Stable carbon and oxygen isotope ratios of benthic foraminifera from ODP Site 184-1146
| Cobertura |
LATITUDE: 19.456700 * LONGITUDE: 116.272917 * DATE/TIME START: 1999-03-21T00:00:00 * DATE/TIME END: 1999-03-29T00:00:00 * MINIMUM DEPTH, sediment/rock: 371.43 m * MAXIMUM DEPTH, sediment/rock: 469.30 m |
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| Data(s) |
07/01/2013
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| Formato |
text/tab-separated-values, 7970 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.825478 doi:10.1594/PANGAEA.825478 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.825480 Holbourn, Ann; Kuhnt, Wolfgang; Clemens, Steven C; Prell, Warren L; Andersen, Nils (2013): Middle to late Miocene stepwise climate cooling: Evidence from a high-resolution deep water isotope curve spanning 8 million years. Paleoceanography, 28, 1-12, doi:10.1002/2013PA002538 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #184-1146; AGE; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Foraminifera, benthic d13C; Foraminifera, benthic d18O; Intercore correlation; Joides Resolution; Leg184; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; South China Sea |
| Tipo |
Dataset |
