-8 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #22-217; Calculated from stable oxygen isotopes; Deep Sea Drilling Project; delta 13C, skeletal carbonate; delta 18O, skeletal carbonate; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//RIDGE; Leg22; Mass spectrometer VG Micromass 602; ODP sample designation; ORDINAL NUMBER; Sample code/label; Temperature, water |
| Tipo |
Dataset |
