(Fig. 3) Lithic concentration derived from sediment brightness and iron intensity of sediment core GeoB7186-3
| Cobertura |
LATITUDE: -44.149330 * LONGITUDE: -75.158160 * DATE/TIME START: 2001-05-05T15:48:00 * DATE/TIME END: 2001-05-05T15:48:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 6.10 m |
|---|---|
| Data(s) |
10/01/2007
|
| Formato |
text/tab-separated-values, 1159 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.676708 doi:10.1594/PANGAEA.676708 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.726864 Mohtadi, Mahyar; Romero, Oscar E; Kaiser, Jérome; Hebbeln, Dierk (2007): Cooling of the southern high latitudes during the Medieval Period and its effect on ENSO. Quaternary Science Reviews, 26(7-8), 1055-1066, doi:10.1016/j.quascirev.2006.12.008 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB7186-3; Gravity corer (Kiel type); Iron; Lithic grains; MARUM; off Chile; PUCK; see reference(s); SL; SO156/3; Sonne; X-ray fluorescence core scanner (XRF) |
| Tipo |
Dataset |
