Figure 5. Stable oxygen isotope ratios on Neogloboquadrina pachyderma of sediment core MD95-2024
| Cobertura |
LATITUDE: 50.206667 * LONGITUDE: -45.687000 * DATE/TIME START: 1995-06-18T00:00:00 * DATE/TIME END: 1995-06-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 26.15 m |
|---|---|
| Data(s) |
22/04/2001
|
| Formato |
text/tab-separated-values, 5137 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.779741 doi:10.1594/PANGAEA.779741 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.778950 Weber, Michael E; Mayer, Larry A; Hillaire-Marcel, Claude; Bilodeau, G; Rack, Frank R; Hiscott, Richard N; Aksu, Ali E (2001): Derivation of d18O from sediment core log data: Implications for millennial-scale climate change in the Labrador Sea. Paleoceanography, 16(5), 503-514, doi:10.1029/2000PA000560 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #CALYPSO; Calypso Corer; delta 18O; DEPTH, sediment/rock; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne; Mass spectrometry; MD101; MD952024; MD95-2024; Neogloboquadrina pachyderma dextral and/or sinistral, d18O; Orphan Knoll; predicted |
| Tipo |
Dataset |
