(Table S3, Figure 3b) Major element concentrations of sediment core GeoB16224-1
| Cobertura |
LATITUDE: 6.656333 * LONGITUDE: -52.083167 * DATE/TIME START: 2012-03-08T16:07:00 * DATE/TIME END: 2012-03-08T16:07:00 * MINIMUM DEPTH, sediment/rock: 0.04 m * MAXIMUM DEPTH, sediment/rock: 7.44 m |
|---|---|
| Data(s) |
19/10/2015
|
| Formato |
text/tab-separated-values, 300 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.854047 doi:10.1594/PANGAEA.854047 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.854054 Zhang, Yancheng; Chiessi, Cristiano Mazur; Mulitza, Stefan; Zabel, Matthias; Trindade, Ricardo; Hollanda, Maria Helena B M; Dantas, Elton L; Govin, Aline; Tiedemann, Ralf; Wefer, Gerold (2015): Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas. Earth and Planetary Science Letters, 432, 493-500, doi:10.1016/j.epsl.2015.09.054 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #087-1; Aluminium; Aluminium/Silicon ratio; Calculated; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Energy dispersive polarization X-ray fluorescence spectrometer (EDP-XRF); French Guiana; GeoB16224-1; Gravity corer (Kiel type); Maria S. Merian; MARUM; MSM20/3; Rubidium; Rubidium/Strontium ratio; Silicon; SL; Strontium |
| Tipo |
Dataset |
