Stable oxygen isotope ratios of U. peregrina from sediment core V25-59
| Cobertura |
LATITUDE: 1.367000 * LONGITUDE: -33.480000 * DATE/TIME START: 1968-02-26T00:00:00 * DATE/TIME END: 1968-02-26T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 0.82 m |
|---|---|
| Data(s) |
26/01/2006
|
| Formato |
text/tab-separated-values, 32 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.355355 doi:10.1594/PANGAEA.355355 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Mix, Alan C (1986): Late Quaternary paleoceanography of the Atlantic Ocean: Foraminiferal faunal and stable-isotopic evidence. PhD Thesis, Columbia University, New York, 321 pp |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #DEPTH, sediment/rock; Isotope ratio mass spectrometry; Lamont-Doherty Earth Observatory, Columbia University; LDEO; Neogloboquadrina dutertrei, d18O; PC; Piston corer; V25; V25-59; Vema |
| Tipo |
Dataset |
