Ocean temperture reconstruction for sediment core NBP99-03_10
| Cobertura |
LATITUDE: -64.883330 * LONGITUDE: -64.200000 * MINIMUM DEPTH, sediment/rock: 0.04 m * MAXIMUM DEPTH, sediment/rock: 13.25 m |
|---|---|
| Data(s) |
30/08/2013
|
| Formato |
text/tab-separated-values, 84 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.818911 doi:10.1594/PANGAEA.818911 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.818912 Etourneau, Johan; Collins, LG; Willmott, Verónica; Kim, Jung-Hyun; Barbara, Loïc; Leventer, Amy; Schouten, Stefan; Sinninghe Damsté, Jaap S; Bianchini, A; Klein, V; Crosta, Xavier; Massé, Guillaume (2013): Holocene climate variations in the western Antarctic Peninsula: evidence for sea ice extent predominantly controlled by changes in insolation and ENSO variability. Climate of the Past, 9(4), 1431-1446, doi:10.5194/cp-9-1431-2013 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Calculated from TEX86 (Kim et al., 2010); Climate Change: Learning from the past climate; DEPTH, sediment/rock; Nathaniel B. Palmer; NBP99-03; NBP99-03_10; Palmer Deep Basin; Past4Future; PC; Piston corer; Sea surface temperature, annual mean |
| Tipo |
Dataset |
