Stable carbon and oxygen isotope ratios of planktonic foraminifera of sediment core GeoB1032
Cobertura |
MEDIAN LATITUDE: -22.914167 * MEDIAN LONGITUDE: 6.031667 * SOUTH-BOUND LATITUDE: -22.915000 * WEST-BOUND LONGITUDE: 6.026667 * NORTH-BOUND LATITUDE: -22.913333 * EAST-BOUND LONGITUDE: 6.036667 * DATE/TIME START: 1988-03-04T00:00:00 * DATE/TIME END: 1988-03-04T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 3.78 m |
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Data(s) |
01/06/1996
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Formato |
text/tab-separated-values, 780 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.54655 doi:10.1594/PANGAEA.54655 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.738529 Wefer, Gerold; Berger, Wolfgang H; Bickert, Torsten; Donner, Barbara; Fischer, Gerhard; Kemle-von Mücke, Sylvia; Pätzold, Jürgen; Meinecke, Gerrit; Müller, Peter J; Mulitza, Stefan; Niebler, Hans-Stefan; Schmidt, Heike; Schneider, Ralph R; Segl, Monika (1996): Late Quaternary surface circulation of the South Atlantic: The stable isotope record and implications for heat transport and productivity. In: Wefer, G; Berger, W H; Siedler, G & Webb, D (eds.), The South Atlantic: Present and Past Circulation, Springer, Berlin, Heidelberg, 461-502 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Angola Basin; DEPTH, sediment/rock; Event label; GeoB; GeoB1032-2; GeoB1032-3; Geosciences, University of Bremen; Giant box corer; GKG; Globigerinoides ruber white, d13C; Globigerinoides ruber white, d18O; Globorotalia inflata, d13C; Globorotalia inflata, d18O; Globorotalia truncatulinoides sinistral, d13C; Globorotalia truncatulinoides sinistral, d18O; Gravity corer (Kiel type); M6/6; Mass spectrometer Finnigan MAT 251; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Walvis Ridge |
Tipo |
Dataset |