(Table 2) Calcium carbonate and stable oxygen isotope ratios of Globorotalia tumida from sediment core W8803B-T-47
| Cobertura |
LATITUDE: 0.500000 * LONGITUDE: -133.300000 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 0.470 m |
|---|---|
| Data(s) |
17/07/1993
|
| Formato |
text/tab-separated-values, 36 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.76271 doi:10.1594/PANGAEA.76271 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.729776 Murray, Richard W; Leinen, Margaret W; Isern, Alexandra R (1993): Biogenic flux of Al to sediment in the central Pacific Ocean: evidence for increased productivity during glacial periods. Paleoceanography, 8(5), 651-670, doi:10.1029/93PA02195 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Calcium carbonate; Department of Geology, Oregon State University; DEPTH, sediment/rock; Element analysis coulometric; GC; Globorotalia tumida, d18O; Gravity corer; Mass spectrometer VG Isogas Prism; OSU; W8803B; W8803B-T-47; Wecoma |
| Tipo |
Dataset |
