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Yu, Jimin; Elderfield, Henry; Hönisch, Bärbel (2007): (Table 3) δ¹⁸O, B/Ca and Mg/Ca ratios in Globorotalia inflata from sediment core CHAT_16k [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.833116, In supplement to: Yu, J et al. (2007): B/Ca in planktonic foraminifera as a proxy for surface seawater pH. Paleoceanography, 22(2), PA2202, https://doi.org/10.1029/2006PA001347

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Coverage:
Latitude: -42.390000 * Longitude: -178.500000
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.81 m
Event(s):
CHAT_16k * Latitude: -42.390000 * Longitude: -178.500000 * Penetration: 3.03 m * Method/Device: Gravity corer (GC)
Comment:
AGE after I.N. Mc Cave, personal communication, 2006.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2AGEAgeka BPGeocode
3Globorotalia inflata, δ18OG. inflata δ18O‰ PDBYu, Jimin
4Globorotalia inflata, Magnesium/Calcium ratioG. inflata Mg/Cammol/molYu, Jimin
5Globorotalia inflata, Boron/Calcium ratioG. inflata B/Caµmol/molYu, Jimin
6Sea surface temperature, annual meanSST (1-12)°CYu, JiminCalculated from Mg/Ca ratios (Mashiotta et al. 1999)
7pHpHYu, JiminCalculatedassuming (B)tot changing with salinity, total scale
8Carbon dioxide, partial pressurepCO2µatmYu, JiminCalculatedassuming (B)tot changing with salinity
9pHpHYu, JiminCalculatedassuming a constant (B)tot of 410 µmol/kg, total scale
10Carbon dioxide, partial pressurepCO2µatmYu, JiminCalculatedassuming a constant (B)tot of 410 µmol/kg
Size:
242 data points

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