(Appendix 2) Redox-sensitive trace-element contents in the Valanginian samples for the studied sections
| Cobertura |
LATITUDE: 31.577630 * LONGITUDE: 157.297700 * DATE/TIME START: 2001-10-04T03:00:00 * DATE/TIME END: 2001-10-09T19:00:00 * MINIMUM ELEVATION: -3882.6 m * MAXIMUM ELEVATION: -3882.6 m |
|---|---|
| Data(s) |
27/09/2010
|
| Formato |
text/tab-separated-values, 133 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.789178 doi:10.1594/PANGAEA.789178 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.789179 Westermann, Stéphane; Föllmi, Karl B; Adatte, Thierry; Matera, Virginie; Schnyder, Johann; Fleitmann, Dominik; Fiet, Nicolas; Ploch, Izabela; Duchamp-Alponse, Stéphanie (2010): The Valanginian d13C excursion may not be an expression of a global oceanic anoxic event. Earth and Planetary Science Letters, 290(1-2), 118-131, doi:10.1016/j.epsl.2009.12.011 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #198-1213B; Aluminium; Arsenic; Chromium; Cobalt; Comment; Copper; DRILL; Drilling/drill rig; ICP-MS, Inductively coupled plasma - mass spectrometry; Iron; Joides Resolution; Leg198; Manganese; Molybdenum; North Pacific Ocean; ODP sample designation; Sample code/label; Sample ID; Uranium; Vanadium; Zinc |
| Tipo |
Dataset |
