Table 1. Bulk (trisilver phosphate) δ18Ophos data from the Comley Limestones and SSTs exploring the influence of different values for δ18Osw.
Temperatures calculated from Eq. 1 (22). T1 δ18Osw = −6.5‰, the most reasonable value; T2 δ18Osw = −6‰, assumes no latitudinal P-E effects; T3 δ18Osw = −1‰, the most commonly used Paleozoic value; T4 δ18Osw = −8‰, incorporating the maximum likely latitudinal P-E effect of −2‰. Temperature uncertainty (2 SD T1) calculated from δ18O measurement SDs, assuming that δ18Osw = −6.5‰. See data S1.
| Sample | Triplicate mean δ18Ophos (‰ VSMOW) | Triplicate 1 SD (‰ VSMOW) | T1 (°C) | T2 (°C) | T3 (°C) | T4 (°C) | 2 SD T1 (°C) |
| Pristine brachiopods | |||||||
| Aa-Br-L | 15.17 | 0.18 | 20 | 22 | 45 | 13 | 1.6 |
| Ad-Br-L | 15.06 | 0.03 | 20 | 23 | 45 | 14 | 0.3 |
| La2-Br-L | 13.93 | 0.22 | 25 | 28 | 50 | 19 | 2.0 |
| Lb-Br-L | 14.63 | 0.14 | 22 | 25 | 47 | 16 | 1.3 |
| Sa-Br-L | 14.62 | 0.15 | 22 | 25 | 47 | 16 | 1.3 |
| Pristine Torellella | |||||||
| Lb-To-To | 14.70 | 0.14 | 22 | 24 | 47 | 15 | 1.3 |
| Sa-To-To | 14.59 | 0.07 | 22 | 25 | 47 | 16 | 0.6 |
| Altered brachiopods | |||||||
| La2-Br-D | 13.33 | 0.17 | 28 | 30 | 53 | 21 | 1.5 |
| Lb-Br-D | 14.31 | 0.23 | 24 | 26 | 49 | 17 | 2.1 |
| Sa-Br-D | 13.94 | 0.18 | 25 | 28 | 50 | 19 | 1.7 |
| Sedimentary phosphate | |||||||
| HG-A | 13.95 | 0.05 | 25 | 28 | 50 | 19 | 0.5 |
| HG-A-DC | 14.07 | 0.21 | 25 | 27 | 50 | 18 | 1.9 |
| HG-B | 12.77 | 0.09 | 31 | 33 | 55 | 24 | 0.8 |
| HG-B-DC | 12.78 | 0.20 | 31 | 33 | 55 | 24 | 1.8 |