(Table 1b) Stable oxgen isotope ratio measured on G. ruber from sediment core KET82-22
| Cobertura |
LATITUDE: 37.560000 * LONGITUDE: 16.530000 * DATE/TIME START: 1982-01-01T00:00:00 * DATE/TIME END: 1982-01-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.0 m * MAXIMUM DEPTH, sediment/rock: 1.6 m |
|---|---|
| Data(s) |
01/09/1989
|
| Formato |
text/tab-separated-values, 17 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.726980 doi:10.1594/PANGAEA.726980 |
| 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; ETNA82; Globigerinoides ruber, d18O; Isotope ratio mass spectrometry; KET82-22; Mediterranean Sea; PC; Piston corer |
| Tipo |
Dataset |
