Stable isotope analysis on planktic foraminifera in sediment core GIK23074-3
| Cobertura |
LATITUDE: 66.673333 * LONGITUDE: 4.906660 * DATE/TIME START: 1986-07-13T00:00:00 * DATE/TIME END: 1986-07-13T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.10 m * MAXIMUM DEPTH, sediment/rock: 0.15 m |
|---|---|
| Data(s) |
09/07/2003
|
| Formato |
text/tab-separated-values, 4 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.107749 doi:10.1594/PANGAEA.107749 |
| 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; Giant box corer; GIK/IfG; GIK23074-3; GKG; Institute for Geosciences, Christian Albrechts University, Kiel; M2/2; Mass spectrometer Finnigan MAT 250; Meteor (1986); Neogloboquadrina pachyderma sinistral, d13C; Neogloboquadrina pachyderma sinistral, d18O; Norwegian Sea |
| Tipo |
Dataset |
