Dissolution index and stable oxygen isotope ratios of planktonic foraminifera of sediment core GeoB3910-2
| Cobertura |
LATITUDE: -4.245000 * LONGITUDE: -36.345000 * DATE/TIME START: 1996-03-30T00:00:00 * DATE/TIME END: 1996-03-30T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.000 m * MAXIMUM DEPTH, sediment/rock: 0.545 m |
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| Data(s) |
03/04/2001
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| Formato |
text/tab-separated-values, 326 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.58290 doi:10.1594/PANGAEA.58290 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.735159 Arz, Helge W; Gerhardt, Sabine; Pätzold, Jürgen; Röhl, Ursula (2001): Millennial-scale changes of surface- and deep-water flow in the western tropical Atlantic linked to Northern Hemisphere high-latitude climate during the Holocene. Geology, 29(3), 239-242, doi:10.1130/0091-7613(2001)029<0239:MSCOSA>2.0.CO;2 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Calculated, see reference(s); DEPTH, sediment/rock; GeoB; GeoB3910-2; Geosciences, University of Bremen; Globigerinoides sacculifer, d18O; Globorotalia tumida, d18O; Gravity corer (Kiel type); Limacina dissolution index; M34/4; Mass spectrometer Finnigan MAT 251; Meteor (1986); Northeast Brasilian Margin; SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents |
| Tipo |
Dataset |
