(Table 1) Age control-points for the oxygen-isotope curve of sediment core GeoB1711-4
| Cobertura |
LATITUDE: -23.315000 * LONGITUDE: 12.376667 * DATE/TIME START: 1992-01-11T00:00:00 * DATE/TIME END: 1992-01-11T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.91 m * MAXIMUM DEPTH, sediment/rock: 10.71 m |
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| Data(s) |
02/03/1997
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| Formato |
text/tab-separated-values, 18 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.734359 doi:10.1594/PANGAEA.734359 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.734360 Little, Mark G; Schneider, Ralph R; Kroon, Dick; Price, B; Bickert, Torsten; Wefer, Gerold (1997): Rapid paleoceanographic changes in the Benguela Upwelling System for the last 160,000 years as indicated by abundances of planktonic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130(1-4), 135-161, doi:10.1016/S0031-0182(96)00136-8 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Age model; Age model, stable isotope stratigraphy; DEPTH, sediment/rock; GeoB; GeoB1711-4; Geosciences, University of Bremen; Gravity corer (Kiel type); Isotopic event; M20/2; Meteor (1986); Namibia continental slope; SL |
| Tipo |
Dataset |
