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. 2018 May 9;4(5):eaar5690. doi: 10.1126/sciadv.aar5690

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