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):
Comment:
AGE after I.N. Mc Cave, personal communication, 2006.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | AGE | Age | ka BP | Geocode | ||
3 | Globorotalia inflata, δ18O | G. inflata δ18O | ‰ PDB | Yu, Jimin | ||
4 | Globorotalia inflata, Magnesium/Calcium ratio | G. inflata Mg/Ca | mmol/mol | Yu, Jimin | ||
5 | Globorotalia inflata, Boron/Calcium ratio | G. inflata B/Ca | µmol/mol | Yu, Jimin | ||
6 | Sea surface temperature, annual mean | SST (1-12) | °C | Yu, Jimin | Calculated from Mg/Ca ratios (Mashiotta et al. 1999) | |
7 | pH | pH | Yu, Jimin | Calculated | assuming (B)tot changing with salinity, total scale | |
8 | Carbon dioxide, partial pressure | pCO2 | µatm | Yu, Jimin | Calculated | assuming (B)tot changing with salinity |
9 | pH | pH | Yu, Jimin | Calculated | assuming a constant (B)tot of 410 µmol/kg, total scale | |
10 | Carbon dioxide, partial pressure | pCO2 | µatm | Yu, Jimin | Calculated | assuming a constant (B)tot of 410 µmol/kg |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
242 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 G. inflata δ18O [‰ PDB] | 4 G. inflata Mg/Ca [mmol/mol] | 5 G. inflata B/Ca [µmol/mol] | 6 SST (1-12) [°C] (Calculated from Mg/Ca ratios ...) | 7 pH (assuming (B)tot changing with...) | 8 pCO2 [µatm] (assuming (B)tot changing with...) | 9 pH (assuming a constant (B)tot of...) | 10 pCO2 [µatm] (assuming a constant (B)tot of...) |
---|---|---|---|---|---|---|---|---|---|
0.00 | 0.00 | 1.68 | 1.27 | 58 | 9.20 | 8.11 | 321 | 8.12 | 318 |
0.02 | 1.31 | 2.27 | 1.26 | 56 | 9.17 | 8.09 | 348 | 8.10 | 332 |
0.04 | 2.63 | 1.25 | 1.35 | 53 | 9.79 | 8.06 | 365 | 8.06 | 371 |
0.06 | 3.94 | 1.96 | 1.35 | 53 | 9.80 | 8.05 | 387 | 8.06 | 374 |
0.08 | 5.26 | 2.11 | 1.10 | 54 | 7.87 | 8.12 | 310 | 8.13 | 308 |
0.10 | 6.57 | 2.64 | 1.31 | 59 | 9.48 | 8.10 | 344 | 8.12 | 322 |
0.12 | 7.89 | 3.34 | 1.30 | 57 | 9.43 | 8.07 | 380 | 8.11 | 339 |
0.14 | 9.20 | 2.22 | 1.43 | 61 | 10.31 | 8.09 | 352 | 8.11 | 334 |
0.16 | 10.51 | 2.45 | 1.37 | 62 | 9.93 | 8.11 | 335 | 8.13 | 314 |
0.18 | 11.83 | 3.08 | 1.28 | 57 | 9.26 | 8.08 | 367 | 8.11 | 333 |
0.20 | 13.14 | 4.26 | 1.02 | 58 | 7.15 | 8.15 | 308 | 8.19 | 270 |
0.22 | 14.14 | 3.65 | 1.10 | 55 | 7.86 | 8.11 | 340 | 8.15 | 304 |
0.24 | 14.83 | 3.53 | 0.88 | 57 | 5.82 | 8.21 | 254 | 8.23 | 237 |
0.26 | 15.52 | 3.48 | 0.98 | 56 | 6.83 | 8.16 | 289 | 8.19 | 267 |
0.28 | 16.21 | 3.59 | 0.97 | 62 | 6.67 | 8.21 | 256 | 8.24 | 234 |
0.30 | 16.90 | 3.43 | 1.15 | 59 | 8.27 | 8.13 | 321 | 8.16 | 292 |
0.32 | 17.59 | 3.53 | 0.94 | 59 | 6.35 | 8.20 | 262 | 8.22 | 244 |
0.34 | 18.28 | 3.32 | 1.05 | 68 | 7.42 | 8.23 | 242 | 8.25 | 224 |
0.36 | 18.97 | 3.63 | 0.93 | 62 | 6.28 | 8.22 | 246 | 8.25 | 226 |
0.38 | 19.66 | 3.52 | 0.97 | 58 | 6.70 | 8.18 | 274 | 8.21 | 254 |
0.41 | 20.69 | 3.48 | 0.93 | 61 | 6.32 | 8.22 | 248 | 8.24 | 229 |
0.45 | 22.07 | 3.93 | 0.97 | 60 | 6.65 | 8.19 | 273 | 8.23 | 245 |
0.49 | 23.44 | 3.46 | 60 | ||||||
0.53 | 24.82 | 3.61 | 0.91 | 54 | 6.14 | 8.17 | 285 | 8.20 | 263 |
0.57 | 26.20 | 3.40 | 0.97 | 61 | 6.70 | 8.20 | 257 | 8.23 | 238 |
0.61 | 27.33 | 3.59 | 0.93 | 56 | 6.30 | 8.18 | 277 | 8.20 | 257 |
0.65 | 28.46 | 3.47 | 0.95 | 53 | 6.49 | 8.15 | 300 | 8.17 | 278 |
0.69 | 29.59 | 3.18 | 1.11 | 58 | 7.92 | 8.14 | 310 | 8.16 | 286 |
0.73 | 30.72 | 2.98 | 1.22 | 63 | 8.84 | 8.14 | 306 | 8.17 | 282 |
0.77 | 31.86 | 2.83 | 1.25 | 62 | 9.10 | 8.13 | 318 | 8.15 | 295 |
0.81 | 32.99 | 2.28 | 1.23 | 61 | 8.90 | 8.14 | 303 | 8.15 | 291 |