Table A1. Age model of sediment core GeoB1710-3
| Cobertura |
LATITUDE: -23.431667 * LONGITUDE: 11.698333 * DATE/TIME START: 1992-01-11T00:00:00 * DATE/TIME END: 1992-01-11T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.64 m * MAXIMUM DEPTH, sediment/rock: 10.64 m |
|---|---|
| Data(s) |
21/10/1997
|
| Formato |
text/tab-separated-values, 50 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.728683 doi:10.1594/PANGAEA.728683 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.728744 Schmiedl, Gerhard; Mackensen, Andreas (1997): Late Quaternary paleoproductivity and deep water circulation in the eastern South Altantic Ocean: Evidence from benthic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130(1-4), 43-80, doi:10.1016/S0031-0182(96)00137-X |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Age, comment; Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); AWI_Paleo; DEPTH, sediment/rock; GeoB1710-3; Gravity corer (Kiel type); M20/2; Meteor (1986); Namibia continental slope; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; SL |
| Tipo |
Dataset |
