(Table A2) Stable oxygen isotope ratios of planktonic foraminifera from sediment core GeoB1016-3
| Cobertura |
LATITUDE: -11.770500 * LONGITUDE: 11.681900 * DATE/TIME START: 1988-02-25T00:00:00 * DATE/TIME END: 1988-02-25T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.04 m * MAXIMUM DEPTH, sediment/rock: 9.33 m |
|---|---|
| Data(s) |
12/08/1995
|
| Formato |
text/tab-separated-values, 341 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.263934 doi:10.1594/PANGAEA.263934 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.726545 Schneider, Ralph R; Müller, Peter J; Ruhland, Götz (1995): Late Quaternary surface circulation in the east-equatorial South Atlantic: evidence from alkenone sea surface temperatures. Paleoceanography, 10(2), 197-220, doi:10.1029/94PA03308 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Angola Basin; DEPTH, sediment/rock; GeoB1016-3; Globigerina bulloides, d18O; Globigerinoides ruber pink, d18O; Gravity corer (Kiel type); M6/6; Mass spectrometer Finnigan MAT 251; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents |
| Tipo |
Dataset |
