Planktonic foraminifera of IODP Hole 339-U1387C
| Cobertura |
LATITUDE: 36.805232 * LONGITUDE: -7.718795 * MINIMUM DEPTH, sediment/rock: 731.50 m * MAXIMUM DEPTH, sediment/rock: 865.55 m |
|---|---|
| Data(s) |
30/03/2016
|
| Formato |
text/tab-separated-values, 1057 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.859196 doi:10.1594/PANGAEA.859196 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.859197 Van der Schee, Marlies; Sierro, Francisco Javier; Jiménez-Espejo, Francisco J; Hernandéz-Molina, Francisco Javier; Flecker, Rachel; Flores, José-Abel; Acton, Gary D; Gutjahr, Marcus; Grunert, Patrick; García-Gallardo, Ángela; Andersen, Nils (2016): Evidence of early bottom water current flow after the Messinian Salinity Crisis in the Gulf of Cadiz. Marine Geology, in press |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #339-U1387C; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp339; Foraminifera, planktic; Globorotalia margaritae; Globorotalia menardii sinistral; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mediterranean Outflow; Neogloboquadrina acostaensis dextral; Neogloboquadrina acostaensis sinistral; Sample code/label |
| Tipo |
Dataset |
