Stable isotopes and Mg/Ca ratios of Globorotalia tumida of ODP Site 138-849
| Cobertura |
LATITUDE: 0.183330 * LONGITUDE: -110.518330 * DATE/TIME START: 1991-06-12T00:00:00 * DATE/TIME END: 1991-09-07T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 156.79 m |
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| Data(s) |
25/07/2012
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| Formato |
text/tab-separated-values, 1075 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.834322 doi:10.1594/PANGAEA.834322 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.834324 Ford, Heather L; Ravelo, Ana Christina; Hovan, Steven A (2012): A deep Eastern Equatorial Pacific thermocline during the early Pliocene warm period. Earth and Planetary Science Letters, 355-356, 152-161, doi:10.1016/j.epsl.2012.08.027 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #138-849; AGE; Calculated from Mg/Ca ratios (Anand et al., 2003); COMPCORE; Composite Core; DEPTH, sediment/rock; Globorotalia tumida, d13C; Globorotalia tumida, d18O; Globorotalia tumida, Magnesium/Calcium ratio; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Isotope ratio mass spectrometry; Joides Resolution; Leg138; North Pacific Ocean; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; Subsurface temperature |
| Tipo |
Dataset |
