(Table S3, Figure 3c) XRF-calibrated ln(Fe/Ca) of sediment core GeoB16206-1
| Cobertura |
LATITUDE: -1.579167 * LONGITUDE: -43.023667 * DATE/TIME START: 2012-02-24T02:00:00 * DATE/TIME END: 2012-02-24T02:00:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 8.10 m |
|---|---|
| Data(s) |
19/10/2015
|
| Formato |
text/tab-separated-values, 398 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.854043 doi:10.1594/PANGAEA.854043 |
| 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 | #057-1; Calibrated after Weltje & Tjallingi (2008); Center for Marine Environmental Sciences; Continental Slope Northeast Brazil; DEPTH, sediment/rock; GeoB16206-1; Gravity corer (Kiel type); ln-Iron/Calcium ratio; Maria S. Merian; MARUM; MSM20/3; SL |
| Tipo |
Dataset |
