Organic carbon and d13C of sediment core GIK16772-2 (Table A5)
| Cobertura |
LATITUDE: -1.350000 * LONGITUDE: -11.961667 * DATE/TIME START: 1988-01-21T00:00:00 * DATE/TIME END: 1988-01-21T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 14.870 m |
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| Data(s) |
29/01/2003
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| Formato |
text/tab-separated-values, 1017 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.89392 doi:10.1594/PANGAEA.89392 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
Westerhausen, Lothar (1992): Organische Sedimente im äquatorialen Ostatlantik: Einflüsse von Herkunft, Transportmustern, Diagenese und Klimaschwankungen. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 48, 109 pp, doi:10.2312/reports-gpi.1992.48 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Accumulation rate, total organic carbon; AGE; Carbon, organic, total; Carbon dioxide, total; delta 13C, organic carbon; Depth, composite; DEPTH, sediment/rock; eastern Romanche Fracture Zone; Element analyser CHN, LECO; GIK/IfG; GIK16772-2; Institute for Geosciences, Christian Albrechts University, Kiel; Intercore correlation; KOL; M6/5; Mass spectrometer Finnigan MAT 251; Meteor (1986); Normalized; Piston corer (Kiel type) |
| Tipo |
Dataset |
