(Table 5) Oxygen and carbon isotopes of Orbulina universa at DSDP Hole 72-518
| Cobertura |
LATITUDE: -29.973700 * LONGITUDE: -38.135300 * DATE/TIME START: 1980-04-02T00:00:00 * DATE/TIME END: 1980-04-02T00:00:00 * MINIMUM DEPTH, sediment/rock: 28.0 m * MAXIMUM DEPTH, sediment/rock: 43.7 m |
|---|---|
| Data(s) |
30/05/1983
|
| Formato |
text/tab-separated-values, 105 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.814008 doi:10.1594/PANGAEA.814008 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.814013 Hodell, David A; Kennett, James P; Leonard, Kathleen A (1983): Climatically induced changes in vertical water mass structure of the Vema Channel during the Pliocene: evidence from Deep Sea Drilling Project Holes 516A, 517, and 518. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 907-919, doi:10.2973/dsdp.proc.72.146.1983 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #72-518; AGE; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg72; Mass spectrometer VG Micromass 602; ODP sample designation; Orbulina universa, d13C; Orbulina universa, d18O; Sample code/label; South Atlantic/CONT RISE |
| Tipo |
Dataset |
