Thermocline of sediment core GeoB1105-4
| Cobertura |
LATITUDE: -1.665000 * LONGITUDE: -12.428333 * DATE/TIME START: 1989-01-26T00:00:00 * DATE/TIME END: 1989-01-26T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 10.78 m |
|---|---|
| Data(s) |
17/12/2004
|
| Formato |
text/tab-separated-values, 111 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.223474 doi:10.1594/PANGAEA.223474 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Wolff, Tobias (1998): Mixed layer characteristics in the equatorial Atlantic during the late Quaternary as deduced from planktonic foraminifera. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 125, 132 pp, urn:nbn:de:gbv:46-ep000102448 Wolff, Tobias; Mulitza, Stefan; Rühlemann, Carsten; Wefer, Gerold (1999): Response of the tropical Atlantic thermocline to Late Quaternary trade wind changes. Paleoceanography, 14(3), 374-383, doi:10.1029/1999PA900011 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Calculated; DEPTH, sediment/rock; Depth of thermocline; Equatorial Atlantic; GeoB; GeoB1105-4; Geosciences, University of Bremen; Gravity corer (Kiel type); M9/4; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents |
| Tipo |
Dataset |
