(Table 4) Stable oxygen and carbon isotopic composition from plankton sample Site GeoB8305
| Cobertura |
MEDIAN LATITUDE: -33.471417 * MEDIAN LONGITUDE: 17.169333 * SOUTH-BOUND LATITUDE: -33.475333 * WEST-BOUND LONGITUDE: 17.169167 * NORTH-BOUND LATITUDE: -33.467500 * EAST-BOUND LONGITUDE: 17.169500 * DATE/TIME START: 2003-01-23T13:56:00 * DATE/TIME END: 2003-01-23T14:51:00 * MINIMUM DEPTH, water: 10 m * MAXIMUM DEPTH, water: 400 m |
|---|---|
| Data(s) |
18/05/2006
|
| Formato |
text/tab-separated-values, 68 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.323636 doi:10.1594/PANGAEA.323636 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.738238 Wilke, Iris (2005): The influence of seasonal distribution patterns, ecological preferences and calcification process on the incorporation of stable oxygen and carbon isotopes in planktic foraminiferal clacite shells. PhD Thesis, Elektronische Dissertationen an der Staats- und Universitätsbibliothek Bremen, Germany, urn:nbn:de:gbv:46-diss000012356 Wilke, Iris; Peeters, Frank JC; Bickert, Torsten (2006): The influence of seawater carbonate ion concentration [CO32-] on the stable isotope composition of planktic foraminifera species Globorotalia inflata. Marine Micropaleontology, 58(4), 243-258, doi:10.1016/j.marmicro.2005.11.005 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Calculated; Center for Marine Environmental Sciences; delta 13C, dissolved inorganic carbon; delta 18O; Depth, bottom/max; Depth, top/min; DEPTH, water; Event label; GeoB; GeoB8305-4; GeoB8305-5; Geosciences, University of Bremen; Globorotalia inflata, d13C; Globorotalia inflata, d18O; M57/1; MARUM; Mass spectrometer Finnigan MAT 252; Meteor (1986); MSN; Multiple opening/closing net; Temperature, water |
| Tipo |
Dataset |
