IRD, foraminifera abundance, stable isotope ratios of Cassidulina teretis and susceptibility of sediment core MD95-2010
| Cobertura |
LATITUDE: 66.684167 * LONGITUDE: 4.566160 * DATE/TIME START: 1995-06-07T00:00:00 * DATE/TIME END: 1995-06-07T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 11.025 m |
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| Data(s) |
18/10/1999
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| Formato |
text/tab-separated-values, 5078 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.61471 doi:10.1594/PANGAEA.61471 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.735730 Dokken, Trond; Jansen, Eystein (1999): Rapid changes in the mechanism of ocean convection during the last glacial period. Nature, 401(6752), 458-461, doi:10.1038/46753 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; CALYPSO; Calypso Corer; Cassidulina teretis, d13C; Cassidulina teretis, d18O; Counting; Counting >150 µm fraction; Counting >500 µm fraction; DEPTH, sediment/rock; Foraminifera, per unit sediment mass; Geological High-resolution Magnetic Tool (GHMT); Ice rafted debris; IMAGES; IMAGES I; International Marine Global Change Study; Isotope ratio mass spectrometry; Magnetic susceptibility; Marion Dufresne; MD101; MD952010; MD95-2010; Neogloboquadrina pachyderma sinistral, d13C; Neogloboquadrina pachyderma sinistral, d18O; Rock fragments per unit mass; Voring Plateau |
| Tipo |
Dataset |
