Highly branched isoprenoids in core JPC38
| Cobertura |
LATITUDE: -63.717000 * LONGITUDE: -57.411000 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 19.85 m |
|---|---|
| Data(s) |
02/03/2016
|
| Formato |
text/tab-separated-values, 1398 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.858523 doi:10.1594/PANGAEA.858523 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.858524 Barbara, Loïc; Crosta, Xavier; Leventer, Amy; Schmidt, S; Etourneau, Johan; Domack, Eugene W; Massé, Guillaume (2016): Environmental responses of the Northeast Antarctic Peninsula to the Holocene climate variability. Paleoceanography, 31(1), 131-147, doi:10.1002/2015PA002785 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Calculated; DEPTH, sediment/rock; Highly branched isoprenoids, diunsatured; Highly branched isoprenoids, triunsatured; Nathaniel B. Palmer; NBP00-03; NBP00-03-JPC38; PC; Piston corer; Ratio; Vega Drift, Prince Gustav Channel, Antarctic Peninsula |
| Tipo |
Dataset |
