(Table S1) In situ d18O measurements in the basal areas of muricae from ODP Site 143-865
| Cobertura |
MEDIAN LATITUDE: 18.440350 * MEDIAN LONGITUDE: -179.555000 * SOUTH-BOUND LATITUDE: 18.440300 * WEST-BOUND LONGITUDE: -179.555000 * NORTH-BOUND LATITUDE: 18.440400 * EAST-BOUND LONGITUDE: -179.555000 * DATE/TIME START: 1992-03-27T00:00:00 * DATE/TIME END: 1992-04-04T14:15:00 * MINIMUM DEPTH, sediment/rock: 71.70 m * MAXIMUM DEPTH, sediment/rock: 105.00 m |
|---|---|
| Data(s) |
04/11/2013
|
| Formato |
text/tab-separated-values, 1587 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.821635 doi:10.1594/PANGAEA.821635 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.821636 Kozdon, Reinhard; Kelly, Daniel Clay; Kita, Noriko T; Fournelle, John H; Valley, John W (2011): Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene. Paleoceanography, 26(3), PA3206, doi:10.1029/2010PA002056 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #143-865; 143-865C; Comment; COMPCORE; Composite Core; Date; delta 18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Error, absolute; Event label; Ion microprobe; Joides Resolution; Leg143; North Pacific Ocean; Number; Ocean Drilling Program; ODP; Oxygen 16, secondary ion intensity; Oxygen 16, secondary ion yield; Sample comment; Sample ID; Standard deviation |
| Tipo |
Dataset |
