d13C, dissolved inorganic carbon of CTD station NIOP-C2_926-1
| Cobertura |
LATITUDE: 14.850000 * LONGITUDE: 51.485000 * DATE/TIME START: 1993-03-03T00:00:00 * DATE/TIME END: 1993-03-03T00:00:00 * MINIMUM DEPTH, water: 9.9 m * MAXIMUM DEPTH, water: 100.1 m |
|---|---|
| Data(s) |
02/04/2003
|
| Formato |
text/tab-separated-values, 10 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.94724 doi:10.1594/PANGAEA.94724 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Moos, Christopher (2000): Reconstruction of upwelling intensity and paleo-nutrient gradients in the northwest Arabian Sea derived from stable carbon and oxygen isotopes of planktic foraminifera. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 156, 103 pp, urn:nbn:de:gbv:46-ep000102766 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #CTD/Rosette; CTD-RO; delta 13C, dissolved inorganic carbon; DEPTH, water; GeoB; Geosciences, University of Bremen; Gulf of Aden; Mass spectrometer Finnigan Delta-S; Netherlands Indian Ocean Programme; NIOP; NIOP-C2; NIOP-C2_926-1; Pressure, water; Tyro |
| Tipo |
Dataset |
