(Table 2) Occurrence of sapropels
| Cobertura |
MEDIAN LATITUDE: 38.025833 * MEDIAN LONGITUDE: 17.300750 * SOUTH-BOUND LATITUDE: 35.033333 * WEST-BOUND LONGITUDE: 16.530000 * NORTH-BOUND LATITUDE: 41.310000 * EAST-BOUND LONGITUDE: 18.033000 * DATE/TIME START: 1965-07-24T00:00:00 * DATE/TIME END: 1982-01-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.090 m * MAXIMUM DEPTH, sediment/rock: 0.750 m |
|---|---|
| Data(s) |
01/09/1989
|
| Formato |
text/tab-separated-values, 16 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.726983 doi:10.1594/PANGAEA.726983 |
| 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 | #Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; ETNA82; Event label; KET82-16; KET82-22; Marion Dufresne; MD84-658; Mediterranean Sea; NOE; PC; Piston corer; RC09; RC09-191; Robert Conrad |
| Tipo |
Dataset |
