(Table 3) d18O, B/Ca and Mg/Ca ratios in Globorotalia inflata from sediment core CHAT_16k
| Cobertura |
LATITUDE: -42.390000 * LONGITUDE: -178.500000 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 0.81 m |
|---|---|
| Data(s) |
03/06/2007
|
| Formato |
text/tab-separated-values, 242 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.833116 doi:10.1594/PANGAEA.833116 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.833117 Yu, Jimin; Elderfield, Henry; Hönisch, Bärbel (2007): B/Ca in planktonic foraminifera as a proxy for surface seawater pH. Paleoceanography, 22(2), PA2202, doi:10.1029/2006PA001347 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #AGE; Calculated; Carbon dioxide, partial pressure; CHAT_16k; DEPTH, sediment/rock; GC; Globorotalia inflata, Boron/Calcium ratio; Globorotalia inflata, d18O; Globorotalia inflata, Magnesium/Calcium ratio; Gravity corer; pH; Sea surface temperature, annual mean; SST, from Mg/Ca ratio after calibration curve (Mashiotta et al. 1999) |
| Tipo |
Dataset |
