(Figure 4) Comparison of LDI-inferred SST with UK'37 inferred SST from sediment core GeoB6518-1
| Cobertura |
LATITUDE: -5.588300 * LONGITUDE: 11.221700 * DATE/TIME START: 2000-06-20T15:23:00 * DATE/TIME END: 2000-06-20T15:23:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 7.18 m |
|---|---|
| Data(s) |
14/01/2012
|
| Formato |
text/tab-separated-values, 285 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.825999 doi:10.1594/PANGAEA.825999 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.825638 Rampen, Sebastiaan W; Willmott, Verónica; Kim, Jung-Hyun; Uliana, Eleonora; Mollenhauer, Gesine; Schefuß, Enno; Sinninghe Damsté, Jaap S; Schouten, Stefan (2012): Long chain 1,13- and 1,15-diols as a potential proxy for palaeotemperature reconstruction. Geochimica et Cosmochimica Acta, 84, 204-216, doi:10.1016/j.gca.2012.01.024 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Congo Fan; DEPTH, sediment/rock; GeoB6518-1; Gravity corer (Kiel type); M47/3; Meteor (1986); Sea surface temperature, annual mean; SL; SST, from long chain diol index (LDI); SST, from UK'37 |
| Tipo |
Dataset |
