(Table 1) Stable isotope ratios of foraminifera in sediment core CH82-20
| Cobertura |
MINIMUM DEPTH, sediment/rock: 0.035 m * MAXIMUM DEPTH, sediment/rock: 1.030 m |
|---|---|
| Data(s) |
09/12/1994
|
| Formato |
text/tab-separated-values, 630 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.52678 doi:10.1594/PANGAEA.52678 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.729844 Keigwin, Lloyd D; Lehmann, Scott J (1994): Deep circulation change linked to Heinrich event 1 and Younger Dryas in a middepth North Atlantic core. Paleoceanography, 9(2), 185-194, doi:10.1029/94PA00032 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; CH82-20pc; CH82-20pg; CH8X; Counting >150 µm fraction; Depth, composite; DEPTH, sediment/rock; Event label; Foraminifera, per unit sediment mass; Globigerina bulloides, d13C; Globigerina bulloides, d18O; Ice rafted debris; Intercore correlation; Isotope ratio mass spectrometry; Jean Charcot; Neogloboquadrina pachyderma sinistral; PC; Piston corer; Planulina wuellerstorfi; Planulina wuellerstorfi, d13C; Planulina wuellerstorfi, d18O; TC; Trigger corer |
| Tipo |
Dataset |
