Sea surface temperature based on TEX86 as well as mean annual air temperature based on CBT and MBT from IODP Hole 318-U1356A
Cobertura |
LATITUDE: -63.310230 * LONGITUDE: 135.998960 * MINIMUM DEPTH, sediment/rock: 900.76 m * MAXIMUM DEPTH, sediment/rock: 999.81 m |
---|---|
Data(s) |
04/07/2013
|
Formato |
text/tab-separated-values, 1287 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.816366 doi:10.1594/PANGAEA.816366 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.816368 Bijl, Peter K; Bendle, James A; Bohaty, Steven M; Pross, Jörg; Schouten, Stefan; Tauxe, Lisa; Stickley, Catherine E; McKay, Robert M; Röhl, Ursula; Olney, M; Sluijs, Appy; Escutia Dotti, Carlota; Brinkhuis, Henk; Expedition 318 Scientists (2013): Eocene cooling linked to early flow across the Tasmanian Gateway. Proceedings of the National Academy of Sciences of the United States of America, doi:10.1073/pnas.1220872110 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #318-U1356A; AGE; Calculated; Cyclization ratio of branched tetraethers; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Exp318; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Methylation index of branched tetraethers; ODP sample designation; Sample code/label; Sea surface temperature; Temperature, air, annual mean; Tetraether index of 86 carbon atoms; Wilkes Land |
Tipo |
Dataset |