Stable isotope analysis on planktic foraminifera in sediment core SU90-I04
| Cobertura |
LATITUDE: 57.978333 * LONGITUDE: -45.896667 * DATE/TIME START: 1990-01-01T00:00:00 * DATE/TIME END: 1990-01-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 0.49 m |
|---|---|
| Data(s) |
09/07/2003
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| Formato |
text/tab-separated-values, 42 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.107752 doi:10.1594/PANGAEA.107752 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Schulz, Hartmut (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp, doi:10.2312/reports-gpi.1995.73 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #DEPTH, sediment/rock; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Le Suroît; Mass spectrometer Finnigan MAT 250; Neogloboquadrina pachyderma sinistral, d13C; Neogloboquadrina pachyderma sinistral, d18O; North Atlantic; PALEOCINAT; PC; Piston corer; SU90-I04 |
| Tipo |
Dataset |
