Stable oxygen and carbon isotope ratios measured on benthic foraminifera from ODP Site 202-1237
| Cobertura |
LATITUDE: -16.007017 * LONGITUDE: -76.378083 * DATE/TIME START: 2002-04-26T00:00:00 * DATE/TIME END: 2002-04-26T00:00:00 * MINIMUM DEPTH, sediment/rock: 182.67 m * MAXIMUM DEPTH, sediment/rock: 213.91 m |
|---|---|
| Data(s) |
26/09/2007
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| Formato |
text/tab-separated-values, 2728 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.658952 doi:10.1594/PANGAEA.658952 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.658956 Holbourn, Ann; Kuhnt, Wolfgang; Schulz, Michael; Flores, José-Abel; Andersen, Nils (2007): Orbitally-paced climate evolution during the middle Miocene "Monterey" carbon-isotope excursion. Earth and Planetary Science Letters, 261(3-4), 534-550, doi:10.1016/j.epsl.2007.07.026 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #202-1237; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Foraminifera, benthic d13C; Foraminifera, benthic d18O; Intercore correlation; Isotope ratio mass spectrometry; Joides Resolution; Leg202; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; South Pacific Ocean |
| Tipo |
Dataset |
