(Table 1b) Stable oxgen isotope ratio measured on G. ruber from sediment core RC09-191
| Cobertura |
LATITUDE: 38.200000 * LONGITUDE: 18.033000 * DATE/TIME START: 1965-07-24T00:00:00 * DATE/TIME END: 1965-07-24T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.15 m * MAXIMUM DEPTH, sediment/rock: 1.64 m |
|---|---|
| Data(s) |
01/09/1989
|
| Formato |
text/tab-separated-values, 20 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.358894 doi:10.1594/PANGAEA.358894 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.726985 Fontugne, Michel R; Paterne, Martine; Calvert, Stephen E; Murat, Anne; Guichard, Francois; Arnold, Maurice (1989): Adriatic deep water formation during the Holocene: implication for the reoxygenation of the deep eastern Mediterranean Sea. Paleoceanography, 4(2), 199-206, doi:10.1029/PA004i002p00199 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #DEPTH, sediment/rock; Globigerinoides ruber, d18O; Isotope ratio mass spectrometry; PC; Piston corer; RC09; RC09-191; Robert Conrad |
| Tipo |
Dataset |
