(Appendix A2) Stable carbon and oxygen isotope ratio of Globorotalia inflata from sediment core GeoB1706-2
| Cobertura |
LATITUDE: -19.561667 * LONGITUDE: 11.175000 * DATE/TIME START: 1992-01-08T00:00:00 * DATE/TIME END: 1992-01-08T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 11.08 m |
|---|---|
| Data(s) |
02/03/1997
|
| Formato |
text/tab-separated-values, 441 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.218244 doi:10.1594/PANGAEA.218244 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.734360 Little, Mark G; Schneider, Ralph R; Kroon, Dick; Price, B; Bickert, Torsten; Wefer, Gerold (1997): Rapid paleoceanographic changes in the Benguela Upwelling System for the last 160,000 years as indicated by abundances of planktonic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130(1-4), 135-161, doi:10.1016/S0031-0182(96)00136-8 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #DEPTH, sediment/rock; GeoB; GeoB1706-2; Geosciences, University of Bremen; Globorotalia inflata, d13C; Globorotalia inflata, d18O; Gravity corer (Kiel type); Isotope ratio mass spectrometry; M20/2; Meteor (1986); SL; Walvis Ridge |
| Tipo |
Dataset |
