(Table 1b) Stable oxgen isotope ratio measured on G. ruber from sediment core MD84-658
| Cobertura |
LATITUDE: 35.033333 * LONGITUDE: 17.050000 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 0.42 m |
|---|---|
| Data(s) |
01/09/1989
|
| Formato |
text/tab-separated-values, 9 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.358893 doi:10.1594/PANGAEA.358893 |
| 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; Marion Dufresne; MD84-658; Mediterranean Sea; NOE; PC; Piston corer |
| Tipo |
Dataset |
