Stable oxygen isotopic composition of Globigerinoides ruber of sediment core KNR140-37JPC
| Cobertura |
LATITUDE: 31.690000 * LONGITUDE: -75.430000 * MINIMUM DEPTH, sediment/rock: 14.52 m * MAXIMUM DEPTH, sediment/rock: 19.98 m |
|---|---|
| Data(s) |
04/06/2001
|
| Formato |
text/tab-separated-values, 136 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.846757 doi:10.1594/PANGAEA.846757 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.846758 Oppo, Delia W; Horowitz, Michael; Lehmann, Scott J (1997): Marine core evidence for reduced deep water production during Termination II followed by a relatively stable substage 5e (Eemian). Paleoceanography, 12(1), 51-63, doi:10.1029/96PA03133 Oppo, Delia W; Keigwin, Lloyd D; McManus, Jerry F; Cullen, James L (2001): Persistent suborbital climate variability in marine isotope stage 5 and termination II. Paleoceanography, 16(3), 280-292, doi:10.1029/2000PA000527 Marine isotope stage 5/Termination II data (URI: https://www.ncdc.noaa.gov/paleo/study/2563) |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; DEPTH, sediment/rock; Globigerinoides ruber, d18O; Isotope ratio mass spectrometry; Knorr; KNR140; KNR140-37JPC; North Atlantic Ocean; Ocean Drilling Program; ODP; PC; Piston corer |
| Tipo |
Dataset |
