(Table 2) Organic carbon content and stable carbon isotope ratios, and hydrogen and oxygen index of sediment core BX-4
| Cobertura |
LATITUDE: -15.263300 * LONGITUDE: -75.391700 * MINIMUM DEPTH, sediment/rock: 0.015 m * MAXIMUM DEPTH, sediment/rock: 0.330 m |
|---|---|
| Data(s) |
05/05/1986
|
| Formato |
text/tab-separated-values, 20 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.714828 doi:10.1594/PANGAEA.714828 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.714865 Dean, Walter E; Arthur, Michael A; Claypool, George E (1986): Depletion of 13C in Cretaceous marine organic matter: Source, diagenetic, or environmental signal? Marine Geology, 70(1-2), 119-157, doi:10.1016/0025-3227(86)90092-7 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #BC; Box corer; BX-4; Carbon, organic, total; delta 13C, organic carbon; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Hydrogen/Carbon ratio; Mass spectrometer Finnigan MAT 251 |
| Tipo |
Dataset |
