(Figure 4) Stable oxygen isotope ratios of benthic foraminifera from sediment core Alkor_159_225514 from the Skagerrak, North Sea
| Cobertura |
LATITUDE: 57.840556 * LONGITUDE: 8.709083 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 1.90 m |
|---|---|
| Data(s) |
10/01/2006
|
| Formato |
text/tab-separated-values, 226 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.676721 doi:10.1594/PANGAEA.676721 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.676724 Brückner, Sylvia (2008): Climatic and hydrographic variability in the late Holocene Skagerrak as deduced from benthic foraminiferal proxies (Klimatische und hydrographische Variabilität im holozänen Sagerrak, abgeleitet aus benthischen Foraminiferen). Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 572, 139 pp, hdl:10013/epic.28879 Brückner, Sylvia; Mackensen, Andreas (2006): Deep-water renewal in the Skagerrak during the last 1200 years triggered by the North Atlantic Oscillation: evidence from benthic foraminiferal d18O. The Holocene, 16(3), 331-340, doi:10.1191/0959683605hl931rp |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Age; AL159; AL159_225514; Alkor (1990); AWI_Paleo; Bulimina marginata, d18O; DEPTH, sediment/rock; GC; Gravity corer; Mass spectrometer Finnigan MAT 251; Melonis barleeanus, d18O; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Skagerrak; Uvigerina mediterranea, d18O |
| Tipo |
Dataset |
