Table 1. Organic carbon isotopic signal in core MD04-2876
| Cobertura |
LATITUDE: 24.842830 * LONGITUDE: 64.008160 * MINIMUM DEPTH, sediment/rock: 3.15 m * MAXIMUM DEPTH, sediment/rock: 18.30 m |
|---|---|
| Data(s) |
04/09/2007
|
| Formato |
text/tab-separated-values, 10 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.727156 doi:10.1594/PANGAEA.727156 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.727157 Pichevin, Laetitia E; Bard, Edouard; Martinez, Philippe; Billy, Isabelle (2007): Evidence of ventilation changes in the Arabian Sea during the late Quaternary: Implication for denitrification and nitrous oxide emission. Global Biogeochemical Cycles, 21, GB4008, doi:10.1029/2006GB002852 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; CALYPSO; Calypso Corer; CHAMAK; delta 13C, organic carbon; DEPTH, sediment/rock; Isotope ratio mass spectrometry; Marion Dufresne; MD04-2876; MD143; Pakistan continental margin |
| Tipo |
Dataset |
